Abstract

The characterization of the structural arrangement of an unsaturated soil is important for the understanding of its behavior. For expansive soils, obtaining this information and combining it with an understanding of their intrinsic and extrinsic properties, makes it possible to predict their performance. The experimental procedure for this study was developed using the expansive soil of the Maria Farinha formation in the city of Paulista, in Pernambuco, Brazil. Physical and chemical characterization tests, edometric tests with wetting, and structural analysis through X-Ray computed tomography were performed for both undisturbed and compacted samples, before and after wetting and swelling. The compaction process was performed without any prior air drying and without loosening, beginning with the field moisture level. Based on its liquid limit and plasticity index, the soil can be classified as CH according to the USCS, moderately acidic, with a swelling potential ranging from high to very high, depending on the initial suction of the sample. The analysis of the soil macro-structure revealed a smaller number of voids in the compacted samples. In addition, it was found that the wetting process caused a reduction of the soil macro pores, in both cases.

Highlights

  • The growing development of contemporary society has brought with it ever greater geotechnical challenges, making testing methodologies consecrated in the past no longer sufficient to provide support for current decisionmaking, which must deal with new problems

  • Expansive soils stand out because they vary volumetrically due to cyclical changes in moisture/suction, and are under practically constant tensions

  • Vilar & Ferreira (2015) [1] define expansive soils as unsaturated soils consisting of 2:1-type laminar clay minerals, such as montmorillonites and vermiculites

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Summary

Introduction

The growing development of contemporary society has brought with it ever greater geotechnical challenges, making testing methodologies consecrated in the past no longer sufficient to provide support for current decisionmaking, which must deal with new problems. Current knowledge about the structural arrangement and hydromechanical properties of unsaturated soils are seen as essential for understanding and predicting their behavior. In this context, expansive soils stand out because they vary volumetrically due to cyclical changes in moisture/suction, and are under practically constant tensions. Vilar & Ferreira (2015) [1] define expansive soils as unsaturated soils consisting of 2:1-type laminar clay minerals, such as montmorillonites and vermiculites. Their presence can be associated with places where evapotranspiration exceeds precipitation, such as arid and semi-arid regions with a tropical or temperate climate, as is the case in northeastern Brazilian (where this study took place). Construction problems associated with the presence of expansive soils are described by Morais (2017) [2], who reports: cracks in slabs, walls, and foundations of small buildings; cracks in pavement; and even ruptures in pipes and canals

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