中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Statistical Determination of Rainfall-Runoff Erosivity Indices for Single Storms in the Chinese Loess Plateau

文献类型:SCI/SSCI论文

作者Zheng M. G.; Chen, X. A.
发表日期2015
关键词flow-sediment relationship hilly areas hyperconcentrated flow interrill erosion soil-erosion steep slopes climate yield river
英文摘要Correlation analysis is popular in erosion-or earth-related studies, however, few studies compare correlations on a basis of statistical testing, which should be conducted to determine the statistical significance of the observed sample difference. This study aims to statistically determine the erosivity index of single storms, which requires comparison of a large number of dependent correlations between rainfall-runoff factors and soil loss, in the Chinese Loess Plateau. Data observed at four gauging stations and five runoff experimental plots were presented. Based on the Meng's tests, which is widely used for comparing correlations between a dependent variable and a set of independent variables, two methods were proposed. The first method removes factors that are poorly correlated with soil loss from consideration in a stepwise way, while the second method performs pairwise comparisons that are adjusted using the Bonferroni correction. Among 12 rainfall factors, I-30 (the maximum 30-minute rainfall intensity) has been suggested for use as the rainfall erosivity index, although I-30 is equally correlated with soil loss as factors of I-20, EI10 (the product of the rainfall kinetic energy, E, and I-10), EI20 and EI30 are. Runoff depth (total runoff volume normalized to drainage area) is more correlated with soil loss than all other examined rain-fall-runoff factors, including I-30, peak discharge and many combined factors. Moreover, sediment concentrations of major sediment-producing events are independent of all examined rainfall-runoff factors. As a result, introducing additional factors adds little to the prediction accuracy of the single factor of runoff depth. Hence, runoff depth should be the best erosivity index at scales from plots to watersheds. Our findings can facilitate predictions of soil erosion in the Loess Plateau. Our methods provide a valuable tool while determining the predictor among a number of variables in terms of correlations.
出处Plos One
10
3
收录类别SCI
语种英语
ISSN号1932-6203
源URL[http://ir.igsnrr.ac.cn/handle/311030/39079]  
专题地理科学与资源研究所_历年回溯文献
推荐引用方式
GB/T 7714
Zheng M. G.,Chen, X. A.. Statistical Determination of Rainfall-Runoff Erosivity Indices for Single Storms in the Chinese Loess Plateau. 2015.

入库方式: OAI收割

来源:地理科学与资源研究所

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