Abstract

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?m3/m3, PWP?=?0.068?m3/m3, and AW?=?0.140?m3/m3 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?m3/m3, PWP?=?0.184?m3/m3, and AW?=?0.071?m3/m3 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.

Highlights

  • This work introduces a new methodology for calculating the field capacity (FC), Permanent Wilting Point (PWP), and available (AW), using the soil aggregates structure instead of soil texture

  • 2 Macro-pore region, representing the pore volume and structure outside the primary peds. It may contain two types of water: (a) non-swelling macro-water, known as macro-water content (Wma), and (b) swelling macro-water or interpedal water content (Wip), which corresponds to the interpedal saturation shrinkage phase of the shrinkage curve

  • This work builds on the work of Assi et al [3] and Braudeau et al [2] to develop a methodology for calculating the FC, permanent wilting point (PWP), and available water (AW)

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Summary

Method Article

Soil pedostructure-based method for calculating the soil-water holding properties. Mohtara,b,c, Erik Braudeaua a Department of Biological and Agricultural Engineering, Texas A&M University, College Station, TX 778432117, USA b Zachry Department of Civil Engineering, Texas A&M University, College Station, TX 77843-2117, USA c Faculty of Agricultural and Food Sciences, American University of Beirut, Beirut 1107 2020, Lebanon

Method details
Materials and methods
FAO Method
Full Text
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