67 The Soil Record of Quaternary Climate Change
Tuesday, 29 July 2003
8:00 AM - 12:00 PM
MODELLING THE DISTRIBUTION OF SOILS AND SOIL PROPERTIES ACROSS THE AUSTRALIAN CONTINENT
Paper number: 67-10
Program: SYMPOSIA
Time: 10:50 AM – 11:10 AM
Authors
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Brent L. HendersonCanberra, N/A
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Karin ViergeverWageningen Univ and Rsch Centre, Wageningen, N/A
Abstract
The climatic variables feature prominently in all models but different climatic variables appear in different models. For the topsoil pH model, the precipitation in the driest month and the annual mean soil moisture feature most prominently in the condition (sub-setting) rules and in the regression rules. For the subsoil pH model, the annual mean soil moisture and the lowest monthly solar radiation are most important. For the topsoil organic C model, the annual mean soil moisture is most important. The most used terrain attributes are generally elevation, relative elevation, and relief. The four bands from the Landsat MSS are also important predictors in all models. What and where variables are being used in each of the predictions will be presented and discussed.