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Hydrologic (discharge, level, pressure, voltage, electrical conductivity, and temperature) and atmospheric (pressure and temperature) data from injection experiments and a rain event at Bear Spring, MN, USA – June 10-12, 2016
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| Type: | Resource | |
| Storage: | The size of this resource is 4.6 MB | |
| Created: | Mar 27, 2023 at 3:09 a.m. (UTC) | |
| Last updated: | Jul 20, 2025 at 10:57 p.m. (UTC) | |
| Published date: | Jul 20, 2025 at 10:57 p.m. (UTC) | |
| DOI: | 10.4211/hs.74a7fedb4f694ab6aafa3e6d6f47d129 | |
| Citation: | See how to cite this resource |
| Sharing Status: | Published |
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| Views: | 2230 |
| Downloads: | 33 |
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Abstract
We conducted water injection experiments at Bear Spring in southeastern Minnesota, USA, and we monitored responses from the experiments and a rain event (Bilek et al., 2023; Luhmann et al., in press). We injected water from a pool into the overflow spring and monitored hydrologic responses at the perennial spring. The experiments were conducted to monitor for seismic signals as water flows through the karst aquifer, and all corresponding seismic data are provided in Bilek (2016). The experiments confirmed that the overflow spring and perennial spring were connected by at least one conduit in the karst aquifer. The overflow spring was dry for the first two experiments, but it started flowing after a large rainfall event. Because the overflow spring was flowing during the third experiment, the water from the pool simply flowed across the overflow spring run instead of entering the conduit. The hydrologic data are provided that illustrate the response to the three injection experiments and the rain event. Information about the field site and the methods are described below.
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Funding Agencies
This resource was created using funding from the following sources:
| Agency Name | Award Title | Award Number |
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| National Science Foundation | Collaborative Research: Geophysical characterization of a karst aquifer using dynamic recharge events | EAR 1850667 |
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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