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Groundwater Isotopic Evidence for Paleorecharge in U.S. High Plains Aquifers

Published online by Cambridge University Press:  20 January 2017

Alan R. Dutton
Alan R. Dutton*
Affiliation:
Bureau of Economic Geology, The University, of Texas at Austin, University Station, Box X, Austin, Texas 78713-7508
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Abstract

Compositions of δD, δ18O, 14C, and 3H are distinct in unconfined and confined groundwaters beneath the nonglaciated U.S. High Plains and reflect differences in average paleoclimatic conditions between the Holocene and the Middle to Late Wisconsinan. δD and δ18O are more depleted in confined groundwaters than in unconfined groundwaters beneath the southern and central Plains but are more enriched in confined than in unconfined groundwaters beneath the northern Plains. The range in stable isotopic composition of meteoric water north-to-south across the High Plains was apparently smaller during the Middle to Late Wisconsinan than it has been during the Holocene. The greater δD and δ18O depletion of confined groundwater beneath the southern and central Plains agrees with isotopic and noble gas data on other paleowaters that suggest Middle to Late Wisconsinan recharge temperatures were cooler than average Holocene temperatures by 5 to 8°C. The greater δD and δ18O enrichment of confined groundwater beneath the northern High Plains adds to previously reported evidence for stable isotope enrichment in glacial age precipitation across the northern Plains to the eastern United States. Additional research is needed to evaluate how patterns and mechanisms of moisture transport and other climatic variables might explain isotopic composition of paleorecharge during the last glacial period.

Type
Research Article
Information
Quaternary Research , Volume 43 , Issue 2 , March 1995 , pp. 221 - 231
Copyright
University of Washington

