Abstract
Eight primary catchments within the Western Australian wheatbelt were surveyed
in detail to examine the abilities of conventional soil classification and
geostatistical analysis to provide detailed information of soil spatial
variation for catchment-scale hydrologic modelling. Nine soil physical
properties were measured. The results illustrate potential diculties with both
methods. Classification by using the Factual Key was unable to describe the
major component of soil property variation. The relative variance accounted
for by soil classes was usually <10%. Only the yellow duplex soils
appeared distinct from other soil classes. Potential diculties with
geostatistical analysis also arose because of fluctuations in the variogram
models. Contrasts occurred between variograms for the same property over
different catchments and for different properties over the same catchment.
Within the areas studied, nugget and linear (unbounded) variogram models were
more common than spherical or exponential models. It is proposed that the
surveyor would have to select a survey method on the basis of prior knowledge
about which model of variation is more likely to be successful for the scale
and location of survey.
Subject
Earth-Surface Processes,Soil Science,Environmental Science (miscellaneous)
Cited by
3 articles.
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