The southern slope of the Bamboutos Mountains extends over the locality of Bafou North (latitude 5˚06' to 5˚10' N, longitude 10˚26' to 10˚43' E), in Nkong-Ni sub-division (Nkong-Zem council), Menoua division, West Cameroon region. That locality has a temperate Sudano-Guinean climate, also known as a high-altitude Cameroonian climate. This climate is characterized by a long rainy season of 8 months from mid-March to mid-November, and a short dry season of 4 months from mid-November to mid-March, with average annual precipitation of 2388.93 mm. The average wind speed of 1.19 m/s is not an obstacle to sprinkler irrigation, as the recommended wind speed limit for sprinkler irrigation is 4 m/s [9] . With an annual average monthly irradiance of 5.08 kWh/m²/day, July is the least sunny month with 4.14 kWh/m²/day, and February the sunniest with 5.96 kWh/m²/day. Under these climatic conditions, farmers on the southern slope of the Bamboutos Mountains produce three cycles of vegetables per year: first cycle (March-June); second cycle (July-October) and third cycle (November-February) with irrigation. The climatic variability observed in recent years, forces farmers to start irrigation some years in October and extend it until March. The production basin lies between 1600-2740 m altitude; the soils are of volcanic origin and among the most fertile in the country. Over the last 2 decades, there has been an accelerated degradation of the vegetation cover around the Bamboutos Mountains due to the intensity of human action [10] . The southern slope of the Bamboutos Mountains has more or less seasonal streams and springs, which dry up in the dry season. One of the most significant reasons for the drying up of watercourses is the informal but widespread cultivation of market garden crops on the banks of watercourses, which leads people to divert the watercourses to water their farms [11] .

Direct observations, field measurement and survey with questionnaire consisting of open and closed questions, were used to collect data characterizing the irrigation systems installed on the slope.

The size of the sample of irrigators to be surveyed was determined by the formula expressed in Equation 1. The number of producers engaged in irrigation during the data collection period (between the end of December 2022 and mid-March 2023) was about 170.

$n=\frac{\left(N\right)\left(p\right)\left(1-p\right)}{\left(N-1\right){\left(\frac{B}{C}\right)}^2+\left(p\right)\left(1-p\right)}$ (1)

Where: n = sample size;

N = population size;

p = degree of variability (p = 0.8);

B = precision level (B = 5%);

C = associated Z statistic at the 95% confidence level (C = 1.96).

The questionnaire was administered to 100 irrigators randomly selected. Interviews with irrigators took place in the field, so that direct observations and measurements could also be done. Among the irrigators surveyed were producers designated as the pioneers and benchmark for irrigation on the slope, and whose irrigation practices are copied by several irrigators.

Documents from Nkong-Zem council departments (communal development plans and data consolidation documents) were also consulted, and interviews were held with agricultural officials for the Nkong-Ni sub-division (Sub-divisional delegate of the Ministry of Agriculture and Rural Development and the Head of agricultural post of Djuttitsa), and with staff from the local water boardof Nkong-Zem counsil. These interviews covered the local water and energy resources (typology of sources, facilities, works and installations in place), the management of these resources (resource allocation systems and the role of the State in managing resources and conflicts) and irrigation-related projects or actions completed or underway in the basin.

Following data collection, the qualitative data obtained were analyzed using a systematic diagnostic approach; and the quantitative data were tabulated, coded and analyzed using Xlstat software.

The questionnaire used covered the typology of irrigation systems installed, sources of water and energy used, irrigated crops, and water management at farm and basin level.

Visits to irrigated farms in the basin enabled us to identify the different types of irrigation system (surface, gravity or pump sprinkler irrigation), using direct observations and a questionnaire. The geographical coordinates of all the irrigation systems identified were taken at the level of the irrigated plots using a Garmin GPS with 3 m accuracy. The QGis software was then used to map these irrigation systems using the coordinates taken on the field. Tracking the irrigation systems from the point of water withdrawal to the irrigated farm enabled us to identify and characterize the components of the irrigation systems. With the help of irrigators, the characteristics of irrigation system components (water intake, pump, main, secondary and lateral pipes and sprinklers) were obtained. A Fisher’s exact test was performed on the data in Table 1 (α = 5%), in order to assess the relationship between change of irrigation system type and water availability.

