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Effects of slope gradient on runoff from bare-fallow purple soil in China under natural rainfall conditions

机译:自然降雨条件下坡度对裸露紫色土壤径流的影响

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摘要

Purple soil is highly susceptible for overland flow and surface erosion,therefore understanding surface runoff and soil erosion processes in the purple soil region are important to mitigate flooding and erosion hazards.Slope angle is an important parameter that affects the magnitude of runoff and thus surface erosion in hilly landscapes or bare land area.However,the effect of slope on runoff generation remains unclear in many different soils including Chinese purple soil.The aim of this study was to investigate the relationship between different slope gradients and surface runoff for bare-fallow purple soil,using 5 m × 1.5 m experimental plots under natural rainfall conditions.Four experimental plots (10°,16°,20° and 26°) were established in the Yanting Agro-ecological Experimental Station of Chinese Academy of Science in central Sichuan Basin.The plot was equipped with water storage tank to monitor water level change.Field monitoring from July 1 to October 31,2012 observed 42 rainfall events which produced surface runoff from the experimental plots.These water level changes were converted to runoff.The representative eight rainfall events were selected for further analysis,the relationship between slope and runoff coefficient were determined using ANOVA,F-test,and z-score analysis.The results indicated a strong correlation between rainfall and runoff in cumulative amount basis.The mean value of the measured runoff coefficient for four experimental plots was around 0.1.However,no statistically significant relationship was found between slope and runoff coefficient.We reviewed the relationship between slope and runoff in many previous studies and calculated z-score to compare with our experimental results.The results of z-score analysis indicated that both positive and negative effects of slope on runoff coefficient were obtained,however a moderate gradient (16°-20° in this study) could be a threshold of runoff generation for many different soils including the Chinese purple soil.
机译:紫色土极易受到陆上径流和地表侵蚀的影响,因此了解紫色土区的地表径流和土壤侵蚀过程对于减轻洪水和水土流失危害非常重要。坡度角是影响径流大小和地表侵蚀程度的重要参数然而,在包括中国紫色土壤在内的许多不同土壤中,坡度对径流产生的影响仍不清楚。本研究的目的是研究裸露淡紫色的不同坡度梯度与地表径流之间的关系。土壤,在自然降雨条件下使用5 m×1.5 m的试验区。在中国科学院四川盆地中部盐亭农业生态试验站建立了四个试验区(10°,16°,20°和26°)该样地装有储水罐以监测水位变化.2012年7月1日至10月31日的现场监测发现有42处降雨从试验区产生地表径流的事件。将这些水位变化转换为径流。选择代表性的八种降雨事件进行进一步分析,使用ANOVA,F检验和z分数确定坡度与径流系数之间的关系。结果表明,降雨与径流量以累积量为基础有很强的相关性。四个试验区测得的径流系数的平均值约为0.1,但在坡度与径流系数之间没有统计学意义的相关性。先前许多研究中的斜率与径流量之间的关系以及计算的z分数与我们的实验结果进行比较。z分数分析的结果表明,坡度对径流系数具有正向和负向影响,但存在中等梯度(16°在本研究中为-20°)可能是许多不同土壤(包括中国)的径流产生的阈值紫色土。

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  • 来源
    《山地科学学报(英文版)》 |2018年第4期|738-751|共14页
  • 作者单位

    Graduate School of Life and Environmental Sciences, University of Tsukuba, 1-1-1 Tennodai, Tsukuba, Ibaraki 305-8572, Japan;

    Center for Research in Isotopes and Environmental Dynamics, University of Tsukuba, 1-1-1 Tennodai, Tsukuba, Ibaraki 305-8572, Japan;

    Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, No.9, Block 4, Renminnan Road,Chengdu 610041, China;

    Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, No.9, Block 4, Renminnan Road,Chengdu 610041, China;

    Graduate School of Life and Environmental Sciences, University of Tsukuba, 1-1-1 Tennodai, Tsukuba, Ibaraki 305-8572, Japan;

    Faculty of Health and Sport Sciences, University of Tsukuba, 1-1-1 Tennodai, Tsukuba, Ibaraki 305-8574, Japan;

    Center for Research in Isotopes and Environmental Dynamics, University of Tsukuba, 1-1-1 Tennodai, Tsukuba, Ibaraki 305-8572, Japan;

  • 收录信息 中国科学引文数据库(CSCD);中国科技论文与引文数据库(CSTPCD);
  • 原文格式 PDF
  • 正文语种 eng
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