The development of a typical red-brown earth
- 1 January 1974
- journal article
- Published by CSIRO Publishing in Soil Research
- Vol. 12 (2) , 97-105
- https://doi.org/10.1071/sr9740097
Abstract
Translocation of clay did not play a significant role in the development of the Urrbrae loam, a typical red-brown earth. This is shown by the manner of variation with depth of several features of the profile. Both A and B horizons apparently originated as distinct sedimentary deposits containing clay, any additional clay being formed in position.Keywords
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