The criteria proposed by Dixon-Woods et al. (2006), for assessing the quality of all empirical papers for Center for Internet Security (CIS), regardless of study type, were used. These have been adapted from the National Electronic Library for the evaluation of qualitative research.

Soils play an important role in climate change mitigation by storing carbon and decreasing global greenhouse gas emissions in the atmosphere (Lal, 2004). However, poor soil management through unsustainable agricultural practices could release nitrous oxide (N₂O), methane (CH₄) and carbon dioxide (CO₂) into the atmosphere (IPCC, 2013). The adoption of sustainable management of soil resources aims at increasing soil quality favorable for mitigating greenhouse gas emissions (Sharma et al., 2011). The impact of carbon smart strategies on greenhouse gas emission and the mechanism causing emissions has been diverse. It is prudent that a systematic review is conducted to understand the influence of carbon smart strategies on GHG emission and the underlying mechanism in different agro ecological environments.

According to Saggar et al. (2010) N₂O emissions are driven by the applications of fertilizer nitrogen (N), soil tillage and crop type, with their effect dependent on soil and weather conditions. Different results have been reported regarding the influence of tillage and straw practices on N₂O flux. Some research has shown that conservation tillage, especially no–tillage, results in increased N₂O emissions relative to intensive tillage systems (Hermle et al., 2008). Increased denitrification under reduced tillage has been attributed to decreased water filled pore space and mineral nitrogen concentration (Oorts et al., 2007), reduced gas diffusivity and increased water and reduce soil bulk density content (Hermle et al., 2008). Minimum conservation tillage maintains higher soil moisture levels and surface soil organic matter than where more intensive tillage practices are used. In addition, Bhatia et al. (2010) noted that the emissions of N₂O were higher in minimum till vs. conventional till system since soils under minimum tillage were generally more moist and had organic matter concentrated near the soil surface, which favored N₂O production. Other studies have observed no difference in N₂O emissions between minimum and conventional tillage treatments (Choudhary et al., 2002). However, no–tillage system has been reported to produce less N₂O than that of conventional tillage (Duan et al., 2013). This has been attributed to conventional tillage causing more soil organic C decomposition due to higher levels of soil–residue mixing and higher soil temperatures (Duan et al., 2013). In a study conducted by Yeboah et al. (2016) reported that N₂O emissions were comparatively higher under conventional tillage treatments soils than those from no–till or minimum tillage treatments with straw retention (Figure 2). The low N₂O emission in the minimum tillage plots is therefore, a significant finding in this study as many other agricultural practices that are meant to limit CO₂ emission also increase N₂O emissions, which does not seem to be the case in this review.

These data are in accord with those reported by Chatskikh and Olesen (2007), but contrary to reports by Gregorich et al. (2008) who found that N₂O emissions can be higher from no-tillage when compared to conventional tillage plots. The authors attributed the decreased N₂O emission by improving soil water drainage and soil structure, as shown by soil bulk density and soil hydraulic conductivity. This result support the assertion that increasing soil carbon stock and reducing soil disturbances could help reduce N₂O emission in agricultural systems. In this regards, application of conservation agriculture practices, including minimum tillage and increased residue incorporation has a higher potential to reduce nitrous oxide emission and to promote low emission cropping system.

Most previous studies indicate that conservation tillage couple with appropriate straw application acts as a net sinks for methane. However, both increased and decreased CH₄ consumption has been reported in no-till soils (Venterea et al., 2005). Changes in land use, especially cultivation of formerly undisturbed soils, strongly decrease the CH₄ oxidation and consequently the uptake of atmospheric CH₄ by the soil (Hütsch, 1998). Reduced and no-tillage practices have been proposed as alternative system for restoring the CH₄ uptake capacity of soils (Hütsch, 2001). This is because the improvement of soil quality through these practices is beneficial to methanotrophs (Hütsch, 1998, 2001). Agricultural soils exhibit both minor emitters of CH₄ to sinks for atmospheric CH₄ (Mosier et al., 2006). Agricultural soils become sinks of CH₄ when methanotrophic bacteria take up CH₄ to oxidize it for energy production (Hütsch, 1998). There is evidence that tillage reduces this oxidation in soils leading to less CH₄ removal (Hütsch, 1998). In a study by Yeboah et al. (2016), greater uptake of CH₄ was observed in the minimum till soils under rainfed conditions (Figure 3).

