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| Type: | Resource | |
| Storage: | The size of this resource is 2.0 MB | |
| Created: | May 25, 2021 at 3:42 p.m. (UTC) | |
| Last updated: | Jun 02, 2021 at 7:15 p.m. (UTC) (Metadata update) | |
| Published date: | Jun 02, 2021 at 7:15 p.m. (UTC) | |
| DOI: | 10.4211/hs.bb01ce1e21214f93b197d6855823af53 | |
| Citation: | See how to cite this resource | |
| Content types: | Single File Content |
| Sharing Status: | Published |
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| Views: | 3131 |
| Downloads: | 63 |
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Abstract
San Salvador Island is a small isolated carbonate platform on the southeastern edge of the Bahamian Archipelago. The Line Hole well field is located on an eogenetic karst aquifer on San Salvador Island's northern coast. The island's negative water budget and extensive lake cover have resulted in the upconing of saline water that has fragmented the once continuous freshwater lens. The Line Hole well field consists of several 15-cm diameter wells drilled into the fresh-water lens and arranged in a line perpendicular to the shore. The well field also has two monitoring wells (LH 1, and LH 13), that penetrate approximately 7 m below the water table into higher salinity groundwater. The well field was abandoned in 2016 upon saltwater intrusion to the aquifer. To evaluate the connectivity between the eogenetic karst aquifer monitored by the Line Hole well field and the ocean, we instrumented wells with HOBO U20L-04 loggers to measure pressure and temperature timeseries. We instrumented wells LH4, and LH8, in addition to the monitoring wells LH1 and LH13.
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Additional Metadata
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| Data types, measurements, and unit descriptions | Each datafile is structured with the following three columns: index/column 0: Date, UTC-5 (str) : "YYYY-MM-DD hh:mm:ss" with precision to the minute. Time stamp associated with each measurement, times are reported in UTC-5. column 1: P_kPa (float) : Water pressure in kilopascals column 2: Temp_C (float) : Water temperature in degrees Celsius Null values: "NaN" |
Related Resources
| This resource is described by | Breithaupt, C. I. (2020). Porosity and Permeability Extremes in an Eogenetic Carbonate Platform: Mechanisms for Formation and Implications for Fluid Flow (Order No. 28155419). Available from Dissertations & Theses @ University of South Florida - FCLA; ProQuest Dissertations & Theses A&I; ProQuest Dissertations & Theses Global. (2475129033). http://ezproxy.lib.usf.edu/login?url=https://www.proquest.com/dissertations-theses/porosity-permeability-extremes-eogenetic/docview/2475129033/se-2?accountid |
| This resource is referenced by | Breithaupt CI, Gulley JD, Moore PJ, Fullmer SM, Kerans C, Mejia JZ. Flank margin caves can connect to regionally extensive touching vug networks before burial: Implications for cave formation and fluid flow. Earth Surf. Process. Landforms. 2021;1–24. https://doi.org/10.1002/esp.5114 |
Credits
Funding Agencies
This resource was created using funding from the following sources:
| Agency Name | Award Title | Award Number |
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| U.S. National Science Foundation | Collaborative Research: How does groundwater inundation of carbonate island interiors from sea level rise impact surface water-aquifer interactions and evaporative losses? | 1743383 |
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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