Climate Resilient Agriculture. An
implementation and support guide:
Field cropping and livestock
E Kruger, MC Dlamini, T Mathebula, P Ngcobo, BT Maimela & L Sisitka
Report to the
Water Research Commission
Mahlathini Development Foundation
Report is submitted as one of a set for “Climate Change Adaptation for Smallholder farmers
in South Africa: An implementation and decision support guide”
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firstname.lastname@example.org download from www.wrc.org.za
The publication of this report emanates from a project entitled Collaborative knowledge
creation and mediation strategies for the dissemination of Water and Soil Conservation
practices and Climate Smart Agriculture in smallholder farming systems (WRC Project No.
WRC Report No. (WRC will insert)
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This report has been reviewed by the Water Research Commission (WRC) and
approved for publication. Approval does not signify that the contents necessarily reflect
the views and policies of the WRC, nor does mention of trade names or commercial
productsconstitute endorsement or recommendation for use.
The following individuals and organisations deserve acknowledgement for their invaluable
contributions and support to this project:
Chris Stimie (Rural Integrated Engineering – RIEng)
Dr Brigid Letty and Jon McCosh (Institute of Natural Resources – INR)
Nqe Dlamini (StratAct)
Catherinevan den Hoof (Researcher)
Dr Sharon Pollard, Ancois de Villiers, Bigboy Mkabela and Derick du Toit (Association for Water and
Hendrik Smith (GrainSA)
Marna de Lange (Socio-Technical Interfacing)
Matthew Evans (Web developer)
MDF interns and students: Khethiwe Mthethwa, Samukhelisiwe Mkhize, Sylvester Selala, Palesa
Motaung and Sanelise Tafa
MDF board members: Timothy Houghton and Desiree Manicom
PROJECT FUNDED BY:
REFERENCE GROUP MEMBERS
Prof S MpandeliWater Research Commission
Dr S Hlophe-Ginindza Water Research Commission
Dr L NhamoWater Research Commission
Dr O CrespoUniversity of Cape Town
Dr A MansonKZN Department of Agriculture and Rural Development
Prof S WalkerAgricultural Research Council
Prof CJ RautenbachPreviously of WeatherSA
Prof RE SchulzeUniversity of KwaZulu-Natal
ABBREVIATIONS AND ACRONYMS
CCA Climate change adaptation
CRAClimate resilient agriculture
MDFMahlathini Development Foundation
SOCSoil organic carbon
SOMSoil organic matter
Table of Contents
Abbreviations and acronyms...............................................................................................................ii
1Background and introduction..........................................................................................................1
1.1Climate resilient field cropping practices................................................................................1
1.2Sites and participants.............................................................................................................1
1.2.1Innovation system process................................................................................................. 2
1.3Current status of field cropping..............................................................................................3
1.3.3Farmers comments regarding CC impacts on field cropping.............................................3
2CRA implementation: Field cropping..............................................................................................4
2.2Results: KwaZulu-Natal (KZN).............................................................................................10
2.2.1Rainfall and runoff summaries for 2019-2020 season.....................................................10
2.2.2Soil health considerations................................................................................................16
2.2.6Examples of farmer-level experimentation in Bergville....................................................30
2.3.1Cover crop mixes.............................................................................................................31
2.3.2Winter fodder supplementation experimentation..............................................................31
2.3.3Strip cropping with perennial fodder species...................................................................33
3Learning and best practice options...............................................................................................36
3.2.2Facilitators’ reflections on the CA learning process.........................................................39
1 BACKGROUND AND INTRODUCTION
1.1CLIMATE RESILIENT FIELD CROPPING PRACTICES
CRA field cropping practices include a suite of practices that focus on soil and water conservation and
soil health alongside the conventional soil fertility and soil structure considerations. Attention is also
given to crop diversification, crop types and varieties that are more suitable to the changing conditions.
Different planting dates are considered, as are options for extending the growing season. Livestock
integration is considered to be an important aspect of the process and in the development of climate
resilient local value chains.
Sustainable and regenerative agricultural practices such as conservation agriculture (CA), that
conserve and increase soil organic carbon (SOC) and improve soil health, are increasingly promoted
in Southern Africa as an alternative to conventional farming systems(Smith et al., 2017). CA depends
on the simultaneous implementation of three linked principles: (1) continuous zero or minimal soil
disturbance, (2) permanent organic soil cover, and (3) crop diversification, specificallywith the inclusion
of legumes and/or cover crops(FAO, 2013).
Complementary practices supporting CA implementation in smallholder farming systems include
appropriate nutrient management and stress-tolerant crop varieties, increased efficiency of planting and
mechanisation, integrated pest and disease and weed management, livestock integration, and enabling
political and social environments(Thierfelder et al., 2018).
To pilotthese practices in different localities, participants organised into learning groups, considered
local adaptive measures and included practices promoted through the smallholder decision support
system that wereappropriate to their own systems. Generally, these practices are piloted through the
innovation system development process and local farmer-level experimentation. Farmersdeepen and
expand their experimentation options over a three- to four-year period of learning and try out different
options. This is crucial in knowledge-intensive farming systems.
Practices that werepiloted by the learning groups included:CA,intercropping, crop rotation, micro-
dosing withfertilizer, drought tolerant crops, integrated weed and pest management and livestock
integration through production of cover crops appropriate for livestock fodder as well as production of
hay and winter supplementation.Soil and water conservation practices included planting on contour,
stone lines, check dams and planting agroforestry species such as Pigeon pea and Sesbania sesban.
1.2SITES AND PARTICIPANTS
Sites werechosen to be representative of different agroecological conditions within South Africa.
Number of participants(No. in
brackets indicate those who
CA, intercropping, drought tolerantcrops,
livestock integration, stone lines, check dams
and planting agroforestry species
CA, intercropping, crop rotation, micro-dosing
withfertilizer, drought tolerant crops, integrated
weed and pest management and livestock
CA, intercropping, crop rotation, micro-dosing
withfertilizer, drought tolerant crops, integrated
weed and pest management and livestock
CA, intercropping, micro-dosing withfertilizer,
drought tolerant crops, integrated weed and
pest management and livestock integration
CA, deep ripping, intercropping,crop
diversification and short furrow irrigation
The process starts with an introductory workshop with each of the learning groups, to introduce the
concepts and practices and discuss inclusionof theseinto their present farming systems, followed by
practical demonstrations and setting up the farmer-level experimentationtrial plots.
Interested individuals in a local area or village come together to form a learning group. Several farmers
in that group then volunteer to undertake on-farm experimentation, which creates an environment where
the whole group learns throughout the season through observations and reflections on the trials’
implementation and results. They compare various treatments with their standard practices, which are
planted as control plots.
For the field cropping piloting process, CA formed the backbone of the experimentation process, around
which other practices werebuilt and included. The CA principles best embody the adaptive processes
required, with outcomes that include improved soil organic matter, soil aggregationand soil health as
well as improved water holding capacity and reduced runoff.
A detailed description of the community-level process for introduction and experimentation for CA is
provided in the text box below.
SELECTION AND COMMUNITY-LEVEL PROCESS
PRECONDITION: Farmers active in field cropping with some level of social organisation.
1.Entry into community – through word of mouth from community members (individual and group
requests), government officials, other service organisations.
2.Set up introductory meetings at community level, including authorities, to introduce CA and the
3.Set up learning or interest group (20-30 people).
a.Setting up of VLSA’s (village savings and loan associations), farmer centres and joint
harvesting, storage and milling options are promoted
4.Members of learning group volunteer for farmer-led experimentation (usually 9-12 members in the first
year), while the rest of the group learns alongside them.
5.These members agree to do a CA trial alongside their control (normal way of planting).
a.Trials are usually 100 m2, 400 m2or 1 000 m2(small areas to reduce risk).
6.The programme provides inputs for the trial; the inputs for control and all labour are provided by the
farmer (the risk of implementing the new idea initially sits with the programme not the farmers. From
the second year the farmers pay a standard 30% subsidy towards the costs of inputs for their trials).
a.Planters and knapsack sprayers are provided to the learning group to share, manage and
7.Farmers are trained in the implementation of CA – pre-planting spraying (use of knapsack sprayers)
and field preparation, use of herbicides, layout of plots and planting in basins and rows using a range
of no-till tools (hand planters, animal drawn planters and/or two-row tractor-drawn planters). The
choice of implements depends on the scale of farming and farmers’ choices. Aspects such as top
dressing, weeding and pest control are covered during the season as well. Organic CA cropping
systems are explored in areas where participants prefer this option*.
a.As a minimum, 2-4 learning sessions per season in the learning group are held each year,
building in complexity and content. This includes one review session for the season and one
planning session to plan experimentation for the upcoming season.
8.The first-year trial layout is predetermined through the programme – to include close spacing,
intercropping and different varieties of maize (choice of traditional OPV or hybrid seed, according to
farmer preferences) and legumes (sugar beans, cowpeas).
9.From the second year, farmers start to add their own elements to theexperimentation depending on
their learning, questions and preferences. Cover crops (both summer and winter) and crop rotation
options are introduced.
10.Researcher-managed “trials” are also set up at individual homesteads to work alongside the more
enthusiastic and committed participants and to explore issues such as soil health, carbon
sequestration, soil fertility, water productivity, moisture retention, runoff and specific aspects of the CA
system, such as seeding and seeding rates of cover crops, etc.
11.Each season farmers days are organised in each area, jointly with the learning groups. CA forums and
innovation platforms are promoted where all stakeholders in a region join these forums to share,
discuss and plan together. This includes role players such as DARD, Social Development, LandCare,
Local and District Municipalities, Agribusiness service providers and NGOs
*Introducing organic CA options into a farming system where soil structure has been destroyed through repeated
ploughing, where there is very low fertility and soil organic matter and where weed pressure is high due to ongoing
lack of management is particularly challenging. Rehabilitation of such systems is unlikely to gain traction unless
initial remedial activities are undertaken, which should include incorporationof large amounts of organic matter,
some form of mulching and soil cover, soil and water conservation structures and soil pH amelioration through
addition of lime and/or gypsum.
This report focuses on a qualitative assessment of CA introduction in Limpopo and inclusion of several
quantitative assessments for the Bergville area in KwaZulu-Natal. In theEastern Cape, crop failurewas
experienced for all three seasons of implementation, which reduced opportunities for learning and
continued farmer-level experimentation.
1.3CURRENT STATUS OF FIELD CROPPING
Dryland cropping is a common practice in the area, although it has declined dramatically with the five-
year drought in the area, compounding ongoing reduction in cropping due to low soil fertility, access to
seed and inputs, and lack of labour.
