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Theory, Construction and Operation of Simple Tensiometers
Author(s) -
Stannard David I.
Publication year - 1986
Publication title -
groundwater monitoring and remediation
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.677
H-Index - 47
eISSN - 1745-6592
pISSN - 1069-3629
DOI - 10.1111/j.1745-6592.1986.tb00952.x
Subject(s) - tensiometer (surface tension) , water potential , tension (geology) , geotechnical engineering , soil water , engineering , water content , environmental science , surface tension , soil science , materials science , composite material , physics , quantum mechanics , ultimate tensile strength
The tensiometer, introduced by Richards and Gardner (1936) has been a tool often ignored in unsaturated zone investigations. Hazardous waste disposal studies that require values of unsaturated zone matric potentials will expand tensiometer use. Familiarity with operation and installation principles is necessary to ensure quality data collection. The essential elements of a tensiometer are a porous cup connected with tubing to a vacuum gauge; all are filled with water. When the porous cup is buried in unsaturated soil, the soil draws water through the cup wall, until the water tension inside the cup equals the surrounding soil‐water tension. The tension is transmitted through the water filled tube to an accessible vacuum gauge (manometer or transducer) and is recorded manually or automatically. Although specialized tensiometers exist, the tensiometer presented here in detail is suited to diverse on‐site applications. Constructed from readily available, inexpensive parts, it can measure as much as 0.85 bar of tension. Design features include a flushing system for removal of entrapped air or mercury, and an easily maintained modular network of nylon manometers and water‐supply tubes. Good hydraulic connection between porous cup and soil and meticulous backfill procedures are necessary for accurate measurement of representative matric potentials. Proper and consistent use of tensiometers should yield reliable values of matric potentials, and lead to a better understanding of unsaturated zone processes.