Pedotransfer函数
土壤质地
导水率
渗透(HVAC)
环境科学
土壤科学
水文学(农业)
浸出模型
堆积密度
土壤盐分
土壤水分
地质学
岩土工程
材料科学
复合材料
作者
K. E. Saxton,W. J. Rawls
标识
DOI:10.2136/sssaj2005.0117
摘要
Hydrologic analyses often involve the evaluation of soil water infiltration, conductivity, storage, and plant‐water relationships. To define the hydrologic soil water effects requires estimating soil water characteristics for water potential and hydraulic conductivity using soil variables such as texture, organic matter (OM), and structure. Field or laboratory measurements are difficult, costly, and often impractical for many hydrologic analyses. Statistical correlations between soil texture, soil water potential, and hydraulic conductivity can provide estimates sufficiently accurate for many analyses and decisions. This study developed new soil water characteristic equations from the currently available USDA soil database using only the readily available variables of soil texture and OM. These equations are similar to those previously reported by Saxton et al. but include more variables and application range. They were combined with previously reported relationships for tensions and conductivities and the effects of density, gravel, and salinity to form a comprehensive predictive system of soil water characteristics for agricultural water management and hydrologic analyses. Verification was performed using independent data sets for a wide range of soil textures. The predictive system was programmed for a graphical computerized model to provide easy application and rapid solutions and is available at http://hydrolab.arsusda.gov/soilwater/Index.htm
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