Proceedings of the 16th Multidisciplinary Conference on Sinkholes and the Engineering and Environmental Impacts of Karst 2020
DOI: 10.5038/9781733375313.1012
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Combining high resolution spring monitoring, dye tracing, watershed analysis, and outcrop and borehole observations to characterize the Galena Karst, Southeast Minnesota, USA

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Cited by 4 publications
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“…Water, and accompanying neonicotinoids can therefore quickly exchange with the shallow system. A hydrogeologic survey of the region conducted by Barry et al (2020) showed many highly fractured aquifer materials with groundwater flow rates of 1.6 to 4.8 km/d. The well with the highest total neonicotinoid concentration (817784; Figure 3) was located in this shallow subsurface (depth to bedrock 2.1 m; Supplemental Data, Table S4).…”
Section: Discussionmentioning
confidence: 99%
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“…Water, and accompanying neonicotinoids can therefore quickly exchange with the shallow system. A hydrogeologic survey of the region conducted by Barry et al (2020) showed many highly fractured aquifer materials with groundwater flow rates of 1.6 to 4.8 km/d. The well with the highest total neonicotinoid concentration (817784; Figure 3) was located in this shallow subsurface (depth to bedrock 2.1 m; Supplemental Data, Table S4).…”
Section: Discussionmentioning
confidence: 99%
“…Median neonicotinoid concentrations in groundwater (Figure 5 and Table 3) were less than the other hydrologic compartments (Figures 2–4 and 6 and Table 3). Hydrogeologic variables, such as groundwater recharge rates, water flow paths, and groundwater age, especially in southeastern Minnesota (Barry et al 2020), influence the movement and occurrence of neonicotinoids. For example, despite the abundance of agriculture in Dodge and Olmstead Counties, much of the shallow subsurface in the region contains highly degraded karst features, including sinkholes, and allows rapid infiltration to groundwater (Steenberg 2019).…”
Section: Discussionmentioning
confidence: 99%
“…We conducted artificial recharge experiments near Bear Spring, which emanates from the Ordovician Prosser Limestone of the Galena Group (Mossler, 2008) and is located west of Eyota, Minnesota, USA (4,869,610N, 557,713E, UTM Zone 15; Figure 1). The current estimated springshed size of Bear Spring is 4.4 km 2 based on hydrograph analysis (Barry et al., 2020) and ongoing dye tracing work is further refining the springshed extent. Baseflow discharge is generally 0.017–0.034 m 3 /s, although high flow events may approach ∼1 m 3 /s (Barry et al., 2020).…”
Section: Study Areamentioning
confidence: 99%
“…The current estimated springshed size of Bear Spring is 4.4 km 2 based on hydrograph analysis (Barry et al., 2020) and ongoing dye tracing work is further refining the springshed extent. Baseflow discharge is generally 0.017–0.034 m 3 /s, although high flow events may approach ∼1 m 3 /s (Barry et al., 2020). The average annual precipitation (1991–2020) for the area of 89 cm (Minnesota Department of Natural Resources, 2021).…”
Section: Study Areamentioning
confidence: 99%