Determination Of Plant Available Soil Water Storage In Agricultural Land Of The Nitra River Catchment

Andrej Tárník, D. Igaz
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引用次数: 1

Abstract

Abstract Soil water storage and its spatial pattern is one of the biggest tasks in agricultural field of study. Correct spatial interpretation and quantification of soil water storage are considered crucial for correct hydrological zonation of agricultural lands. This paper is focused on determination of amount of plants available soil water in the Nitra River Catchment in 2013. Available soil water storage was computed for each quarter of the year (I.–IV.; V.–VIII.; IX.–XII.) for 60 cm soil horizon. Amount of available water was determined as a difference between actual soil moisture and hydrolimits of water availability. Actual soil moisture was interpolated from point’s values from net of hydrological stations in the Nitra River Catchment. Limited water availability was calculated by retention curves from soil samples taken in the Catchment. Available soil water storage was the highest in the first quarter (36.74 mm). In the second quarter, it decreased to 26.93 mm and in the third quarter it was only 4.11 mm. In the fourth quarter, it increased to 30.13 mm.
尼特拉河流域农田植物有效土壤储水量的测定
土壤水分储存及其空间格局是农业领域研究的重要课题之一。正确的空间解译和土壤储水量量化被认为是正确的农业用地水文区划的关键。本文对2013年尼特拉河流域植物有效土壤水分进行了测定。计算了一年中每个季度的有效土壤储水量(i - iv);V.-VIII。),适用于60厘米土层。有效水量由土壤实际湿度与水分有效限度之间的差值确定。实际土壤湿度由尼特拉河流域水文站网的点值插值得到。有限的水可用性是通过在集水区采集的土壤样本的保留曲线来计算的。有效土壤储水量在第一季度最高(36.74 mm)。第二季度下降到26.93毫米,第三季度仅为4.11毫米。第四季度增加到30.13毫米。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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