Learning group participants are very keen to re-initiate or continue field cropping aspects of their
farming. Presently most participants undertake this activity within their extended homestead plots, with
only a smallproportion of participants having access to larger fieldsand or supplementary irrigation
With the shift in weather patterns and climate variability, (increased heat, late onset and unpredictability
of rains)the field cropping practice in the area has already shifted; surprisingly away from the more
drought tolerant cropssuch as millet and sorghum, towards maize with supplementary irrigation. This
is due tomuch greater predation of themillet and sorghum by birds(in particular), but also monkeys
and wildlife than was experienced in the past.Farmers are aware of bird-resistant sorghum varieties
buthave not been able to access seed. They also practice protection of the seed heads with netting as
an adaptive strategy. Planting of traditional leguminous crops such as ground nuts, jugo beans
(bambara ground nut) and cowpeasis still popular, as is planting of pigeon pea and moringa.Other
field crops include pumpkin and watermelon. Some farmers have started experimentation with different
In the Bergville area, communities still practice field cropping primarily for food security and rely on their
maize harvests for food. Dryland cropping, focusing almost exclusively on maize and extensive livestock
management are the main activities.There has been a sharp reduction in field cropping over the last
15years, given stress factors such as uncontrolled livestock, increased poverty, difficulties in accessing
tractors, expensive inputs and climate change.
In the Midlands and SKZN regions, with higher rainfalls and easieraccess to markets in urban centres,
the focus has been more on the production of green mealies and livestock feed (yellow maize). These
farmers also focus on other field crops such as amadumbe(taro), pumpkin, beans and sweet potato,
and produce a range of vegetables. Here a much larger proportion of the fields arefenced, compared
to Bergville, as livestock invasionsin these more densely populated areas is a large risk factor with
In more general terms, field cropping in KZN is hampered by soilacidity, lack of appropriate nutrient
and weed management and continued monocropping ofmaize. Mazie yields are generally very low and
Farmers comments regarding Climate Changeimpactson field cropping
•“Lack of rainfall and changes in rainfall patterns havebeen a major challenge with regard to
both field cropping and homestead gardening.”
•“Pest outbreaks which are associated with extreme heat have been worse, especially on
•“Repeated crop failure has meant that we no longer have seed to plant our field crops.”
•“When it does rain there is now a lot more erosion, because the soil is not covered.”
Farmers comments regarding CA implementation in the context of CC
•“The CA processhas brought the community together and is helping farmers to groom each
other to improve our farming.”
•“Better yields have been observed, specifically for maize, as wellas better weed knowledge
and management skills.”
•“Maize plantedafterLablab can be highly productive. However, lablab and cover crops are
inedible and they are very attractive to livestock, hence most farmers are resistant to
diversifying, they only use maize.”
•“Those who obtain higher yields are the hard workers, as weeds are likely to be a big problem
if weeding is not done carefully and on time.”
•“Soil management has improved under CA, both soil fertility and much reduced erosion and
yields have improved dramatically.”
•“CA is cost effective and cheaper than conventional tillage as tractors need not be hired and
fertilizer and other inputs are used sparingly.”
•“Most of the participants have decreased fertilizer use and increased use of manure on their
fields. The results are still good.”
•“Havingsavings groups has helped a lot in terms of buying inputs.”
2 CRAIMPLEMENTATION:FIELD CROPPING
During each season, a set of CA experiments is decided upon, followed by demonstration workshops
at farm level, implementation by all volunteers and ongoing monitoring. Observations are recorded and
discussed with the learning groups in their seasonal review of their experimentation process,to allow
for planning of the next experimentation cycle.
For the results section below, the Limpopo CA implementation activities have been divided into specific
experiments, with aims, process and observations recorded for each.
AIM:Introduction of CA principles and close spacing, intercropping with legumes, planting bird-resistant
sorghum and CA planters.
Planting demonstrations for the CA experiments
were done in three villages. We demonstrated the
•Intercropping maize with sugar
beans/cowpeas. Tramlines with 50cm
spacing for maize and 25cm for the legumes
(in and betweenrows). Lime and bonemeal
wereadded to the planting stations and the
basins were covered with leaves as a mulch.
•Use of a Knapick planter with donkeys in a
larger field with single crop options.
Figure 1. The Turkey learning group planting a CA
demonstration plot, using 50cm-spaced basins
This season resultedin total crop failure for all the participants, as the area was still in the grips of a
severe drought. The total summer rainfall was less than 200 mm.
1.Animal-drawn planters are appropriate for larger fields
Farmers in the area use donkeys for ploughing as they do not have access to oxen. A Knapick planter
was introduced and participants were given a chance to change the different seed plates and adjust the
setting in the seed and fertilizer bins. The donkeys managedreasonably well withthe planter, despite
fears that the planter would be too heavy for them.
Figure 2. Left: Introducing the Knapick planter to the learning group and demonstrating the changing of seed plates.
Right: The oxen-drawn planter has been hitched to a team of donkeys for planting.
Some of the challenges were:
•Not being able to control the donkeys (they could not plant in astraightline, meaning it was
hard to maintain a consistent inter-row spacing) – this could have been because the donkeys
were not well trained.
•Learning to change the planting discs requires hands-on practice for each participant, which
took a lot of time.
•The soils at planting werevery wet and clayey (a sandy clay), which meant that the planting
tines kept getting blocked. This showed the group that planting with this planter would need to
be undertaken once the soil has drained.
•Transporting the planter from one site to the other was a problem, as it requires a long-wheel-
Despite the above-mentioned challenges, participants liked the planter and felt it would be very useful
to have one in each of the villages.
AIM: Review of CA principles and practice to date and close spacingandintercropping with legumes.
For this season, CA principleswere reviewed,and experimentation focused on close spacing and
intercropping as these aspects were not well internalised in the first cropping season.
Planting demonstrations for the CA experiments were done in three villages. We demonstrated the
•Intercropping maize with sugar beans/cowpeas.
•Tramlines with50cm spacing for maize and 25cm for the legumes (in and between rows).
1.Close spacingand intercropping improvescrop stand and growth.
Farmers noticed the difference between their local system and the CA experiments. First, they noticed
that the narrow spacing of crops in the CA system worked a lot better than the preferred wider spacing
in the area. They worked on the understanding that the wider spacingreduces water stress, as does
monocropping, but found that the intercropping and close spacing increased the potential of survival of
their crops considerably. They realised that the cover provided by the closely spaced grain-legume
intercrop improves water holding and reduces the effect of extreme heat.
Figure 3. Left: Mpelesi Sekgobela from Sedawa intercropped, with close spacing, her maize, beans and pumpkins
and found that crop growth was very good compared to her mono-cropped plots. Right: In Turkey, the closely
spaced maize survived well and grew tall. Towards the end of the season beans were harvested between these
rows and the stover left on the ground.
2.Using soil and water conservation practices alongside CA improves crop growth and reduces
A few farmers combined the traditional practice of furrows and ridges into their CA trials. This increased
the survival, specifically of maize considerably and reduced runoff in their CA trial plots.
Figure 4.Left: Meisie Mokwena’s intercropped plot of maize and cowpeas, where maize did not germinate at all.
Right: A plot of maize, cowpeas and pumpkin planted in furrows and ridges, showing much improved germination
and growth of all three crops.
Magdeline Malepe, who struggled with poor soil and soil erosion, installed stone bunds in her field and
planted in between them and has planted millet which has helped herto increase hersoil cover. She
believes this is already contributing to improving her soil.
Figure5. Magdalene Malepe’s planted field,showing the stone lines
above and below the four rows of maize in the picture
Other observations made by farmers for this season of
experimentation included the following:
•Farmers observed thatsoil in the CA plot holds moisture
longer than their traditionally planted plots.
•Farmers observed less competition between the crops in
their CA plots compared to their traditional planting
•Mr Mogofe: “I triedwhat we were taught last year and I
realised that the moisture lasts longer in the CA plot
compared to the normal plot.”
•Sarah Madire added that with addition of manure and
leaving soil covereven the colour of the soil was starting
to change: “this could indicate that with time, yes, this can
help improve our soil.”
•Some participants felt that they could see some
improvement in the CA trials fromlast season, but not that
much.Some participants, however, felt that CA was a
long-term strategy and it will take a while before they see some of the benefits ofCA(e.g.
improvement in soil structure).
AIM: Review of CA principles and practice to date and conscious inclusion of summer cover crops and
Dolichos(Lablab) beans into the cropping system.
Farmer-level experiments were introduced –differing depending on whether participants had already
planted portions of their fields and on the cover crops they were interested in trying. Sunflower is known
as a heat- and drought-resistant crop butis not grown much anymore as participants are no longer
keeping poultry (due to lack of water). They asked about potential markets. Dolichos is popular as both
the leaves and seed can be eaten.
Planting demonstrations for the CA experiments were done in four villages. We demonstrated the
•Planting maize with a summer covercrop mix (Babala/millet, sunflower and Sun hemp), or
individual cover crops such as sunflowers. Fourrows of maize were planted in basins 50cm
apart and fourrows of cover crops planted in furrows 25cm apart at a rate of 10kg/ha. Cover
crops were relay planted into the maize, threeto four weeks after planting maize, to reduce
moisture competition between the crops.
•Intercropping maize with sugar beans/cowpeas. Tramlines with
50cm spacing for maize and 25cm for the legumes (in and
•Dolichos (Lablab beans) were planted along fence lines
according to the local practice. Participants did not want to plant
Dolichos as an intercrop, fearing competition with other crops.
•Bales of grass were used to mulch portions ofthe CA trials, to
test the effect on weed suppression and moisture retention.
•Hand weeding was undertakenduring the season and weeds
were left on the soil surface as a mulch.
Figure 6. Right: Mulching a portion of the CA trial plot in Turkey
Only tenof the 35 participants in the CA experimentation cycle managed to grow crops that were
harvestable.For most of the participants, germination was low,and crops died back soon after
germination. Weather conditions wereunconducive, with intense heat and low rainfall between
December 2019 and January 2020. In addition, lack of soil fertility and soil organic matter was a major
1.Summer cover crops (Sun hemp, sunflower and millet)survived where maizeand legumes
such as beans and cowpeas died back due to heat and drought stress.
Magdalene Malepe: “Sun hemphas grown very well and it is a good crop for provision of fodder for
goats. Intercropping with Sun hempworks much better because I have seen an improvement in my
Figure 7. Left: Magadelene’s Sun hemp, intercroppedwith maize growing very well. The maize, however, is
showing strong signs of heat and water stress and most has already died back. Right: Maize roots are stunted and
growing horizontally, indicative of a highly compacted soil and a shallow plough pan typical of plots where hand
hoes have been used for tillage formany years.
