The Effects of Litter Layer and Topsoil on Surface Runoff during Simulated Rainfall in Guizhou Province, China: A Plot Scale Case Study

Litter layers and topsoil have important effects on surface runoff. To investigate these effects at the plot scale, artificial rainfall experiments were conducted on micro-runoff plots in Guizhou Province, China. Three types of plots were selected, the thin litter layer with low soil bulk density ty...

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Main Authors: Qiuwen Zhou, Xu Zhou, Ya Luo, Mingyong Cai
Format: Article
Language:English
Published: MDPI AG 2018-07-01
Series:Water
Subjects:
Online Access:http://www.mdpi.com/2073-4441/10/7/915
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spelling doaj-dda929fa118a4c2c9fef221d6d42c1612020-11-25T02:34:04ZengMDPI AGWater2073-44412018-07-0110791510.3390/w10070915w10070915The Effects of Litter Layer and Topsoil on Surface Runoff during Simulated Rainfall in Guizhou Province, China: A Plot Scale Case StudyQiuwen Zhou0Xu Zhou1Ya Luo2Mingyong Cai3School of Geographic and Environmental Science, Guizhou Normal University, Guiyang 550001, ChinaSchool of Geographic and Environmental Science, Guizhou Normal University, Guiyang 550001, ChinaSchool of Geographic and Environmental Science, Guizhou Normal University, Guiyang 550001, ChinaSatellite Environment Center of MEP, Beijing 100094, ChinaLitter layers and topsoil have important effects on surface runoff. To investigate these effects at the plot scale, artificial rainfall experiments were conducted on micro-runoff plots in Guizhou Province, China. Three types of plots were selected, the thin litter layer with low soil bulk density type (T-L type), the thick litter layer with high soil bulk density type (T-H type), and the moderate litter depth and soil bulk density type (M type), and three artificial rainfall intensities (30 mm/h, 70 mm/h, 120 mm/h) were used. The runoff volume was largest in the T-H type plot at different rainfall intensities and durations. Runoff in the M type plot had characteristics of both the T-L and T-H type plots. The runoff yielding speed was significantly higher and the runoff yielding time was significantly lower in the T-H type plot. In general, the runoff coefficient was the smallest in the T-L type plot and largest in the T-H type plot. The variations in the runoff coefficient were 15.6%, 19.3%, and 5.8% for the T-L, T-H, and M type plots respectively. The results of this study can improve the understanding of surface runoff processes at the plot scale under different litter and surface soil conditions.http://www.mdpi.com/2073-4441/10/7/915runoffsimulated rainfallplot scalelitter layertopsoilkarst
collection DOAJ
language English
format Article
sources DOAJ
author Qiuwen Zhou
Xu Zhou
Ya Luo
Mingyong Cai
spellingShingle Qiuwen Zhou
Xu Zhou
Ya Luo
Mingyong Cai
The Effects of Litter Layer and Topsoil on Surface Runoff during Simulated Rainfall in Guizhou Province, China: A Plot Scale Case Study
Water
runoff
simulated rainfall
plot scale
litter layer
topsoil
karst
author_facet Qiuwen Zhou
Xu Zhou
Ya Luo
Mingyong Cai
author_sort Qiuwen Zhou
title The Effects of Litter Layer and Topsoil on Surface Runoff during Simulated Rainfall in Guizhou Province, China: A Plot Scale Case Study
title_short The Effects of Litter Layer and Topsoil on Surface Runoff during Simulated Rainfall in Guizhou Province, China: A Plot Scale Case Study
title_full The Effects of Litter Layer and Topsoil on Surface Runoff during Simulated Rainfall in Guizhou Province, China: A Plot Scale Case Study
title_fullStr The Effects of Litter Layer and Topsoil on Surface Runoff during Simulated Rainfall in Guizhou Province, China: A Plot Scale Case Study
title_full_unstemmed The Effects of Litter Layer and Topsoil on Surface Runoff during Simulated Rainfall in Guizhou Province, China: A Plot Scale Case Study
title_sort effects of litter layer and topsoil on surface runoff during simulated rainfall in guizhou province, china: a plot scale case study
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2018-07-01
description Litter layers and topsoil have important effects on surface runoff. To investigate these effects at the plot scale, artificial rainfall experiments were conducted on micro-runoff plots in Guizhou Province, China. Three types of plots were selected, the thin litter layer with low soil bulk density type (T-L type), the thick litter layer with high soil bulk density type (T-H type), and the moderate litter depth and soil bulk density type (M type), and three artificial rainfall intensities (30 mm/h, 70 mm/h, 120 mm/h) were used. The runoff volume was largest in the T-H type plot at different rainfall intensities and durations. Runoff in the M type plot had characteristics of both the T-L and T-H type plots. The runoff yielding speed was significantly higher and the runoff yielding time was significantly lower in the T-H type plot. In general, the runoff coefficient was the smallest in the T-L type plot and largest in the T-H type plot. The variations in the runoff coefficient were 15.6%, 19.3%, and 5.8% for the T-L, T-H, and M type plots respectively. The results of this study can improve the understanding of surface runoff processes at the plot scale under different litter and surface soil conditions.
topic runoff
simulated rainfall
plot scale
litter layer
topsoil
karst
url http://www.mdpi.com/2073-4441/10/7/915
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