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Accession Number:
ADA399589
Title:
Capillary Tension in Rotting Ice Layers
Descriptive Note:
Technical rept.
Corporate Author:
ENGINEER RESEARCH AND DEVELOPMENT CENTER HANOVER NH COLD REGIONS RESEARCH AND ENGINEERING LAB
Report Date:
2001-09-01
Pagination or Media Count:
21.0
Abstract:
This study examines the moisture tension constituent relationship of ice near 0 C by measuring its moisture characteristic curve. In this novel approach, we held ice samples in a Tempe cell submerged in a cold bath and removed water from the ice veins through incremental increases in air pressure. Observed air entry and water re-entry pressures generally support an idealized flow path model of alternating vein segments and nodes. Re-entry of water into the air-filled ice samples occurred slowly over a period of weeks, suggesting low permeabilities on the order of 1 x 10-18 m2. We conclude that ice desaturates and rewets in a manner similar to soils, with entry pressures on the order of silts.
Distribution Statement:
APPROVED FOR PUBLIC RELEASE