The greater uptake of methane in the no tillage plots, especially with straw application may be due to better aeration and less soil degradation which enhanced methanotroph activity. A well-drained soil provides ideal environment for the methanotrophs which are key bacteria in enhancing CH₄ uptake. The mulch layer on top of minimum tillage soils provided soil organic carbon and strengthened the stability of soil aggregates making them resist soil erosion caused by water and wind. When eroded soil particles do not fill pore spaces, porosity is increased and bulk density decreases. McLain and Martens (2006) noted that methanotroph activity was enhanced under adequate diffusion of gases in the niche of microbial activities. Plowing disrupts the ecological niche for methanotrophic bacteria, influence the gaseous diffusivity, and affect the rate of supply of atmospheric CH₄ (Hütsch, 1998). Straw returned in no-till system tends to increase soil C and reduce soil density, which may lead to lower risk of CH₄ emissions. Mosquera-Losada et al. (2007) reported that soil degradation can reduce the ability of soils to consume or oxidize atmospheric CH₄ by as much as 30–90%. However, Omonode et al. (2007), hold a contrary view to the above indicating that anaerobic conditions are prevalent under no-tillage and consequently lead to CH₄ emission. The high potential of conservation tillage in reducing methane emission is significant since current increases in atmospheric GHG levels require that innovative strategies are undertaken to mitigate impacts of climate change, particularly management practices capable of improving soil C sequestration.

Crop residue retention is related to the increase in organic C concentration and thus reduces CO₂ emission (Zhang et al., 2013). Sequestration of C and N in soils could be achieved through adoption of conservation tillage methods and crop residue retention (Zhang et al., 2013). Minimum tillage retains more plant residue on the soil surface and has greater near–surface soil C contents than conventional tillage (Lal, 2009). The decomposition of plant residue is also slower in conservation tillage as a result of reduced soil–residue contact compared with residue that is completely incorporated by conventional tillage (Lal and Pimentel, 2009). According to Reicosky and Archer (2007) the amount of C lost in the form of CO₂ due to soil tillage practices is depended on tillage intensity volume of soil disturbed. Lower CO₂ emissions were observed in minimum tillage plots with residue (Yeboah et al., 2016, 2018) as shown in Figure 4.

The lower CO₂ emissions could be attributed to the significant improvement in the soil organic carbon from the residue retention, which has been reported by other researchers (Zhang et al., 2013; Wang et al., 2020; Tiefenbacher et al., 2021). There is a general consensus that no–till with straw covering on the soil surface decreases soil CO₂ emissions, as suggested by Andruschkewitsch et al. (2013), soil disturbances due to tillage increase organic matter contact with microorganism leading to rapid decomposition. Higher CO₂ emissions in conventional tillage soils, especially with residue removal was attributed to the increased surface roughness and pores that are created by soil disturbance that accelerate decomposition of SOM (Ussiri et al., 2009). The aggregates 'disruption due to tillage renders the initially protected organic matter (OM) accessible to decomposers. Higher CO₂ emissions in conventional treated soils was attributed to the increased surface roughness and voids that are created by soil disturbance that accelerate. Conservation tillage enhance residue cover on the soil surface and have greater upper surface soil C contents than conventional tillage, the decomposition of plant residue is slower in conservation tillage as a result of reduced soil–residue contact compared with residue that is completely incorporated by conventional tillage (Lal, 2009). The review has highlighted the use of minimum tillage to reduce GHG (N₂O; CO₂; CH₄) emissions resulting from agriculture practices. For smallholder famers, there is a unique advantage for encouraging the use of minimum tillage. This because it can easily fit into their farming operations since cultivation and farming operations are on small scale and normally does not involve sophisticated farm implements.

Previous researches have shown that conservation tillage can improve crop yields (Huang et al., 2008; Zhang et al., 2013). In a study by Yeboah et al. (2016, 2018) minimum tillage couple with straw retention soils improved wheat grain yield by 49.78% on average compared to conventional tillage system with residue removed (Figure 5). The differences in grain yield could be related to the improved soil quality (Huang et al., 2008; Zhang et al., 2013). A possible explanation could be that minimum tillage with residue retention promoted wheat growth by increasing soil water availability and lowering bulk density that enhance root penetration.