Figure 8. In Turkey, all
cover crops survived well
(Babala, sunflower and
Sun hemp), along with a
few straggly maize plants
2.Cowpeas can still do well under difficult conditions if adequate mulching is provided.
MagdaleneMalepeis aware that her soil is not very fertile and has issues. In this regard, she decided
to do a small experiment with lime by herself– she added lime to a section of her plot where she planted
cowpeas and another small area with cowpeas without lime.She also mulched these plots.She saw
that the cowpeas that received lime and mulch grewmuch better andwerea good dark green colour
compared to those without lime or mulch, which showed purpling on the leaves.
Figure 9. Right: Cowpeas growing well, with added lime and mulch
Note: From soil fertility samples analysed for
these participants, it was determinedthat lime is
not required in this system and pH of the soil
averages around pH 7,5.
3.Adding organic matter to the
soil for improved soil fertility
allows maize to grow where it
otherwise would not– where
conditions are hot and dry.
Meisie Mokwena from Sedawa makes
piles of organic matter in her field atthe
end of the season to improve her soil
fertility and makes and adds compost to her soil.
Figure 10. Meisie’smaize, gourd and
moringaintercropped plot, planted in
soil with organic matter added. Her
maize has thrived, while that of her
neighbours, who do not add organic
matter, died back.
can assistin survival of
crops, specifically maize.
Angelina Thekwane from Turkey intercropped maize with Sun hempand provided supplementary
irrigation, using municipal water. This provided for good growth of both crops, although the maize lacked
nutrients (as she plants without adding anything to the soil) and maize roots were shallow, indicative of
Figure 11. Left:
Angelina’s maize and
well. Centre: Angelina
holding a maize cob.
Right: A root ball of
one of the maize
plants. This indicates
compacted, low fertility
5.Traditional legumes that are heat- and drought-tolerant such as groundnutsand jugo beans are
a good alternative to maize.
Some participants decided against planting maize, given the bad track record for this crop overthe last
few years. One such participant is Mmatshego Shaai fromTurkey. She planted only legumes–
groundnuts and jugo beans, for a second season in a row. She found these crops survived better and
provided for better soil moisture due to their canopy, as well as reduced erosion in her plot.
Figure 12. Mmatshego
Shaai’sfield planted to
ground nuts and jugo
beans, which she sells
in the community.
Silence Malapane in
legumes in basins
and in ridges and
furrows. He felt that
uncovered soil is a problem under the present conditions. This can be considered a local adaptation
and is important to note.
In KZN, co-funding from the Maize Trust to implement a smallholder farmer innovation programme in
CA has allowed formore intensive farmer-level experimentation and quantitative assessments of the
results. The CA implementation has been undertaken for a longer period (4-7 years), for the five villages
(Stulwane, Eqeleni, Ezibomvini, Ndunwane and Mhlwazini), prioritised for this research process. This
has allowed us to assess some of the longer-term impacts of CA. The results presented are primarily
for the most recent cropping seasons (2019/20).
Results for the quantitative assessments undertaken (rainfall, runoff, soil fertility, soil health, bulk density
and water productivity) are presented below, followed by examples of the farmer-level experimentation
for a selection of participants.
Rainfall and runoff summaries for 2019-2020 season
In general, the average annual rainfall for the Drakensberg region ranges between 750mmand 1 350
mm. The actual amount of rainfall has not variedmuch over time (besides a potential 20-year
periodicity), even for long term studies over 50years, but the monthly variability has been increasing
Rainfall variabilityrelates to the amount of annual rainfall as well as its seasonal distribution. This
periodicity affects the potential surface runoff, as well as subsurface and basalflows in a catchment.
To illustrate this, the following two figures indicate the monthly rainfall averages inthe 2016/17 and
2019/20 seasons; indicating a shift to late onset of summer rains and increased late season rainfall
between these two seasons.
Figure 13. Monthly rainfall averages (mm) for Ezibomvini (2016/17)
Figure 14. Monthly rainfall averages (mm) for Ezibomvini (2019/20)
These seasonal rainfall differences have implications both for runoff and crop performance.
Runoff (stormflow or surface runoff of water)is generated by rainstorms and its occurrence and quantity
are dependent on the characteristics of the rainfall event, i.e. intensity, duration and distribution
(Schulze, 2011). There are, in addition, other important factors which influence the runoff-generating
process. These factors include the infiltration capacity of the soil, the soil moisture content when the
rainfall event occurred, the soil type,presence of capping/crusting, and slope.
In addition, the presence of above-ground vegetation intercepts some of the rainfall and reduces
raindrop impact and thus crusting of the soil. Vegetationalso has a significant effect on the infiltration
capacity ofthe soil. The root system and organic matter in the soilincrease the soil porosity thus
allowing more water to infiltrate. Vegetation also retards the surface flow, particularly on gentle slopes,
giving the water more time to infiltrate and to evaporate. Thus, vegetation reduces runoff substantially,
compared to bare ground (Critchley & Siegert, 1991).
For the purposes of comparing the effect of Conservation Agriculture on runoff in the context of an
agricultural cropping field, only surface runoff has been considered.
Runoff plots are used to measure surface runoff as well as erosion through removal of sediment under
controlled conditions. In this instance, runoff microplots, as designed previously by UKZN researchers,
(Mutema, et al., 2017)have been used.
Runoff microplots consist of galvanised metal sheeting frames 1m by 1 m, inserted 10cm into the
ground and leaving another10 cm above ground to eliminate run-on water during rain events. A spirt
level was used to keep the runoff plots levelled and the slope was considered (runoff plots were not
installed on slopes greaterthan 7%) when installing the runoff plots. Surface water and sediment
generated are collected in a protected gutter through openings in a downslope-side metal sheet. The
gutter is fitted with a delivery pipe connected to a reservoir (in our case, a 25 L bucket with a lid) about
1,5 m downslope. After each rainfall event, the total runoff volume (ml) from each microplot replicate
October November December January February March April May
Rainfall mm4,375,4 152,2160,8304,3 87,6 134,10,0
Monthly Rainfall in Ezibomvini 2019-2020
September October November December January February March April May
Monthly Rainfall2,640,3 118,4 98,710297,544518
Monthly Rainfall in Ezibomvini 2016-2017
was measured with a measuring cylinder(Dlamini, et al., 2011). Sediment was noted on occasion, but
Figure 15: Above left: A runoff microplot installed in a CA trial plot with maize and beans, Above Centre: Installing
a runoff microplot in a conventionally tilled plot with maize and Above Right: In – season maintenance of collection
The aims of the experiments are:
1.To ascertain differences in runoff when comparing minimal tillage to conventional tillage.
2.To ascertain differences in runoff between different cropping options between the CA trialplots.
126.96.36.199Methods and results
Runoff pans were installed for four participants across four villages in the Bergville area,for the
2019/2020 planting season: Nelisiwe Msele (Stulwane), Phumelele Hlongwane (Ezibomvini), Boniwe
Hlatshwayo (Ndunwane) and Ntombakhe Zikode (Eqeleni).
Each participant also had a rain gauge set up in her homestead. Participants tookrecords for both
rainfall and runoff for the cropping season (usually Octoberto April). The period, however, depends on
the start and end of the rainy season.
Below is a small illustrative table indicating the number of rainfall events recorded for each participant,
with the number of runoff events recorded in brackets alongside. The number of rainfall events recorded
need to coincide closely with the number ofrunoff measurements taken. It is not expected that the
number of rainfall events recorded should be the same across the villages, as it is quite common in this
mountainousregion for rain to fall in onevillage but not anothernearby, due to the increasingly localised
pattern of rainfall events.
Table 1. Outline of rainfall data recorded across four village rain gauges in Bergville (2019/20)
Number of rainfall and runoff (in brackets) measurements taken
Record keeping in Stulwane, Ezibomvini and Ndunwane is considered reliable. In Eqeleni, in addition
to the mismatch between the number of rainfall events and runoff measurements taken, all the runoff
measurements were recorded as 0,5 L or 1L, indicating to the team that these were mostly fabricated.
In this case, Mrs Zikode tasked her matriculating daughter with the record keeping, given that she is
not herself literate. The Eqeleni results will thus not be considered.
Table 2. Percentage rainfall converted to runoff for three villages in Bergville (2019/20)
Percentage rain converted into runoff
(October 2019-April 2020)
SAEON weather station at Didima
(January 2020-April 2020)
(October 2019-April 2020)
Note 1: The controlplot for Boniwe Hltashwayo in Ndunwane was also a minimum tillage plot (0%-15% soil disturbance), planted
to single-cropped maize with different spacing and fertilizer application regimes to her CA trial plot.
Note 2: Conventional control plots in Stulwane and Ezibomvini consisted of tilled plots (>30% soil disturbance), planted to single-
cropped maize with different spacing and fertilizer application regimes to her CA trial plot.
Note 3: Weather station data from the Ezibomvini weather station werelost and replaced by data from a SAEON weather station
at Didima (~12km away).
The rainfallresults asrecorded for the rain gauge at Ndunwane
most closely resemble the data obtained from SAEON for a
weather station at Didima (KZN Parks)– 641mm and 687mm
respectively. This makes sense, as the community is very close
to the edge of the national park and at a similar elevation. We
suspect the rainfall data in Stulwane to be an underestimate and
that for Ezibomvini to be an overestimate. The averaged data
across the three sites,however, closely resemble the rainfall data
from the weather station used.
Figure 16: Right: Uploading data at the Ezibomvini weather station.
From Table 2 it can be seen that the percentagerunoff in the
conventional control plots in Stulwane and Ezibomvini is1,46%
and 5,26% higher than for the average CA trial plots in these
villages. In Ndunwane, runoff in both the CA trial and control plots
The rainfall and runoff measurements were initiated in 2016/17 in Phumelele Hlongwane’s (Ezibomvini)
CA experimentation plots.The table below gives a summary of her runoff results for the last four
cropping seasons. She has practiced CA for sixconsecutive seasons.
Table 3. Comparison of percentage rainfall converted into runoff for Ezibomvini 2016/17 to 2019/20
Rainfall recorded by PhumeleleHlongwane from her rain gauge is similar to therainfall measured by
the local weather station.