Irrigated crops were also identified during farm visits. For the irrigators surveyed, the areas occupied by these crops were measured using GPS. Irrespective of the varieties grown, yields were estimated with the contribution of irrigators, by dividing harvested quantities by irrigated areas.

For installed irrigation systems, the nature (surface water or groundwater) of the water source used was identified. Irrigators gave precisions on the availability of water throughout the irrigation season, the reasons for choosing the water source to use and the difficulties associated with irrigation water. The low-water flows of two rivers were measured, and also the dimensions of groundwater catchment structures. Surface water flows were calculated using the median section method. To this end, water velocity was measured using a Qualimetrics micro-spinner with an accuracy of 0.01, considering the orientations given by [12] . Discharge was obtained by multiplying water velocity by stream cross-section (product of average stream width and depth, measured with a decameter).

Since salinity is usually the most serious problem resulting from the use of poor water quality for irrigation, a water quality meter was used to measure the electrical conductivity of the identified water sources.

During the survey, irrigators provided information on water availability throughout the irrigation season, motivations for choosing water sources to use, and difficulties related to irrigation water.

While the geographical coordinates of the irrigation systems were being taken, the energy source used by each irrigation system was also recorded. This data was used to draw up a map showing the typology of irrigation energy sources. During the interviews, each irrigator indicated the source of energy used, giving details of availability, access and cost. In addition to the information provided by the irrigators on fossil fuels, discussions on fuel prices and availability were also held with fuel sellers of the local markets (Ndoh and Djuittitsa), and the main fuel supply points for irrigators, in villages Meloung and Lingang.

To understand irrigation management at farm level, irrigators were asked about their irrigation management (watering duration, irrigation interval, quantity of water applied), and the criteria they use to make irrigation decisions. A Kruskal-Wallis test was used to determine whether the differences in watering duration and irrigation intervals by type of energy source used were significant. Multiple comparisons were made using Dun’s test.

On a basin-wide scale, irrigators shared their views on possible associations of irrigators, established allocation systems and the involvement of the State or other bodies in irrigation.

The matrix of strengths, weaknesses, opportunities and threats of an activity is a tool whose aim is to guide possible actions, projects or interventions aimed at improving this activity, by acting on one or more points highlighted by this matrix. The analysis and interpretation of data collected through surveys, observations and field measurements served as the basis for drawing up this matrix for irrigation practices on the southern slope of the Bamboutos Mountains. The technical, social, economic and environmental aspects of the situation were identified:

This analysis enabled us to identify the causes of the main existing problems in irrigated systems and to propose possible solutions.

A total of 226 irrigation systems were identified in 09 hillside villages (Tallé, Femock, Meloung, Loung, Lingang, Ngui, Pastoral, Aghong 1 and Aghong 2).

(a) Typology of irrigation systems

Bafou North farmers use surface irrigation (furrow irrigation) at 15.04% and sprinkler irrigation at 84.96%; water transport in both cases may be by gravity or motorized. The following types of irrigation are used:

Figure 1 shows the distribution of these different types of irrigation system in the basin. It should be noted that some irrigators (3.98%) simultaneously use sprinkler irrigation on parts of their farms, and furrow irrigation on other parts.

The choice between sprinkler and furrow irrigation depends on water availability and the crop being irrigated. Indeed, when water is plentiful, some irrigators prefer to apply water in the furrows, particularly for crops such as green peppers, which are highly susceptible to disease and insects when the leaves are constantly wet.

More than four decades ago, furrow irrigation was the most common method of irrigation on the slope, but over time, sprinkler irrigation has become more widespread: 45% of irrigators surveyed said they had switched from furrow irrigation to sprinkler irrigation. Irrigators justify the move from surface irrigation to sprinkler irrigation (installed on 84.96% of farms) by the increase in the number of irrigators, which has led to a reduction in the quantity of water available per irrigator, and by the advantages of sprinkler irrigation (less arduous, more water-efficient and less favourable to aphids and whiteflies). The probability of Fisher’s exact test (p = 0.001) leads us to accept the hypothesis that the change in the type of irrigation system is linked to the availability of irrigation water.

