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The temporal variation of farmland soil surface roughness with various initial surface states under natural rainfall conditions

机译:自然降雨条件下具有各种初始表面状态的农田土壤表面粗糙度的时间变化

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摘要

Soil surface roughness not only affects the hydrological and erosive behavior of soils, but also influences their spectral reflectivity in the optical and microwave bands. Field measurement of soil surface roughness is time-consuming, laborious, costly, and, for vegetated areas, impractical. We attempt to find a method to predict the dynamics of soil surface roughness for various soil surface states for black soils in Northeast China. In this study, four soil surfaces with different roughness were designed, and three kinds of roughness parameters, root-mean square height (rmsh), correlation length (cl) and rmsh/c1, of each soil surface were measured. The results of soil surface roughness were as follows: (1) a decrease over time was observed for rmsh and rmsh/cl as well as an increase in cl over time; (2) an exponential relationship was confirmed between roughness parameters (rmsh, c1, and rmsh/c1) and cumulative rainfall (CR) for soil plots without ridge, as well as for the relative change (RC) of roughness parameters and CR; (3) a significant difference in change of soil surface roughness with CR existed for soil surfaces with ridge and without ridge, and a Gaussian function was more suitable for describing the dependence of soil roughness evolution on CR than an exponential function. These results indicate that the temporal change of soil surface roughness in the black soil of Northeast China could be predicted by CR based on the empirical relationship achieved in this study regardless of whether soil surface has a ridge and of different initial roughness.
机译:土壤表面粗糙度不仅影响土壤的水文和腐蚀行为,而且影响光学和微波带中的光谱反射率。土壤表面粗糙度的田间测量是耗时,费力,昂贵的,并且对于植被领域,不切实际。我们试图找到一种方法来预测东北地区黑土的各种土壤面积状态的土壤表面粗糙度动态。在本研究中,设计了四种具有不同粗糙度的土壤表面,并测量了三种粗糙度参数,根平均正方形高度(RMSH),每个土壤表面的相关长度(CL)和RMSH / C1。土壤表面粗糙度的结果如下:(1)对于RMSH和RMSH / CL以及RMSH / CL的增加,随着时间的推移增加,观察到随时间的减少; (2)在没有脊的粗糙度参数(RMSH,C1和RMSH / C1)和累积降雨(CR)之间证实了指数关系,以及粗糙度参数的相对变化(RC)和CR; (3)用脊和没有脊的土壤表面的土壤表面粗糙度变化变化的显着差异,高斯函数更适合于描述土壤粗糙度进化对CR而不是指数函数的依赖性。这些结果表明,基于本研究中实现的实证关系,CR可以预测东北地区黑土的土壤表面粗糙度的时间变化,无论土壤表面是否具有脊和不同的初始粗糙度。

著录项

  • 来源
    《Polish Journal of Soil Science》 |2016年第1期|共10页
  • 作者单位

    Chinese Acad Sci Northeast Inst Geog &

    Agroecol Changchun 130102 Peoples R China;

    Chinese Acad Sci Northeast Inst Geog &

    Agroecol Changchun 130102 Peoples R China;

    Chinese Acad Sci Northeast Inst Geog &

    Agroecol Changchun 130102 Peoples R China;

    Northeast Normal Univ Sch Geog Sci Changchun 130024 Peoples R China;

    Chinese Acad Sci Northeast Inst Geog &

    Agroecol Changchun 130102 Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 农业科学;
  • 关键词

    Soil surface roughness; Rainfall; Farmland;

    机译:土壤表面粗糙度;降雨;农田;

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