Percentage rain converted into
From Table3 it can be seen that the percentage rainfall converted into runoff depends on the season
andis not directly related to the overall amount of rain. The runoff is much more closely related to
intensity of individual rainfall events, the number of such events in a rainy season, the soil moisture at
the time of the rain, as well as bulk density of the soil,compaction and soil cover. The percentage
conversion of rainfallinto runoff is consistently lower, on average by 9,5% in the CA trial plots compared
to a conventionally tilled plot. These results are similar to a study conducted in Potshini village in
Bergville (Mchunu & Chaplot, 2012)which showedthat minimal tillagein a small-scale agriculture
context, even with <10% crop residue cover has the potential to significantly reduce soil and soil organic
carbon losses by water.”
The layout of the CA experiment/trial is a combination of tensingle, intercropped or multicropped plots,
which are rotated annually.
Table 4. Runoff measured in different plots within Nelisiwe Msele’s experiment; Stulwane (2019/20)
Stulwane: Nelisiwe Msele (2019/2020)
Plot 1 (L)
Note: M+CP = maize and cowpea intercrop;M= maize single crop; B = bean single crop; SCC= summer cover crop mix of
sunflower, millet and Sun hemp; LL= Dolichos beans
Data indicate increased runoff with increased monthly rainfall, which is to be expected, andquite
significantvariations in runoff between the CA trial plots monitored, even though the average runoff
across these plots is lower than the runoff on the conventionally tilled control plot.
The highest recorded runoff amounts are for February and April, with highest monthly runoff for the
single cropped legume (LLand B)plots and the maize controlplot. Legumes did not provide good soil
cover and neither didthe maize in the control plot, planted witha wider spacing than the CA plots.
The lowest recorded runoff amounts are for early season rain in January for the single cropped CA trial
plots (B and M) that follow on from a rotation of a single crop (M and B, respectively). It appears that
for these CA plots the prior multi-crop rotations (M+CP and SCC) led to increased runoff early in the
The layout of the CA experiment/trial is a combination of tensingle, intercropped or multi-cropped plots
which are rotated annually.
Table 5. Runoff measured in different plots within Phumelele Hlongwane’s experiment; Ezibomvini (2019/20)
Ezibomvini:Phumelele Hlongwane (2019/2020)
Plot 2 (L)
Plot 4 (L)
Plot 6 (L)
Plot 9 (L)
Note: M+CP = maize and cowpea intercrop;M= maize single crop; B = bean single crop; SCC= summer cover crop mix of
sunflower, millet and Sun hemp; LL= Dolichos beans
Data indicate the highest runoff amounts in January, which was the month with the highest rainfall for
all the plots (both CA and control), which is expected, and in March (again, for all the plots – both CA
and control), which is not expected. Very low runoff amounts in February coincide with a relatively high
monthly rainfall for the CA plots. This could indicate increased soil permeability due to somemoisture
in the soil already present which temporarily increases infiltration until field capacity is reached, which
could also explain the increased runoff in the following month.
Generally,the overall runoff for all the CA plots issimilar, but it islowest for the M+CP and SCC plots
and highest for the two M+B plots, which can be explained bythe increased cover provided by the
higher biomass mixed crop plot compared to that which beans provide.
Overall runoffon the conventionally tilled plot is higher than all the CA plots. It is also higher towards
the end of the rainy season; an effect that has been well recorded in the past(Mchunu & Chaplot, 2012).
Early in the season, more water can infiltrate into the disturbed soil, but later, as thesoil settles and
compacts, more runoff is generated.
The layout of the CA experiment/trialis a combination of foursingle or intercropped plots, which are
Table 6: Runoff measured in different plots in Boniwe Hlatshwayo’s experiment; Ndunwane (2019/20)
Nduwane; Boniwe Hlasthwayo (2019/2020)
CA plot (L)
Note: M+B = maize and beanintercrop; M = maize single crop
Data indicate extremely low runoff amounts for both the CA and control plots throughout the season.
Higher runoff coincides with higher monthly rainfall averages. Overall, the runoff is negligible, indicating
very well-structured soils with high organic matter. Thisrepresents the ideal situation possible for these
Conservation Agriculture reduces annualrunoff compared to conventional tillage. Soil cover
provided by a mixture of growing crops,closely spaced, also reduces runoff. Single-cropped
beans increase runoff due to lack ofsoil cover and low rooting capacity, which also reduces the
infiltration capacity during the season.
Soil health considerations
The intention is to compare the soil health characteristics for severalcropping options within the CA
trials, with conventionally tilled mono-cropped control plots, over time.
The soil health tests (as analysed by Soil Health Solutions in the Western Cape and Ward Laboratories
in the USA) provide insight into microbial respiration and populations in the soil, organic and inorganic
fractions of the main nutrients N, P and K, and assessment of organic carbon and percentage organic
matter (%OM). An overall soil health score (SH) is also provided for each sample.
Sampling is done at the same time every year, during September, after harvest and prior to the start of
seasonal rain, according to international conventions (Stolbovoy, et al., 2007).
•CA plots: 10m x 10m plots are marked,and 10cm depth cores are taken (with a soil auger),
taking 20 samples along a zigzag pattern across the plot. These are combined, thoroughly
mixed and then 500g is placed in a plastic bag and sealed. These bags are kept in a cool, dark
place until delivery to the soil health analysis laboratory – usually within four to sixweeks of
taking the sample.
•Control plots: 20 samples are taken in a zigzag pattern across the dimension ofthe control plot;
these vary from one participant to the next and are otherwise treated in the same manner as
the CA plot samples above.
•Veld samples: This changed after the first two seasons to reduce potential variability in the
samples. A patch ofundisturbed veld, as close as possible to the participant’s cropping field
was chosen, to also have the same basic visual characteristics as the field in question.Four
subsamples weretaken at 10cm depth at the fourcompass positions adjacent to the cropping
field. It is important to notethat it wasthe team’s experience that the values of theveld samples
variedsubstantially even in the same village or in the same vicinity as a field. The practice of
using one veld sample for two to three different farmersin the same village was thus
discontinued and a decision made to use a section of veld as close as possible to the cropping
field. In addition, veld in smallholder farming areas under communal tenure cannot be regarded
as “pristine”, given heavy grazing patterns and frequent burning.It is, however, assumed that
the soil is undisturbed in terms of tillage and gives an indication of the general conditions of the
soil in the vicinity of the cropping fields.
Samples were air dried and stored for a period of two to four weeks atroom temperature (20-24°C),
prior to analysis.
For the 2018/19 cropping season, soil health analysis was undertaken for tenparticipants across five
villages in Bergville:
•Eqeleni (2); Stulwane (2); 6thyear of implementation.
•Ezibomvini (2); 5thyear of CA implementation.
•Mhlwazini (2); 3rd year of CA implementation.
•Ndunwane (2); 3rdyear of CA implementation.
For the 2019/20 cropping season, soil health analysis was undertaken for eightparticipants across
three villages inBergville:
•Stulwane (3); 7thyear of implementation.
•Ezibomvini (3); 6thyear of implementation.
•Ndunwane (2); 4thyear of implementation.
Laboratory analysis was undertaken by Soil Health Solutions, linked to WARD Laboratories in the USA.
Each soil sample received in the lab is dried at 50°C for 24 hours and ground to pass a 4,75mm sieve.
The dried and ground samples are scooped, with the weight recorded using a Sartorius Practum 2102-
1S, into two 50 ml centrifuge tubes (4 g each) and one 50 ml plastic beaker (40 g) that is perforated
and has a Whatman GF/D glass microfibrefilter to allow water infiltration. The two 4 g samples are
extracted with 40 ml of DI water and 40 ml of H3A respectively, for a 10:1 dilution factor. The samples
are shaken for tenminutes, centrifuged forfiveminutes, and filtered through Whatman 2V filter paper.
The water and H3A extracts are analysed on a Seal Analytical rapid flow analyser for NO3-N, NH4-N,
and PO4-P. The water extract is also analysed on an ElementarTOC select C:N analyser for water-
extractable organic C and total N. The H3A extract is also analysed on an Agilent MP-4200 microwave
plasma for Al, Fe, P, Ca, and K.
The 40 g soil sample is analysed for CO2-C ppm after a 24-hour incubation at 25°C. Initially, the sample
is wetted through capillary action by adding 18 ml ofDI water to an8 oz. glass jar (ball jar with a convex
bottom), placed in the jar and then capped. Solvita paddles can be placed in the jar at this time and
analysed after 24 hours with a Solvita digital reader. Alternatively, we use a system that we call HT-1,
where, at the end of 24-hour incubation, the CO2in the jar can be pulled through a LiCor840A IRGA,
which is a non-dispersive infrared (NDIR) gas analyser based upon a single-path, dual wavelength
infrared detection system.
SOM% is a gravimetric expression ofthe organic material fraction lost from combustion at 360°C for
threehours, and is also termed the loss in ignition calculation method (LOI%).
188.8.131.52Soil health test parameters
The method uses nature’s biology and chemistry by: (1) using a soil microbial activity indicator; (2) a
soil water extract (nature’s solvent); and (3) the H3A extractant, which mimics the production of organic
acids by living plant roots to temporarily change the soil pH, thereby increasing nutrient availability.
These analyses are benchmarked against natural veld for each participant, due to high local variation
in soil health properties, and measured at different times. The veld scores provide for high benchmarks
against which to compare the cropping practices.
Soil Respiration one-day CO2-C:This resultis one of the most important numbers in this soil test
procedure. This number (in ppm) is the amount of CO2-C released in 24 hours from soil microbes after
soil has been dried and rewetted (as occurs naturally in the field). This is a measure of the microbial
biomass in the soil and is related to soil fertility and the potential for microbialactivity. In most cases,
the higher the number the more fertile the soil.
Microbes exist in soil in great abundance. They are highly adaptable to their environmentand their
composition, adaptability, and structure are a result of the environment they inhabit. They have adapted
to the temperature, moisture levels, soil structure, crop and management inputs, as well as soil nutrient
content. Since soil microbes are highly adaptive and are driven by their need to reproduce and by their
need to acquire C, N, and P in a ratio of 100: 10: 1 (C:N:P), it is safe to assume that soil microbes are
a dependable indicator of soil health. Carbon is the driver ofthe soil nutrient-microbialrecycling system.
Water extractable organic C (WEOC):Consists of sugars from root exudates, plus organic matter
degradation. This number (in ppm) is the amount oforganic C extracted from the soil with water. This
C pool is roughly 80 times smaller than the total soil organic C pool (% Organic Matter) and reflects the
energy source that feeds soil microbes. A soil with 3% soil organic matter when measured with the
same method (combustion) at a 0-10cmsampling depth produces a 20000 ppm C concentration.
When the water extract from the same soil is analysed, the number typically ranges from 100-300 ppm
C. The water extractable organic C reflects the qualityof the C in the soil and is highly related to the
microbialactivity. On the other hand, percentage SOM is about the quantity of organic C. In other words,
soil organic matter is the house thatmicrobes live in, but what is being measured is the food they eat
(WEOC and WEON).
