Abstract

This paper presents a study research in the laboratory of three clayey soils from the depression of the Lama, a tropical climate area where disorders appear on construction and roads. Samples were tested to establish the relationship between their mineralogy and their geotechnical properties. On the three clayey soils, analyses were performed to characterize the macroscopic behavior (physical tests, free swelling test and compressibility tests) and the microstructural, chemical and mineralogical characterizations by thermal analysis, chemical analysis, X-Ray diffraction, Scanning Electron Microscopy observations complementary X-ray EDS analyses. At first glance, the results of physical and compressibility tests appear not to be consistent with the free swelling test results. Indeed, these results highlighted differences in the behaviors of the samples because the swelling potential revealed by the results of physical and compressibility test does not follow the same trend as the one given by the free swelling test result. The main clay minerals in the studied clayey soils varied from fibrous clays (palygorskite) to best-known clays such as smectite and kaolinite. Microstructural, chemical and mineralogical analyses allowed to understand and explain the different trends obtained by the different types of geotechnical characterization tests of studied clayey soils.

Highlights

  • For Lama1 the Differential Thermal Analysis (DTA) curve showed essentially peak at 485 ̊C characteristic of kaolinite and a peak at 766 ̊C characteristic of smectite

  • Lama2 DTA curve showed two mains peaks (124 ̊C and 484 ̊C) below 600 ̊C which are characteristic of fibrous clays [17] [18]

  • The analyses presented in what follows aimed at identifying the presence of other compounds such as silica, oxides that are expected to enter into the composition of these clayey soils

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Summary

Introduction

Expansive soils are widely distributed in the world and in tropical areas. Y. Tankpinou Kiki et al 306 where their formation is related to contrasting seasons. The alternation of seasons (dry and rainy) promotes variations of clayey soils volume resulting in shrinkage/swelling cycles. Several studies based on laboratory tests focused on the cycling behavior of clays [4]-[6]. Many classifications of clayey soils in relation to their sensitivity to water and their swelling and shrinkage potential have been established [7]. Authors studied the influence of shrinkage/swelling cycles on clayey soils and showed different behaviors according to the mechanical initial state and the mineralogical composition [8] [9]

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