Results 201 to 210 of about 1,822 (263)

Spatiotemporal evolution characteristics of freeze-thaw erosion intensity in the high-cold mountainous areas of Northwestern Yunnan from 2017 to 2023. [PDF]

Sci Rep
Ye H, Bai D, Liu S, Tan S, Wang J, Xie F, Zhu Y.   +6 more
europepmc   +1 more source

Evaluation of early warning signals for soil erosion using remote sensing indices in northeastern Iran. [PDF]

Sci Rep
Boali A, Hosseinalizadeh M, Kariminejad N, Asgari HR, Mohamadian Behbahani A, Naimi B, Shafaie V, Movahedi Rad M.   +7 more
europepmc   +1 more source

Increasing riparian vegetation cover to improve water quality: the importance of considering land use. [PDF]

Environ Manage
Te Ngaio PAJ, McMahon JM, van den Berg D, Healy A, Turner RDR, Marsh A.   +5 more
europepmc   +1 more source

Influence of Grassland Habitats on Acridoidea (Orthoptera) Species Diversity in Different Divisions of the Xinjiang Production and Construction Corps. [PDF]

Biology (Basel)
Liu Y, Wang S, He Y, Yuan G, Pu X, Zhou C.   +5 more
europepmc   +1 more source

Rill erosion dynamics in smallholder farming systems of wet tropical Africa. [PDF]

Sci Rep
Wilken F, Fiener P, Batista P, Cooper M, Haist J, Muhindo D, van Oost K, Rueegg M, Doetterl S.   +8 more
europepmc   +1 more source

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Mapping soil erodibility over India

Catena, 2023
Soil erosion is a major environmental problem worldwide, and almost half of India’s total geographical area is susceptible to it. The Revised Universal Soil Loss Equation (RUSLE) has been widely used globally to estimate soil erosion, and Soil erodibility factor, denoted by K-factor, is an essential component of RUSLE.
Manabendra Saharia, Ravi Raj, Sumedha Chakma   +2 more
exaly   +2 more sources

Climate effects on soil erodibility

Earth Surface Processes and Landforms, 2007
AbstractSoil erodibility data, calculated using measured soil loss from standard runoff plots, collected over at least one year and applying the standard requirements for calculating the soil erodibility factor (K) of the Universal Soil Loss Equation (USLE), have been analysed to investigate whether climate affects the susceptibility of soils to water ...
Salvador Sanchis MP, Torri D, Borselli L, Poesen J   +3 more
openaire   +2 more sources

SOIL ERODIBILITY, FALL AND SPRING

Canadian Journal of Soil Science, 1966
In a 7-year study of eight summerfallow treatments, the percentage of erodible soil (soil particles < 0.84 mm in diameter) at the completion of tillage in the fall, and prior to preseeding tillage the following spring, was significantly influenced by the summerfallow method.
C. H. Anderson, A. Wenhardt
openaire   +1 more source

Temporal Changes in Soil Erodibility

Soil Erosion, 2013
Soil erodibility has been considered to depend on soil permanent properties (e.g., texture and organic matter content). In this presentation the dependence of interrill and rill erodibility on prewetting rate (PWR) and aging, respectively, is discussed. Slow wetting of soils reduces seal formation, runoff, and interrill erosion.
null G.J. Levy, null I. Shainberg, null J. Letey   +2 more
openaire   +1 more source

Restoration of Eroded and Degraded Soils

2010
Restoration refers to the process of repairing and returning damaged or degraded soils (e.g., eroded agricultural soils, mined soils) to a condition similar to the predegradation level of capability for supporting plant growth and maintaining environmental quality. Degradation, which broadly refers to decline in soil’s capacity for a specific use (e.g.,
Humberto Blanco-Canqui, Rattan Lal
openaire   +1 more source