Research paperHydrogeology and geochemistry of the Ogallala aquifer, Southern High Plains☆
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Cited by (69)
The occurrence and distribution of strontium in U.S. groundwater
2021, Applied GeochemistryCitation Excerpt :These elevated concentrations have been attributed to upward cross-formational flow from hydrologically continuous underlying units; Nativ and Smith (1987) document upward hydraulic gradients from underlying units into the SHP aquifer, driving this upward flow, which is also supported by geochemical studies (Scanlon et al., 2009; Langman and Ellis, 2010). Previously published groundwater compositions from underlying Cretaceous, Triassic (Dockum Group), and Permian units (Nativ and Smith, 1987; Scanlon et al., 2009) and deep Permian basinal brines (Fisher and Kreitler, 1987) are used to assess upwelling fluids as a source of Sr to the SHP. Dilute samples from the SHP and the median value for basinal brines are considered as endmembers for mixing models.
Utilization of produced water baseline as a groundwater monitoring tool at a CO<inf>2</inf>-EOR site in the Permian Basin, Texas, USA
2020, Applied GeochemistryCitation Excerpt :Dockum Group waters are under consideration for irrigation and municipal water use due to water shortages near the study area (Cirrus Associates, 2011) and are already used for such purposes regionally (Bradley and Kalaswad, 2003). The Ogallala Formation is an important groundwater source for drinking water and agricultural irrigation in this section of the Permian Basin (Wheeler et al., 2006; George et al., 2011); additionally, this formation overlies numerous oil fields in the Permian Basin (Nativ and Smith, 1987; Rajagoplan et al., 2006). Ogallala groundwaters in this study are sampled from depths of ~45–55 m.
Calcrete uranium deposits in the Southern High Plains, USA
2019, Ore Geology ReviewsPotential chemical impacts of CO<inf>2</inf> leakage on underground source of drinking water assessed by quantitative risk analysis
2016, International Journal of Greenhouse Gas ControlCitation Excerpt :A 2-D radial model was assembled and simulated to analyze the potential risks to groundwater quality due to CO2 leakage (Fig. 3). Regional groundwater flow may dilute potential contaminants, but this was neglected for simplicity in this study, because regional flow velocities in this basin that are maximum ∼10 m/year (Nativ and Smith, 1987) is not significant for our simulations to achieve such dilution. In the initial simulation step to quantify CO2 leakage rate, all simulations assumed that CO2 dissolves in water instantly when it was injected with gaseous CO2 injected into the system at a constant rate.
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