Journal
GEODERMA
Volume 160, Issue 3-4, Pages 579-589Publisher
ELSEVIER SCIENCE BV
DOI: 10.1016/j.geoderma.2010.11.006
Keywords
Sorptivity; Hydrophobicity; Air encapsulation; Early-time infiltration; Lysimeter; Tension infiltrometer
Categories
Funding
- AgMardt
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Accurate measurement of infiltration attributes for the soil's surface layer is critical for understanding the dynamics of soil water in response to rainfall or irrigation. This study used four large lysimeters to measure the early-time infiltration behaviour of a structured, well-drained, silt loam Dystric Cambisol. For each lysimeter there were four separate infiltration experiments, with a 480-mm-diameter tension infiltrometer used to supply infiltrating water under suctions of 0, 0.5, 1, and 1.5 kPa. We consistently observed a lack of clear sorptivity-driven infiltration behaviour for all lysimeters under all surface-imposed suctions. Having ruled out artefacts of the tension infiltrometer-lysimeter system, surface seal development, air confinement, and a limited 'infiltration capacity' of the soil's top 50 mm layer, we conclude that direct and indirect effects of weak hydrophobicity and air encapsulation are the most important controls. Hydrophobicity, which appears to restrict the first 5-10 mm of infiltration, occurs despite the soils being close to field capacity. During unsaturated infiltration some macropores are non-fillable to infiltrating water, and we suggest that these pores may also act to isolate parts of the Pore network that could otherwise exhibit sorptivity, and thus restrict early-time infiltration. The interaction between hydrophobicity and the non-fillable pore network may be an important mechanism causing non-uniform infiltration through preferential flowpaths. This may enhance air encapsulation by effectively blocking the escape path for the displaced air from parts of the pore network, further restricting the expression of sorptivity. In this sense the early-time infiltration behaviour of this soil is seen to be governed by the dynamic interaction between sorptivity, hydrophobicity, the network of air-filled pores, preferential flow and air encapsulation. (C) 2010 Elsevier BV. All rights reserved.
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