If this value is low, it will reflect in the C02evolution,which will also be low. So, less organic carbon
means lessrespiration from microorganisms, but againthis relationship is unlikely to be linear. The
Microbially Active Carbon(MAC = WEOC/ppm CO2) content is an expression of this relationship. If the
Haney/Soil Health Test Information Rev. 1.0 (2019). Lance Gunderson, Ward Laboratories Inc.
percentage MAC is low, it means that nutrient cycling will also be low. One needs a %MAC of at least
20% for efficient nutrient cycling.
Water extractable organic N (WEON):Consists of Atmospheric N2sequestration from free living N
fixers, plus organic matter degradation. This number is the amount of the total water-extractable N
minus the inorganic N (NH4-N + NO3-N). This N poolis highly related to the water extractable organic
C pool and will be easily broken down by soil microbes and released to the soil in inorganic N forms
that are readily plant available.
Organic C:Organic N:This number is the ratio of organic C from the water extract to the amount of
organic N in the water extract. This C:N ratio is a critical component of the nutrient cycle. Soil organic
C and soilorganic N are highly related to each other as wellas the water extractableorganic C and
organic N pools. Therefore, we use the organic C:N ratio of the water extract since this is the ratio the
soil microbes have readily available to them and is a more sensitive indicator than the soil C:N ratio. A
soil C:N ratio above 20:1 generally indicates that no net N and P mineralisation will occur. As the ratio
decreases, more N and P are released to the soil solution which can be taken up by growing plants.
This same mechanism is applied to the water extract. The lower this ratio is, the more organisms are
active and the more available the food is to the plants. Good C:Nratios for plant growth are <15:1. The
most ideal values for this ratio are between 8:1 and 15:1.
Soil Health Calculation:This number is calculated as one-day CO2-C/10 plus WEOC/50 plus
WEON/10 to include a weighted contributionof water-extractable organic C and organic N. It represents
the overall health of thesoil system. It combines fiveindependent measurementsof the soil’sbiological
properties. The calculation looks at the balance of soil C and N and their relationship to microbial activity.
Thissoil health calculation number can vary from 0 to more than 50. This number should be above
sevenand increase over time.
184.108.40.206Soil health scores
Three assumptions are made regarding SH scores:
•SH scores for the CA trial plots will be higher than for the conventionally tilled control plots.
•SH scores will increase over time for CA trial plots.
•SH scores for different cropping combinations, such as monocropped plots, intercropped plots and
multicropped plots will be different.
SH scores over time
SH scoresfor fiveparticipants (Dlezakhe Hlongwane, Mtholeni Dlamini, Phumelele Hlongwane, Smephi
Hlatshwayo and Ntombakhe Zikode) across three villages (Stulwane, Ezibomvini and Eqeleni) in
Bergville have been calculated from 2015/16 to 2019/20.
The figure below provides a summary of the results.
Figure 17: SH scores between 2015/16 and 2019/20 for 5 participants in Bergville
From the above figure the following trends are visible:
•Soil health scores increased between 2015and 2018, but then decreased again for the
2019/20 season. This is primarily due to a much lower value for the CO2-C respiration value
•The lower respiration value for 2019/20 is not due to reduced levels oforganic C, which
increased from theprevious season; meaning that it could be due either to lower microbial
levels in the soil and/or lower levels of microbially active carbon. Both these factors are
closely related to climatic conditions.
•Organic C has increased substantially over time, although the relationship is not linear.
•Organic N has increased substantially over time, again not linearly.
•The C:N ratio increased systematically for the first four years of measurement and then
decreased to 12,8:1 in the 2019/20 season. It indicates a higher proportional increase in
organic nitrogen in the soil compared to organic carbon, through the CA practices employed
in the programme. The lower this ratio is, the more organisms are active and the more
available the food is to the plants. The most ideal values for this ratio are between 8:1 and
15:1. The 2019/20 value thus points towards a lower microbial populationin this season,
rather than a lower level of microbially active carbon and is an effect of the environmental
conditions – increased heat during the growing season.
•The extreme climatic conditions in the area, including heat and dry soil profiles, reduces
the soil health impact of the CA practices andincreases variability in the results for different
The general assumptionhere is that if the levelof organic C in a plot is high, then the microbial
respiration will also be high, as will the soil health score and vice versa. This is not always the case,
however, as the relationship is not necessarily linear.
The CO2-C respiration also gives an indication of the potential mineralisation of N for the soil as well as
organic matter content. The small table below indicates these relationships.
Test results ppm
N mineralisation potential
HighN-potential soil. Likely sufficient N
for most crops
Soil very well supplied with organic matter.
Moderatelyhigh. This soil has limited
need for N supplementation
Ideal state of biological activity and adequate
Moderate. Supplemental N required
Requires new applications of stable organic
matter. Biomass <1200ppm
Moderate-low. Will not provide sufficient
N for most crops
Low in organic structure and microbial activity
CO2 - C(ppm)Organic C (ppm)Organic N (ppm)C:N ratioSoil health
2015 132,7118,511,7 12,1 13,6
2016 73,0 198,6 14,014,68,5
2017 86,2280,519,4 14,0 15,2
2018 149,7227,014,6 16,6 18,7
2019 70,8267,021,1 12,8 14,6
SH scores in Bergville; 2015-2019
Little biological activity. Requires
Very inactive soil. Biomass<100ppm.
Consider long term care
For the above figure, the following trends can be seen:
•All the CA samples for all three villages fall within the >100ppm and 61-100ppm C02-C respiration
categories, indicating adequate to high levels of organic matter, an ideal state of biological activity
and a moderate to high N mineralisation potential.
•These results indicate an ideal state of biological activity, with minimal need for N supplementation
and adequate organic matter in the soil.
In conclusion, the soil health status of the CA trial plots is moderately high to high, with good
organic matter content and ideal states of biological activity.
2.Different CA cropping options
The CA experimentation process has been designed to maximise crop diversity.
The following progression has been used:
•Years 1 and 2: Single cropped plots of maize (M) and beans(B) and intercropped plots of M+B
and M+C (cowpea).
•Year 3: Inclusionof cover crops; a 3-species mix of summer cover crops (SCC) including
sunflower, millet and Sun hempand a 3-species mix of winter cover crops (WCC), Saia/black
oats, fodder rye and fodder radish.
•Year 3+: Inclusion of legume cover crop – Lab-labbeans (LL).
•Year 3+: Rotation of the above-mentioned plots within the CA trial (tenplots).
The assumption is that the combination of multi-cropping and crop rotation would provide for the fastest
build-up of organic matter and improvement of SH for thissmallholder CA system.
The table below outlines the cropping pattern for Phumelele Hlongwane’s CA trial (Ezibomvini,
Bergville),consisting of tenCA plots, as well as her control plots. Control plots are planted to maize
only, using the farmer’s choice of spacing, maize variety and nutrient provision (fertilizer and/or
Analysis for the first two seasons 2015/16 and 2016/17, showed a trend of higher SH values for
intercroppedand multi-cropped plots (SCC), compared to single cropped CA plots (M), indicating the
importance of crop diversification for soil health in the CAsystem.
Greysquares indicate plots
sampled for SH analysis
Rotations have been done,
attempting to ensure a
different crop/crop mix on
each plot in each
The assumption was then made thatif crop rotation is included as a practice in such a multi-cropping
system, then the SH for all the plots would increase over time and that variability between the plots
would decrease, as each plot undergoes a rotation of multiple crops.
This trend of higher SH scores that are similar across plots, wasnot realised for Phumelele in herfourth
season of crop rotation with multiple cropping options, as variability between the SH scores for her
different plots was still quite high.
Below are two graphs comparing her thirdand seventh year of implementation.
Figure 18: SH scores for different CA plots and cropping options for Phumelele Hlongwane; 3rdand 7thyearsof
CA implementation (2016 and 2019)
The results from the figure above indicate that:
•Plot 5 still has the lowest SH score, as was the case for the previous two years of analysis as
well. This is considered to be due to particular soil conditions in that plot.
Average of % OM3,40 3,20 3,30 3,10 5,30 4,23 2,90
Average of CO2 - C, ppm C90,20 68,70 78,40 54,50 62,70 97,47 52,30
Average of Organic C ppm C203,00 157,00 222,00 204,00 201,00 245,08 216,00
Average of Organic N ppm N13,706,5015,20 13,40 12,50 76,05 11,80
Average of C:N ratio14,82 24,15 14,61 15,22 16,08 17,43 18,31
Average of Soil health Calculation9,49 5,06 9,11 6,96 7,16 9,65 6,20
Soil health for different CA plots and cropping options; Phumelele
Hlongwane; 2016 (3rd year of CA implementation)
Average of %
CO2 - C,
2 - M+B3,7 61,1280,028,6 9,8 14,6
4 - M+C3,6 48,0219,023,6 9,3 11,5
5 - LL3,940,5 191,0 16,811,49,6
6 - SCC3,5 52,8199,023,0 8,7 11,6
9 - M+B4,062,0328,028,9 11,3 15,7
(blank) - CA control M2,953,7227,016,0 14,2 11,5
(blank) - Veld4,176,4221,017,1 12,9 13,8
Soil health for different CA plots and cropping options; Phumelele
Hlongwane; 2019 (7th year)
•All CA plots (2,4,5,6,9) have a higher %SOM than the CA control plot for 2019, but not 2016,
indicating a build-upof OM over this period for the multi-cropped and rotated CA plots.
•Variability between the plots for CO2-C respiration, organic C and organic N is quite high for the
2019 season, following a similar trend to2016. This was also noted for the 2017 and 2018
seasons, although the results are not presented here.
•There is, however, an increase in Organic C and Organic N across all the CA plots (2,4,5,6,
9) for 2019, compared to 2016.
•There is a decrease in the C:N ratios for all the CA plots (2,4,5,6,9) for 2019, compared to
•SH scores for 2019for the CA plots (2,4,5,6,9) are substantially higher than those for 2016.
•SH scores for the veld sample are also much higher. This is considered to be due to
environmental factors rather than to a change in condition of the veld where the sample was
taken. Note that the veld sample was taken from the same place, in the same way for both
seasons. This also indicates that the higher SH scores for 2019 for the CA plots cannot be
attributed only to the cropping practices.
In conclusion, it has not been possibleto contribute differences in SH directly to different
cropping options within a multi-cropping rotation CA system. It has also not been possible to
attribute a decrease in SH score variability to rotation of multi-crop options. It is, however, clear
that the combination of crop rotation of multi-crop options has improved and stabilised SH
scores over time.
