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首页> 外文期刊>African Journal of Agricultural Research >Properties, classification, genesis and agricultural suitability of soils in a semiarid pediplain of North Cameroon
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Properties, classification, genesis and agricultural suitability of soils in a semiarid pediplain of North Cameroon

机译:喀麦隆北部半干旱平原上土壤的性质,分类,成因和农业适宜性

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摘要

The aim of the study was to determine the morphological and physicochemical characteristics, classification, genesis and suitability of soils developed on pediplain around granitic hills in Minawao in the Far North region of Cameroon. The studied soil profile had 450 cm thick. It is composed of two subsections formed by erosion and cumulization. The upper subsection classified as typic ustifluvents clayey isohyperthermic is characterized by the high content of coarse elements showing stratifications in some part of the horizons. It recovers the below subsection classified as thapto typic haplustalfs clayey isohyperthermic. They are clayey, with clay contents ranging from 45 to 49%, and slightly acidic. Total nitrogen and organic carbon contents are very low ranging respectively from 0.05 to 0.11 and 0.25 to 0.63. Available phosphorous contents are below critical level. Calcium and Magnesium dominate the exchange complex of these soils. Their values range respectively from 12.96 to 15.04 cmol (+)/kg and 3.52 to 6.56 cmol (+)/kg. The CEC values are high, ranging from 44.64 to 57.84 cmol(+)/kg of soil. The CEC clay range from 89.92 to 117.02 cmol(+)/kg of clay. Base saturation percentage values are low, ranging from 37.05 to 42%, corresponding to a mean value of 39.74%. The studied soils are globally subjected to problems of low organic matter content, high coarse material content and low pH for the cultivation of Sorghum, Cotton, Soya, Groundnut, Maize and Cowpea. These problems could be solved through introduction of DMC systems, addition of available organic substrates, restoration of the cation balance and liming.
机译:这项研究的目的是确定在喀麦隆极北地区Minawao花岗岩山丘周围的pediplain上发育的土壤的形态和理化特性,分类,成因和适宜性。研究的土壤剖面厚度为450厘米。它由侵蚀和累积形成的两个部分组成。归类为典型的ustifluvents粘性等温热的上半部分的特征是,在某些水平层中,高含量的粗元素显示出分层。它恢复了归类于典型典型的haplustalfs黏土等高热的以下小节。它们是黏土,黏土含量为45%至49%,略带酸性。总氮和有机碳含量非常低,分别为0.05至0.11和0.25至0.63。有效磷含量低于临界水平。钙和镁在这些土壤的交换复合物中占主导地位。它们的值分别为12.96至15.04 cmol(+)/ kg和3.52至6.56 cmol(+)/ kg。 CEC值很高,范围从44.64至57.84 cmol(+)/ kg土壤。 CEC粘土的范围为89.92至117.02 cmol(+)/ kg粘土。基本饱和度百分比值较低,范围从37.05到42%,相当于平均值39.74%。对于高粱,棉花,大豆,花生,玉米,Cow豆,所研究的土壤普遍存在有机物含量低,粗物质含量高和pH低的问题。这些问题可以通过引入DMC系统,添加可用的有机基质,恢复阳离子平衡和石灰来解决。

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