अवक्षेपण का वह भाग जो अन्त:स्यन्दन के पश्चात मृदा की ऊपरी सतह में पार्श्व गति से मृदा की सतह पर अपने प्रवेश बिन्दु से कुछ दूर पुन: वापिस आ जाता है।
Also called interflow, it is a part of precipitation which after infiltration moves laterally through upper crusts of the soil and returns to the surface at some location away from the point of entry into the soil.
Also called interflow, it is a part of precipitation which after infiltration moves laterally through upper crusts of the soil and returns to the surface at some location away from the point of entry into the soil.