220.127.116.11Soil organic matter
Soil organic matter is where soil carbon is stored andisdirectly derived from biomass of microbial
communities in the soil (bacterial,fungal, and protozoan), as well as from plant roots and detritusand
biomass-containing amendments like manure, green manures, mulches, composts and crop residues
(Motaung, 2020). Soil organic carbon refers to the carbon component of soil organic matter (SOM) that
is measuredin mineral soil which passes through a 2mm sieve. Itis the largest componentof SOM
(approximately 45%) and the easiest and cheapest to measure. The SOC content of agricultural soils
is generally between 0,5% and 4%.
There is general agreementamong researchers that CA improves soil health by increasing soil organic
matter (SOM). Increased soil organic carbon (SOC) also sequestrates atmospheric carbon and thereby
contributes to climate change mitigation targets (Swanepoel, et al., 2017).
Despite this agreement, some studies in Africa and Southern Africa have reported only small increases,
or very slow build-up of SOC and negligible increases compared to conventional systems. It is being
argued that the build-up of SOM in CA systems is related more to increased biomass and organic mulch
than a reduction in tillage(Giller, et al., 2009). It has also been suggested that in drierclimates with
sandier soils it may take up to tenyears to detect a noticeable difference in SOC accumulation(GRDC,
In addition, it has been suggested that to get reliable data on changes in SOC related to land use
patterns, large numbers of samples need to be taken – between 80and 500 on average for croplands
and undisturbed soils such as forests, respectively (Stolbovoy, et al., 2007). This is not financially
feasible for small, multifaceted programmes such as the CA-SFIP.
Sampling for laboratory analysis of soil health is, as described above in section 1, with 20 subsamples
making up any one sample, generallywithin a 100m2area, taken during the fallow season and air dried
and stored at room temperature prior to analysis. Soil depth for samples is 0-10cm, as this is the depth
of soil where the most change in SOC is likely to occur.
Percentage SOC (kg C/kg soil x 100)has been provided for these samples (Soil Health Solutions
Laboratory, WC). A constant factor of 1,72 is used in South Africa, to convert %SOC to %SOM (GRDC,
For the 2018/19 cropping season, sampling was done for tenparticipants across five villages between
their third and sixthyear of CA implementation, and for the 2019/20 cropping season sampling was
done for eight participants across three villages between their fourth and seventhyear of
implementation (including all previous participants from the corresponding villages).
The table below is a summary ofthe %OM for a combination ofall CA experimentation plots (B, M,
M+B, M+CP and SCC) as well as the CA control plots (maize only), compared to veld benchmark
CA control M
*This value is a combination of control plots in 2018, which included CA control plots as well as conventionally tilled plotsplanted
to sweet potato, as an alternative was sought for the control plots that could more closely represent tilled plots. However, since
the planting and crop histories of these alternative controls were not properly considered, they were removed for the 2019
SOC and %OM derived from this declined in the veld samples between 2018 and 2019, leading to a
soil carbon density calculation of 4,2tC/ha and 3,5tC/ha respectively. At the same time, the CA plots
(which area combination of all treatments or different cropping options) and the CA controls (which are
for monocropped maize), evened out in 2019 to the same value of 3,6tC/ha.
Carbon accumulation for the whole CA system(experimentation plots and control plots)is
between 0,2 tC/ha and 0,5tC/ha. This provides an indication that CA can allow for SOC
accumulation even under adverse climatic conditions (late onset of summer rainfall, high
temperatures and mid-season dry spells), although longer-term averages wouldneed to be
calculated to verify this trend.
Yield measurements wereundertaken annually for both the CA trial options (maize, beans, cowpeas,
summer cover crops) and CA control (maize only) plots.
For maize, the cob and grain weight for each participant wasaveraged prior to a count of the number
of cobs per 50kg bag and then a count of the numberof bags per plot, to estimate the yields. Maize
was assumed to be between 70% and 80% dry, based on visual assessments made in the field.
In Bergville, yields for maize and beans in the CA trial plots werecalculated for a selection ofparticipants
(N=70)in their second to seventhyear of CA implementation, to get an overall average for the season.
Table 7: Average yields for maize and beans in CA trial plots; Bergville (2014-2019)
Maize and bean yields (CA
No. of villages
No. of trial participants
Area planted (trials) (ha)
Average yield maize (t/ha)
Min. and max. maize yield
Average trial quantity of
Rand replacement value of
Average yield of beans (t/ha)
Due to climate variability (late onsetrains and rainfall variability in season) the initial gainsin average
maize yields under CA implementation from 3,6t/ha to 5,7t/ha on average between 2014and 2017
could not be maintained into 2018 and 2019.Maximum yields obtained by individual smallholders have,
however, increased from 7,6t/ha to 12,8 t/ha in that time, indicating that for high performing
smallholder farmers a yield gain of around 1t/ha per annum is possible under CA cropping
systems despite difficult climatic conditions. During this period, average maize control plot
yields didnot increase but remained stable at between 2,5 t/ha to 3,5t/ha.
When the average yields for participants arecompared with their length of involvement in CA
implementation (between twoand sevenyears), it was found that there is a general increase in yield
linked to number of years of involvement, starting with an average of 1,8t/ha for secondyear
participants and ending with an average yield of 4,5t/ha for seventhyear participants. A similar trend
cannot be seen for the CAcontrols which remained reasonably constant at 2,5t/ha for thirdyear and
seventhyear participants, as shown in the line figure below.
Figure 19: Yield averages for CA trial and control maize for participants in their 2ndto 7thyear of implementation
The difference in treatments betweenCAtrial plots and CAcontrol plots is that the latter havebeen
planted to maize only throughout and there may be further differences in fertilizer application and seed
Here the results indicate the potential for incremental improvement in maize yields using the
multi-cropping CA system, as opposed to a CA monocropping system where the yields
remained similar across six years of CA implementation.
We undertooka comparison of yields for thisseason across thevillagesto ascertain how big these
differences were. As shownin the figure below, these differences are reasonably substantial– between
2,4 t/ha to 5,1t/ha for the CA trial plots and 0,9 t/ha to 4,4 t/ha for the CA control plots. A lot of this
variation has depended on how well the CA principles have been implemented over time.
Average of CA trial yield (t/ha)1,8 3,6 3,8 2,7 5,3 4,5
Average of CA control yield
(t/ha) 2,5 2,2 3,2 3,3 2,5
Yield for CA trial and control maize for 2nd-7th year participants; 10
Figure 20: Average maize yields (t/ha) for CA trial and CA control plots across tenvillages in Bergville (2019/20).
In Vimbukhalo, Ngoba andNdunwane,the participant farmers wereslow to implement all three
principles of CA, opting repeatedly for wider spacing and single crop planting. Yields in these three
villages averaged 2,5t/ha this season. Eqeleni, Ezibomvini and Stulwane are the three villages where
participants have most consistently employed multiple cropping options and rotations in their sixyears
of involvement and yields for these three villages averaged around 4t/ha this season.
For the villages involved for threeto fouryears in CA implementation, a similar trend can be seen. For
the two villages where participants did not consistently undertake multiple cropping and crop rotation
options (Thamela and Mahlathini), the average yield is around 3,1t/ha and for the two villageswhere
these options wereincluded (Emabunzini and Emadakaneni), the average yield this season was5 t/ha.
In conclusion, there isnolinear relationship between yield and length of involvement in CA
implementation, but there is a definite trend ofimproved yields for those participants who more
consistently included the multiple cropping options in their CA trials.
Soilbulk density (BD), also known as dry bulk density, is the weight of dry soil (mass of solids) divided
by the total soil volume (Vsoil). Total soil volume is the combined volume of solids and pores which may
contain air (Vair) or water (Vwater), or both.
High bulk density is an indicator of low soil porosity and soil compaction, whichmay cause restrictions
to root growth, and poor movement of air and water through the soil. It has also been shown that
minimum tillage practices increase bulk density withoutrestricting aeration and water movement in the
soil, compared to the same soils under tillage (Cavalieri, da Silva, Leão, Dexter, & Håkansson, 2009).
In general, bulk densities greater than 1,6 g/cm3tend to restrict root growth(McKenzie, Jacquier, Isbell,
& and Brown, 2004). Sandy soils usually have higher bulk densities (1,3–1,7 g/cm3) than fine silts and
clays (1,1–1,6 g/cm3) because they have larger, but fewer pore spaces. In clay soils withgood soil
structure, there is more pore space because the particles are very small, and many small pore spaces
fit between them. Soils rich in organic matter (e.g. peaty soils) can have densities of less than 0,5 g/cm3.
On cropland, long-term solutions tobulk density and soil compaction problems revolve around
decreasing soil disturbance and increasing soil organic matter. A system that uses cover crops, crop
residues and/or reduced tillage results in increased soil organic matter, less disturbance and reduced
bulk density. Additionally, the use of multi-crop systems involving plants with different rooting depths
can help break up compacted soil layers.
The small table below outlines the relationship between soil type and bulk density (NRCS, 2011).
General relationship of soil bulk density to root growth based on soil texture
Average of CA trial yield (t/ha)5,1 4,9 4,7 3,6 2,9 2,5 2,4 3,6 3,3 2,5
Average of CA control yield (t/ha)3,9 2,4 4,4 3,2 2,9 2,5 2,5 0,9
Average maize yields across villages; 2019/20; N=70
Ideal bulk densities for plant
Bulk densities that restrict root
Samples werecollected from the top 5cm of soil using sampling rings 7,2cm in diameter using the
•The ring was pushed (buried) into the ground using a piece of wood and a hammer (the
piece of wood was used to protect the ring).
•A spade was used to dig the ring out of the soil.
•Excess soil sticking out of the ring was cut using aknife to ensurethe soil fittedperfectly
into the ring (making sure the volumewas the same for all samples).
•The soil samples (in the ring) were wrapped with aluminium foil and transported to the lab
•At the lab, samples were unwrapped, placed in aluminium dishes, weighed and assigned
codes, and put in an oven to dryat 100°C for 48 hours.
•After 48 hours, samples were weighed and the masses were recorded for calculation of dry
Figure 21: Left to right: Sampling procedure for bulk density
The equation used to calculate the total soil volume is shown below.
𝑉𝑜𝑙𝑢𝑚𝑒'!"#$%&' =𝜋𝑟'× 𝑑
Where, π is pi, r is radius and d is depth for the ring, volume was calculated in cm3and mass ofthe
sample was measured in grams (g).