(b) Irrigation systems structure

Irrigation systems in Bafou North consist of a water intake, a pumping system (if necessary), a water transport system, a plot distribution system and a sprinkler system shown on Figure 2 .

(c) Irrigated crops

Irrigation on the southern slopes of the Bamboutos Mountains is mainly used to grow market garden crops, the main crops being potatoes, leeks, cabbage, carrots and peppers. Most irrigators divide their irrigated plots into “squares”, on which they grow two or three pure crops. Table 2 shows the distribution of irrigated crops on the southern slopes of the Bamboutos Mountains.

The suitability of de farm’s soil for a crop, the crop’s market (price and easiness to sell), crop profitability and length of crop cycle are the main criteria for choosing which crops to irrigate. Farmers cultivate market garden crops because the slope’s soil is favorable to these crops, particularly potatoes, which are widely grown. According to the irrigators, the advantage of leeks, which are the most widely produced crop under irrigation, is their high resistance to water stress and the fact that, once mature, harvesting can be postponed if the market price is too low for the farmer.

In terms of the origin of irrigated land, 36% is family heirloom, 32% leased and 32% purchased by irrigators. Small-scale irrigated plots (less than 1500 m²) are, in most cases, family heirlooms resulting from shares between brothers, while relatively large areas are rented or purchased.

(d) Irrigation water

Irrigation on the southern slope of the Bamboutos Mountains is carried out using surface water (rivers and streams) and groundwater (ponds, springs and boreholes). Of the irrigators surveyed, 64% use exclusively surface water, 34% use groundwater and 2% use both sources of water (when surface water is still abundant, they capture it by gravity, and resort to groundwater when stream flows drop and competition for surface water begins).

As far as surface water is concerned, three main rivers (Femock, Meloung and Lingang) along which water is collected by gravity or pumping have been identified in the basin, as well as creeks. The flow of the Femock stream measured in January was 0.004 m³/s; that of the Meloung stream was 0.005 m³/s in January and 0.002 m³/s in February 2023. At the catchment point located downstream of the flow measurement point on the Meloung stream, 15 pipes were installed, making only 0.33 l/s and 0.13 l/s available per irrigator in January and February respectively. On these rivers and creeks, dykes ( Figure 3 ) are sometimes built by hand and without prior study, to increase the water level in the reservoir created and thus facilitate water withdrawal.

These watercourses experience a gradual decline in flow with the dry season, while most creeks dry up. At the beginning of the irrigation season (usually in November and some years, in October), water is abundant and most irrigate by gravity. As the dry season drags on (from mid-January onwards), flows drop considerably and some streams dry up ( Figure 4(a) ), creating competition for water. Those who have no other alternative for obtaining water are forced to abandon their crops for lack of water to irrigate ( Figure 4(b) ), while others resort to water sources that can only be mobilized by pumping.

This competition is reflected in the presence of several pipes at a catchment point, whereas there are several along each watercourse. At the end of the dry season, the number of irrigators per catchment point varies between 10 and 25, with an average of 15 irrigators per point. This number is higher at the beginning of the irrigation season.

Groundwater is collected by boreholes (two identified at the pastoral site, one of which is 56 m deep) and by ponds created by farmers whose plots are close to marshy areas. These ponds vary in cross-section (1 to 10 m²) and are generally 2 to 4 m deep. It should be noted that groundwater catchment structures are for personal use or are operated by a maximum of three neighboring irrigators who have built the structure together. The irrigators who use the groundwater report that the flow rate or quantity is stable throughout the year. Based on this observation, the widespread use of groundwater catchment structures could help alleviate the shortage of irrigation water during low-water periods.

