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Effects of initial soil water content, layering compaction and surface conditions on solute movement in soils

By: Material type: TextTextPublication details: Ludhiana 1996Description: 71,30LSubject(s): DDC classification:
  • 631.432 S16E
Summary: 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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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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