Preprint Article Version 1 Preserved in Portico This version is not peer-reviewed

Research on Anti-Scourability of Slope Eroded Soil

Version 1 : Received: 12 May 2021 / Approved: 13 May 2021 / Online: 13 May 2021 (13:06:26 CEST)

How to cite: Chun, L.X.; Yongde, K.; Na, C.H.; Hui, L. Research on Anti-Scourability of Slope Eroded Soil. Preprints 2021, 2021050291 (doi: 10.20944/preprints202105.0291.v1). Chun, L.X.; Yongde, K.; Na, C.H.; Hui, L. Research on Anti-Scourability of Slope Eroded Soil. Preprints 2021, 2021050291 (doi: 10.20944/preprints202105.0291.v1).

Abstract

Purpose - Soil aggregates are of great significance to soil and water conservation and ecological environment construction in arid area of northwest district.Methods - Exploring the effects of different vegetation includes types and land use methods on the stability of soil aggregates in the Loess Plateau, and provide reference for the rational use and management of land, also the improvement of soil structure in the region. Select 9 types of samples of 0-30 cm of typical soil plots as the research objects, compare and analyze the particle size index, stability differences and anti-erodibility of soil aggregates under various vegetation cover. Results - The results show that P value, MWD value, GMD value, D value, and AI value of the 0-10cm surface soil all show the maximum value. As the depth increases, the size distribution of the above index values of each soil sample in the 10-20cm and 20-30cm layers is different; P value in the 0-30cm depth layer is linearly positively correlated with the AI value and MWD value, and linearly negatively correlated with the D value. The correlation coefficient R between each variable is in the range of 0.78-0.97, and the D value reflects the Loess Plateau area stability and erosion resistance of soil aggregates better. GMD and MWD value show an exponential relationship, the correlation coefficient R value of 10-20cm height layer is 0.46; AI and MWD value in 0-10cm, 20-30cm height layer have a power function relationship, 10-20cm height layer has a polynomial function, the correlation coefficient R value is 0.97. The scour coefficient of different soil samples has a high degree of dispersion, the maximum CV value is 1.92, and the minimum value is 0.49. Conclusions - The results of this study can provide a theoretical basis for the ecological and hydrological benefit evaluation of slope erosion control and vegetation restoration on the Loess Plateau.

Subject Areas

Soil anti-scourability; Soil erodibility; Artificial simulated rainfallSoil aggregates; Erodibility

Comments (0)

We encourage comments and feedback from a broad range of readers. See criteria for comments and our diversity statement.

Leave a public comment
Send a private comment to the author(s)
Views 0
Downloads 0
Comments 0
Metrics 0


×
Alerts
Notify me about updates to this article or when a peer-reviewed version is published.
We use cookies on our website to ensure you get the best experience.
Read more about our cookies here.