Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Rain energy and soil amendments effects on infiltration and erosion of three different soil types

View through CrossRef
The effect of rain kinetic energy and soil amendments on infiltration and erosion from three Israeli soils was studied using a drip-type simulator. The soil samples were from the top layer (0-250 mm depth) of cultivated fields differing in their texture, specific surface area and lime content. Three kinetic energies of raindrops were obtained by varying heights of fall (h = 0.4, 1-0 and 1.6 m) of 3 mm diameter drops. The soil types studied were Typic Chromoxerert, Typic Rhodoxeralf and Calcic Haploxeralf. Soil amendments were phosphogypsum (PG) and a combined application of an anionic polyacrylamide (PAM) with PG. An increase in the impact energy of the raindrops reduced depth of rain before ponding, final infiltration rate (FIR), cumulative infiltration (i.e. infiltration parameters) and increased soil erosion. The addition of PAM+PG to the soil surface significantly increased the infiltration parameters and reduced erosion compared with the PG and control treatments. The Typic Chromoxerert was the least susceptible of the three soils to sealing, probably because of its high smectitic clay content, high specific surface area and high CaCO3 content which stabilize soil structure. The Typic Rhodoxeralf with the lowest specific surface area was the most susceptible to clay dispersion, and seal formation. Relative to the Typic Chromoxerert and the Typic Rhodoxeralf, the Calcic Haploxeralf was intermediate in its susceptibility to seal formation.
Title: Rain energy and soil amendments effects on infiltration and erosion of three different soil types
Description:
The effect of rain kinetic energy and soil amendments on infiltration and erosion from three Israeli soils was studied using a drip-type simulator.
The soil samples were from the top layer (0-250 mm depth) of cultivated fields differing in their texture, specific surface area and lime content.
Three kinetic energies of raindrops were obtained by varying heights of fall (h = 0.
4, 1-0 and 1.
6 m) of 3 mm diameter drops.
The soil types studied were Typic Chromoxerert, Typic Rhodoxeralf and Calcic Haploxeralf.
Soil amendments were phosphogypsum (PG) and a combined application of an anionic polyacrylamide (PAM) with PG.
An increase in the impact energy of the raindrops reduced depth of rain before ponding, final infiltration rate (FIR), cumulative infiltration (i.
e.
infiltration parameters) and increased soil erosion.
The addition of PAM+PG to the soil surface significantly increased the infiltration parameters and reduced erosion compared with the PG and control treatments.
The Typic Chromoxerert was the least susceptible of the three soils to sealing, probably because of its high smectitic clay content, high specific surface area and high CaCO3 content which stabilize soil structure.
The Typic Rhodoxeralf with the lowest specific surface area was the most susceptible to clay dispersion, and seal formation.
Relative to the Typic Chromoxerert and the Typic Rhodoxeralf, the Calcic Haploxeralf was intermediate in its susceptibility to seal formation.

Related Results

Modeling infiltration into water repellent soil
Modeling infiltration into water repellent soil
Infiltration is an important hydrological process impacting ecology, forestry, agronomy, civil- and environmental engineering. Most infiltration models assume soils to be &#822...
Movement of Water Across Soils (Erosion)
Movement of Water Across Soils (Erosion)
Erosion is the physical wearing away of the land surface by running water, wind, or ice. Soil or rock is initially detached by falling water, running water, wind, ice or freezing c...
The Effect of Land Use/Cover Change on Soil Erosion Change by Spatial Regression in Changwu County on the Loess Plateau in China
The Effect of Land Use/Cover Change on Soil Erosion Change by Spatial Regression in Changwu County on the Loess Plateau in China
Changwu County is a typical soil and water loss area on the Loess Plateau. Soil erosion is an important ecological process, and the impact of land use/cover change on soil erosion ...
Two-dimensional hydrodynamic robust numerical model of soil erosion based on slopes and river basins
Two-dimensional hydrodynamic robust numerical model of soil erosion based on slopes and river basins
<div> <div> <div> <p>Erosion is an important issue in soil science and is related to many environmental problems, such as so...
ASSESSING SOIL EROSION SEVERITY IN TEMPORAL AND SPATIAL PATTERN: A CASE STUDY IN THE PLEIKU PLATEAU, GIA LAI PROVINCE
ASSESSING SOIL EROSION SEVERITY IN TEMPORAL AND SPATIAL PATTERN: A CASE STUDY IN THE PLEIKU PLATEAU, GIA LAI PROVINCE
Soil erosion is one of the major causes of land degradation and negatively impacts the soil environment in the world. There are two approaches to assessing soil erosion severity (S...
AWESOME: Archive for Water Erosion and Sediment Outflow MEasurements
AWESOME: Archive for Water Erosion and Sediment Outflow MEasurements
Abstract. Soil erosion is a major threat to soil resources, causing environmental degradation and contributing to poverty in many parts of the world. Many field experiments have be...
Integrating Remote Sensing, GIS, and AI Technologies in Soil Erosion Studies
Integrating Remote Sensing, GIS, and AI Technologies in Soil Erosion Studies
Soils are one of the most valuable non-renewable natural resources, and conserving them is critical for agricultural development and ecological sustainability because they provide ...
Ecological soil physics as section of ecological soil science
Ecological soil physics as section of ecological soil science
Nowadays, there is a general penetration of ecology in other related sciences. Soil science is not an exception. To the evidence of this, the works of soil scientists may serve, th...

Back to Top