USE OF DEUTERATED WATER AS A CONSERVATIVE ARTIFICIAL GROUNDWATER TRACER

dc.contributor.author	Becker M.
dc.contributor.author	Coplen T.
dc.date.accessioned	2021-03-15T07:09:54Z
dc.date.available	2021-03-15T07:09:54Z
dc.date.issued	2001
dc.identifier	https://www.elibrary.ru/item.asp?id=815149
dc.identifier.citation	Hydrogeology Journal, 2001, 9, 5, 512-516
dc.identifier.issn	1431-2174
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/26726
dc.description.abstract	Conservative tracers are necessary to obtain groundwater transport velocities at the field scale. Deuterated water is an effective tracer for this purpose due to its similarity to water, chemical stability, non-reactivity, ease of handling and sampling, relatively neutral buoyancy, and reasonable price. Reliable detection limits of 0.1 mg deuterium/L may be obtained in field tests. A field example is presented in which deuterated water, bromide, and pentafluorobenzoic acid are used as groundwater tracers. Deuterated water appeared to be transported conservatively, producing almost identical breakthrough curves as that of other soluble tracers.
dc.subject	TRACER TESTS
dc.subject	STABLE ISOTOPES
dc.subject	SOLUTE TRANSPORT
dc.subject	FRACTURED ROCKS
dc.subject	GROUNDWATER DENSITY
dc.subject	DEUTERIUM
dc.title	USE OF DEUTERATED WATER AS A CONSERVATIVE ARTIFICIAL GROUNDWATER TRACER
dc.type	Статья

Files in this item

Files	Size	Format	View
There are no files associated with this item.