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The field water regime in a deformable sub-irrigated peat-moorsh soil profile

机译:可变形亚灌溉泥炭泥土剖面处的现场水域

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The paper presents the results of analysis of the soil water regime in a deep fen peat-moorsh soil located in the Middle Biebrza Basin (Poland) within the Kuwasy drainage sub-irrigation system used as permanent grassland.The observed values for pressure head,moisture content and groundwater level show that the required water conditions were present in the root zone of grasslands even during dry periods with low sums of precipitation in June and July 2006.Changes in the soil surface level of up to 42 mm were also observed during the period considered.
机译:本文介绍了位于植物盆地(波兰)的深芬泥炭土壤中土壤水域的分析结果,该灌溉亚灌区灌溉系统用作永久草地。压力头,水分的观测值含量和地下水位表明,即使在6月和2006年7月的降水量低和的降水量的干燥期间,也存在所需的水条件。在期间,在期间也观察到较高42毫米的土壤表面水平高达42毫米的凸缘。经过考虑的。

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