In the Mexican highlands improved high-yielding wheat varieties yielded double under conservation agriculture compared to the farmer practice or zero tillage with residue removal, all with the same fertilizer inputs (Govaerts et al., 2005). However, Lampurlanes et al. (2002) found no difference among tillage systems in crop yield. There was a direct and significant relation between the soil quality status of the soil and the crop yield, and no tillage with crop residue retention showed the highest crop yields as well as the highest soil quality status. In contrast, the soil under no tillage and conventional tillage with crop residue removal showed the lowest soil quality and thus produced the lowest yields. This is in line with other studies, for instance Ozpinar and Cay (2006) found that wheat grain yield was greater when tillage practices resulted in improved soil quality. Management strategies in agroecosystems may influence C balance in soil through differences in soil C input and soil C output (Ghoshal and Singh, 2010). In agricultural system when C input to the soil exceeds the C output from the soil, a positive imbalance occurs which subsequently results in C sequestration in soil (Mukherjee and Lal, 2015). Minimum tillage and straw application significantly have been noted to enhanced soil C balance (Figure 6).

Zhang et al. (2012) found the beneficial role of straw returned for C sequestration. When C inputs and outputs are in balance with one another, there is no net change in soil C levels. Also, straw treated plots had higher C sequestration potential in terms of soil C balance particularly that of tillage removal with residue retained plots. On the other hand, soils without carbon inputs with or without tillage treatment had negative C balanced. The increased in annual C inputs could translate into higher C storage in terms of soil C build-up and thus enhanced C sequestration.

Africa just as the whole world faces the change of feeding increasing population against limited land resources in the face of climate change. Technologies that enable improved and sustainable intensification of crop production will be a way forward. The loss of soil organic carbon (SOC) and soil nutrients especially N has been observed to be the most limiting factor of crop production in the tropics and sub-Saharan Africa (Zingore et al., 2015; Liu et al., 2021). Using a crop model Liu et al. (2021) observed that, as a result of N deficiency, the yield of yam a very important food security crop along the West African yam belt including Ghana was limited for 69, 77, 82, and 92% land area at the savannah, forest, forest-savannah transition and coastal savannah respectively of Ghana. Also, APSIM showed that lack of synchronization of sowing date of maize with optimum radiation, rainfall, and nutrients (especially N) is the cause of the huge maize yield gap in Ghana (Owusu Danquah et al., 2020). For rice production, N is the most limiting nutrient followed by Phosphorus (P). The absence of N, P, and Potassium (K) resulted in a yield reduction of 32, 16, and 11%. The study suggested N application of 56, 91, and 122 kg N ha⁻¹ would result in a yield of 3, 5, and 7 t ha⁻¹ respectively (Saito et al., 2019). An on-station and on-farm evaluation on cassava in Uganda and Kenya revealed poor soil fertility as one of the major limiting factors. Cassava productivity was limited as much as 6.7 t ha⁻¹ compared to 5.4 and 5.0 t ha⁻¹ limitations resulting from early water stress and weed management respectively (Fermont et al., 2009). The yield gap of food crops improved with the use of fertilizers and improved seeds. Also, the yield and poverty gap are directly related, and thus yield improvement would reduce poverty and improve farmers' livelihoods (Dzanku et al., 2015). To ensure food security in the face of limited land resources and climate change for the increasing population calls for urgent need to address these yield limitations with improved climate smart technologies. Mueller et al. (2012) observed a high chance of meeting sustainable intensification and food security challenges if changes can be made in soil nutrition and water management. Environmental impact as results of agriculture can be minimized whiles increasing important and major cereals such as maize, wheat, and rice by 30%. This is where agroforestry can play a vital role by providing options that enable efficient and sustainable use of the resources whiles conserving them for future generations. Agroforestry is a collective name for land use practice which incorporate growing trees and shrubs with crops and or livestock so that they interact to facilitate productivity (Nair et al., 2010). This practice has recently received considerable attention as a biological strategy for carbon sequestration for mitigating greenhouse gas emissions recognized by the Kyoto Protocol. This is because interactions between trees and shrubs used in agroforestry systems are managed to facilitate the growth of the associated food crop.

Agroforestry practice involves the cultivation of more than one plant species on the same piece of land, at least two plant species or more. The selection of the species is very important and relies on the ecological principles of reducing competition and maximizing complementation or facilitation (Erskine et al., 2006; Rao et al., 2007). Competition is where the two or more plant species used in the agroforestry system interact in such a way that at least one exerts a negative influence on the growth and development of the other species. Whiles complementation or facilitation is where the two or more plant species used in the agroforestry system interact in such a way that it exerts a positive influence on at least one or more of the species. When all the species exert positive influence on each other it is termed mutualism (Van Noordwijk et al., 2015). However, in agroforestry systems mutualism is hardly attained. Figure 7 shows how the presence of trees/shrubs in cropping systems facilitates resource use to the benefit of the associated food crop. Yang et al. (2020) observed that rubber tree takes more than 40% of its soil water from the shallow horizon (0–20 cm) of the soil resulting in an interspecific competition between rubber tree and their intercrop. However, the intercrop facilitated soil water to the rubber enabling it to acquire about 9–24% of its soil moisture requirement from the shallow soil horizon (0–20 cm).

