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dc.contributor.authorBogart, Daniel Frederick
dc.description.abstractMicrotopography is an important factor in hydrologic processes. The purpose of this research was to study the effects of microtopography on runoff generation. Specifically, this was performed through an array of physical experimentation comparing “rough” and “smooth” surfaces under natural and simulated rainfall. Utilizing these types of rainfalls required experimentation to take place in both field and laboratory settings. The range of control factors in this study varied from surface microtopography to soil type, rainfall intensity/pattern, and ambient moisture content. The recorded results of the laboratory study were further compared with the output of a puddle-to-puddle (P2P) overland flow model. The physical experiments showed a trend initially favoring neither the rough nor smooth surface in runoff production. However, in subsequent experiments the rough surface appeared to substantially increase runoff production relative to the smooth surface. Additionally, good agreement was found between the results of the physical experimentation and the model.en_US
dc.publisherNorth Dakota State Universityen_US
dc.rightsNDSU Policy 190.6.2
dc.titleHydrologic Experiments and Analysis: The Effect of Microtopography on Runoff Generationen_US
dc.typeThesisen_US
dc.date.accessioned2018-01-10T21:19:13Z
dc.date.available2018-01-10T21:19:13Z
dc.date.issued2014
dc.identifier.urihttps://hdl.handle.net/10365/27197
dc.subjectSurface microtopography
dc.subject.lcshHydrologyen_US
dc.subject.lcshRunoffen_US
dc.rights.urihttps://www.ndsu.edu/fileadmin/policy/190.pdf
ndsu.degreeMaster of Science (MS)en_US
ndsu.collegeEngineeringen_US
ndsu.departmentCivil and Environmental Engineeringen_US
ndsu.advisorChu, Xuefeng


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