
%0 Journal Article
%A Oertel, AC 
%T The development of a typical red-brown earth
%J Soil Research
%D 1974/12/01
%V 12
%N 2
%P 97-105
%K 
%R https://doi.org/10.1071/SR9740097
%U https://www.publish.csiro.au/paper/SR9740097 
%X 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. 