Species diversity in an ecosystem is directly related to productivity and income per plant in the plant ecosystem. The income per plant increased for fruits, firewood, and timber but decreased for bananas and cocoa as diversity increases. This suggests stronger complementarity than competition between plants on the higher strata of the canopy (fruits, firewood, and timber trees) and vice versa for the plants occupying the lower canopy (Banana and Cocoa) (Salazar-Díaz and Tixier, 2019). This study has emphasized the need for the selection and arrangement of agroforestry components to achieve optimum benefits. When the management and spatial influence of tree species such as Eucalyptus spp., Sesbania sesban, Grevillea robusta, Calliandra calothyrsus, Markhamia lutea, and Croton macrostachyus were evaluated on water availability and productivity of maize on smallholders' farms in Kenya, it was observed maize productivity increased with leguminous species. Also, the presence of the tree species significantly influenced soil moisture distribution at the field (Nyaga et al., 2019). Moderate shading by trees in a cocoa farm resulted in improved nutrient assimilation and productivity of cocoa (Asare et al., 2017).

Using pigeonpea in cropping systems has provided readily available and rich N biomass which improved N availability and used resulting in improved crop productivity (Kermah et al., 2018; Owusu Danquah, 2020). Figure 8A shows the sunlight reaching yam leaves above, mid, and below the canopy along the stake. Sunlight reaching the yam leaves was influenced by the cropping system. Sunlight intensity on yam leaves at mid-canopy (MC) of PB and sole yam were similar to the sunlight intensity on the yam leaves above canopy (AC) of PA for both locations and years. Sunlight reaching the below canopy (BC) of both PB and Sole yam cropping systems was higher than the sunlight reaching the mid-canopy (MC) of PA fields. This had implications on soil moisture retention, weed control, and N use by the yam. Although the yam leaves of the yam in the PA field were shaded, this facilitated soil moisture retention, control weeds, and improved N use by the yam. Figure 8B shows the mean relative chlorophyll content of the yam leaves. Yam leaves on PA fields had the best leaf chlorophyll content. Farmers' practice (No fertilizer) and half recommended fertilizer rate (23–23–30 N–P₂O₅-K₂0 kg/ha) followed the order of PA>PB> sole yam in leaf chlorophyll content whiles the full fertilizer rate (45–45–60 N–P₂O₅-K₂O kg/ha) followed the order of PA=PB>sole yam.

Thus, the presence of the pigeonpea though shaded the yams, shading was positive, it protected the yam ridges from erosion, suppressed weeds, made N available to the yams facilitating yam productivity. As a C3 plant species, it becomes saturated upon receiving 50% of the required light intensity. High environmental temperature conditions around crops especially C3 plants increases oxygenation reaction along the photorespiratory pathway resulting in about 25–30% loss in carbon fixation (Slattery and Ort, 2019). Thus, proving some level of shading is necessary for staple food crops (root and tuber and legume food crops) which are C3 plants so as to operate under full photosynthetic potential for improved productivity (Huang et al., 2020; Owusu Danquah, 2020). In the face of climate change integrating trees into cropping systems on smallholder farmers would play a dual role of shading and conserving moisture and also provide food and income from their produce.

If the trees and shrubs used fixes N through biological nitrogen fixation (BNF) it will improve N availability. This strategy of intentionally using legumes trees and shrubs would facilitate N availability in cropping systems to reduce N inorganic fertilizer application. Since N fixation and availability to the associated crop is a factor of the biomass of the legume grown, the N per unit area fixed by tree legumes are better than major crop legumes used in cropping systems (Mthembu et al., 2018). Also, N fixation can be high when N in the medium or soil is limited (Ennin et al., 2002). Thus, it presents the opportunity to integrate tree legumes into cropping systems in sub-Saharan Africa where the soils are limited in N and other nutrients for sustainable food crop production. Owusu Danquah et al. (2017) observed that when pigeonpea (a legume tree) preceded yam cultivation, half recommended poultry manure (3 t ha⁻¹) and a third recommended fertilizer rate (15–15–20 N–P₂O₅-K₂O kg ha⁻¹) was enough for sustainable yam production on continuously cropped fields. Also, when yam was cultivated in alleys of pigeonpea and the pigeonpea biomass pruned on the soil, half the recommended fertilizer rate (23–23–30 N–P₂O₅-K₂O kg ha⁻¹) was enough for sustainable yam production on continuously cropped fields (Owusu Danquah, 2020).

