导水率
堆积密度
土壤科学
渗透(HVAC)
环境科学
黄土
Pedotransfer函数
土壤水分
水文学(农业)
地质学
材料科学
岩土工程
地貌学
复合材料
作者
Roya Jafari,Vahedberdi Sheikh,Mohsen Hosseinalizadeh,Hasan Rezaii-Moghadam
标识
DOI:10.1080/00103624.2017.1323086
摘要
Saturated hydraulic conductivity (Ksat) is regarded as a key soil physical variable to determine soil infiltration rate, percolation depth and other hydrological processes. The purpose of this study was to determine the best soil sampling's ring size for measuring Ksat. For this purpose, 25 rings with five different diameters (2, 3, 4, 5 and 6 inch) and with the same depth of 20 cm (five replicates) were hammered in close vicinity to each other into the ground of undisturbed loess deposits of a small farm to measure Ksat and bulk density. Hydraulic conductivity was measured at three constant loads of 22, 27 and 32 cm. The results showed that the ring with the internal diameter of 6 inches had the minimum variation coefficient and maximum Ksat for all the three hydraulic heads. In addition, the bulk density of this ring size was less than the other rings.
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