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024 8    |a FI14082570
024 7    |a 10.1029/2002WR001929 |2 doi
245 00 |a Use of tritium and helium to define groundwater flow conditions in Everglades National Park |h [electronic resource].
260        |a [S.l.] : |b American Geophysical Union, |c 2003.
490        |a Water Resources Research.
506        |a Please contact the owning institution for licensing and permissions. It is the users responsibility to ensure use does not violate any third party rights.
510        |a Price, R. M., Z. Top, J. D. Happell, and P. K. Swart, Use of tritium and helium to define groundwater flow conditions in Everglades National Park, Water Resour. Res., 39(9), 1267, doi:10.1029/2002WR001929, 2003.
520 3    |a The concentrations of tritium (3H) and helium isotopes (3He and4He) were used as tracers of groundwater flow in the surficial aquifer system (SAS) beneath Everglades National Park (ENP), south Florida. From ages determined by 3H/3He dating techniques, groundwater within the upper 28 m originated within the last 30 years. Below 28 m, waters originated prior to 30 years before present with evidence of mixing at the interface. Interannual variation of the 3H/3He ages within the upper 28 m was significant throughout the 3 year investigation, corresponding with varying hydrologic conditions. In the region of Taylor Slough Bridge, younger groundwater was consistently detected below older groundwater in the Biscayne Aquifer, suggesting preferential flow to the lower part of the aquifer. An increase in 4He with depth in the SAS indicated that radiogenic 4He produced in the underlying Hawthorn Group migrates into the SAS by diffusion. Higher Δ4He values in brackish groundwaters compared to fresh waters from similar depths suggested a possible enhanced vertical transport of4He in the seawater mixing zone. Groundwater salinity measurements indicated the presence of a wide (6–28 km) seawater mixing zone. Comparison of groundwater levels with surface water levels in this zone indicated the potential for brackish groundwater discharge to the overlying Everglades surface water.
533        |a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software.
650        |a Hydrogen |z Florida |z Everglades National Park |x Isotopes.
650        |a Tritium |z Florida |z Everglades National Park.
650        |a Helium |z Florida |z Everglades National Park.
650        |a Groundwater |z Florida |z Everglades National Park.
655    4 |a article.
655    7 |a serial |2 sobekcm
700 1    |a Price, Rene´ M..
700 1    |a Top, Zafer.
700 1    |a Happell, James D..
700 1    |a Swart, Peter K..
830    0 |a dpSobek.
830    0 |a Everglades Digital Library: Reclaiming the Everglades.
852        |a dpSobek |c Everglades Digital Library: Reclaiming the Everglades
856 40 |u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI14082570/00001 |y Click here for full text
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/14/08/25/70/00001/FI14082570thm.jpg
997        |a Everglades Digital Library: Reclaiming the Everglades


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