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Characterization of the Least Limiting Water Range of Soils
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1994
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Geotechnical EngineeringSoil PropertySoil CharacterizationEngineeringSoil MechanicsCivil EngineeringAgricultural EconomicsMechanical ResistanceSoil StructureSoil Physical QualitySoil PropertiesSoil ResistanceSoil Structural FormSoil PhysicHydrologyEarth ScienceUnsaturated Soil Mechanics
Soil oxygen, water supply, and mechanical impedance are governed by soil structure, and the least limiting water range (LLWR) is the interval of soil water content where matric pressure, aeration, and mechanical resistance constraints are minimal. The study aimed to evaluate LLWR as an index of soil structural quality. Undisturbed cores from 5–10 cm depth of a silt loam and a loamy sand were analyzed for water retention, soil resistance, air‑filled porosity, and bulk density, and LLWR was calculated from predicted critical limits for each bulk density. Natural variation in bulk density produced a wide LLWR range (0–0.14 cm³ cm⁻³ for silt loam, 0.05–0.13 cm³ cm⁻³ for loamy sand), with LLWR declining sharply above bulk densities of 1.36 g cm⁻³ and 1.43 g cm⁻³, respectively.
Abstract The supplies of O 2 and water and the mechanical impedance of soil are determined by soil structural form and soil water content. The range in soil water content in which limitations for plant growth associated with matric pressure, aeration, and mechanical resistance are minimal was defined as the least limiting water range (LLWR). This study was carried out to evaluate the LLWR as an index of the structural quality of soils. Undisturbed soil cores were taken from the 5‐ to 10‐cm depth of a silt loam and a loamy sand, cropped to corn ( Zea mays L.) and red clover ( Trifolium pratense L.). Soil water retention, soil resistance, air‐filled porosity, and bulk density ( D b ) were measured. Water contents at critical limits associated with field capacity (−0.01 MPa), wilting point (−1.5 MPa), air‐filled porosity (10%), and soil resistance (2.0 MPa) were predicted and the LLWR calculated for each measured D b . The natural variation in D b on both soils gave rise to a wide variation in LLWR. Values of LLWR varied from 0 to 0.14 cm 3 cm −3 for the silt loam soil and from 0.05 to 0.13 cm 3 cm −3 for the loamy sand soil. At D b above 1.36 g cm −3 for the silt loam and 1.43 g cm −3 for the loamy sand, the LLWR declined sharply with increasing bulk density. Further research relating LLWR to crop response is required before LLWR can be recommended as a soil structural quality index for crop production.