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Busenberg, Eurybiades, Plummer, L. Busenberg, Eurybiades, Weeks, E. Dissertation, Department of Geology, Indiana University.
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Ground-water dating at Valdosta helps define the susceptibility to contamination of the ground-water resources. Ground-water dating reveals a pattern of high nitrate concentrations moving slowly toward the estuary. For best results, the apparent age should be determined using multiple dating techniques because each dating technique has limitations. This indicates that these waters passed rapidly through the unsaturated zone to the water table, rather than recharging by slow percolation.
- Measurements of dissolved nitrogen and argon can be used to help determine recharge temperature and excess air and to recognize environments undergoing denitrification.
- Modica, Edward, Buxton, H.
- As with any environmental tracer, age applies to the date of introduction of the chemical substance into the water, and not to the water itself.
- For example, measurements of concentrations of dissolved gases, such as dissolved oxygen, help to define the potential for microbial degradation.
The samples are then transported to the U. Shallow ground-water systems are commonly used for drinking water sources and they make up a large part of the baseflow in rivers and lakes. See research for more information. In the atmosphere, smell dating app these substances have mixed and spread worldwide.
USGS Groundwater Dating Lab
- References Cited Bayer, R.
- Department of the Interior U.
- Temperatures derived from gas solubilities in ground water suggest that the aquifer is recharged locally.
- Locating the position of the mids bomb peak is difficult due to the required high density of vertical sampling and, therefore, is often an impractical means of obtaining ground-water age information.
- Tritium measurements alone can be used to locate the depth of the mids bomb peak, but, because of radioactive decay, many samples may need to be collected and analyzed today to locate its position.
- Busenberg, Eurybiades, and Plummer, L.