农田土壤含水量空间分布影响因子的时间依赖性研究

D. Jacques , B. Mohanty , A. Timmerman , J. Feyen
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引用次数: 23

摘要

土壤含水量的时空变异是降雨持续时间和频率、土壤分层、植被和地形等不同因素复杂相互作用的结果。本研究的目的是:(i)使用一种抗阻力的中间抛光方案来量化加性模型中深度和水平位置因素的时间变化,以及(ii)在不同的渗透和再分布周期中,在详细的时间尺度上研究这两个因素的时间稳定性。利用时域反射仪(TDR)测量了沿6 m样带在5个深度和12个位置的时间序列含水量。在自然边界条件下,每2小时重复测量一次,持续168天。在每个时间步,估算了土壤剖面的平均含水量、5个深度因子和12个位置因子。对这些因子的时间序列进行了定性解释,并与大气和盛行土壤条件有关。研究发现,即使在如此小的情节尺度下,微观异质性也起着重要作用。各因子的相对贡献取决于前一土壤湿度条件。此外,含水量的确定性方差,即由确定性因素解释的方差,与观测方差的比值随时间变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study of time dependency of factors affecting the spatial distribution of soil water content in a field-plot

Temporal and spatial variability of water content in soil results from a complex interaction of different factors such as duration and frequency of rainfall, soil layering, vegetation, and topography. The objectives of this study were (i) to use a resistant median-polishing scheme to quantify the temporal variability of a depth and a horizontal location factor in an additive model, and (ii) to investigate the time stability of those two factors at a detailed temporal scale during different infiltration and redistributions cycles. Time series of water content were measured at 5 depths and 12 locations along a transect of 6 m using Time Domain Reflectometry (TDR). Measurements were repeated every 2-hours for 168 days under natural boundary conditions. At each time step, the mean water content of the soil profile, 5 depth factors and 12 location factors were estimated. The time series of these factors were qualitatively interpreted and related to the atmospheric and prevailing soil conditions. It was found that micro-heterogeneity plays an important role, even at this small plot-scale. The relative contributions of the factors were dependent on the antecedent soil moisture conditions. Also, the ratio of the deterministic variance, i.e., variance explained by the deterministic factors, of water content to the observed variance is variable in time.

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