Groundwater is located at distances of between 0 and 300 m from the irrigated plots, for an average of 82 m, while surface water is collected at distances of between 1 and 5000 m, for an average of 823 m. Among the irrigators surveyed, 41.86% find that water is not sufficient for their plants, particularly those who use surface water. While some irrigators use a water source because the position of their plot gives them no other alternative, others prefer water that will be collected by gravity because it is cheaper, and others opt for water that is close to the plot and does not dry up. In 50% of cases, the water sources are used exclusively for irrigation, and in the remaining cases, the water taken for irrigation is also used for laundry, domestic chores and drinkable water. These other uses of water are detrimental to irrigation, as the abundance of soap in the water causes damage to plants, and local residents disconnect pipes to obtain water for domestic use.

The electrical conductivities of water used for irrigation are between 0.028 and 0.153 dS/m. They therefore have no restrictions on their use for irrigation. Indeed, the degree of restriction on the use of water for irrigation is zero for electrical conductivities below 0.7 dS/m; mild to moderate when the electrical conductivity is between 0.7 and 3 dS/m and severe when it is greater than 3 dS/m.

(e) Irrigation energy

Irrigation water mobilization on the southern slopes of the Bamboutos Mountains is 50% gravity-fed, 45% motorized and 5% mixed (gravity-fed and motorized), as shown on Figure 5 .

The choice of irrigation energy source depends on the topographical position of the plot to be irrigated in relation to the water withdrawal point: when it is favourable to pressurizing the water by gravity, gravity irrigation is used, and when it is not, pump irrigation is adopted. Because it’s free, gravity is the preferred method for mobilizing water, despite the amount of money required to purchase pipes when the water has to be transported over several kilometers. However, because of the water shortage at the height of the low-water period, some people prefer to pump (electrically or using fossil fuels) from permanent water sources. Pumping is very common in low-lying areas such as Loung, as these are swampy areas where stream flows are stable during the irrigation season, and where ponds are created.

Motorized withdrawal uses three energy sources, namely fossil fuels (motor-driven pumps) at 69.03%, electric power (submersible electric pumps) at 29.20% and solar power (solar-powered pumps) at 1.77%. It should be pointed out that the use of electric power for irrigation in the basin is recent and booming, as all irrigators using electric pumps installed them less than 4 years ago. Motor-driven pumps are gradually being replaced by electric pumps, due to their relatively high operating costs.

Regardless of the energy source used, irrigators find it accessible, but expensive. Petrol is available in the various villages, but at an average cost of $1.41 per liter, while monthly electricity bills average at least $41.39 for those using electric pumps. Solar energy, on the other hand, requires a substantial initial investment, which most irrigators cannot afford. For a 4 ha farm, the installation of a solar field consisting of 48 panels, with a theoretical power of 18.89 kW, and the construction of a 56 m deep borehole, required around $1,903.97. Given that 85.33% of farms in Bafou Noth are less than 1 ha in size [13] , similar installations could be set up for community use. This could help solve the problems of water scarcity and the high cost of irrigation energy. It should be pointed out that the proximity of the farm to be irrigated to the Energy of Cameroon (Enéo) network is the main condition to be met by irrigators wishing to switch from fossil fuels to hydroelectric power. This condition is a limiting factor for hydroelectric pumping, as many irrigators are forced to continue using motor-driven pumps because their farms are so far from the power grid. This explains why the cost of renting plots meeting this condition is relatively higher in the basin.

The main difficulties linked to irrigation energy that were highlighted by irrigators are the high cost of petrol for fossil energy; voltage drops and power cuts for electrical energy.

(f) Irrigation management at farm and basin level

On the southern slopes of the Bamboutos Mountains, 82.5% of sprinkler irrigation systems are mobile. For these mobile sprinkler systems, the turnstile stake is moved from one sprinkler station to another. The decision to move sprinklers around the farm is justified on the one hand by the impossibility for an irrigator to have a water flow capable of supplying all the sprinklers needed to cover the entire farm in one irrigation episode, and on the other by the high cost of a fixed installation. Of those with fixed systems, over 70% are irrigators using fossil fuels (motor-driven pumps). Irrigation times per station depend on the energy source used, as shown in Table 3 .

The difference between these watering times is significant (p < 0.0001), with the fossil fuel time being different from the other two. Because of the relatively higher cost of fossil fuels, irrigators who use them have shorter watering times. This would lead to differences in application and requirement efficiencies.

