The Role of Rainstorm Properties on Crop-Land Soil Erosion: Coupling Event-Scale Modeling with a Stochastic Rainfall Generator for Estimating Erosion Risks

2021 ◽  
Author(s):  
Yuval Shmilovitz ◽  
Francesco Marra ◽  
Haiyan Wei ◽  
Eli Argaman ◽  
Mark Nearing ◽  
...  
Author(s):  
Maria Nedealcov ◽  

Excessive amounts of atmospheric precipitation can cause intense soil erosion, landslides, inundation and floods. Torrential rains have the force to displace and transport soil particles, so the risk of soil erosion becomes real, as many times as atmospheric precipitations have a devastating character. In this context, it is extremely useful to know the particularities of the torrential rains in the current regional climate. At this stage, the Fournier (IF) pluvial aggression index is becoming more and more prevalent. This paper is dedicated to the use of this index with the pluviometric Excess Danger index (IPP) developed at regional level. The results obtained show close concordance between these indices for temporal estimations. Spatial analyzes highlight the role of slopes' orientation in distributing the pluviometric Excess Danger index and slopes' degree of inclination in the case of the Fournier pluvial aggression index. The results obtained are useful in the efficient use of agricultural land and in the elaboration of measures for the improvement of degraded soils.


1996 ◽  
Vol 19 ◽  
pp. 93-114
Author(s):  
Antonio José Teixeira Guerra ◽  
Rosangela Garrido Machado Botelho

This paper regards the role of soil characteristics and properties on pedological surveys and soil erosion investigations. Therefore, the main factors of soil formation are here discussed. Furthermore, the main chemical and physical soil properties are also taken into consideration, in order to approach this subject. Finally, some erosion processes are also carried out, together with the main erosion forms and the environmental impacts caused by these associated processes.


1989 ◽  
Vol 65 (2) ◽  
pp. 167 ◽  
Author(s):  
Brian W. Gould ◽  
William E. Saupe ◽  
Richard M. Klemme

2020 ◽  
Vol 26 (4) ◽  
pp. 2642-2655 ◽  
Author(s):  
Zeli Tan ◽  
L. Ruby Leung ◽  
Hong‐Yi Li ◽  
Teklu Tesfa ◽  
Qing Zhu ◽  
...  

2020 ◽  
Vol 582 ◽  
pp. 124290 ◽  
Author(s):  
Jian Duan ◽  
Yao-Jun Liu ◽  
Jie Yang ◽  
Chong-Jun Tang ◽  
Zhi-Hua Shi

2016 ◽  
Vol 550 ◽  
pp. 330-336 ◽  
Author(s):  
Agata Novara ◽  
Saskia Keesstra ◽  
Artemio Cerdà ◽  
Paulo Pereira ◽  
Luciano Gristina

2020 ◽  
Author(s):  
Katharina Lehmann ◽  
Robert Lehmann ◽  
Kai Uwe Totsche

<p>The mobile inventory in soil seepage is of fundamental importance for soil development and for functioning of subsurface ecosystem compartments. The mobile inventory may encompass inorganic, organo-mineral and organics, dissolved and colloidal, but also particulate matter and microbiota. Still unknown are the conditions and factors that trigger the release and export of seepage-contained mobile matter within soil, and its translocation through the subsurface of the critical zone. Long-term and high-resolution field studies that includes the mobile particulate inventory are essentially lacking. To overcome this knowledge gap, we established long-term soil monitoring plots in the Hainich Critical Zone Exploratory (HCZE; NW-Thuringia, central Germany). Soil seepage from 22 tension-supported lysimeters in topsoil and subsoil, covering different land use (forest, pasture, cropland) in the topographic recharge area of the HCZE, was collected and analyzed by a variety of analytical methods (physico-/chemical and spectroscopic) on a regular (biweekly) and event-scale cycle. With our study we proved that substances up to a size of 50 µm are mobile in the soils. The material spectra comprised minerals, mineral-organic particulates, diverse bioparticles and biotic detritus. Atmospheric forcing was found to be the major factor triggering the translocation of the mobile inventory. Especially episodic infiltration events during hydrological winter seasons (e.g. snow melts) with high seepage volume influences seepage hydrochemistry (e.g. pH, EC) and is important for transport of mobile matter to deeper compartments. Seasonal events cause mobilization of significant amounts of OC. On average, 21% of the total OC of the seepage was particulate (>0.45 µm). Furthermore, our results suggest that the formation environment and the geopedological setting (soil group, parent rock, land use) are controlling factors for the composition and the amount of soil-born mobile inventory. Our study provides evidence for the importance of the mobile inventory fraction >0,45 µm for soil element dynamics and budgets and highlights the role of weather events on soil and subsoil development and subsurface ecosystem functioning.</p>


2015 ◽  
Vol 32 (3) ◽  
pp. 220-226 ◽  
Author(s):  
Levin Kuhlmann ◽  
David B. Grayden ◽  
Fabrice Wendling ◽  
Steven J. Schiff

Sign in / Sign up

Export Citation Format

Share Document