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<br />aggregate stability in the B horizons increased, due to inputs of translocated organic matter. <br />However, unlike other studies (e.g. DeBano, et al, 1970) which have attributed post-fIre, <br />subsurface water repellency to translocated organic matter, this investigation found that the <br />underlying horizons remained wettable. The authors suggest that, in this case, fIne-textured <br />soils may have interfered with the development of water repellency. <br /> <br />17 <br />