The objective of this work was study the evolution of the weathering front in gneiss saprolites (felsic rocks) in two profiles of Planosols under different levels of severity of degradation (point 1 incipient degradation and point 2 degradaded area under desertified area in Pernambuco
Unravelling the genesis of polygenetic soils is a complex task because of overprinting and mixing of...
The mineralogical association of the weathering rocks and their pedogenic process is fundamental in ...
ABSTRACT: The evaluation of soils in representative landscapes constitutes an opportunity to evaluat...
ABSTRACTUnderstanding soil formation processes across different landscapes is needed to predict how ...
ABSTRACT Soils formed in high mountainous regions in southern Brazil are characterized by great accu...
Ten soils formed from basic volcanic rocks were studied on a 450 km climosequence transect in Santa ...
Semi-arid environments occupy a large part of the terrestrial territory, are characterized by quite ...
The geomorphic evolution of the south-eastern Brazilian landscape is attributed to climatic changes ...
At the Earth surface, the terrestrial life is supported by a thin soil mantle. Human activities can ...
International audienceNon-lateritic red soils cover vast areas of the semiarid region of Northeast B...
Soils formed in high mountainous regions in southern Brazil are characterized by great accumulation ...
ABSTRACT The semiarid region of northeastern Brazil has a large area occupied by Planosols, where in...
The thick weathering profiles of humid tropical areas are an important, yet generally neglected, sou...
ABSTRACT The micromorphology of deeply weathered soils (Ferralsols/ Latossolos ) from the Central Pl...
The purpose of this work is to identify the pedogenetic processes and to classify chemically, physic...
Unravelling the genesis of polygenetic soils is a complex task because of overprinting and mixing of...
The mineralogical association of the weathering rocks and their pedogenic process is fundamental in ...
ABSTRACT: The evaluation of soils in representative landscapes constitutes an opportunity to evaluat...
ABSTRACTUnderstanding soil formation processes across different landscapes is needed to predict how ...
ABSTRACT Soils formed in high mountainous regions in southern Brazil are characterized by great accu...
Ten soils formed from basic volcanic rocks were studied on a 450 km climosequence transect in Santa ...
Semi-arid environments occupy a large part of the terrestrial territory, are characterized by quite ...
The geomorphic evolution of the south-eastern Brazilian landscape is attributed to climatic changes ...
At the Earth surface, the terrestrial life is supported by a thin soil mantle. Human activities can ...
International audienceNon-lateritic red soils cover vast areas of the semiarid region of Northeast B...
Soils formed in high mountainous regions in southern Brazil are characterized by great accumulation ...
ABSTRACT The semiarid region of northeastern Brazil has a large area occupied by Planosols, where in...
The thick weathering profiles of humid tropical areas are an important, yet generally neglected, sou...
ABSTRACT The micromorphology of deeply weathered soils (Ferralsols/ Latossolos ) from the Central Pl...
The purpose of this work is to identify the pedogenetic processes and to classify chemically, physic...
Unravelling the genesis of polygenetic soils is a complex task because of overprinting and mixing of...
The mineralogical association of the weathering rocks and their pedogenic process is fundamental in ...
ABSTRACT: The evaluation of soils in representative landscapes constitutes an opportunity to evaluat...