Average dry mass for all samples collected in the same plot was used to calculate the bulk density and
the same volume (based on the dimensions of the ring) was used. Equation 2 was used to calculate
Below is a summary of the results of bulk density calculations for differentcropping practices within the
CA system for three participantsin Bergville. They were chosen for having differing periods of cropping
under CA and for inclusion of severalpractices within their CA system– intercropping and planting of
summer cover crops (SCC).
Table 8: Bulk density (pb) results for three CA participants(2019)
Table 9: Bulk density (pb) results for two CA participants(2020)
These results indicate an increase in ρb over the period of involvement in CA. This trend is
expected. There is little to no difference between the CA practices, although for both 2019 and 2020
the planting of SCC reduced the ρb to some extent. These results also indicate that multicropping
options, such as a 3-5 crop summer cover crop mix, reduces bulk density of soil, which provides
a significant advantage for the crops following this rotation.
An explanation for this trend is that ploughing increases the presence of macro-pores in the short term
but less structuralstability under CT can lead to lower porosity, higher bulk densities and greater soil
strength with time, as tillage-induced pores readily collapse. Although initial conversion from CT to CA
usually results in higher bulk densities it is unlikely that plant growth will suffer markedly because of
insufficient moisture and poor aeration status. Improved aggregation and pore connectivity under CA
allow the soil to maintain an adequate supply of moisture and air(Cavalieri, et al., 2009).
These results for both 2018 and 2020 also indicate that the bulk density of the soils isquite high, in fact,
close to being restrictive to root growth, as ideal ρb for clayey soils is <1,10 g/cm3(NRCS, 2011).
An average ρb of1,3g/cm3is used for the water productivity calculations.!
Crop water productivity (CWP) relates to the amount of yield per unit of water used. It is an important
measure of the impact of different practices on productivity in rain-fed agricultural systems. Methods for
improving CWP at field level include crop selection, planting methods, minimum tillage, nutrient
management and improved drainage, where appropriate.Average WP for maize is1,2-2,3 kg/m3(FAO,
In this research process, WP has been compared for different crops and crop combinations under CA.
Average bulk density
Average bulk density
The main variables used in calculating water productivity (WP) are yields and volume of water used to
produce that yield. There are standard methods for working out the yield (e.g. putting the harvested
grain or biomass on a scale and weighing it,weighinga sample of maize cobs and estimating yield
using the plant population). The challenge is in determining the volume of water used to produce the
yield. There are a couple of methods (simple and more complicated) used in determining the volume of
To determine waterproductivity, parameters (temperature, relative humanity, solar radiation, wind
speed, wind direction to calculated ET0) are required and these parameters are gathered from automatic
weather stations. This information can beused to benchmark simpler methods used in the field that
farmers can be involved in. These ET0values are then multiplied by the crop coefficient to find the
actual evapotranspiration (Etc), which is the volume of water used to produce the yield.
To calculate the ET0, the equation below is used. The weather station calculates the reference
evaporation ET0using the Penman Monteith equation shown below.
𝑇 + 273 𝑢'(𝑒"− 𝑒+)
∆ + 𝛾(1 + 0.34𝑢')'
ET0is reference evapotranspiration (mm/day)
Rnis net radiation at the crop surface (MJ m-2day-1)
G is soil heat flux density (MJ m-2day-1)
T is air temperature at 2 m height (°C)
u2is wind speed at 2 m height (m s-1)
esis saturation vapour pressure (kPa)
D is slope vapour pressure curve (kPa °C-1)
g is psychrometric constant (kPa °C-1).
Water productivity was calculated for two participants in Bergville (2019), Phumelele Hlongwane
(Ezibomvini) and Ntombakhe Zikode (Eqeleni). Both participants had beenimplementing CA for a
period of fiveyears. Water productivity for differentCA cropping options was calculated for both
participants; in this case using the grain weight only.
The options werea M-CA control (consecutively mono-cropped maize); M-CA trial (single cropped
maize in a rotation system); M+C-CA trial (maize and cowpea intercropped plot in a rotation system)
and CA-M+B trial (maize and bean intercropped plot in a rotation system). The aim was to ascertain
whether thedifferent cropping options within the CA system provide for different water productivity
outcomes. The results are shown in the figure below.
Figure 22: Water productivity for different CA cropping options for 2participants (2019)
M + B-
M + B-
M + B-
PH PH PH PH NZ NZ NZ NZ
WP (kg/m3)2,18 3,53 3,17 4,40 1,04 1,15 1,33 0,86
Water Productivty (kg/m3)
PH -Phumelele Hlongwane
NZ -Ntombakhe Zikode
M=Maize B=Beans C=Cowpeas
A similar processwas undertaken for 2020, but in this case WP calculations were done for four
participants across fourvillages, to expand the exploration.
Figure 23: Water productivity for different CA cropping options for 4 participants (2020)
Comparing Figures 20 and 21, the following trends can be seen:
•Water productivity for both Phumelele Hlongwane and Ntombakhe Zikode are lower for the
2020 season than in2019.
•In both seasons, PhumeleleHlongwane’s water productivity, for all the crop combinations
tested, are higher than that of the other participants.
•For both seasons, intercropped CA plots (both M+B and M+CP) are higher than single
cropped CA-M plots.
•Water productivity for conventionally tilled maize is lower than the CA control maizeplot.
Water productivity for CA maize grown as anintercrop with beans orcowpeas is higher than
single cropped CA maize and water productivity for CA plots ishigher than conventionally tilled
plots. Despite annual differences in water productivity, these trends remained the same across
The CWP was also calculated
for the above-ground maize
plant material (stalks and
leaves). Again, there is a very
clear trend of much improved
WP for the maize when
intercroppedwith either beans or
cowpeas. The small figure
alongside provides an average
for Bergville (four participants
across fourvillages) for the
2019/20 cropping season.
M+B CA-M Contr
M+B CA-M CA-
NZNZNZNZNZNM NM NM NM NM NMPH PH PH PH PH PH PH BH BH BH
EqeEqeEqeEqeEqeStu Stu Stu Stu Stu StuEziEziEziEziEziEziEziNdu Ndu Ndu
Water Productivity (kg/m3)1,55 1,03 0,75 0,86 1,54 0,71 1,56 1,21 1,99 1,40 0,85 0,58 1,16 2,37 1,93 1,67 2,38 1,16 1,11 1,10 2,19
Water Productivty (kg/m3)
Contr CA-MCA-M+B CA-M+CPConv.
Total 6,297,0613,66 12,473,17
Maize biomass CWP
Examples of farmer-level experimentation in Bergville
The photographs below provide a visual snapshot of some of the farmer-level experiments undertaken.
Figure 24: Stuwlane; Left: Chupile Buthelezi’s maize and scc (sunflower, Sun hempand millet) intercrop. Centre:
Khulekani Dladla’s maize and bean intercrop and a plot of sunflowers. Right: Nelisiwe Msele’s CA trial with SCC
in the foreground.
Figure 25: Ezibomvini: Left: Nombono Dladla’sCA trial with Dolichos(LL) and a maize and cowpea intercropped
plot in the foreground. Centre: Phumelele Hlongwane’s maize and bean intercropped CA plot. Right: Velephi
Zimba standing in her SCC plot (Sun hemp, millet and sunflower).
Figure 26: Eqeleni: Left: Ntbombakhe Zikode’s WCC Isaia oats, fodder rye, fodder radish) CA trial plot. Centre:
Smephi Hlatshwayo’s single cropped CA maize. Right:Thulile Zikode’s SCC (millet, Sun hempand sunflower)
Livestock are an important component of the smallholder farming systemand crop-livestock integration
can offer important gains in terms of sustainability and climate resilience.
Aspects of crop-livestock integration that wereconsidered are the following:
•Inclusion of fodder species for poultryand livestock into the cover crop mixes in the rotation
and multi-cropping system, including summer (sunflower, millet, Sun hemp, Dolichos
beans, cowpeas) and winter (Saia oats, fodder rye, fodder radish)covercropping options.
•Winter fodder supplementation.
•Strip cropping with perennial fodder species.
Cover crop mixes
The summer cover crops (millet, Sun hemp, sunflower, sorghum) have been planted either in separate
blocks or as intercropping options with maize. Some participants practiced a cut and carry system for
their livestock, but mostly these crops areleft to seed and the seed used as feed for poultry.Winter
cover crops have been grazed directly off the fields when cattle are let in, usually towards the end of
Figure 27: Examples of cover crop seeds kept by participating farmers. Left: sorghum. Centre: Sun hemp and
forage sorghum. Right: Babala (millet).
Despite the advantages in soil health, yields and fodder availability that these experiments have shown,
farmers have been slow to expand the areas under cover crop production due to a combination both of
difficulty inpaying for seed and a conception that
due to limited field sizes and labour, a focus
entirely on food production for themselves is the
Winter fodder supplementation
Participants undertook to provide
supplementation for a selection of their livestock
whichrequired supplementation, mainly cows
with calves or sick and ailing animals. A body
condition score sheet (shown right) was used to
assess the outcome of the supplementation,
which was continued fora minimum of one
A process was undertaken to cut and bale veld
grass as well as a proportionof the cover crop
residues participants had planted – namely cowpea, Dolichos bean, teff and maize. In addition,
supplements were introduced that could be included in these “rations” for winter feeding. These included
LS 33 and Premix 450. Seven participants undertook this experimentation process and five of these
participants recorded their feeding as well as the results using the livestock condition scoring sheet, as
shown in the table below.
Table 10: Fodder supplementation experimentation (2018/19)
(with start date)
32 – veld grass
premix 450 (2x50
2 cows – 1x/day (1
From 2 to 4
40 – veld grass
4 of 16 cows – every
From 2 to 4
9 – Lab-lab
3 – grass, maize stalks,
LS33 (4,8 L)
5 of 17 – every 2nd
From 2 to 3
10 –veld grass, Lablab,
cowpeas, maize stalks
LS33 (4L), premix
4 of 19– every 2nd
From 0 to 3
6 – veld grass
2 – teff
LS33 (4L), premix
1 of 4 – every 2nd
From 2 to 4
In general, this process managed to either maintain or improvethe livestock’s condition for all seven
participants. At the end of the experimental process, livestock were all scored at ratings 3 (ribs well
covered and body outline smooth) or 4 (ribs not visible and body outlinerounded), according to the
condition scoring sheet shown above.
Participants werevery satisfied with the outcomes of these experiments and feltthat they couldcontinue
with supplementation in future. The supplements are relativelycheapand now that they have some
experience with cutting and baling grass, they also feel this is manageable and a good idea.
Participants also commented that they did not need to herd the animals that were being fed as they all
startedcominghome to the kraal in the evenings for their “meals”. This is a major advantage.
