Abstract
Hydraulic conductivities of Houston Black clay were measured in relatively large undisturbed cores, and in small disturbed cores. Conductivities averaged about 2. 5 cm/day for the field basins but were about 10 times less for the core samples. Using water tagged with fluorescein to displace deionized water in an undisturbed core, pores in distinctive isolated areas were found to be conducting most of the water.
Cite
CITATION STYLE
APA
Ritchie, J. T., Kissel, D. E., & Burnett, E. (1972). WATER MOVEMENT IN UNDISTURBED SWELLING CLAY SOIL. Soil Sci Soc Am Proc, 36(6), 874–879. https://doi.org/10.2136/sssaj1972.03615995003600060015x
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