dc.publisher | North Dakota State University | |
dc.rights | North Dakota State University | en |
dc.title | Influence of Tillage Interval of Fallow on Soil Water Storage | en |
dc.type | Article | en_US |
dc.source | Farm Research; 35:4; Mar/Apr 1978 | |
dc.description | Fallowing 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.date.accessioned | 2009-06-15T23:39:04Z | |
dc.date.available | 2009-06-15T23:39:04Z | |
dc.date.issued | 1978 | |
dc.identifier.uri | http://hdl.handle.net/10365/4861 | |
dc.creator | Conlon, Thomas J. | |
dc.creator | Bauer, Armand | |
dc.subject.lcsh | Soil water | en_US |
dc.subject.lcsh | Tillage | en_US |
dc.creator.author | Conlon, Thomas J. | |
dc.creator.author | Bauer, Armand | |
dc.relation.ispartof | Farm Research; 35:4; Mar/Apr 1978 | |