Participants also agreed that the cattle prefer the LS33 over the premix 450. The LS33 however, is a
bit more expensive (R180/20L versusR230/50kg).Sixteenparticipants (50% were women)
volunteered to try out the supplementation experimentation process in the coming season. In addition,
a brush cutter was procured for the learning groups to facilitate the cutting and baling of grass.
Figure 28: Left: A manual baler (background) being used to make veld grass bales (foreground). Centre:
Phumelele Hlongwane measuring out the daily Premix 450 ration for her cows. Right: Khulekani Dladla’s bales
stored in an unused rondavel for lateruse.
Strip cropping with perennial fodder species
Perennial grasses are planted once, require no repurchasing of seed and act as a good cover forthe
soil all year round.
Strip cropping with perennial grass speciescan be achieved in twoways:
a.Selected by using a broad leaf herbicide and repeated mowing–which selects for
perennial grasses such as Digiteria/Catstail grass (Msila wekathi)
b.Planting specific species such as
i.Paspalum/Bahia grass (Mbiligrass),
ii.Lespediza/poor man’s Lucerne, which is a hardier legume than Lucerne
without the high liming requirement, that can also be interplanted with grass.
There are low tanninvarieties now available, which removes the need for
carefully managed intake by livestock,
iii.Tall fescue, whichis a grass planted in either spring/autumn, that remains
green throughout winter, and
iv.Napier grass, which grows considerably more slowlythan the other perennials
but lasts longer. It is grown extensively in otherAfrican countries such as
Kenya where it is cut and fed to cattle.
An experimental layout plan was consideredfor the farmer-level experimentsas follows: strips of2,5m
x 10m, with fourrows/stripand a seeding rate 20kg/ha (thus 50g per strip for perennials).
Bahia grass (Pensicola)
Maize (Short season)
Poor man’s Lucerne (Lespedeza)
Maize (Short season)
Mooiriver mix (Digiteria spp)
Maize (Short season)
Tall fescue (Festuca arundinacea)
Thereafter a list of participants who wanted to undertake the experiments wascompiled.
Name and surname
Strip cropping with SCC
(and cutting for hay)
Strip cropping with perennial
grasses and legumes
Strip cropping trials were initiated in the middle of January 2020. Ten of the 15volunteers planted their
strip cropping trials. Germination of the grass species was, however, extremely patchy and quite low in
most cases. Some of the plots were overrun by weeds, at which pointneither the farmers northe
facilitators could identify the grass species from the weed species.
Figure 29:. Left: Nothile Zondi’sstrip cropping trial with the short season maize strips growing vigorously and the
Lespedeza strip showing some growth. Right: The Mooiriver mix (Digiteria) did not germinate.
Figure 30: Right: An overgrowth of weeds in
Thulani Dlamini’s strip cropping trial plot made
identification of the planted grass species virtually
Khulekani Dladla triedto deal with the hot dry
conditions in his strip cropping trial plot by
mulching,which helped,and he managed to
get the Lespdeza and Pensacola (Tall Fescue)
Figure 31:. Left: Kulekhani Dladla mulched his strip cropping trail. Right: Germination and initial growth for
Pensacola (Bahia grass) was promising, upon monitoring in early March 2020.
Figure 32:. Left: Mtholeni Dlamini’s Bahia grass growing very well in a strip between late season beans and short
season maize. It appears soil moisture conditions in his field were much better and we suspected an
underground spring or high watertable here. Right: Thulile Zikode’s Bahia grass eightweeks after germination
It was decided to replant Lespedeza in early March 2020 by the following participants, as rain was
unusually plentiful this late in the season. Ten of the participantsdid the planting.
Figure 33: Left: Thulile Zikode’s Lesepdeza, planted in mid-March germinated and grew well. Right: the same plot
tenweeks after germination (early June).
As can be seen from the figure above and from farmers’ comments made, it is clearthat the fodder
species that germinated established well but grew very little in the following months; mostly as a result
of planting so late in the season.
In conclusion: Further experimentation with strip cropping only makes sense if participants can
plant earlier in the season, with careful management and weeding. The two most likely options
to continue with (those that were hardy enough to survive this season) wereLespedeza and Tall
Fescue grass. The Mooiriver mix only survived for one participant.
3 LEARNING AND BEST PRACTICE OPTIONS
The CA experimentation workshops are run over a period of twoto threedays, starting with a day of
theory and discussion followed by practical demonstrations, after whichthe farmer volunteers plant their
own trial and control plots.
Minimum tillage and soil cover are not intuitive concepts for smallholders,as thesedirectly oppose their
normal or habitual farming practices. The presentation of the CA principles and reasoning is done with
as many photographs and visual examples as possible; either using a PowerPoint presentation or using
A4 colour platesas visuals.Topics covered in the
presentation includeprinciples of CA, different planting
options and planters, farmer-level experimentation and layout
of CA trials,intercropping examples, reduction in runoff,
cover crop options (summer and winter combinationsand a
Figure 34:. Introduction of concepts in CA and cover crops using printed slidesintwo different villages
Comments from the Limpopo groups included:
•“Use of pictures in the slides helpedus to visualise what was being taught.”
•“Maybe you should make notes on the flipchart in Sepedi and not English to allow us to also
•“You keep showing us examples of CA from other places, is it because you do not have local
•“One thing that is clear is that we have not left as much soil cover as we see in the pictures.
This could be because in winter we clear and turn the field croppingplotsinto a garden. This
also means that we till the soil, so we haven’t minimised the tilling. This has led to a lot of runoff
in the plots and in summer the rain washes away the seed and causes erosion.”
•“Seeing examples of places where CA has worked gives us courage to keep trying. One day
we might realise the same benefits. Even with the high level of uncertainty it is worth trying.”
•“It seems in the examples shown on the slides, the people have access to water or it rains a lot
in their area.”
These comments have assisted the team to fine-tune the learning process to be as participatory and
locally appropriate as possible.
For the practical demonstrations, a template using knotted ropes and pegs isused to assist farmers to
understand and internalise the layout and the importance of close spacing.The conceptof staggered
or zigzag planting is also demonstrated. The spacing is designed to ensure the development of an early
canopy cover for weed control, while minimising competition between plants.
Figure 35: Left: A demonstration plot in Bergville, working with therope templates for planting. Right: Mpelesi
Sekgobelafrom Sedawaplanting using the template.
In Limpopo, we also worked with participants to draw the layout on flip chart paper, for them to keep as
a record and reminder. This practice worked quite well here, but not in KZN, where literacy levels in the
learning groups was generally lower.
Figure 36: Left: Mr S Selala, the facilitator, showing the layout drawing/template in Turkey. Centre: Using a
variation with the actual seed laid out on the paper. Right: Abitha Shaai in Willows drawing out her learning
For the demonstrations and farmer-led trials, participants weresupported with provision of seed,
planters and other inputs as agreed upon. This was to reduce the risk in trying out new and unfamiliar
practices. The control plots weremanaged by participants in their normal way.
Farmer comments regarding the learning demonstrations:
•“This is the easiest way to plant. If I had used this method from the beginning, I would have
finished planting the whole yard in less than twodays.”
•“This CA method requires less labour and also less seed than our normal way of planting.”
•“We are not used to leaving residues on the soil surface; we usually remove weedsand organic
matter and then burn it. We see nowthat maybe residue is important, but it is difficult, as we
are used to seeing nice clean plots and this looks very messy. It is going to take us a while to
get used to this.”
•“We would need to make some adjustments in the way we do our cropping; dividing our fields
into two parts (garden area) and (fieldcropping area) andminimising or stopping burning of dry
weeds and crop residues, even though this is tricky as the crop residues take some time to
break down in the soil and snakes can hide in this mulch and make it unsafe for children to play
•“The spacing, especially between the beans, really seems to be too narrow. We are sure there
will be competition.”
•“We appreciated that you are patient with us, it helps us when our memories are being
refreshed; even though we should know this very well by now.”
•“You always try new methods to help us understand the subject matter.”
•“Please provide us with some sort of a template on how to plant different combinations under
CA, something that will look like a calendar that I can paste on a wall.”
•“We don’t collect wood anymore as such and ropes are not really available in the households,
but we will share the existing rope templates and try our best.”
•“Making the template was easy and it made the job a lot easier.”
•“Overall, we loved the layout made with seed on paper, I don’t think I can forget this.”
•“It is a good idea to work together to plant these trials. That way we can remind each other and
also plant faster.”
No-till planters are an important aspect of implementation of a CA cropping system. These areprovided
to the learning groups to share and use. As farmers become more familiar with the process, they are
encouraged to purchase their own planters, either as individuals or as groups.
Different planters have been introduced:
•Hand-held planters (MBLI planters and Harakaplanter).
•Animal-drawn planters (modified Magoye rippers and Knapick planters).
•Tractor-drawn planters (Eden Equip two-row planter).
Some illustrative photographsare shown below.
Figure 37: Left: Using MBLI planters. They operate similarly to hand hoes and are thus intuitive to use. Left:
Using a Haraka wheel planter. This planter only works with seed (and not fertilizer) butis much easier to use on
larger fields than the MBLI planters. Right: Three pictures illustrating use of a two-row tractor-drawn CA planter.
Figure 38:Left: Using a modified Magoye ripper no-till planter with oxen in KZN. Right: Testing the Knapick
planter with donkeys in Limpopo.
Facilitators’reflections on the CA learning process
•The concept of CA is knowledge intensive and difficult to convey in one learning session,
especially linked to deeply entrenched habits that work in opposition to the principles,such as
clearing and burning of weeds, wide spacing and the like.
•It would be ideal to be able to run workshops through the whole cropping season to make
observations and deepen the learning.
•Because the innovation system approach to learning relies on positive results from the farmer-
level experimentation, seasons such as the present one, where hot and dry conditions have
seriously hampered germination and growth, tend to be difficult for introduction of a new
practice. Farmers associate the lack of results with the practice, rather than theseason. It can
be almost impossible to disentangle different factors, such as lack ofsoil fertility on the
performance of the trials as well. It is thus common to have very variable results within a group,
with some participants faring reasonably well and other failing completely. Under such
conditions, uptake of these practices tends to be low.
•Participants somehow believe thatthis method cannot be used on larger fields as they have
now got into the habit of believing this is only possible with tractors and with assistance provided
in provision of seed. The concept of manual weeding is one they are not prepared to consider.
•The habit of planting without any addition of soil nutrients or manure is a very common practice,
specifically in Limpopo, andisa big challenge when trying to improve yields. It is,however,
extremely difficult to persuade participants to collect and use manure. Many have no access
and would need to buy this from people who do, which is a constraint.
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