Particle Size Distribution of Eroded Spoil Materials

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dc.creatorGilley, J. E.
dc.creatorGee, G. W.
dc.creatorBauer, Armand
dc.creator.authorGilley, J. E.
dc.creator.authorGee, G. W.
dc.creator.authorBauer, Armand
dc.date.accessioned2014-11-06T20:21:43Z
dc.date.available2014-11-06T20:21:43Z
dc.date.issued2014-11-06
dc.date.issued1976
dc.descriptionErosion has been a heavily studied phenomenon since 1926 in the United States with an emphasis on soil losses from cultivated lands. This led to the adoption of cultural practices to reduce sediment production and to maintain agricultural productivity at a high rate. Determinations were made of the particle-size distribution of the soil surface prior to runoff and of the eroded material under conditions of tillage and no tillage. Evaluations were made of changes in particle-size distribution in runoff samples collected during the course of a storm.
dc.identifier.urihttps://hdl.handle.net/10365/24267
dc.publisherNorth Dakota State University
dc.relation.ispartofFarm Research; 34:2; Nov/Dec 1976
dc.rightsNorth Dakota State Universityen_US
dc.titleParticle Size Distribution of Eroded Spoil Materialsen_US
dc.typeArticleen_US

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Farm Research; 34:2; Nov/Dec 1976