TY - JOUR
AU1 - Eswaran, H.
AU2 - Bin, Wong Chaw
AB - To facilitate description and study, the deep profile is divided into several morphological zones, via., α, γm, γp and δ zones. Clay content progressively increases from the rock zone δ to the soil zone α. The silt/clay ratio increases from the δ to the upper part of the γp zone and then decreases again. These changes are explained in terms of the fragmentation or aggregation of various minerals during the clay separation procedure. Estimates of the mineralogical composition in the fine earth shows differences in the zones, and the charge characteristics are related to these.
TI - A Study of a Deep Weathering Profile on Granite in Peninsular Malaysia: I. Physico‐Chemical and Micromorphological Properties
JF - Soil Science Society of America Journal
DO - 10.2136/sssaj1978.03615995004200010032x
DA - 1978-01-01
UR - https://www.deepdyve.com/lp/wiley/a-study-of-a-deep-weathering-profile-on-granite-in-peninsular-malaysia-F1M1XpM0V6
SP - 144
EP - 149
VL - 42
IS - 1
DP - DeepDyve
ER -