A tensiometer for measuring hydraulic potentials on surfaces of porous rock
- 1 June 1997
- journal article
- Published by American Geophysical Union (AGU) in Water Resources Research
- Vol. 33 (6) , 1509-1513
- https://doi.org/10.1029/97wr00474
Abstract
A laboratory method for obtaining tensiometer measurements on surfaces of porous rock and soil is presented. The construction and performance of two versions of the “surface tensiometer,” developed for determining near‐zero values of matric potential on rock surfaces, are described. Laboratory surface tensiometer measurements were made on a natural fracture surface of a Bishop Tuff block equilibrated with a water table boundary set at elevations ranging from −51 to +25 mm relative to the tensiometers. All equilibrium readings were within 10 Pa of ideal values, and most were within 5 Pa. Response times associated with this instrument‐rock system were in qualitative agreement with the matric potential–dependent hydraulic properties of the rock block.Keywords
This publication has 7 references indexed in Scilit:
- Steady State Flow in an Unsaturated, Two‐Dimensional, Macroscopically Homogeneous, Miller‐Similar MediumWater Resources Research, 1995
- Recommended practice for probe permeametryMarine and Petroleum Geology, 1993
- THE PRESSURE RESPONSE OF THE SOIL WATER SAMPLER AND POSSIBILITIES FOR SIMULTANEOUS SOIL SOLUTION SAMPLING AND TENSIOMETRYSoil Science, 1992
- THE TRANSIENT INSTABILITY OF TENSIOMETER READINGS DURING INFILTRATIONSoil Science, 1991
- A Wick Tensiometer to Measure Low Tensions in Coarse SoilsSoil Science Society of America Journal, 1990
- The Bishop Tuff: Evidence for the origin of compositional zonation in silicic magma chambersPublished by Geological Society of America ,1979
- METHODS OF MEASURING SOIL MOISTURE TENSIONSoil Science, 1949