Linear extensibility, water sorption and cracking pattern of vertisol. Note.
1987
Bharambe P.R. | Yewale P.T. | Varade S.B.
The soils of high clay content exhibited more visible and numerous cracks than the soils of low clay content. The depth and width of cracks were also more in clay soils as compared to silty loam. This may be ascribed to the dominance of clay minerals possessing expansion and contraction characteristics.
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