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References

Andrews, J. N. Fontes, J.-C. Aranyossy, J.-F. Dodo, A. Edmunds, W. M. Joseph, A., and Travi, Y. (1994). The evolution of alkaline groundwaters in the continental intercalate aquifer of the Irhazer Plain, Niger. Water Resources Research 30, 45–61.Google Scholar
Baker, R. G., and Wain, K. A. (1985). Quaternary pollen records from the Great Plains and central United States. In “Pollen records of Late-Quaternary North American Sediments” (Bryant, V. M. Jr., and Holloway, R. G., Eds.), pp. 191–203. American Association of Stratigraphic Palynologists, Dallas, TX,Google Scholar
Belitz, Kenneth, , and Bredehoeft, J. D. (1988), Hydrodynamics of Denver Basin: Explanation of subnormal fluid pressures. American Association of Petroleum Geologists Bulletin 72, 1334–1359.Google Scholar
Bredehoeft, J. D. Back, William, , and Hanshaw, B. B. (1988). Regional ground-water flow concepts in the United States: Historical perspective. In “Recent Trends in Hydrogeology” (Narasimhan, T. N., Ed.), pp. 297–316. Geological Society of America Special Paper 189.Google Scholar
Claassen, H. C. (1986). Late-Wisconsinan paleohydrology of the westcentral Amargosa Desert, Nevada, U.S.A. Chemical Geology 58, 311–323.Google Scholar
COHMAP Members (1988). Climatic changes of the last 18,000 years: Observations and model simulations. Science 241, 1043–1052.Google Scholar
Craig, Harmon, (1961). Isotopic variations in meteoric waters. Science 133, 1702–1703.Google Scholar
Dansgaard, W. (1964). Stable isotopes in precipitation, Tellus 16, 436–468.Google Scholar
Dansgaard, W. Johnsen, S. J. M0ller, J., and Langway, C. C. Jr., (1969). One thousand centuries of climatic record from Camp Century on the Greenland ice sheet. Science 166, 377–381.Google Scholar
Davidson, M. R., and Airey, P. L. (1982). The effect of dispersion on the establishment of a paleoclimatic record from groundwater. Journal of Hydrology 58, 131–147.CrossRefGoogle Scholar
Davisson, M. L. Smith, D. K. Macfarlane, P. A. Whittemore, D. O. Hudson, G. B., and Caffee, M. (1993). Isotopic indications of age and flow characteristics of ground water in the Dakota aquifer, eastern Colorado through central Kansas. Geological Society of America, Abstracts with Programs 25, 145 [Abstract].Google Scholar
Dray, M. Gonfiantini, R., and Zuppi, G. M. (1983). Isotopic composition of groundwater in the southern Sahara. In “Palaeodimates and Palaeowaters: A Collection of Environmental Isotope Studies,” Panel Proceedings Series, pp. 187–199. International Atomic Energy Agency, Vienna.Google Scholar
Domenico, P. A., and Robbins, G. A. (1985). The displacement of connate water from aquifers. Geological Society of America Bulletin 96, 328–335.Google Scholar
Dutton, A. R., and Simpkins, W. W. (1989). Isotopic evidence for paleohydrologic evolution of ground-water flow paths, Southern Great Plains, U.S.A. Geology 17, 653–656,Google Scholar
Epstein, Samuel, (1993). The D/H ratio of hydrogen in plant remains which grew 8 to 12 x 1G3 years B.P. on the north slope of Alaska. Geological Society of America Abstracts with Programs 23, A456 [Abstract].Google Scholar
Galloway, R. W. (1983). Full-glacial southwestern United States: Mild and wet or cold and dry? Quaternary Research 19, 236–248.Google Scholar
Gat, J. R. (1983). Precipitation, groundwater, and surface waters; control of climatic parameters on their isotopic composition and their utilization as palaeoclimatological tools. In “Palaeoclimates and Palaeowaters: A Collection of Environmental Isotope Studies,” Panel Proceedings Series, pp. 3–12. International Atomic Energy Agency, Vienna.Google Scholar
Grootes, P. M. (1993). Interpreting continental oxygen isotope records. In “Climate Change in Continental Isotopic Records” (Swart, P. K. Lohman, K. C. McKenzie, J., and Savin, S., Eds.), pp. 37–46. American Geophysical Union, Geophysical Monograph 78.Google Scholar
Gustavson, T. C., and Finley, R. J. (1985). “Late Cenozoic Geomorphic Evolution of the Texas Panhandle and Northeastern New Mexico—Case Studies of Structural Controls on Regional Drainage Development.” Bureau of Economic Geology Report of Investigations 148. University of Texas, Austin.Google Scholar
Gutentag, E. D. Heimes, F. J. Krothe, N. C. Luckey, R. R., and Weeks, J. B. (1984). “Geohydrology of the High Plains Aquifer in Parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming,” Professional Paper 1400-B. U.S. Geological Survey.Google Scholar
Hassan, A. (1982). “Methodologies for Extraction of Dissolved Inorganic Carbon for Stable Carbon Isotope Studies: Evaluation and Al-ternatives.” Water Resources Investigations 82-6. U.S. Geological Survey.Google Scholar
Hills, J. M., and Kottlowski, F. E. (1983). “Southwest/Southwest Mid-Continent Region: Correlation of Stratigraphic Units of North America (COSUNA) Project,” Correlation Chart Series. American Association of Petroleum Geologists.Google Scholar
Holliday, V. T. (1987). Re-examination of late-Pleistocene boreal forest reconstruction for the southern High Plains. Quaternary Research 28, 238–244.Google Scholar
Jacobson, G. Calf, G. E. Jankowski, J., and McDonald, P. S. (1989). Groundwater chemistry and palaeorecharge in the Amadeus Basin, Centra) Australia. Journal of Hydrology 109, 237–266.Google Scholar
Kent, H. C. Couch, E. L., and Knepp, R. A. (1988). “Centra! and Southern Rockies Region: Correlation of Stratigraphic Units of North America (COSUNA) Project,” Correlation Chart Series. American Association of Petroleum Geologists.Google Scholar
Kutzbach, J. E., and Wright, H. E. Jr., (1985). Simulation of the climate of 18,000 years BP: Results for the North American/North Atlantic/European sector and comparison with the geologic record of North America. Quaternary Science Reviews 4, 147–187.Google Scholar