Integration of trees and shrubs in cropping systems improves the general productivity of the cropping systems compared to their monocrop. This is because the presence of the trees and shrub makes available nutrient-rich biomass which improves nutrient and water use efficiency to the benefit of the associated food crop (Ribeiro-Barros et al., 2018; Kuyah et al., 2019; Akoto et al., 2020). Tsufac et al. (2021), evaluated the role of agroforestry as a sustainable agricultural practice option for soil fertility management in Cameroon. The study revealed a significant improvement in soil with agroforestry practice which was also perceived by most farmers. The productivity of maize significantly improved when integrated with pigeonpea (Musokwa et al., 2019). The productivity and profitability of cowpea, maize, and cassava significantly improved over their monocrop counterpart upon integration with bamboo (Akoto et al., 2020). The integration of Agroforestry trees such as Gliricidia sepium and Leucaena leucocephala into yam cropping system improved yam productivity (Maliki et al., 2017). Table 1 shows the land Equivalent Ratio (LER) and improvement in pigeonpea–yam intercrop compared to their monocrops. More than one (1) LER indicates the significant improvement of yam productivity resulting from the integration of pigeonpea. When yam was planted in alleys of pigeonpea (PA) with pigeonpea as live-stakes, the productivity was better than when yam was planted with the borders of pigeonpea (PB) and pigeonpea stakes cut and used as stakes. Intercropping efficiency of 39–69 and 27–44% were observed for planning yam in alleys of pigeonpea and planning yam with pigeonpea as border respectively. Thus 27–69% land area of the monocrop yam would be needed to achieve a similar yield as the pigeonpea–yam intercrop. This has implications on forest conservation and land use management especially for yam which is associated with deforestation and land degradation (Ennin et al., 2014; Owusu Danquah et al., 2015). According to the report of (Ministry of Food Agriculture (MoFA), 2018), yam production in Ghana increased by 2.39% while the area under yam cultivation within the same period also increased by 2.21 suggesting about 1:1 direct relation between area under cultivation and production. This means yam production in Ghana increases as areas under production increase. This has bad implications for land resource conservation and climate change.

The resource use efficiency and productivity increase associated with the integration of trees and shrubs has demonstrated agroforestry's ability to improved and sustained productivity whiles conserving the resources on which production depends (the land). Promotion and adoption of the pigeonpea–yam cropping system as an improved technology option for yam production in Ghana would at least conserved about 27% of the land currently under yam production without affecting production. This is also welcoming since to be able to mitigate climate change, forest and tree conservation would be needed as carbon sinks.

The increasing greenhouse gases (GHG) (Carbon dioxide, nitrous oxide, methane) in the atmosphere continues to be a challenge and result of global climate change. The warmest earth's surface temperature has been recorded since 2016 resulting in extreme weather conditions and its adverse effect on crop production (Gupta et al., 2017; Jones, 2017). There is, therefore, the need to pursue climate-smart technologies that increase carbon storage especially for smallholder farmers who have been predicted to be worse affected by climate change due to their limited adaptive capacity (Manaye et al., 2021). Agroforestry has been observed to be one of the low costs and sustainable technologies for mitigating climate change. This is because of its ability to provide many ecosystem services which improve agroecosystem biodiversity and productivity (Goncalves et al., 2021). Global agricultural land is about 10% with a carbon stock of about 3–18 t C ha⁻¹ (Zomer et al., 2009). Agroforestry could sequester about 0.29–15.21 and 30–300 Mg C ha⁻¹ year⁻¹ carbon in the biomass above and below ground (soil) respectively (Nair et al., 2009; Nath et al., 2021). Brown et al. (2012) observed that agroforestry systems in East and West Africa alone has the potential to store about 6–22 Mg CO₂ ha⁻¹ year⁻¹. Manaye et al. (2021) evaluated tree diversity and carbon stocks in agroforestry systems in Ethiopia and observed a high tree species diversity and potential above and below ground carbon stock of about 77–135 Mg ha⁻¹ on smallholder farmers' fields. The study suggested, agroforestry to be a very important means of storing carbon. Figure 9 shows SOC loss from the Forest, transition, savannah, and coastal soils of Ghana when subjected to pigeonpea residue incorporation in the soil, pigeonpea rotation with yam, and use of sole inorganic fertilizer. Long-term (10 years) stimulation of soil organic matter showed a decline in SOC on all treatments. However, the decline was least when pigeonpea biomass was incorporated (−0.3 Mg ha⁻¹ year⁻¹) followed by when sole fertilizer (−0.43 Mg ha⁻¹ year⁻¹) and pigeonpea rotation with yam (−0.42 Mg ha⁻¹ year⁻¹) with the control of sole inorganic fertilizer recording the worse decline in SOC of −0.51 Mg ha⁻¹ year⁻¹ (Liu et al., 2021).

