4.7 Article

Non-linear response of sediment size characteristics and associated transport patterns to soil structural stability in sheet erosion under field rainfall simulation

相关参考文献

注意:仅列出部分参考文献,下载原文获取全部文献信息。
Article Environmental Sciences

Sediment transport mechanisms and selective removal of soil particles under unsteady-state conditions in a sheet erosion system

Elham Sirjani et al.

Summary: Selective removal of particles and nutrients by water erosion is a key factor in soil erosion studies. Most studies have focused on high-slope gradients, but there is a need for further research on low-slope agricultural soils.

INTERNATIONAL JOURNAL OF SEDIMENT RESEARCH (2022)

Article Geosciences, Multidisciplinary

Insights into the sediment transport processes operating in rain-impacted flows

P. I. A. Kinnell

Summary: The laboratory experiments discovered that raindrops induce different modes of motion in particles of different sizes, and that the particle distribution of rain-impacted sediment discharge changes over time. The experiments also found that sediment discharge induced by raindrops peaks at a specific flow depth. The assumption that rain erosion is solely determined by flow discharge and rainfall intensity is proven to be false.

CATENA (2022)

Article Engineering, Civil

Identifying interrill, rill, and ephemeral gully erosion evolution by using rare earth elements as tracers

Hongqiang Shi et al.

Summary: This study used rare earth elements as tracers to monitor the successive development of different erosion processes on hillslopes, revealing that hillslope erosion went through five evolutionary stages: interrill erosion, rill development, stabilized rill, ephemeral gully development, and stabilized ephemeral gully. Hydrological parameters played a significant role in explaining channel evolution and particle size changes.

JOURNAL OF HYDROLOGY (2022)

Article Soil Science

Quantifying the contribution of phyllosilicate mineralogy to aggregate stability in the East Asian monsoon region

Xinliang Wu et al.

Summary: Aggregate stability strongly depends on the phyllosilicate mineralogy, particularly vermiculite, showing a dominant role. Geographic location shows a unimodal trend in influencing aggregate stability, with greater disruptive forces leading to more prominent effects. In combination, soil organic carbon, exchangeable sodium, and calcium play a complementary role in affecting aggregate stability.

GEODERMA (2021)

Article Soil Science

Modeling land management effects on the size distribution of eroded sediment

Gang Liu et al.

SOIL & TILLAGE RESEARCH (2019)

Article Environmental Sciences

Modeling aggregate size distribution of eroded sediment resulting from rain-splash and raindrop impacted flow processes

Selen Deviren Saygin et al.

INTERNATIONAL JOURNAL OF SEDIMENT RESEARCH (2019)

Review Soil Science

Soil structure as an indicator of soil functions: A review

E. Rabot et al.

GEODERMA (2018)

Article Environmental Sciences

Raindrop Size and Flow Depth Control Sediment Sorting in Shallow Flows on Steep Slopes

L. Wang et al.

WATER RESOURCES RESEARCH (2018)

Article Engineering, Civil

Interrill soil erosion processes on steep slopes

X. C. (John) Zhang et al.

JOURNAL OF HYDROLOGY (2017)

Article Environmental Sciences

Size characteristics of sediments eroded from three soils in China under natural rainfall

Yanfang Hao et al.

JOURNAL OF SOILS AND SEDIMENTS (2016)

Article Soil Science

Size Selectivity of Eroded Sediment Associated with Soil Texture on Steep Slopes

L. Wang et al.

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL (2015)

Article Environmental Sciences

Can control of soil erosion mitigate water pollution by sediments?

R. J. Rickson

SCIENCE OF THE TOTAL ENVIRONMENT (2014)

Article Engineering, Civil

Flow-driven soil erosion processes and the size selectivity of sediment

H. Asadi et al.

JOURNAL OF HYDROLOGY (2011)

Article Engineering, Civil

An investigaion of flow-driven soil erosion processes at low streampowers

H. Asadi et al.

JOURNAL OF HYDROLOGY (2007)