Developing countries of sub-Saharan Africa, including rural communities, face a myriad of challenges that impede agricultural productivity. Climate change, land degradation, population growth, and heavy reliance on rainfed agriculture are among the social and biophysical constraints that hinder progress (Ngigi 2009). In particular, sub-Saharan African soils are characterized by inherent fertility deficiency, low productivity, and the compounding effects of nutrient scarcity, land degradation, and water stress, which significantly hamper agricultural development in the region (Lahmar et al. 2012). These obstacles pose potential setbacks to agricultural efforts in numerous countries within sub-Saharan Africa, Mali being one of them. Situated in West Africa and landlocked, Mali is among the least developed nations, heavily reliant on rainfed agriculture and livestock for its economy (Ebi et al. 2011). The smallholder agricultural sector primarily focuses on rainfed crops such as millet, sorghum, maize, and cotton for both domestic consumption and market demands. However, agricultural production falls short of meeting Mali's population needs, which are growing at an alarming rate of nearly 3% per year. Currently, over a quarter of Mali's population suffers from malnourishment (IMF 2013). The Malian economy heavily depends on cotton exports, contributing 10% to the national GDP and serving as the primary source of income for 2.5 million farmers in the southern region (Valenghi D 2001).
Mali is traversed by two major rivers, the Niger and the Senegal. Farmers in Mali, particularly in the southern part, confront numerous challenges, including excessive rainwater during the rainy season, water scarcity in the dry season, soil acidity, and nutrient depletion (Yayé et al. 2013). Insufficient land, water, and crop management practices have been identified as key factors contributing to yield gaps in the semi-arid regions of West Africa (Rockstrom et al. 2007). In southern Mali, water runoff was estimated to be between 20–40% of annual rainfall and up to 70% during individual rainstorms (Roose 1987). Cultivated soils experienced significant soil losses, with 25 kg of nitrogen and 20 kg of potassium per hectare per year. These losses in soil fertility accounted for 44% of farmers' income depletion. Southern Mali receives an average annual rainfall ranging from 500 to 1000 mm, characterized by strong variations and irregular rainfall patterns (Akinseye et al. 2016). The scarcity of water due to annual rainfall instability poses a major obstacle in achieving food security and reducing poverty in the region. Recent reports (Serigne et al. 2006; Lobell et al. 2011; Vgen & Gumbricht 2012) indicate that rainfall has become less reliable, and growing seasons have shortened in several areas of West African countries, creating a shift in farming and natural resource management practices.
Groundwater plays a pivotal role as an essential resource in sub-Saharan Africa, where approximately 300 million people depend on aquifers for domestic water supply (Foster & Garduño 2013). Groundwater is generally abundant, of good quality, sufficient in quantity, and affordable (Adelana & MacDonald 2008). Aquifers serve as a dependable source of freshwater during dry spells, particularly in regions with semi-arid climates where rainfall and surface water may be absent for extended periods. This is precisely the case in Mali, where groundwater constitutes the primary source of drinking water supply. Birhanu Zemadim and Ramadjita have conducted extensive studies, mapping and geo-referencing shallow wells in the southern districts of Bougouni and Koutiala in Mali. Out of the 484 wells studied, water availability was observed at an average depth ranging from 5.5 to 15.5 meters in most cases (Birhanu & Tabo 2016).
Water well pumps play a vital role in bringing water from wells and springs to the surface, ensuring a reliable water supply. These pumps can generally be categorized into two main types: shallow well pumps and deep well pumps. Shallow well pumps are typically situated above ground level and operate by creating suction to lift water out of the ground through a suction pipe (Sivasamy et al. 2018). Generally utilized when the water source is close to the surface or in an artesian well, these pumps, often in the form of jet pumps, effectively meet the demand for water extraction. At sea level, the typical lift for suction pumps ranges from 8 to 9 meters, showcasing their efficiency in accessing water from relatively shallow depths.
Deep well pumps are specifically designed to tackle the challenge of pumping water uphill from wells with greater depths. They come in two main variations: submersible pumps and deep well jet pumps. Submersible pumps are designed to be submerged in the water, with the inlet below the water level, enabling them to efficiently lift water to the surface (Zhou et al. 2020). On the other hand, deep well jet pumps utilize a different configuration. They are not limited by suction lift restrictions and have the advantage of a significantly increased depth limit for water well applications, up to four times that of shallow well pumps. Deep well jet pumps are commonly employed in situations where the water source is located at considerable depths. Submersible pumps are impeller-style, ensure effective water extraction and delivery (Sivasamy et al. 2018).
In the context of this study, a deep well jet pump was utilized to investigate its performance and suitability for the specific application. Deep well jet pumps are known for their recirculating-type systems, primarily employed to draw commercial, industrial, and residual water from deep wells. These pumps incorporate deep well ejectors (ecological), which play a crucial role in lifting water and maintaining a net positive suction head (NPSH) (Schiavello & Visser 2009) at the surface mechanical pump. The deep well jet pump, equipped with hose connections, is carefully lowered into the well casing, with its discharge outlet situated at the surface. To initiate the pumping process, an initial priming is required and sustained by a foot valve positioned at the suction inlet of the pump. Once the jet pump is in operation, the flow through the ejector effectively entrains and lifts water from the well, ensuring a continuous supply. The capacity of this type of system is dependent on the depth of the well and the specific capacity of the jet pump, highlighting the importance of selecting the appropriate equipment for optimal performance. In addition, polyethene pipes were selected for water transportation due to their numerous advantages (Wang et al. 2012). Listing some of them: Corrosion resistance — PE pipes are no electrochemical corrosion and no anti-corrosion layer and can be used up to 50 years; PE pipes are excellent bending performance use fewer accessories; strong resistance to low temperature performance; good impact resistance; light weight and economical.
In this study, the conventional use of jet pumps, was pushed further. A groundbreaking approach was introduced, a single, high-performance jet pump to extract water from multiple wells simultaneously. This innovative method ensures an uninterrupted water supply, even if one of the wells becomes depleted. In contrast, the traditional approach would require a separate pump for each well, resulting in higher costs (Billington et al. 1994). The need for multiple pumps and associated equipment was eliminated, leading to cost reduction. Moreover, the utilization of a single pump across multiple wells guarantees a continuous water supply, meeting various demands such as domestic, irrigation, and industrial. Another advantage is the reduction in power consumption. By maximizing energy efficiency through the use of a single high-performance pump, energy consumption was minimized compared to operating multiple individual pumps. This not only contributes to cost-effectiveness but also aligns with sustainable practices, reducing environmental impact.