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210512 ||| eng |
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|a 9783039430024
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|a 9783039430031
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|a books978-3-03943-003-1
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1 |
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|a Hrissanthou, Vlassios
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| 245 |
0 |
0 |
|a Modeling of Soil Erosion and Sediment Transport
|h Elektronische Ressource
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| 260 |
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|a Basel, Switzerland
|b MDPI - Multidisciplinary Digital Publishing Institute
|c 2020
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| 300 |
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|a 1 electronic resource (298 p.)
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| 653 |
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|a gully erosion
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| 653 |
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|a Yang formula
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| 653 |
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|a sediment re-suspension
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| 653 |
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|a deposition range
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| 653 |
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|a dam failure
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| 653 |
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|a land cover change
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| 653 |
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|a soil erosion
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| 653 |
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|a the Loess Plateau
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| 653 |
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|a small water reservoir
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| 653 |
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|a black soil
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| 653 |
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|a total load
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| 653 |
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|a calibration
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| 653 |
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|a SWAT
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| 653 |
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|a model validation
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| 653 |
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|a stream sediment transport
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| 653 |
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|a NLDAS-2
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| 653 |
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|a rainfall-runoff
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| 653 |
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|a uncertainty
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| 653 |
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|a sediment rating curve (SRC)
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| 653 |
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|a vegetation
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| 653 |
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|a History of engineering and technology / bicssc
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| 653 |
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|a Brenne
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| 653 |
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|a precipitation intensity
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| 653 |
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|a rainfall event
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| 653 |
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|a sediment entrainment
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| 653 |
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|a HEC-RAS
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| 653 |
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|a CORINE erosion model
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| 653 |
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|a sediment accumulation
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| 653 |
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|a urbanization
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| 653 |
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|a land management
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| 653 |
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|a fuzzy coefficients
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| 653 |
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|a precipitation
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| 653 |
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|a bed erosion
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| 653 |
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|a clogging
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| 653 |
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|a residue cover
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| 653 |
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|a statistical modeling
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| 653 |
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|a impact force
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| 653 |
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|a colmation
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| 653 |
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|a sediment bed fluidization
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| 653 |
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|a infiltration estimation
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| 653 |
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|a time-area method
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| 653 |
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|a seasonality
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| 653 |
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|a ponds
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| 653 |
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|a Goodwin Creek Experimental Watershed
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| 653 |
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|a TUSLE
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| 653 |
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|a Tarbela Reservoir
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| 653 |
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|a filtration
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| 653 |
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|a EROSION-3D
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| 653 |
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|a terrace
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| 653 |
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|a limnology
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| 653 |
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|a scenario analysis
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| 653 |
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|a soil conservation stone structures
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| 653 |
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|a Besham Qila
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| 653 |
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|a fuzzy logic
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| 653 |
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|a MUSLE
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| 653 |
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|a numerical modeling
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| 653 |
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|a sediment transport
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| 653 |
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|a debris blocking dam
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| 653 |
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|a sediment concentration
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| 653 |
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|a AnnAGNPS model
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| 653 |
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|a SWAT modeling
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| 653 |
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|a tailings pond
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| 653 |
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|a Upper Indus Basin (UIB)
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| 653 |
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|a WRF-Hydro
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| 653 |
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|a fuzzy regression
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| 653 |
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|a leaked tailings flow
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| 653 |
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|a sediment yield
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| 653 |
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|a wavelet transform analysis-artificial neural network (WA-ANN)
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| 653 |
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|a sediment modeling
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| 653 |
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|a CASC2D-SED
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| 653 |
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|a catchment area
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| 653 |
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|a mountainous catchment
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| 653 |
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|a model calibration
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| 653 |
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|a soil and water loss
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| 653 |
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|a sediment budget
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| 700 |
1 |
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|a Hrissanthou, Vlassios
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| 041 |
0 |
7 |
|a eng
|2 ISO 639-2
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| 989 |
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|b DOAB
|a Directory of Open Access Books
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| 500 |
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|a Creative Commons (cc), https://creativecommons.org/licenses/by/4.0/
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| 028 |
5 |
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|a 10.3390/books978-3-03943-003-1
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| 856 |
4 |
2 |
|u https://directory.doabooks.org/handle/20.500.12854/69012
|z DOAB: description of the publication
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| 856 |
4 |
0 |
|u https://www.mdpi.com/books/pdfview/book/2781
|7 0
|x Verlag
|3 Volltext
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|a 900
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|a 380
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|a 700
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|a 600
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|a 620
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|a The Special Issue entitled "Modeling of Soil Erosion and Sediment Transport" focuses on the mathematical modeling of soil erosion caused by rainfall and runoff at a basin scale, as well as on the sediment transport in the streams of the basin. In concrete terms, the quantification of these phenomena by means of mathematical modeling and field measurements has been studied. The following mathematical models (software) were used, amongst others: AnnAGNPS, SWAT, SWAT-Twn, TUSLE, WRF-Hydro-Sed, CORINE, LCM-MUSLE, EROSION-3D, HEC-RAS, SRC, WA-ANN. The Special Issue contains 14 articles that can be classified into the following five categories: Category A: "Soil erosion and sediment transport modeling in basins"; Category B: "Inclusion of soil erosion control measures in soil erosion models"; Category C: "Soil erosion and sediment transport modeling in view of reservoir sedimentation"; Category D: "Field measurements of gully erosion"; Category E: "Stream sediment transport modeling". Most studies presented in the Special Issue were applied to different basins in Europe, America, and Asia, and are the result of the cooperation between universities and/or research centers in different countries and continents, which constitutes an optimistic fact for the international scientific communication.
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