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dc.contributor.authorMontgomery, Brandon
dc.description.abstractQuantifying long-term, global soil change is of the utmost importance as the human population continues growing and food security needs intensify. North Dakota presents a unique opportunity to study dynamic soil change because of its agricultural prominence and extensive soil survey data. A resampling method to characterize soil change from legacy soil survey data was utilized on a benchmark soil series, the Barnes, in North Dakota. Significant decreases (p<0.05) in soil organic carbon (SOC) were measured in surface horizons of three Barnes pedons, and depending upon management practices, morphologic changes ranged from highly eroded, with the complete loss of the A horizon, at two sites, to non-eroded conditions at sites returned to CRP 25 years ago. Additionally, using remotely sensed evapotranspiration (ET) data as a non-biased proxy for soil function shows modeling potential. These results serve as a proof of concept and demonstrate the need for more comprehensive research.en_US
dc.publisherNorth Dakota State Universityen_US
dc.rightsNDSU policy 190.6.2
dc.titleEvaluating Dynamic Soil Change in the Barnes Soil Series Across Eastern North Dakotaen_US
dc.typeThesisen_US
dc.date.accessioned2018-01-31T20:25:41Z
dc.date.available2018-01-31T20:25:41Z
dc.date.issued2015
dc.identifier.urihttps://hdl.handle.net/10365/27384
dc.description.sponsorshipUnited States Department of Agriculture-Natural Resources Conservation Service’s National Soil Survey Centeren_US
dc.rights.urihttps://www.ndsu.edu/fileadmin/policy/190.pdf
ndsu.degreeMaster of Science (MS)en_US
ndsu.collegeAgriculture, Food Systems and Natural Resourcesen_US
ndsu.departmentSoil Scienceen_US
ndsu.departmentSchool of Natural Resource Sciencesen_US
ndsu.programSoil Scienceen_US
ndsu.advisorHopkins, David


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