Mountainous ecosystem soils are subject to colonization nowadays for agri</span><span style="font-family:Verdana;">cultural purposes due to an increasing population in towns making the</span&g...Mountainous ecosystem soils are subject to colonization nowadays for agri</span><span style="font-family:Verdana;">cultural purposes due to an increasing population in towns making the</span><span style="font-family:Verdana;"> detailed </span><span style="font-family:Verdana;">characterization of such soils indispensable. This work aims to characterize</span><span style="font-family:Verdana;"> the steep slopes soils of the Dschang hills and to evaluate their fertility level for </span><span style="font-family:Verdana;">agricultural valorization. Thus, four soil profiles were dug at various topographic</span><span style="font-family:Verdana;"> positions (summit (SP), shoulder (MP), backslope (BP) and footslope (PP)) following a toposequence. Samples of disturbed and undisturbed soils were taken and analyzed in the laboratory according to standard methods. The Fertility</span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;">Capability</span></span></span><span><span><span style="font-family:""> </span></span></span><span><span><span style="font-family:""><span style="font-family:Verdana;">Classification (FCC) and simple limitation methods were used to identify major agricultural constraints. The main results show that </span><span style="font-family:Verdana;">profiles thickness is moderate, between 0 and 120 cm, with a high sand</span><span style="font-family:Verdana;"> content </span><span style="font-family:Verdana;">(at least 50%) over the entire toposequence, especially at the surface. The</span><span style="font-family:Verdana;"> study site has four types of soils, namely Eutric</span></span></span></span><span><span><span style="font-family:""> </span></span></span><span><span><span style="font-family:""><span style="font-family:Verdana;">Cambisols (ochric) in SP and L</span><span style="font-family:Verdana;">eptic</span></span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;">Eutric</span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;">Cambisols (Humic) in MP, Eutric</span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;">Cambisols (Humic) in BP</span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;"> and Stagnic</span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;">Oxygleyic</span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;">Dystric</span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;">Gleysols</span></span></span><span><span><span style="font-family:""> </span></span></span><span><span><span style="font-family:""><span style="font-family:Verdana;">(Humic) in pp. The soils are very acidic at PP, moderately acidic at BP and SP and slightly acidic at MP. Organic matter is higher at the surface than at depth at the topographic segments of MP, BP and PP and low to SP. The C/N ratio is high (>17) in all profiles except P4 </span><span style="font-family:Verdana;">(<10). In addition, the cation exchange capacity (CEC), the sum of</span><span style="font-family:Verdana;"> exchangeable bases, total nitrogen and available phosphorus is low in all profiles. The Ca/</span></span></span></span><span><span><span style="font-family:""> </span></span></span><span><span><span style="font-family:""><span style="font-family:Verdana;">Mg/K balance in all the profiles shows a cation imbalance and a relatively </span><span style="font-family:Verdana;">high concentration of exchangeable potassium compared to the ideal</span><span style="font-family:Verdana;"> situation (76% Ca, 18% Mg and 6% K). The major constraints to crop production are: aluminum toxicity (a) and nutrients leaching (e), textural discontinuity (LS), flooding (g), low nutrient reserve (k), sand (S), clay (C) and slope (t). Hence the fertility capacity classes of these soils are CCaegk (PP), SSek (BP), SSte (MP) and LSaek (SP). To improve the yield, it will require off-season crop cultivation, fertilization and liming, and earthworks.展开更多
文摘Mountainous ecosystem soils are subject to colonization nowadays for agri</span><span style="font-family:Verdana;">cultural purposes due to an increasing population in towns making the</span><span style="font-family:Verdana;"> detailed </span><span style="font-family:Verdana;">characterization of such soils indispensable. This work aims to characterize</span><span style="font-family:Verdana;"> the steep slopes soils of the Dschang hills and to evaluate their fertility level for </span><span style="font-family:Verdana;">agricultural valorization. Thus, four soil profiles were dug at various topographic</span><span style="font-family:Verdana;"> positions (summit (SP), shoulder (MP), backslope (BP) and footslope (PP)) following a toposequence. Samples of disturbed and undisturbed soils were taken and analyzed in the laboratory according to standard methods. The Fertility</span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;">Capability</span></span></span><span><span><span style="font-family:""> </span></span></span><span><span><span style="font-family:""><span style="font-family:Verdana;">Classification (FCC) and simple limitation methods were used to identify major agricultural constraints. The main results show that </span><span style="font-family:Verdana;">profiles thickness is moderate, between 0 and 120 cm, with a high sand</span><span style="font-family:Verdana;"> content </span><span style="font-family:Verdana;">(at least 50%) over the entire toposequence, especially at the surface. The</span><span style="font-family:Verdana;"> study site has four types of soils, namely Eutric</span></span></span></span><span><span><span style="font-family:""> </span></span></span><span><span><span style="font-family:""><span style="font-family:Verdana;">Cambisols (ochric) in SP and L</span><span style="font-family:Verdana;">eptic</span></span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;">Eutric</span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;">Cambisols (Humic) in MP, Eutric</span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;">Cambisols (Humic) in BP</span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;"> and Stagnic</span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;">Oxygleyic</span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;">Dystric</span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-family:Verdana;"><span style="font-family:Verdana;"><span style="font-family:Verdana;">Gleysols</span></span></span><span><span><span style="font-family:""> </span></span></span><span><span><span style="font-family:""><span style="font-family:Verdana;">(Humic) in pp. The soils are very acidic at PP, moderately acidic at BP and SP and slightly acidic at MP. Organic matter is higher at the surface than at depth at the topographic segments of MP, BP and PP and low to SP. The C/N ratio is high (>17) in all profiles except P4 </span><span style="font-family:Verdana;">(<10). In addition, the cation exchange capacity (CEC), the sum of</span><span style="font-family:Verdana;"> exchangeable bases, total nitrogen and available phosphorus is low in all profiles. The Ca/</span></span></span></span><span><span><span style="font-family:""> </span></span></span><span><span><span style="font-family:""><span style="font-family:Verdana;">Mg/K balance in all the profiles shows a cation imbalance and a relatively </span><span style="font-family:Verdana;">high concentration of exchangeable potassium compared to the ideal</span><span style="font-family:Verdana;"> situation (76% Ca, 18% Mg and 6% K). The major constraints to crop production are: aluminum toxicity (a) and nutrients leaching (e), textural discontinuity (LS), flooding (g), low nutrient reserve (k), sand (S), clay (C) and slope (t). Hence the fertility capacity classes of these soils are CCaegk (PP), SSek (BP), SSte (MP) and LSaek (SP). To improve the yield, it will require off-season crop cultivation, fertilization and liming, and earthworks.