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Rainwater harvesting in the Sahel

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Planting pits, Niouma [fr] near Yako, Passoré Province, Burkina Faso

Rainwater harvesting in the Sahel is a combination of "indigenous and innovative"[1] agricultural strategies that "plant the rain" and reduce evaporation, so that crops have access to soil moisture for the longest possible period of time. In the resource-poor drylands of the Sahel region of Africa, irrigation systems and chemical fertilizers are often prohibitively expensive and thus uncommon: so increasing or maintaining crop yields in the face of climate change depends on augmenting the region's extant rainfed agriculture systems to "increase water storage within the soil and replenish soil nutrients."[2] Rainwater harvesting is a form of agricultural water management.[3] Rainwater harvesting is most effective when combined with systems for soil regeneration and organic-matter management.[4]

Background

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Landscape gradient of the Sahel, photographed from space

The Sahel is an ecologically (rather than geopolitically) defined region of Africa. The noun Sahel comes from the Arabic sāḥil (Arabic: ساحل) describing a border, shore or edge, which aptly describes the transitional areas of Africa where savanna becomes the hyper-arid Sahara Desert. (According to the Concise Oxford Dictionary of World Place Names, "The Arabs considered the Sahara to be a huge ocean with the Sahel as its shore."[5]) The Sahel crosses Senegal, The Gambia, Mauritania, Mali, Burkina Faso, Ghana, Niger, Nigeria, Cameroon, Chad, Central African Republic, South Sudan, Sudan, and Eritrea in a belt up to 1,000 km (620 mi) wide that spans 5,400 km (3,360 mi) from the Atlantic Ocean in the west to the Red Sea in the east. The Sahel is marked by decreasing levels of precipitation from south to north, but what defines a dryland ecosystem is not necessarily low rainfall. In some cases the dryness is due to persistent high levels of evaporation (due to heat or desiccating winds). Unpredictable rainfall is often also a factor.[6]

The Sahel
  The Sahara
  The Sahel
  Sub-Saharan Africa

Population estimates of the Sahel vary depending on which political subdivisions are included, but the count is in the vicinity of 100 million people,[7] including nearly a million refugees and internally displaced people.[8] The countries of the Sahel region are mainly poor. For example, the Volta River basin is occupied by about 20 million people who live in the countries of Burkina Faso and Ghana; 61 percent of Burkinabe and 45 percent of Ghanaians live on less than US$1 per day.[9] About 12 million farmers in the region (including people in Niger, Chad, Mauritania, Mali, and probably Burkina Faso and Senegal[10]), are occasionally or "chronically vulnerable to food and nutrition insecurity."[11] The Brookings Institution has described Sahelians as among the "most underprivileged, marginalized, and poorest people" on Earth.[7]

Subsistence food production

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Irrigation in the Sahel tends to be reserved for cash crops like groundnuts; these Nigerian women are selling okpa made from groundnuts.

Agriculture contributes between 10 and 70 percent of GDP to the economies of most sub-Saharan countries.[12] The major agricultural systems of the Sahel are oasis, pastoral, and mixed production of cereals and root crops.[13] The root crops are predominantly sweet potato and cassava; cereals are predominantly millet and sorghum, with some maize; the "north-south rainfall gradient defines...a successive north-south dominance of millet, sorghum and maize."[9] Climate changes over the next 25 years are predicted to decrease Sahelian cereal production by double-digit percentages, largely due to increased heat.[14][11] The Intergovernmental Panel on Climate Change also predicts double-digit decreases due to increased rainfall variability.[15]

Homegrown staple crops account for an estimated 90 percent of food consumption in the Sahel, and 90 percent of these crops are grown using exclusively rain-fed agriculture.[16][11] A general African transition to first-world-style irrigation systems is considered unlikely, and the Sahel region has an "especially limited irrigation potential."[17] According to the United Nations Food and Agriculture Organization, no more than 10 percent of African food production is likely to be grown under irrigation over the next 20 years.[18] Mechanized irrigation, where it exists, is typically limited to more lucrative cash crops, rather than subsistence.[19] Therefore, in order to increase or even maintain the Sahel's dryland agriculture production capacity the "most logical strategy...will be improving rainfed productivity for most staples."[18]

Freshly ground millet flour ready for millet couscous or millet porridge; millet, a staple ingredient for cuisines across the arid and semi-arid Sahelian climatic zone, goes by many local names: in Wolof, soungouf, in French, farine de mil.

