Temperature effects on water absorption by three different porous materials
D. E. SmilesCSIRO Land and Water, PO Box 1666, Canberra, ACT 2601 Australia. Email: david.smiles@csiro.au
Australian Journal of Soil Research 43(4) 533-540 https://doi.org/10.1071/SR04121
Submitted: 13 August 2004 Accepted: 27 January 2005 Published: 30 June 2005
Abstract
Absorption of water by relatively dry soil and by chromatography paper, and desorption of water by clay, were measured at constant temperatures close to 278K, 293K, and 306K. Within experimental error, temperature affected absorption of water by soil and chromatography paper simply according to the temperature dependence of the kinematic viscosity and of the air–liquid surface tension of pure water. Desorption of water by saturated bentonite slurry, where there were no air–water interfaces, scaled simply according to the temperature effects on the kinematic viscosity of pure water.
Additional keywords: unsteady flow, temperature dependence, viscosity, surface tension.
Acknowledgments
Some of these experiments were necessary to define flow properties in soils heavily irrigated with piggery effluent. Australian Pork Ltd supported this aspect of the work.
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