The method of obtaining soil's water-physical properties via their a granulometric composition

V. Kovalchuk
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Abstract

The method of obtaining water-physical properties of soils (basic hydrophysical characteristics (BHC) and moisture conductivity function) is presented. These properties, or functions, allow us to describe the vertical movement of moisture in unsaturated soils as one of the components of the expenditure item of the water balance. They are widely used in the substantiation of water reclamation and in the modeling of moisture transfer in the soil. The method is based on laboratory studies of soil samples taken in the field on the granulometry composition. The results of laboratory test now in Ukraine are usually obtained by the method of Kaczynski with two components, the percentage of clay and sand. They are graphically, with the help of integral (cumulative) curves are transformed into data corresponding to the international classification - with three components: the content of sand, dust, clay. The latter fractional distribution is used by the world community of soil scientists. Therefore, using data on the content of sand, silt, clay, using a computer program with open access "Rosetta" USDA (United States Department of Agriculture) the water-physical properties in the form of water constants: the saturated soil moisture, the residual soil moisture, the saturated hydraulic conductivity, and the coefficients of the equations of the mathematical model of van Genuchten are calculated. The publication provides examples of calculation of water-physical properties of soils by the presented method of dark chestnut soils and ordinary chernozems. The advantages of the proposed method include the low complexity of experimental studies, the availability of analyzes and the presence of many experimental studies of the granulometry composition of soils, including in literary sources. As a development of the research direction, the author shows the application of the obtained dependence for modeling moisture transfer during water reclamation (irrigation in irrigation control systems.). Regarding the directions of future research, the publication recommends comparing the accuracy of obtaining water-physical properties of soils by different methods, as well as obtaining an important water constant - the field capacity (FC) as the lowest field moisture content.
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通过土壤的颗粒组成来获得土壤水物理性质的方法
提出了获取土壤水物理性质(基本水物理特性和水分传导性函数)的方法。这些性质或功能使我们能够将非饱和土壤中水分的垂直运动描述为水平衡支出项目的一个组成部分。它们被广泛应用于水回收的确证和土壤中水分转移的模拟。该方法是基于对田间土壤样品的粒度组成进行实验室研究。现在乌克兰的实验室测试结果通常采用卡钦斯基法,用粘土和沙子的百分比两种成分来获得。在积分(累积)曲线的帮助下,它们被图形化地转换成与国际分类相对应的数据-有三个组成部分:沙子,灰尘,粘土的含量。后一种分数分布被世界土壤科学家所使用。因此,利用砂、粉、粘土含量的数据,利用美国农业部(USDA)开放的“Rosetta”计算机程序,以水常数的形式计算了水的物理性质:饱和土壤水分、残余土壤水分、饱和水导率,以及van Genuchten数学模型方程的系数。该出版物提供了用黑栗子土和普通黑钙土所提出的方法计算土壤水物理性质的例子。所提出的方法的优点包括实验研究的低复杂性,分析的可用性和土壤颗粒组成的许多实验研究的存在,包括文献来源。作为研究方向的发展,作者展示了所获得的依赖关系在灌溉控制系统中水回收(灌溉)过程中水分转移建模中的应用。关于未来的研究方向,该出版物建议比较不同方法获得土壤水物理性质的准确性,以及获得一个重要的水常数——田间容量(FC)作为最低的田间含水量。
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