Rainfall and fertility

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Main articles: Desertification in Africa and Sahel drought

Precipitation patterns and soil quality are "key constraint[s]" in Sahelian food production.[20] Rainfall levels are both generally low to start with and "highly variable" to complicate matters.[21] This variability is a common cause of crop failure due to unpredictable "onset and distribution" of rainfall;[9] cereal yields are impacted by the start date and duration of the rain as much as by the absolute quantity.[15] The majority of the year is the dry season, which ends with harmattan winds blowing dust south from the Sahara; rain usually falls between one and four months of the year, from June through September.[22][23]

Soils in the Sahel are typically degraded, [21] often "crusty, abandoned agricultural lands"[24] and "particularly poor in organic carbon."[25] In Burkina Faso, one-third of all land is degraded.[26] The human-induced structural damage to soils[27] wrought by intensive 20th-century agriculture methods "is especially evident during droughts when the land is stripped bare of vegetation and erosive winds and water take their toll."[28] In addition to the toll of soil and wind erosion on old fields, the practices of burning or removing crop residues, and a shift to fewer or no fallowing periods due to increased population density (and commensurate increased need to cultivate all accessible land) have contributed to further decreases in natural fertility. [29][30]

The Sahel is dappled with "unproductive crusty patches" found on "old dunes, sandy plains, colluvial slopes, and alluvial terraces."[29] These "glazed" patches are regionally known as glacis and are found, for example, on approximately 60 percent of all degraded land in Niger.[31] "Glacis" describes a slope made particularly slippery, for whatever reason, and is related to the Old French glacier.[32] Glacis patches in the Sahel are more or less impermeable; rainwater runs off or evaporates, further immiserating the soil biome, and thus the plants and the people.[31]

Climate change

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Main articles: Climate change in the Sahel and Climate change and food security in Africa

Even before the full impact of climate change is felt in the Sahel, the region struggles with challenges including "unsustainable management strategies, weak economies, weak infrastructure, 'inappropriate resource tenure', inappropriate interventions (such as eucalyptus plantations), [and] ineffective institutions."[33] The future of the Sahel is insecure.[34] Climate change impacts will be variable but there is a "likelihood of negative impacts in most locations from increased temperatures, greater rainfall variability, and more extreme weather events."[35]

In South Sudan, a mother harvests the root crop cassava while her daughter collects firewood.

Rainwater harvesting techniques of the Sahel

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The purpose of rainwater harvesting in the Sahel and other dryland eco-agricultural regions is to extend the usability of irregular water inputs.[25] Banking rainwater (through techniques often summarized by the epigram "slow it, spread it, sink it") is possible with site-appropriate techniques and as more water becomes "available for ecosystems...their capacity to perform their functions is improved."[36] Furthermore, soil restoration is possible and would potentially open up more than 700,000,000 acres (280,000,000 ha) of land in Africa for additional cultivation, which could in turn reduce deforestation for agricultural uses.[26] Niger has implemented several of these techniques on a wide scale beginning in the 1980s and has recovered approximately 250,000 ha (620,000 acres) of degraded land.[37]

Benefits of rainwater harvesting (especially on a community scale) include additional drinking water for animals, land reclamation opportunities, higher soil fertility, accelerated growth of timber for firewood, and reinforcement of a virtuous cycle pattern leading toward additional rainfall[12] (trees make rain).[38] Any or all of the following techniques reduce water runoff and thus increase soil water storage, generally yielding about two to three times more growth than crops grown in the same regions/conditions under a more conventional system.[39] One study found that appropriately managed Sahelian rainwater-harvesting techniques increased runoff retention up to 87 percent, doubled water infiltration rates, and extended the crop-growing season up to 20 days.[40]

Bouli

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Bouli in Rambo-Wottionma, Burkina Faso

A bouli [fr] is a small-scale artificial pond dug "where there is convergence of runoff" at the midpoint or bottom of a slope. This water tends to last for two[41] or even three months into the dry period after the monsoon.[42][43] In addition to supplying additional water for livestock and vegetable gardens the bouli "can recreate an ecosystem favourable to the life of the fauna and the local flora, boosting recharge of water tables during droughts and allowing vegetation to grow even during the dry period."[44] Bouli may be the most poorly studied of the rainwater harvesting techniques appropriate for the Sahel, as there are relatively few studies about the mechanics and benefits of this system.[44]

