
TY  - JOUR
A1  - Oertel, AC 
T1  - The development of a typical red-brown earth
JF  - Soil Research
JO  - Soil Res.
Y1  - 1974
VL  - 12
IS  - 2
SP  - 97
EP  - 105
KW  - 
UR  - https://doi.org/10.1071/SR9740097 
N2  - 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. 
ER  -

