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GIS-based upland erosion mapping

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dc.contributor.authorTeh S.H.en_US
dc.contributor.authorSidek L.M.en_US
dc.contributor.authorJulien P.Y.en_US
dc.contributor.authorLuis J.en_US
dc.contributor.authorid56789696100en_US
dc.contributor.authorid35070506500en_US
dc.contributor.authorid7102246042en_US
dc.contributor.authorid55812209200en_US
dc.date.accessioned2023-05-16T02:46:16Z
dc.date.available2023-05-16T02:46:16Z
dc.date.issued2014
dc.description.abstractThe main source of sediments in reservoirs is from upland erosion. Morgan and Davidson [22] and Julien [15,16] describe soil erosion processes and dynamics that have been studied for decades. The main factors contributing to upland erosion losses include rainfall erosivity, soil erodibility, land topography, land use, and land conservation practices [9]. Specific degradation rates in reservoirs of the United States are typically less than 2000 tons/km2/year [18] and are primarily linked to upland erosion rates. Upland erosion losses have been estimated using well-known methods like the Universal Soil Loss Equation (USLE) from Wischmeier and Smith [34]. The USLE includes all the factors affecting upland erosion from sheet and rill erosion. Renard et al. [25] provided a modified version named the Revised Universal Soil Loss Equation (RUSLE). © 2014 by Taylor & Francis Group, LLC.en_US
dc.description.natureFinalen_US
dc.identifier.doi10.1201/b16683
dc.identifier.epage330
dc.identifier.scopus2-s2.0-85054668875
dc.identifier.spage313
dc.identifier.urihttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85054668875&doi=10.1201%2fb16683&partnerID=40&md5=5238bfe27d1afd24d71f1349338e6435
dc.identifier.urihttps://irepository.uniten.edu.my/handle/123456789/21952
dc.publisherCRC Pressen_US
dc.sourceScopus
dc.sourcetitleHandbook of Engineering Hydrology: Modeling, Climate Change, and Variability
dc.titleGIS-based upland erosion mappingen_US
dc.typeBook Chapteren_US
dspace.entity.typePublication
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