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首页> 外文期刊>The Open Geology Journal >Petrological, Physico-Chemical and Mechanical Characterization of the Topomorphic Vertisols from the Sudano-Sahelian Region of NorthCameroon
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Petrological, Physico-Chemical and Mechanical Characterization of the Topomorphic Vertisols from the Sudano-Sahelian Region of NorthCameroon

机译:喀麦隆北部萨达诺-萨赫勒地区的地形形变溶胶的岩石学,物理化学和力学特征

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In Cameroon, topomorphic vertisols are widespread in the Sudano-sahelian zone above latitude 9oN. With adepth of about 2 to 2.5 m above the water table, these soils show four main horizons from bottom to top: a dark greyhorizon with hydromorphic patches (B3g), dark grey horizon (B21), dark grey horizon with slickensides (B1) and a surficialgrey humiferous horizon (A1) with desiccation cracks. Also, they show a heavy clayey texture, very massive structure,high bulk density, very low porosity and a high compacity. The microfabric of the soils is marked by abundant plasmas,isotic at the surface but birefringent at depth, with numerous stress cutans. The microscopic analysis of heavy mineralsreveals the presence of magmatic and metamorphic minerals from the upper part of the watershed. Quartz grains aremainly angular to sub-angular revealing short fluvial transport distance. The vertisols are thus formed from recent alluvialdeposits from weathering, erosion and deposition of rocks from upper parts of the watershed. Physico-chemically, thestudied soils are characterized by high cation exchange capacity (26-42 meq/100g), high sum of bases (74.30-94.23meq/100g), high base saturation, low organic carbon and a very high C/N ratio. Geochemically, Si and Al are thedominant elements, characterised by a Si/Al ratio range of 2.27 and 2.94. According to this rate, 2/1 clay minerals, namelysmectite, are predominant and their presence confirms the shrink-swell behaviour of the soils. Total base concentrationsare high and could be related to the contrasted climate and the low landscape position. Mechanical analyses revealed veryhigh liquid limits (36-46%), low plastic limits (10-17%), high plasticity indices and high shrinkage limits that permit toclassify those soils as medium to high plasticity inorganic clays. Those soils could be potentially useful in many domainslike the chemical industry, pharmaceutics, petroleum industry, agronomy or environmental protection.
机译:在喀麦隆,9oN以上的Sudano-sahelian带中普遍存在准形态的斜体。这些土壤在地下水位以上约2至2.5 m处显示出从下到上的四个主要层位:具有水溶斑块的深灰层(B3g),深灰层(B21),深层含滑石层(B1)和具有干燥裂缝的浅灰色腐殖质地层(A1)。而且,它们显示出浓厚的粘土质地,非常大的结构,高堆积密度,非常低的孔隙率和高的相容性。土壤的微结构以大量等离子为特征,等离子在表面,但在深度上是双折射的,具有许多应力角质。对重矿物的微观分析揭示了流域上部存在的岩浆和变质矿物。石英颗粒主要是成角到近角的,显示出短的河流运移距离。因此,垂直变质层是由最近的冲积沉积物形成的,该沉积物是来自流域上部的风化,侵蚀和岩石沉积。物理化学研究的土壤特征在于高阳离子交换容量(26-42 meq / 100g),高碱总和(74.30-94.23meq / 100g),高碱饱和度,低有机碳和非常高的C / N比。从地球化学角度看,Si和Al是主要元素,其Si / Al比范围为2.27和2.94。按照该速率,占2/1的粘土矿物(即蒙脱石)占主导地位,它们的存在证实了土壤的收缩膨胀行为。总碱浓度高,可能与对比的气候和低的景观位置有关。力学分析表明,液体极限值很高(36-46%),塑性极限值很低(10-17%),高塑性指数和高收缩率极限使这些土壤可以归类为中高塑性无机粘土。这些土壤可能在化学工业,制药,石油工业,农学或环境保护等许多领域具有潜在用途。

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