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Soil moisture spatial variability in experimental areas of central Italy

机译:意大利中部实验区土壤水分的空间变异性

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The knowledge of soil moisture spatial variability is an important issue for hydrological and climatic studies. This paper investigates the soil moisture spatial pattern obtained from spot measurements carried out in different experimental plots Located in small basins of Central Italy. The near-surface volumetric soil moisture content was measured using a portable time domain reflectometer (TDR) over regular grids whose areas ranging in extension from 9 to 8800 m 2. The sampling in each site was periodically repeated in order to investigate the moisture pattern as function of wetness conditions. The statistical properties of the measurements and the relation of the statistical parameters with the field-mean soil moisture content were analyzed. The results states that the probability distribution can be assumed normal for soil moisture in flat areas and for normalized soil moisture in gentle slope areas. A general decreasing trend of variance with increasing mean moisture content was observed. Moreover, considering the relationship between the field-mean water content and the coefficient of variation an optimal measurements number ranging from 15 to 35, in the worse case, was found for the study areas. The higher number was required for the site with more significant relief. These results were also confirmed through the geostatistical analysis and the correlation with the topographical attributes. Specifically, the correlation lengths were found increasing with the mean areal slope and the mean drainage direction and ranging between 10 and 15 m. This is corroborated through geostatistical analysis showing that the natural logarithm of the specific upstope area was the best spatial predictor for near-surface soil moisture when the water volume in the soil is higher. On this basis, the surface and subsurface lateral redistribution of water can be surmised fundamental in spatial organization of soil moisture. (c) 2006 Elsevier B.V. All rights reserved.
机译:土壤水分空间变异性的知识是水文和气候研究的重要课题。本文研究了从位于意大利中部小盆地的不同实验区进行的现场测量获得的土壤水分空间格局。使用便携式时域反射仪(TDR)在面积从9到8800 m 2的规则网格上测量近地表土壤水分含量。定期调查每个站点的采样,以调查水分分布图。湿度条件的函数。分析了测量的统计特性以及统计参数与田间平均土壤含水量的关系。结果表明,对于平坦区域的土壤水分和在平缓坡度区域的标准化土壤水分,可以假定概率分布为正态。观察到随着平均水分含量增加,方差总体下降的趋势。此外,考虑到田间平均水含量和变异系数之间的关系,在研究区域发现了最坏情况下的最佳测量值,范围是15到35。需要更大数量救济的地点更多。这些结果也通过地统计学分析以及与地形属性的相关性得到了证实。具体而言,发现相关长度随平均面积斜率和平均排水方向而增加,范围在10至15 m之间。地统计学分析证实了这一点,该分析表明,当土壤中的水量较高时,特定上冲区的自然对数是近地表土壤水分的最佳空间预测指标。在此基础上,可以推测水的表面和地下横向重新分布是土壤水分空间组织的基础。 (c)2006 Elsevier B.V.保留所有权利。

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