Bunds

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Barrier to slow down the advance of sand dunes in the outskirts of Chinguetti, Adrar, Mauritania

Mauritian farmers build weirs to trap windblown sand during the dry season and during the "infrequent rains" these weirs serve to minimize water runoff and maximize groundwater recharge; the stone rows of Burkina Faso, Mali, and Niger function by similar principles.[45] Stone rows, typically called bunds, are a traditional and widely used means of land improvement in the Sahel. Laid out on contour, stone rows minimize soil erosion but also minimize rainwater runoff and offer favorable microclimates.[46][1][42] Bunds not laid out in parallel with the natural contours of the land may result in "some gully formation during rainy periods."[47] Bunds can also be made of earth, which was the original practice that preceded the use of stone.[46] Bunds may be laid out up to 30 meters apart and may themselves be planted with indigenous vegetation such as Andropogon gayanus or Piliostigma reticulatum.[46]

Both earth and stone bunds are prone to material deterioration over time and demand periodic maintenance; as a general rule, the more stones used the more stable the row.[46][44] Projet d’aménagement des terroirs et conservation des eaux (PATECORE) popularized the three-stone system for building more durable, animal-disturbance-resistant stone rows, in which one large stone is placed atop three smaller stones.[48][49][50]

Demi-lunes, or half-moons

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Main article: Semicircular bund
Stone bunds and demi-lunes constructed on a farm in Ethiopia

Half-moons, which are known as demi-lunes [fr] through much of the Sahel because of the French colonial influence on regional languages, are a widely used traditional form of semi-circular planting pit. Half-moons are formed by digging a hole up to four meters across but somewhat shallower in depth,[51] and "placing the removed earth on the downhill side." [42] Half-moons are particularly useful for remediating the more or less impermeable glacis soils.[31] These edged planting pits capture and hold organic matter and moisture. The accumulated detritus in turn attracts termites and other invertebrates whose actions create passages and pores in the organic matter, building humus, and permitting better water infiltration.[1][26] Half-moons have been shown to reduce the risk of crop failure and increase agricultural productivity, especially with the use of "complementary inputs" such as animal manures.[52]

Half-moons, however, are extremely labor-intensive: "constructing just one takes several hours"[30] and the preparation of the planting areas must be done during the dry season when the ground is very hard and the heat may be severe. According to one account based on interviews with Sahelian farm families, "preparation of [one hectare of demi-lunes] amounts to two to four person-months of work, and yearly maintenance of approximately one-person month is required."[1]

Zaï, or tassa

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Main article: Zaï
Zaï pit
Zaï pit

A zaï is a "water pocket"[42] and is another indigenous planting method, developed in the Yatenga.[53] The word comes from the Moré language, and means something like "getting up early and hurrying out to prepare the soil" or even "breaking and fragmenting the soil crust before sowing."[15] Tassa is the Hausa language word for this concept.[54] A similar practice in the Yako region is called guendo.[55] Similar to half-moons, but smaller, zaï are usually 24 to 40 cm wide, 10 to 25 cm deep, spaced about 40 cm apart in a grid across the field. Zaï are usually established with "two handfuls" of organic matter in the form of animal manure, crop residues, or a composted combination of the two.[44] These pits were traditionally used on a small scale to remediate degraded zipélé lands but are now being used on much larger plots.[47] Zaï are best-suited for use in areas that see "isohyets of 300 and 800 mm rainfall."[56] Zaï have been shows to increase yields between 2.5 and 20 times normal, "depending on the crop."[57]

As with half-moons, the major drawback of zaï is in the hundreds of man-hours that are necessary to build them.[58] Families must either have a large number of fit and able-bodied workers, or "pay for the services of the young people's association."[59]

Other techniques

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Other beneficial and successful practices in the Sahel include:

Obstacles to implementation

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Dried cow dung near Katari, Nigeria; in some cases a shortage of nitrogen-rich animal manures is a limiting factor on establishing zaï and demi-lunes[61]
Landscape of Mopti Region, Mali, in 1972, a period of severe Sahel drought