Despite the difference in watering times by type of energy source used, there was no significant difference between the irrigation intervals practiced by irrigators. Observed irrigation intervals ranged from 2 to 14 days, with an average of 5 days (4.12, 4.61 and 6.50 days respectively for gravity, fossil and electric energy). The decision to irrigate is taken by most (58%) after observing the appearance of the soil and the plant. While some irrigators only return to a watering station once they have covered the entire farm, others are forced to observe an irrigation interval imposed by the availability of water at the source. To reduce the number of days needed to cover their farm entirely, those with the financial means install two to three “lines” (filter + water transport piping) to collect water by gravity.

Irrigation periods vary from 1 to 3.5 months, with an average of 2.63 months. In fact, some irrigators complete the crop cycle with irrigation after the departure of rain, meanwhile others start cultivation with irrigation and finish with the rains, and others cultivate from sowing to harvesting under irrigation. This depends on the availability of water and market prices.

Irrigation labor is essentially family-based (the irrigator himself or a member of his family) in 92% of cases, and the tasks performed include checking the water supply to the catchment pipes, moving the motor pump, switching the electric pump on and off, moving the turnstiles from one irrigation station to another, and so on. Those who use salaried labor entrust the running of the irrigation to a person who is paid monthly or after the harvest of the irrigated crop, according to an amount agreed in advance, which can be around 16.57 $/month.

At basin level, there is no association of irrigators at Bafou North. There are three possible scenarios for the allocation of water withdrawals from water sources used by several irrigators:

In addition to conflicts between farmers over water resources, there are also conflicts between farmers and herders. In 1984, to ease tensions between farmers and herders, the administrative authorities arbitrarily set a boundary between agricultural and pastoral areas at an altitude of 2000 m. However, when water shortages become acute, irrigators move their pipes upstream from the watercourses, thus violating this boundary to gain access to places reserved for watering animals (cattle), and these pipes are sometimes sabotaged by these animals or by shepherds. Setting up a water management committee or a water users’ association in the basin could help find lasting solutions to this conflictual situation.

Irrigators report that there is currently no State intervention in irrigation water management in the Basin, and most receive no advice/training on irrigation. Some irrigators have in the past received training from the German cooperation agency (GIZ); others who take part in the regional agro-pastoral fair have been awarded irrigation equipment as prizes. ACEFA program (programme d’Amélioration de la Compétitivité des Exploitation Familiales Agropastorales) has also subsidized producer groups with irrigation equipment. Irrigators also mention the initiatives of non-governmental organizations such as Erudef, which have worked on reforestation on the slopes of Mount Bamboutos, and the World Bank-funded Bamboutos reforestation project, whose reforestation activities and waterworks (boreholes and wells) for irrigation and animal watering are still awaited. he decline in water flows over the years, and the resulting shortage of water for irrigation, is attributable to the deforestation and destruction of raffia trees. Hence the initiatives taken by non-governmental organizations to tackle the issue through reforestation projects, which are welcomed by farmers.

Analyses carried out on the types of irrigation systems, crops irrigated, water and energy resources used, and water management at farm and basin level, reveal the strengths, weaknesses, opportunities and threats presented in Table 4 .

Irrigation systems on the southern slopes of the Bamboutos Mountains correspond to the description of individual-type irrigation installations given by [14] : these are installations carried out by the producers themselves, generally without any prior study, and installed anarchically around water points, in a scattered manner, with irrigators working on them individually. Thanks to irrigation, farmers on the southern slopes of the Bamboutos Mountains produce year-round, generating a steady income to support their families. There has been a gradual modernization of irrigation equipment on the southern slopes of the Bamboutos Mountains. This is marked by the introduction of pipes for water transport, hydraulic machines (motor pumps, electric pumps) for water pumping and, more recently, solar installations. Years ago, sprinkler irrigation was done only by gravity, and all the channels used to transport water from the source to the plot were earthen and unpaved [7] . The reduction in the quantities of water available for irrigation over the years has prompted irrigators to acquire equipment and structures to improve the availability of water for their plots throughout the irrigation season. The Water Management Research Unit at the University of Dschang has been working on the understanding and improvement of hydraulic turnstiles. In this case, the work of [15] , whose results led to the recommendation of a turnstile model with a length of 50 cm, a nozzle diameter of 4 mm and 2 nozzles. These features are markedly different from the characteristics of the turnstiles used by irrigators in the field (25 com maximum length, 3 mm nozzle diameter and 2 nozzles), and with which they have found satisfaction.

