Assi Amjad T, Mohtar Rabi H, Braudeau Erik
Department of Biological and Agricultural Engineering, Texas A&M University, College Station, TX 77843-2117, USA.
Zachry Department of Civil Engineering, Texas A&M University, College Station, TX 77843-2117, USA.
MethodsX. 2018 Aug 18;5:950-958. doi: 10.1016/j.mex.2018.08.006. eCollection 2018.
Soil aggregates structure (pedostructure) plays a pivotal role in regulating water and nutrient circulation, and consequently defines soil health, productivity, and water use efficiency. However, the soil aggregates structure is not currently considered in the quantification of soil-water holding properties. The authors applied a thermodynamic and soil structure-based approach to quantify soil-water holding properties. The paper provides a methodology, based on pedostructure concept, to quantify field capacity (FC), permanent wilting point (PWP), and available water (AW). The validity of the developed method was tested through application to two types of soil: a loamy fine sand soil and a silt loam soil. The calculated values for FC, PWP, and AW were compared with the FAO recommended values of FC, PWP and AW. For the loamy fine sand, the calculated values were: FC = 0.208 m/m, PWP = 0.068 m/m, and AW = 0.140 m/m all of which fall within the recommended values of FAO for such a soil type. Similarly, the calculated values for the silt loam were: FC = 0.283 m/m, PWP = 0.184 m/m, and AW = 0.071 m/m all were in agreement with the FAO recommended ranges for such a soil type. •A thermodynamic, structure-based approach for soil water holding properties.•Unique solutions for quantifying both field capacity and permanent wilting point.
土壤团聚体结构(土壤结构)在调节水分和养分循环方面起着关键作用,进而决定了土壤健康状况、生产力和水分利用效率。然而,目前在土壤持水特性的量化中并未考虑土壤团聚体结构。作者采用了一种基于热力学和土壤结构的方法来量化土壤持水特性。本文提供了一种基于土壤结构概念的方法,用于量化田间持水量(FC)、永久凋萎点(PWP)和有效水分(AW)。通过应用于两种土壤类型(壤质细砂土和粉质壤土)对所开发方法的有效性进行了测试。将计算得到的FC、PWP和AW值与粮农组织推荐的FC、PWP和AW值进行了比较。对于壤质细砂土,计算值为:FC = 0.208 m/m,PWP = 0.068 m/m,AW = 0.140 m/m,所有这些值均落在粮农组织针对此类土壤类型推荐的值范围内。同样,粉质壤土的计算值为:FC = 0.283 m/m,PWP = 0.184 m/m,AW = 0.071 m/m,所有这些值均与粮农组织针对此类土壤类型推荐的范围一致。•一种基于热力学和结构的土壤持水特性方法。•量化田间持水量和永久凋萎点的独特解决方案。