Widespread adoption of rainwater harvesting techniques in the Sahel is so far limited by a number of factors including a high upfront cost for labor.[62][63] The massive quantity and weight of stones needed to establish bunds is often prohibitive.[64] It is estimated that 40 long tons (41,000 kg; 90,000 lb) of rock are needed to establish stone rows for just one hectare of arable land.[61] Other limits include lack of knowledge about these techniques and the absence of training programs.[12]

In the words of one development analyst, "agricultural water management strategies have been over-studied, over-promoted, and over-funded. However, despite the efforts of numerous projects, water scarcity still limits agricultural production of most of the smallholder crop-livestock farmers of the basin and cereal yields are still lying far below their potential."[65] One study found that village training programs, "a low-cost policy intervention," were highly effective in increasing uptake of rainwater harvesting techniques.[66][67]

Additional images

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Rainwater harvesting in the Sahel
  • Annual rainfall in the Sahel
    Annual rainfall in the Sahel
  • Example of an arid pastoral-oasis agricultural system in Fada, Chad
    Example of an arid pastoral-oasis agricultural system in Fada, Chad
  • View of the horizon with the harmattan coming on
    View of the horizon with the harmattan coming on
  • "Dawadawa Tree in Clean and Beautiful Environment," Ghana
    "Dawadawa Tree in Clean and Beautiful Environment," Ghana

