Influence of Tillage Interval of Fallow on Soil Water Storage

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dc.creatorConlon, Thomas J.
dc.creatorBauer, Armand
dc.creator.authorConlon, Thomas J.
dc.creator.authorBauer, Armand
dc.date.accessioned2009-06-15T23:39:04Z
dc.date.available2009-06-15T23:39:04Z
dc.date.issued1978
dc.descriptionFallowing is practiced to increase soil water supply for the crop after fallow. But water must penetrate at least a foot below the soil surface of moldboard-plowed fallow to be "safe" from evaporation 108S. Time interval between tillage of fallow to control weeds did not alter the amount of evaporation loss. When available water to 48-inch depth exceeded 4 inches the first spring of the 21-month fallow period, precipitation storage efficiency thereafter was essentially zero.en
dc.identifier.urihttps://hdl.handle.net/10365/4861
dc.publisherNorth Dakota State University
dc.relation.ispartofFarm Research; 35:4; Mar/Apr 1978
dc.rightsNorth Dakota State Universityen
dc.sourceFarm Research; 35:4; Mar/Apr 1978
dc.subject.lcshSoil wateren_US
dc.subject.lcshTillageen_US
dc.titleInfluence of Tillage Interval of Fallow on Soil Water Storageen
dc.typeArticleen_US

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Farm Research; 35:4; Mar/Apr 1978