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contributor authorT. Cássia de Brito Galvão
contributor authorCláudia de Sanctis Viana
contributor authorAbidin Kaya
date accessioned2017-05-08T21:31:21Z
date available2017-05-08T21:31:21Z
date copyrightMay 2003
date issued2003
identifier other%28asce%291527-6988%282003%294%3A2%2895%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/54706
description abstractPhysical, mineralogical, and zeta potential studies were conducted on selected erodible lateritic soils from Belo Horizonte, Brazil. These soils are residual and highly weathered, and they have a very low amount of organic matter and an acid-soil solution natural pH in the range of 4.8–5.3. Engineers consider similar soils to cover 65% of the Brazilian surface. Soil sampling was performed at representative geological sites underlain by gneiss, dolomitic-itabiritic phyllites, and phyllites as parent materials. The soil erosion susceptibility was in the following decreasing order: MA-2 (soil developed from standard gneiss, more coarse materials)
publisherAmerican Society of Civil Engineers
titlePhysical and Zeta Potential Characteristics of Erodible Lateritic Soils
typeJournal Paper
journal volume4
journal issue2
journal titleNatural Hazards Review
identifier doi10.1061/(ASCE)1527-6988(2003)4:2(95)
treeNatural Hazards Review:;2003:;Volume ( 004 ):;issue: 002
contenttypeFulltext


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