Kutzbach, J. E., and Guetter, P. J. (1986). The influence of changing orbital parameters and surface boundary conditions on climate simulations for the past 18,000 years. Journal of the Atmospheric Sciences 43, 1726–1759.Google Scholar
Lawrence, J. R., and White, J. W. C. (1991). The elusive climate signal in the isotopic composition of precipitation. In “Stable Isotope Geochemistry: A Tribute to Samuel Epstein” (Taylor, H. P. Jr. O’Neil, J. R., and Kaplan, I. R., Eds.), Special Publication 3. pp. 169–185. The Geochemical Society.Google Scholar
Lowry, M. E., and Christ, M. A. (1967). “Geology and Ground-Water Resources of Laramie County, Wyoming.” Water-Supply Paper 1834. U.S. Geological Survey.Google Scholar
Macfarlane, P. A. (1993). “The Effect of Topographic Relief and Hydrostratigraphy on the Upper Part of the Regional Ground-Water Flow System in Southeastern Colorado and Western and Central Kansas, with Emphasis on the Dakota Aquifer.” Unpublished Ph.D. dissertation, University of Kansas.Google Scholar
McPhee, J. A. (1986). “Rising from the Plains.” Farrar, Straus, Giroux, New York.Google Scholar
Moser, H. Wolf, M. Fritz, P. Fontes, J.-C. Florkowski, T., and Payne, B. R. (1989). Deuterium, oxygen-18, and tritium in Stripa groundwater. Geochimica el Cosmochimica Acta 53, 1757–1763.Google Scholar
Mul Jican, W. F. III Fryar, A. E., and Johns, N. D. (1994). Vertical transport of contaminants through perched aquifers to the Ogallala aquifer, Pantex Plant area, southern High Plains, Texas. In “Toxic Substances and the Hydrologic Sciences” (Dutton, A. R., Ed.), pp. 547–562. American Institute of Hydrology.Google Scholar
Nativ, Ronit, , and Riggio, Robert, (1989). Meterologic and isotopic characteristics of precipitation events with implications for ground-water recharge, southern High Plains. Atmospheric Research 23, 51–82.Google Scholar
Nativ, Ronit, , and Smith, D. A. (1987). Hydrogeology and geochemistry of the Ogallala aquifer, southern High Plains. Journal of Hydrology 91, 217–253.Google Scholar
Osterkamp, W. R. Fenton, M. M. Gustav son, T. C. Hadley, R. F. Holliday, V. T. Morrison, R. B., and Toy, T. J. (1987). Great Plains. In “Geomorphic systems of North America” (Graf, W. L., Ed.), Centennial Special Vol. 2, pp. 163–210. Geological Society of America, Boulder, CO,Google Scholar
Osterkamp, W. R., and Wood, W, W. (1987). Playa-lake basins on the southern High Plains of Texas and New Mexico: I. hydrologic, geomorphic, and geologic evidence for their development. Geological Society of America Bulletin 99, 215–223.Google Scholar
Parkhurst, D. L. Christenson, S., and Breit, G. N. (1992). “Ground-Water-Quality Assessment of the Central Oklahoma Aquifer, Oklahoma: Geochemical and Geohydrologic Investigations,” Open-File Report 92-642. U.S. Geological Survey.Google Scholar
Perry, E. C. Jr. Grundl, T., and Gilkeson, R, H. (1982). H, O, and S isotopic study of the groundwater in the Cambrian-Ordovician aquifer system of northern Illinois, In “Isotope Studies of Hydroiogic Processes” (Perry, E. C. Jr., and Montgomery, C. W., Eds.), pp. 35–43. Northern Illinois Univ. Press, DeKalb, IL.Google Scholar
Phillips, F. M. Peeters, L. A. Tansey, M. K., and Davis, S. N. (1986). Paleoclimatic inferences from aa isotopic investigation of groundwater in the Central San Juan Basin, New Mexico. Quaternary Research 26, 179–193.CrossRefGoogle Scholar
Plummer, L. N. (1993). Stable isotope enrichment in paleowaters of the southeast Atlantic coastal plain, United States. Science 262, 2016–2020.Google Scholar
Plummer, L. N. Busby, J. F. Lee, R. W., and Hanshaw, B. B. (1990). Geochemical modeling of the Madison aquifer in parts of Montana, Wyoming, and South Dakota. Water Resources Research 26, 1981–2014.Google Scholar
Rozanski, K. (1985). Deuterium and oxygen-18 in European groundwaters—links to atmospheric circulation in the past. Chemical Geology 52, 349–363.Google Scholar
Senger, R. K., and Fogg, G. E. (1987). Regional underpressuring in deep brine aquifers, Palo Duro Basin, Texas. 1. Effects of hydrostratigraphy and topography. Water Resources Research 23, 1481–1493.Google Scholar
Siegel, D, I. (1991). Evidence foT dilution of deep, confined ground water by vertical recharge of isotopically heavy Pleistocene water. Geology 19, 433–436.Google Scholar
Siegel, D. I, (1992). Isotopic evidence from regional ground water and calcite cements that Late Wisconsin continental ice lobes were sustained by tropical air masses. Geological Society of America Abstracts with Programs 24, A240 [Abstract],Google Scholar
Srdoi, D. Obelic, B. Horvatinifc, N. Sliep6evid, A. Stichler, W. Moser, H., and Geyh, M. A. (1982). Isotope analyses of groundwaters of the North African Plain. Catena 9, 253–263.Google Scholar
Stute, M., and Deak, J. (1989). Environmental isotope study (14C, 13C, 180, D, noble gases) on deep groundwater circulation systems in Hungary with reference to paleoclimate. Radiocarbon 31, 902–918.Google Scholar
Stute, M. Schlosser, P. Clark, J. F., and Broecker, W. S. (1992). Paleotemperatures in southwestern United States derived from noble gases in ground water. Science 256, 1000–1003.Google Scholar
Swinehart, J. B. Souders, V. L., DeGraw, H. M., and Diffendal, R. F. Jr., (1985). Cenozoic paleogeography of western Nebraska. In “Cenozoic Paleogeography of West-Central United States” (Flores, R. M., and Kaplan, S. S., Eds.), Rocky Mountain Paleogeography Symposium 3, pp. 209–299. Society of Economic Paleontologists and Mineralogists, Rocky Mountain Section.Google Scholar
Taylor, H. P. Jr., (1974). The application of oxygen and hydrogen isotope studies to problems of hydrothermal alterations and ore deposition. Economic Geology 69, 843–883.CrossRefGoogle Scholar
Yapp, C. J., and Epstein, Samuel, (1977). Climatic implications of D/H ratios of meteoric water over North America (9500-22,000 B.P.) as inferred from ancient wood cellulose C-H hydrogen. Earth and Planetary Science Letters 34, 333–350.Google Scholar