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Climate adaptation in the southwest US: The SWPar4.5 parameter set for stochastic weather generators. [PDF]
Fullhart AT +5 more
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Evaluating the impact of soil erosion on soil quality in an agricultural land, northeastern China. [PDF]
Fang H, Zhai Y, Li C.
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Spatial hotspot analysis of soil erosion rate and classification of homogeneous zones using GIS in a mountainous contrasting land-use watershed. [PDF]
Saeedi Nazarlu F +3 more
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Quantitative evaluation of soil anti-erodibility in the fluctuation zones of rooted soil in a large reservoir, southwest of China. [PDF]
Wang P, Niu X, Xiao H, Tao G, Song Z.
europepmc +1 more source
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Statistical check of USLE‐M and USLE‐MM to predict bare plot soil loss in two Italian environments
Land Degradation and Development, 2018AbstractThe USLE‐M and the USLE‐MM estimate event plot soil loss. In both models, the erosivity term is given by the runoff coefficient,QR, times the single‐storm erosion index,EI30. In the USLE‐MM,QREI30is raised to an exponentb1 > 1 whereasb1 = 1 is assumed in the USLE‐M. Simple linear regression analysis can be applied to parameterize both models,
Vincenzo Bagarello +2 more
exaly +3 more sources
Catena, 2016
Abstract It has been proposed that the best physical model of erosion from a plot is provided by a replicate plot (Nearing, 1998). Event data from paired bare fallow plots in the USLE database were used to examine the abilities of replicate plots, the USLE and the USLE-M to model event erosion on bare fallow plots.
P I A Kinnell
exaly +2 more sources
Abstract It has been proposed that the best physical model of erosion from a plot is provided by a replicate plot (Nearing, 1998). Event data from paired bare fallow plots in the USLE database were used to examine the abilities of replicate plots, the USLE and the USLE-M to model event erosion on bare fallow plots.
P I A Kinnell
exaly +2 more sources
Improvement to the prediction of the USLE K factor
Geomorphology, 2014Abstract In the Universal Soil Loss Equation (USLE), the soil erodibility factor ( K ) corresponds to the collective effects of the detachment susceptibility of soil and the sediment transportability as well as the amount and rate of runoff under a given rainfall erosivity.
Farzin Shabani +2 more
exaly +2 more sources
Communications in Soil Science and Plant Analysis, 2003
Soil loss is estimated by different models in which the soil erodibility factor, K, is one of the important parameters, especially in soils with rock fragments. The objective of this study was to determine the soil erodibility factor by the Universal Soil Loss Equation (USLE) and USLE-M models by direct soil loss measurements for six soil series (three
A R Sepaskhah
exaly +2 more sources
Soil loss is estimated by different models in which the soil erodibility factor, K, is one of the important parameters, especially in soils with rock fragments. The objective of this study was to determine the soil erodibility factor by the Universal Soil Loss Equation (USLE) and USLE-M models by direct soil loss measurements for six soil series (three
A R Sepaskhah
exaly +2 more sources
Proceedings of the Eighth International Symposium on Information and Communication Technology, 2017
Use cases have been widely employed as an efficient means to capture and structure software requirements. A use case model is often represented by a loose combination between a UML use case diagram and a textual description in natural language. The use case model expressed in such a form often contains ambiguous and imprecise parts.
Minh-Hue Chu +4 more
openaire +1 more source
Use cases have been widely employed as an efficient means to capture and structure software requirements. A use case model is often represented by a loose combination between a UML use case diagram and a textual description in natural language. The use case model expressed in such a form often contains ambiguous and imprecise parts.
Minh-Hue Chu +4 more
openaire +1 more source