Under the clean development mechanism (CDM), the approach of afforestation and conservation of forest to serve as carbon sinks is seen as a hindrance to the agenda of increasing food production to feed the increasing population (Apuri et al., 2018; Waldén et al., 2020). Integration of trees and shrubs on farmlands addresses this issue, food production can be sustained whiles maintaining the trees and shrubs to serve as carbon sinks on the same piece of land.

The productivity of crop depends very much on the fertility of the soil. Therefore, improving soil fertility is key to improving smallholder farmers' productivity, income, and livelihood. Soil fertility is on a decline in sub-Saharan African (Nalivata et al., 2017; Stewart et al., 2020). There is a yield gap of about 4.9, 4.5 t ha⁻¹ between potential and actual yields of maize and rice respectively (Rong et al., 2021). According to the [Global Yield Gap and Water Productivity Atlas (GYGA), 2021] (GYGA-www.yieldgap.org), maize a very important food security crop, yield under rainfed conditions is just about 10–30% of the potential yield. Soil nutrition and precipitation have been observed to be the major limiting factors affecting cereals and other crop yields in sub-Saharan Africa (AGRA, 2016; Hadebe et al., 2017; Kihara et al., 2017; Saito et al., 2019; Epule et al., 2021). Fertilizer usage was promoted to address the situation, but the inability of smallholder farmers to afford mineral fertilizers hampers fertilizer usage (Komarek et al., 2017; Patrick et al., 2018). Also, the ability to transport to their fields because of the poor road network and technical know-how in the application and usage of fertilizers are other reasons (Mugwe et al., 2019; Langyintuo, 2020).

The use of fertilizer alone does not promote long-term soil organic carbon buildup, soil fertility, and crop productivity (Raimi et al., 2017; Singh, 2018; Singh et al., 2019). Although, organic fertilizer especially plant biomass has been noted to promote soil health by building soil organic matter, getting sufficient quantities for sustainable soil fertility and food production is a challenge (Place et al., 2003; Biramo, 2018). Therefore, Integrated Soil Fertility Management (ISFM) approach which combines organic and inorganic fertilizers are being promoted as a viable option for sub-Saharan Africa. Integrated Soil Fertility Management (ISFM) is a soil fertility management practice where organic, inorganic (fertilizer), and improved germplasm are combined and adapted to the local conditions resulting in improved nutrient use efficiency and crop productivity (Vanlauwe et al., 2010; Mugwe et al., 2019; Gram et al., 2020). The combined use of organic and Inorganic fertilizers in ISFM resulted in improved productivity of most crops such as maize (Mahmood et al., 2017), Rice (Moe et al., 2017), Tomatoes (Islam et al., 2017), and Yam (Owusu Danquah et al., 2017, 2020). The use of ISFM reduces the inorganic fertilizer requirement whiles improving crop productivity. Figures 10A,B indicates a third and half recommended fertilizer rate of 45–45–60 N–P₂O₅-K₂O kg ha⁻¹ (Ennin et al., 2016) with integration of pigeonpea biomass would be enough for sustainable yam production on continuously cropped fields.

Preceding yam with pigeonpea resulted in a reduction of the inorganic and organic fertilizers required for sustainable yam production to a third (15–15–15 N–P₂O₅-K₂O kg ha⁻¹) and a half (3 t ha⁻¹) respectively (Figure 10A). Also, the integration of pigeonpea into the yam cropping system resulted in the reduction of the inorganic fertilizer required for sustainable yam production to half (23–23–30 N–P₂O₅-K₂O kg ha⁻¹) (Figure 10B). Thus, the integration of agroforestry trees into cropping systems holds a key in making readily available nutrient reach biomass and reducing the quantities and cost of inorganic fertilizers for sustainable soil fertility management and food security in sub-Saharan Africa.