Magnitude of Annual Soil Loss from a Hilly Cultivated Slope in Northern Vietnam and Evaluation of Factors Controlling Water Erosion

A soil erosion experiment was conducted in northern Vietnam over three rainy seasons to clarify the magnitude of soil loss and factors controlling water erosion. The plot had a low (8%) or medium (14.5%) slope with land-cover of cassava or morning glory or being bare. Annual soil loss (177 to 2,361 ...

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Main Authors: Kiyoshi Kurosawa, Nguyen Hai Do, Tat Canh Nguyen, Kazuhiko Egashira
Format: Article
Language:English
Published: Hindawi Limited 2009-01-01
Series:Applied and Environmental Soil Science
Online Access:http://dx.doi.org/10.1155/2009/464767
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spelling doaj-7416b702aaa842aeb815f97c5677680f2020-11-24T23:24:08ZengHindawi LimitedApplied and Environmental Soil Science1687-76671687-76752009-01-01200910.1155/2009/464767464767Magnitude of Annual Soil Loss from a Hilly Cultivated Slope in Northern Vietnam and Evaluation of Factors Controlling Water ErosionKiyoshi Kurosawa0Nguyen Hai Do1Tat Canh Nguyen2Kazuhiko Egashira3Institute of Tropical Agriculture, Kyushu University, Fukuoka 812-8581, JapanFaculty of Natural Resources and Environment, Hanoi University of Agriculture, Hanoi, VietnamFaculty of Natural Resources and Environment, Hanoi University of Agriculture, Hanoi, VietnamFaculty of Agriculture, Kyushu University, Fukuoka 812-8581, JapanA soil erosion experiment was conducted in northern Vietnam over three rainy seasons to clarify the magnitude of soil loss and factors controlling water erosion. The plot had a low (8%) or medium (14.5%) slope with land-cover of cassava or morning glory or being bare. Annual soil loss (177 to 2,361 g/m2) was a tolerable level in all low-slope plots but was not in some medium-slope plots. The effects of slope gradient and seasonal rainfall on the mean daily soil loss of the season were confirmed, but the effect of land-cover was not, owing to the small canopy cover ratio or leaf area index during the season. The very high annual soil loss (>2,200 g/m2) observed in the first year of some medium-slope plots was the site-specific effect from initial land preparation. Since the site-specific effect was large, the preparation must be done carefully on the slope.http://dx.doi.org/10.1155/2009/464767
collection DOAJ
language English
format Article
sources DOAJ
author Kiyoshi Kurosawa
Nguyen Hai Do
Tat Canh Nguyen
Kazuhiko Egashira
spellingShingle Kiyoshi Kurosawa
Nguyen Hai Do
Tat Canh Nguyen
Kazuhiko Egashira
Magnitude of Annual Soil Loss from a Hilly Cultivated Slope in Northern Vietnam and Evaluation of Factors Controlling Water Erosion
Applied and Environmental Soil Science
author_facet Kiyoshi Kurosawa
Nguyen Hai Do
Tat Canh Nguyen
Kazuhiko Egashira
author_sort Kiyoshi Kurosawa
title Magnitude of Annual Soil Loss from a Hilly Cultivated Slope in Northern Vietnam and Evaluation of Factors Controlling Water Erosion
title_short Magnitude of Annual Soil Loss from a Hilly Cultivated Slope in Northern Vietnam and Evaluation of Factors Controlling Water Erosion
title_full Magnitude of Annual Soil Loss from a Hilly Cultivated Slope in Northern Vietnam and Evaluation of Factors Controlling Water Erosion
title_fullStr Magnitude of Annual Soil Loss from a Hilly Cultivated Slope in Northern Vietnam and Evaluation of Factors Controlling Water Erosion
title_full_unstemmed Magnitude of Annual Soil Loss from a Hilly Cultivated Slope in Northern Vietnam and Evaluation of Factors Controlling Water Erosion
title_sort magnitude of annual soil loss from a hilly cultivated slope in northern vietnam and evaluation of factors controlling water erosion
publisher Hindawi Limited
series Applied and Environmental Soil Science
issn 1687-7667
1687-7675
publishDate 2009-01-01
description A soil erosion experiment was conducted in northern Vietnam over three rainy seasons to clarify the magnitude of soil loss and factors controlling water erosion. The plot had a low (8%) or medium (14.5%) slope with land-cover of cassava or morning glory or being bare. Annual soil loss (177 to 2,361 g/m2) was a tolerable level in all low-slope plots but was not in some medium-slope plots. The effects of slope gradient and seasonal rainfall on the mean daily soil loss of the season were confirmed, but the effect of land-cover was not, owing to the small canopy cover ratio or leaf area index during the season. The very high annual soil loss (>2,200 g/m2) observed in the first year of some medium-slope plots was the site-specific effect from initial land preparation. Since the site-specific effect was large, the preparation must be done carefully on the slope.
url http://dx.doi.org/10.1155/2009/464767
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