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| Type: | Resource | |
| Storage: | The size of this resource is 85.2 KB | |
| Created: | Aug 03, 2021 at 1:39 p.m. (UTC) | |
| Last updated: | Aug 03, 2021 at 1:46 p.m. (UTC) (Metadata update) | |
| Published date: | Aug 03, 2021 at 1:46 p.m. (UTC) | |
| DOI: | 10.4211/hs.1beaf29b297b42d394ce4f36f0ab19c3 | |
| Citation: | See how to cite this resource |
| Sharing Status: | Published |
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| Views: | 3369 |
| Downloads: | 76 |
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Abstract
Groundwater recharge in highly-fractured volcanic aquifers remain poorly understood in the humid tropics, whereby rapid demographic growth and unregulated land use changes are resulting in extensive surface water pollution and a large dependency on groundwater extraction. This database presents a multi-tracer approach including δ18O-δ2H, 3H/3He, and noble gases within the most prominent multi-aquifer system of central Costa Rica, with the objective to assess dominant groundwater recharge processes. Wells and large springs were sampled across an elevation gradient from 868 to 2,421 m asl.
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Credits
Funding Agencies
This resource was created using funding from the following sources:
| Agency Name | Award Title | Award Number |
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| International Atomic Energy Agency | None | COS7005; RC-19747; RLA7024 |
Contributors
People or Organizations that contributed technically, materially, financially, or provided general support for the creation of the resource's content but are not considered authors.
| Name | Organization | Address | Phone | Author Identifiers |
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| Empresa de Servicios Públicos de Heredia |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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