中非苏丹-萨赫勒喀麦隆东部梅奥-达内地区土壤敏感性分区

Tiki Denis, Shahina Tariq, Ibrahim Achille, Mamdem Lionelle, Leumbe Olivier, Bitom Dieudonné
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引用次数: 0

摘要

位于喀麦隆热带地区的梅奥-达内(Mayo-Danay)土壤资源的研究表明,土壤具有特定性质的多样性。研究区总体上为平原景观,平均相对海拔为300 m,但植被类型为稀树草原类型,非常占优势。在水文上,研究区有洛贡河、玛加湖和曼达拉山脉的支流定期泛滥。这些参数的共享导致了土壤的成因,洪泛平原土壤具有沙质质地,湖泊土壤具有非常主要的粘土质地。此外,土壤的地球化学特征表明,不同土壤的SiO2含量总体为70%;湖相土壤Al2O3含量小于10%,河漫滩土壤Al2O3含量小于5%;土壤主要元素Fe2O3、CaO和MgO含量较低(≤2%)。此外,蚀变的矿物学指标表明这些土壤发生了中度的蚀变。因此,土壤中这些主要元素的分布揭示了其对地带性的敏感性,这是研究区土壤形成和分化的内在和外在参数的结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Susceptibility Zonation of the Soils of Mayo-Danay in East Part of the Sudano-Sahelian Cameroon, Central Africa
The study of soil resources of Mayo-Danay, located in the tropical zone of Cameroon, shows a diversity of soils characterized by specific properties. Indeed, this study area is generally a plain landscape whose average relative altitude (300 m). However, it indicates a vegetation of savanna type, very dominant. Hydrologically, Logone River, Maga Lake and tributary streams of the Mandara Mountains regularly flood the study area. The sharing of these parameters leads to soil’s genesis, which have a sandy texture for floodplain soils and a very dominant clay texture for lacustrine soils. Otherwise, the geochemistry of these soils shows SiO2 contents globally 70% in the different soils studied; Al2O3 contents are less than 10% in lacustrine soils and less than 5% in floodplain soils; while the major elements data of soils such as Fe2O3, CaO and MgO indicate relatively low contents (≤2%) on soils studied. In addition, the mineralogy index of alteration expresses a moderate alteration of these soils. Thus, the distribution of these major elements of soil reveals its susceptibility to zonation, which is a consequence of intrinsic and extrinsic parameters to formation and differentiation of soils of the study area.
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