The percentages of farmers engaged in irrigated production of the various speculations follow the trends reported by [8] . According to their observations, potatoes, carrots and leeks are the most widely grown speculations in Bafou Nord, with 75%, 37% and 25% of farmers producing them respectively. Observed yields have improved over the years, in the case of leeks whose yield reported by [7] was 4 t/ha; this could be the result of improved irrigation efficiency or agronomic practices (fertilization, pest control, seed variety, etc.), in addition to the legendary fertility of the soils on the slopes of Mount Bamboutos. The access to water in the dry season that characterizes irrigated plots makes them highly prized in an environment where the pressure exerted by agriculture on land has increased with the development of market gardening since the 1980s [16] .

Like the tube-well technology used in Burkina Fasso, Mali and Nigeria [17] , the ponds made by irrigators in the southern slope of Mount Bamboutos enable shallow groundwater to be pumped (aquifers located at depths ranging from 0 to 20 m). However, unlike ponds, which have to be cleaned out every irrigation season, suitably protected tube wells can operate for several years, even in areas flooded during the rainy season.

For irrigators who use groundwater for irrigation, water availability is generally guaranteed throughout the irrigation season. As far as surface water is concerned, as pointed out by [8] , almost all river water is withdrawn for irrigation purposes at the height of the low-water period (between mid-January and mid-March); hence the total drying up of the bed of certain rivers downstream of the withdrawals ( Figure 4(a) ). Despite these abusive withdrawals, surface water drying up is the main problem associated with irrigation, raised by 65% of irrigators surveyed. According to irrigators, the decline in river flows is becoming more pronounced and earlier as the years go by. This constraint was already pointed out by [16] who reported that farmers had been attesting to a decline in water volumes for around 20 years. This poses a threat to irrigation in the basin (especially for those without access to groundwater), as many are forced to reduce the areas they irrigate annually. This drop in water availability can be attributed to inter- and intra-seasonal climatic variability. Indeed, the results of analyses carried out by [18] on rainfall data from Djuttista (on the southern slope of the Bamboutos Mountains) from 1941 to 2013, reveal that the median annual rainfall of the early years (1660.8 mm) is higher than that of recent years (1496.4 mm), with a difference of 164.6 mm. They also show that the length of the rain-fed cropping season has decreased from 245 days to 221 days over the years. Based on their observations, the irrigators point out that the destruction of raffia has led to a decrease in available water over the years in the rivers and streams of the locality. This could be because deforestation accelerates soil erosion, leading to major disruptions to the runoff needed to replenish local streams and rivers. According to [10] , the significant decline in stream flows and the drying up of some between January and March over the years is due to the gradual intensification of human action that is lowering the water table. In addition to withdrawals for irrigation purposes, [19] attributes the drying up of watercourses in the dry season to the dumping of solid waste in watercourses, which gradually leads to the thinning of riverbeds; this also results in flooding during the rainy seasons.

Faced with a shortage of irrigation water due to declining river flows over the years, irrigators are increasingly turning to groundwater as a means of guaranteeing water availability throughout the irrigation period. Irrigation on the southern slopes of the Bamboutos mountains is private and unregulated, as there is no control over the volumes of water withdrawn by individual irrigators. This context is similar to that presented by [20] in India, where an increase in the number of individual boreholes drilled for irrigation purposes (one every 240 metres) has led to over-exploitation of groundwater. Since groundwater mobilization is an option to be explored as a solution to the problem of surface water scarcity currently faced by irrigators, it should be under the supervision of the administration in charge of agriculture.

