Physical and Zeta Potential Characteristics of Erodible Lateritic Soils

dc.contributor.author	T. Cássia de Brito Galvão
dc.contributor.author	Cláudia de Sanctis Viana
dc.contributor.author	Abidin Kaya
dc.date.accessioned	2017-05-08T21:31:21Z
dc.date.available	2017-05-08T21:31:21Z
dc.date.copyright	May 2003
dc.date.issued	2003
dc.identifier.other	%28asce%291527-6988%282003%294%3A2%2895%29.pdf
dc.identifier.uri	http://yetl.yabesh.ir/yetl/handle/yetl/54706
dc.description.abstract	Physical, 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)
dc.publisher	American Society of Civil Engineers
dc.title	Physical and Zeta Potential Characteristics of Erodible Lateritic Soils
dc.type	Journal Paper
dc.journal.volume	4
dc.journal.issue	2
dc.journal.title	Natural Hazards Review
dc.identifier.doi	10.1061/(ASCE)1527-6988(2003)4:2(95)
dc.tree	Natural Hazards Review:;2003:;Volume ( 004 ):;issue: 002
dc.contenttype	Fulltext