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Soil hydraulic conductivities of latosols under pasture, forest and teak in Rondonia, Brazil

✍ Scribed by Helmut Elsenbeer; Bradley E. Newton; Thomas Dunne; Jorge M. de Moraes


Publisher
John Wiley and Sons
Year
1999
Tongue
English
Weight
207 KB
Volume
13
Category
Article
ISSN
0885-6087

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✦ Synopsis


We investigated the changes of saturated hydraulic conductivity, K sat , with depth of latosols developed on Precambrian basement rocks under primary rainforest, pasture and teak. In all cases, K sat decreased with depth, with most of the decrease occurring between the surface and a depth of 30 cm. In conjunction with prevailing rainfall intensities and frequencies, this anisotropy supports a pronounced lateral component of hillslope Β―ow paths, and also of overland Β―ow under pasture. Our results are at variance with data from other latosols where K sat tends to increase with depth, and hence suggest that considerable restraint is needed in generalization and extrapolation until results from a co-ordinated eort at hydrology-oriented data collection become available.


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