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首页> 外文期刊>Communications in Soil Science and Plant Analysis >Calibration of Gypsum Blocks for Measuring Saline Soils Moisture
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Calibration of Gypsum Blocks for Measuring Saline Soils Moisture

机译:用于测量盐渍土壤水分的石膏块的标定

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摘要

The proper management of irrigation requires an accurate measuring of soil moisture. One of the commonly applied methods for measuring soil moisture is the use of gypsum blocks - a method that is simple and quick to apply. However, measuring moisture in saline soils using this method is prone to errors due to the effect of soil salinity on the block. In this study, the effect of different salinities (1, 2, 6, 10, and 18 deci Siemens per meter (dSm(-1)) on the measurements of a gypsum block type 5910 A was investigated with two repetitions in random blocks in sandy loam, loam, and clay loam soils, and corrective functions were obtained using multivariate regression for all soils with different salinity levels. The results showed different trends for measuring the soil moistures for salinities 1-6dSm(-1) compared with salinities 10-18dSm(-1), and the corrective functions in salinities 1-6dSm(-1), which had higher accuracies than those with salinities 10-18dSm(-1).
机译:适当的灌溉管理需要准确测量土壤湿度。测量土壤湿度的一种常用方法是使用石膏块,该方法简便易行。然而,由于土壤盐分对块体的影响,使用这种方法测量盐渍土壤中的水分容易产生误差。在这项研究中,研究了不同盐度(每米1、2、6、10和18分西西门子(dSm(-1))对5910 A型石膏块的测量的影响)的随机性,其中两次重复沙壤土,壤土和黏土壤土,并通过多元回归获得了所有盐度不同的土壤的校正函数,结果表明,与盐度10-相比,盐度1-6dSm(-1)的土壤水分测量趋势不同。 18dSm(-1)以及盐度为1-6dSm(-1)的校正功能,其准确度高于盐度为10-18dSm(-1)的那些。

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