Effects of initial soil water content, layering compaction and surface conditions on solute movement in soils
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- 631.432 S16E
Item type | Current library | Call number | Status | Date due | Barcode | |
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Mohinder Singh Randhawa Library | 631.432 S16E (Browse shelf(Opens below)) | Not for loan | 219711 | ||
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Mohinder Singh Randhawa Library | 631.432 S16E (Browse shelf(Opens below)) | Not for loan | 219712 |
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The solute peak coincided with the wetting front in air-dry soil and it lagged behind the wetting front in initially moist soil With a given amount of water, chloride was displaced deeper in sandy loam as compared to silt loam soil In a layered soil profi
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