See also

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Sources

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  1. ^ a b c d Barry et al. (2008), p. vii.
  2. ^ Aker & Jack (2021), p. 1.
  3. ^ Douxchamps, Ayantunde & Barron (2012), p. 1.
  4. ^ Douxchamps, Ayantunde & Barron (2012), p. 25.
  5. ^ Everett-Heath, John (2020). The concise Oxford dictionary of world place names (Sixth ed.). Oxford. ISBN 978-0-19-190563-6. OCLC 1202624108 – via Oxford Reference Online.{{cite book}}: CS1 maint: location missing publisher (link)
  6. ^ Davies et al. (2016), p. 1.
  7. ^ a b Mbaye, Ahmadou Aly; Signé, Landry (11 March 2022). "Political turmoil in the Sahel: Does climate change play a role?". Brookings. Archived from the original on 2023-04-14. Retrieved 2023-04-14.
  8. ^ Ward (2016), p. 2.
  9. ^ a b c Douxchamps, Ayantunde & Barron (2012), p. 5.
  10. ^ Barry et al. (2008), p. 2.
  11. ^ a b c Berg, Lars (5 December 2018). "Harvesting rain to improve crops across Africa". rethink.earth. Stockholm Resilience Centre. Archived from the original on 2023-03-05. Retrieved 2023-03-05.
  12. ^ a b c Mengistu (2021).
  13. ^ Ward (2016), p. 12.
  14. ^ Sultan, B; Roudier, P; Quirion, P; Alhassane, A; Muller, B; Dingkuhn, M; Ciais, P; Guimberteau, M; Traore, S; Baron, C (1 March 2013). "Assessing climate change impacts on sorghum and millet yields in the Sudanian and Sahelian savannas of West Africa". Environmental Research Letters. 8 (1): 014040. Bibcode:2013ERL.....8a4040S. doi:10.1088/1748-9326/8/1/014040. ISSN 1748-9326. S2CID 53560914.
  15. ^ a b c d Jost et al. (2009), p. 5.
  16. ^ Ward (2016), p. 100.
  17. ^ Ward (2016), p. xxi.
  18. ^ a b Ward (2016), p. xxiii.
  19. ^ Ward (2016), p. 118.
  20. ^ Ward (2016), p. 19.
  21. ^ a b Tabor (1995), p. 83.
  22. ^ Ward (2016), p. 21.
  23. ^ Tabor (1995), p. 90.
  24. ^ Tabor (1995), p. 103.
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  32. ^ "glacis". Oxford English Dictionary (Online ed.). Oxford University Press. (Subscription or participating institution membership required.)
  33. ^ Tabor (1995), p. 83–86.
  34. ^ Jost et al. (2009), p. 4.
  35. ^ Ward (2016), p. 13.
  36. ^ Akuffobea-Essilfie et al. (2019), p. 2.
  37. ^ Jost et al. (2009), p. 6.
  38. ^ "Trees in the Amazon Generate Their Own Clouds and Rain, Study Finds". Yale E360. Archived from the original on 2023-04-16. Retrieved 2023-04-16.
  39. ^ Barry et al. (2008), p. 29.
  40. ^ Tamagnone et al. (2020), p. 1.
  41. ^ Davies et al. (2016), p. 30.
  42. ^ a b c d Barry et al. (2008), p. 4.
  43. ^ Hastrup, Kirsten; Rubow, Cecilie, eds. (2014). Living with Environmental Change : Waterworlds. Hoboken, N.J.: Routledge. p. 77. doi:10.4324/9781315797465. ISBN 978-1-315-79746-5. OCLC 871782134. Archived from the original on 2023-04-17. Retrieved 2023-04-17.
  44. ^ a b c d Davies et al. (2016), p. 29.
  45. ^ Tabor (1995), p. 88.
  46. ^ a b c d e Douxchamps, Ayantunde & Barron (2012), p. 8.
  47. ^ a b Douxchamps, Ayantunde & Barron (2012), p. 13.
  48. ^ Douxchamps, Ayantunde & Barron (2012), p. 18.
  49. ^ Ganaba, Souleymane (1 September 2005). "Impact des aménagements de conservation des eaux et des sols sur la régénération des ressources ligneuses en zone sahélienne et nord soudanienne du Burkina Faso" [Impact of water and soil conservation schemes on the regeneration of ligneous resources in the Sahelian and northern Sudanian zone of Burkina Faso]. VertigO (in French). 6 (2). doi:10.4000/vertigo.4314. ISSN 1492-8442. Archived from the original on 2023-04-20. Retrieved 2023-04-17.
  50. ^ Dugué, Patrick; Roose, Éric; Rodriguez, Luc (1993), "L'aménagement de terroirs villageois et l'amélioration de la production agricole au Yatenga (Burkina Faso) Une expérience de recherche-développement" [The Development of Rural Soils and the Improvement of the Agricultural Production in Yatenga (Burkina Faso). A Research-development Experiment] (PDF), Cahiers Orstom (Office de la Recherche Scientifique et Technique Outre-Mer Paris / Office of Scientific and Technical Research Overseas), Pédol. (in French), XXVIII (2): 385–402, archived (PDF) from the original on 2023-04-17, retrieved 2023-04-17
  51. ^ Douxchamps, Ayantunde & Barron (2012), p. 9.
  52. ^ Aker & Jack (2021), p. 26.
  53. ^ Douxchamps, Ayantunde & Barron (2012), p. 10.
  54. ^ Barry et al. (2008), p. 26.
  55. ^ Kaboré, Daniel; Reij, Chris (2004). "The emergence and spreading of an improved traditional soil and water conservation practice in Burkina Faso". EPTD Discussion Papers. Archived from the original on 2023-04-17. Retrieved 2023-04-17.
  56. ^ Douxchamps, Ayantunde & Barron (2012), p. 32.
  57. ^ Amede, Tilahun; Menza, Mesfin; Awlachew, Seleshi Bekele (January 2011). "Zai Improves Nutrient and Water Productivity in the Ethiopian Highlands". Experimental Agriculture. 47 (S1): 7–20. doi:10.1017/S0014479710000803. ISSN 0014-4797. S2CID 85207282.
  58. ^ Douxchamps, Ayantunde & Barron (2012), p. 30.
  59. ^ Barry et al. (2008), p. 24.
  60. ^ a b c Douxchamps, Ayantunde & Barron (2012), p. TK.
  61. ^ a b Douxchamps, Ayantunde & Barron (2012), p. 29.
  62. ^ Akuffobea-Essilfie et al. (2019), p. 4.
  63. ^ Barry et al. (2008), p. 26–27.
  64. ^ Barry et al. (2008), p. 25.
  65. ^ Douxchamps, Ayantunde & Barron (2012), p. 3.
  66. ^ Scherer, Lauri. "Incentivizing the Farmers of the Sahel to Harvest the Rainfall". National Bureau of Economic Research (NBER). Archived from the original on 2023-03-04. Retrieved 2023-03-04.
  67. ^ Aker & Jack (2021), p. 3.

Bibliography

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Further reading

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