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Ground‐Water Tracers — A Short Review
Author(s) -
Davis Stanley N.,
Thompson Glenn M.,
Bentley Harold W.,
Stiles Gary
Publication year - 1980
Publication title -
groundwater
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.84
H-Index - 94
eISSN - 1745-6584
pISSN - 0017-467X
DOI - 10.1111/j.1745-6584.1980.tb03366.x
Subject(s) - tracer , groundwater , environmental science , hydrogeology , radionuclide , bromide , environmental chemistry , chloride , hydrology (agriculture) , geology , chemistry , nuclear physics , geotechnical engineering , physics , organic chemistry
Tracers are used widely to determine the direction and velocity of ground‐water movement. Failures of tracer tests are most commonly a result of incorrect choice of tracers, insufficient concentrations of tracers, and a lack of an understanding of the hydrogeologic system being tested. Some of the most useful general tracers are bromide chloride, rhodamine WT, and various fluorocarbons. For certain purposes, dyed clubmoss and baker's yeast have proved valuable. Many radionuclides including 3 H, 82 Br, and 198 Au are almost ideal for numerous purposes, but radiation hazards associated with their use together with local, State, and Federal regulations have discouraged widespread field applications in recent years within the United States.