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Chemical, isotopic, age tracer, and noble gas data for Tucson Basin groundwater


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Created: Mar 25, 2024 at 10:13 p.m. (UTC)
Last updated: Jul 28, 2025 at 8:14 p.m. (UTC)
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Abstract

This study combined conventional and more novel groundwater age tracers, including 3H, 85Kr, 39Ar, 14C, and 4He, to determine groundwater age distributions and mean ages of 10 wells along a well-defined groundwater flow path in the Tucson Basin. Noble gases were used to determine temperatures and water tables depths at the time and place of recharge. Major ion and stable water isotope data are also reported. This data accompanies a manuscript accepted in Water Resources Research (Noyes et al., 2025, in press).

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Tucson Basin
North Latitude
32.2567°
East Longitude
-110.7339°
South Latitude
32.1172°
West Longitude
-110.9784°

Temporal

Start Date:
End Date:

Content

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Credits

Funding Agencies

This resource was created using funding from the following sources:
Agency Name Award Title Award Number
U.S. National Science Foundation EAR-2102457

How to Cite

McIntosh, J., C. Noyes, G. Ferguson, A. Seltzer, J. Ng, R. Purtschert, M. Stute, J. Severinghaus (2025). Chemical, isotopic, age tracer, and noble gas data for Tucson Basin groundwater, HydroShare, http://www.hydroshare.org/resource/6cad951e972b4d0a91ab05dc1a861ec9

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/
CC-BY

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