Mineralogical, Chemical, Geotechnical and Mechanical Investigations of Bafang Lateritic Fine Soils Formed on Basalts (West-Cameroon) for Road Embankment Purpose

W. T. Hyoumbi, P. Pizette, A. Wouatong, N. Abriak
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引用次数: 7

Abstract

The present paper treats the relationship between geotechnical parameters and the mineralogical compositions, in order to understand the behavior of the Bafang lateritic fine soils and their efficient use as road embankment materials on the other hand. Thus, the field campaigns have permitted to distinguish two facies of Bafang lateritic fine soils: reddish and yellowish facies. The X-ray diffraction (XRD), the thermo-gravimetry analysis (TGA) and the X-ray fluorescence (XRF) have revealed that the reddish facies contents: kaolinite (53.34% -48.29%); hematite (16.62% - 17.40 %); gibbsite (8.26 % - 16.54%), ilmenite (7.6 % -7.98%), quartz (1.92 % - 4.65 %), illite (2.65% - 1.99 %) and accessories minerals as florencite (1.45%); montmorillonite (0.90 %) and plagioclase (0.69 %); while the yellowish facies is composed of : 65.1 % kaolinite, 11.2 % gibbsite, 9.64 % goethite, 7.02 % quartz, 3.23 % ilmenite and 2.08 % of illite. Their Silica/sexquioxide ratios correspond to those of moderate laterite. The geotechnical and mechanical characteristics have shown that the reddish and yellowish facies are respectively silty clay and sandy silt. They are plastic to very high plastic and moderately clayey to clayey materials. Moreover, they are medium swelling to high swelling. The IBR values more than 40% and the soaked CBR values prove that these materials belong to the S4 bearing capacity class. The minimum values of UCS and Rt are respectively 1.7 MPa and 0.17 MPa. Then, the results of geotechnical and mechanical properties combining to those of XRD, TGA and XRF have demonstrated that the fine lateritic soils with low silica/sexquioxide ratios values (less than 1.6) are suitable for road embankment.
巴方玄武岩(喀麦隆西部)筑路用红土细土的矿物学、化学、岩土和力学研究
本文研究了土工参数与矿物学成分的关系,以了解巴方红土细土的特性及其作为道路路基材料的有效利用。因此,野外活动可以区分出巴方红土细土的两种相:红色相和淡黄色相。x -射线衍射(XRD)、热重分析(TGA)和x -射线荧光(XRF)分析结果表明:微红色相为高岭石(53.34% ~ 48.29%);赤铁矿(16.62% ~ 17.40%);三水长石(8.26% ~ 16.54%)、钛铁矿(7.6% ~ 7.98%)、石英(1.92% ~ 4.65%)、伊利石(2.65% ~ 1.99%)及其附属矿物如萤石(1.45%);蒙脱石(0.90%)和斜长石(0.69%);淡黄色相由65.1%高岭石、11.2%三水铝石、9.64%针铁矿、7.02%石英、3.23%钛铁矿和2.08%伊利石组成。它们的硅/六氧化二氮比值与中等红土相当。岩土力学特征表明,微红色相为粉质粘土相,淡黄色相为砂质粉砂相。它们是塑料到非常高的塑料和中等粘土到粘土的材料。而且,它们是中度肿胀到高度肿胀。IBR值大于40%,浸渍CBR值为S4级。UCS和Rt最小值分别为1.7 MPa和0.17 MPa。然后,结合XRD、TGA和XRF的岩土力学性能分析结果表明,低硅/六氧化二氮比值(小于1.6)的红土土适合用于道路路基。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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