Power cuts last four to six hours in major cities, and in rural areas people can be plunged into darkness for three to four days [21] . The southern slope of the Bamboutos Mountains, a rural area, is indeed subject to load shedding lasting several days and this is harmful to irrigation with the national electricity network. Most irrigators are in favor of the transition from fossil fuels to renewable energies (hydroelectric and solar), but are limited by the distance of the electricity grid from their farm and the high cost of a solar installation. The increase in the price of petrol has accentuated the problem of the high cost of irrigation energy, which irrigators highlight as a constraint to irrigation. Indeed, fuel is sold in the villages at $ 0.17 more per liter than the price at the pump; an increase in the price at the pump would further encourage irrigators to switch to electric power, which is more affordable. However, despite the fact that the rate of access to electricity for households in Bafou North is estimated at 71.39% (adapted from [25] ), the remoteness of farm from the national grid is a problem that could be solved by community solar installations.

Normally, the determination of the water quantity to be applied involves determining the crop’s water requirements throughout its growth phase and determining the water storage capacity of the soil [9] . Once the water requirements of crops throughout their growth phase are known, the next step is to estimate the quantities of irrigation water to be supplied at farm level. To do this, it is necessary to know the soil data. This will enable us to determine the water storage capacity of the soil, and hence the irrigation dose to be applied at a frequency defined by the farmer, in order to cover the crop’s water requirements. However, on the southern slopes of the Bamboutos Mountains, the quantity of water applied and irrigation frequencies are not generally set on the basis of plant water requirements, and do not always take soil properties into account. The practices (fixed or mobile system, watering duration and irrigation interval) adopted by most irrigators are imposed on them by the availability of water, the cost of irrigation energy and the quantity of their irrigation equipment. Those who are not subject to these constraints make the decision to irrigate by observing the appearance of the plants or the soil. It is therefore possible to over- or under-irrigate. This highlights the need for irrigators to be supported in their irrigation decisions.

Small-scale irrigators in the Bamboutos Mountains do not benefit from any form of support in the technical management of irrigation. This situation corroborates the lack of advisory support presented by [3] as one of the constraints suffered by informal irrigators. In reality, even in countries like Niger where irrigation extension services exist, informal irrigators are neglected for lack of administrative existence. The Ministry of Agriculture and Rural Development is one of the most decentralized ministries in Cameroon. Strengthening the irrigation skills of agricultural station chiefs could enable those whose work areas are small-scale irrigation zones to better support irrigators.

The system of irrigation water management with water allocation is similar to that of farmers in Zambia (Mkushi and Mpika regions) and in the highlands of southern Tanzania, whose collective organization to develop and manage small irrigated perimeters is conflict-free [22] . The absence of state support for irrigators may be due to the fact that the State has not yet built irrigation facilities. In fact, according to article 2 of Prime Ministerial Decree 2024/00176, the management procedures relate essentially to irrigated perimeters created by the State, decentralized local authorities, public establishments, a public enterprise or a private legal entity. In the northern region, for example, where the State has built the Logone dike and Maga dam for irrigation, SEMRY (a parastatal agency for agriculture, irrigation and drainage) supports 25,000 rice growers in the Logone zone [23] . It should therefore be noted that private or informal irrigation, such as that on the Bamboutos Mountains, is still awaiting legislation setting out the procedures for its supervision.

On the basis of the SWOT analysis of irrigation on the southern slopes of the Bamboutos Mountains, possible solutions for improving irrigation and the management of water and energy resources in the basin can be proposed.

It is therefore proposed that irrigators:

To state and non-state structures (local elites, non-governmental organizations, international organizations, etc.) likely to carry out actions in the context of irrigation in the slope, it is suggested:

Indeed, investment in solar irrigation systems is likely to offer a higher economic benefit over time, compared with fossil fuels [17] . In addition to the economic benefit, solar pumping of irrigation water is more environmentally friendly (reduced greenhouse gas emissions and noise pollution).

The African Union has defined four avenues to be combined to facilitate the growth and development of Africa’s agricultural sector [1] . One of these is the development of farmer-supported irrigation, which is relatively inexpensive compared with large-scale irrigation, which requires substantial investment in infrastructure. To this end, diagnostic studies such as this one can be carried out in Cameroonian production basins where small-scale irrigation is practiced intensively. The improvements resulting from these studies could give rise to specific interventions, adapted to each context and with lasting positive impacts.