The transport of U-and Th-series nuclides in sandy confined aquifers
暂无分享,去创建一个
[1] B. Bourdon,et al. Erosion timescales derived from U-decay series measurements in rivers , 2001 .
[2] Yemane Asmerom,et al. Late Holocene Climate and Cultural Changes in the Southwestern United States , 2001, Science.
[3] V. Polyak,et al. Wetter and cooler late Holocene climate in the southwestern United States from mites preserved in stalagmites , 2001 .
[4] G. Wasserburg,et al. The transport of U- and Th-series nuclides in sandy confined aquifers , 2001 .
[5] M. Stute,et al. Comparison of 4He ages and 14C ages in simple aquifer systems: implications for groundwater flow and chronologies , 2000 .
[6] G. Wasserburg,et al. Factors controlling the groundwater transport of U, Th, Ra, and Rn , 2000 .
[7] B. Dupré,et al. Global silicate weathering and CO2 consumption rates deduced from the chemistry of large rivers , 1999 .
[8] Andrew C. Morton,et al. Processes controlling the composition of heavy mineral assemblages in sandstones , 1999 .
[9] G. Wasserburg,et al. The importance of colloids and mires for the transport of uranium isotopes through the Kalix River watershed and Baltic Sea , 1997 .
[10] D. Langmuir. Aqueous Environmental Geochemistry , 1997 .
[11] W. Broecker,et al. A 30,000 yr Continental Paleotemperature Record Derived from Noble Gases Dissolved in Groundwater from the San Juan Basin, New Mexico , 1995, Quaternary Research.
[12] W. Burnett,et al. The Distribution of Uranium and Thorium Decay-Series Radionuclides in the Environment—A Review , 1994 .
[13] D. Schink,et al. A method for rapid in situ extraction and laboratory determination of Th, Pb, and Ra isotopes from large volumes of seawater , 1993 .
[14] K. Turekian,et al. Retardation of 238U and 232Th decay chain radionuclides in Long Island and Connecticut aquifers , 1993 .
[15] D. Hammond,et al. Decay-series disequilibria applied to the study of rock-water interaction and geothermal systems.; 2 , 1992 .
[16] G. Wasserburg,et al. 234U—238U—230Th—232Th systematics in saline groundwaters from central Missouri , 1990 .
[17] Thomas M. Semkow,et al. The role of radium distribution and porosity in radon emanation from solids. , 1990 .
[18] T. Semkow. Recoil-emanation theory applied to radon release from mineral grains , 1990 .
[19] A. Long,et al. An isotopic investigation of groundwater in the Central San Juan Basin, New Mexico: Carbon 14 dating as a basis for numerical flow modeling , 1989 .
[20] J. Andrews,et al. Natural radioelement solution by circulating groundwaters in the Stripa granite , 1989 .
[21] J. Hem. Study and Interpretation of the Chemical Characteristics of Natural Water , 1989 .
[22] M. Hoffmann,et al. Reductive dissolution of fe(III) oxides by Pseudomonas sp. 200 , 1988, Biotechnology and bioengineering.
[23] S. Krishnaswami,et al. Comparative study of 222Rn, 40Ar, 39Ar and 37Ar leakage from rocks and minerals: Implications for the role of nanopores in gas transport through natural silicates , 1988 .
[24] L. E. Fox,et al. The solubility of colloidal ferric hydroxide and its relevance to iron concentrations in river water , 1988 .
[25] K. Fröhlich,et al. On the potential use of uranium isotopes for groundwater dating , 1987 .
[26] G. Wasserburg,et al. 238 U, 234 U and 232 Th in seawater , 1986 .
[27] F. Phillips,et al. Paleoclimatic Inferences from an Isotopic Investigation of Groundwater in the Central San Juan Basin, New Mexico , 1986, Quaternary Research.
[28] D. Lal,et al. Preferential solution of234U from recoil tracks and234U/238U radioactive disequilibrium in natural waters , 1986 .
[29] M. Davidson,et al. Interpretation of 234U/238U activity ratios in groundwaters , 1985 .
[30] Rama,et al. Mechanism of transport of U-Th series radioisotopes from solids into ground water , 1984 .
[31] W. C. Graustein,et al. Radium, thorium and radioactive lead isotopes in groundwaters: application to the in situ determination of adsorption-desorption rate constants and retardation factors , 1982 .
[32] R. Fleischer. Alpha-recoil damage and solution effects in minerals: uranium isotopic disequilibrium and radon release , 1982 .
[33] P. Brewer,et al. Elevated Concentrations of Actinides in Mono Lake , 1982, Science.
[34] J. Herman,et al. The mobility of thorium in natural waters at low temperatures , 1980 .
[35] D. Schink,et al. Radium, thorium, and actinium extraction from seawater using an improved manganese-oxide-coated fiber , 1979 .
[36] D. Langmuir,et al. Uranium solution-mineral equilibria at low temperatures with applications to sedimentary ore deposits , 1978 .
[37] K. Kigoshi. Alpha-Recoil Thorium-234: Dissolution into Water and the Uranium-234/Uranium-238 Disequilibrium in Nature , 1971, Science.
[38] M. Land. Weathering of till in northern Sweden and its implications for the geochemistry of soil water, groundwater and stream water , 1998 .
[39] P. Domenico,et al. Physical and chemical hydrogeology , 1990 .
[40] M. Davidson,et al. A Porous Flow Model for Steady State Transport of Radium in Groundwater , 1986 .
[41] J. Laul,et al. The Use of Natural Radionuclides to Predict the Behavior of Radwaste Radionuclides In Far-Field Aquifers , 1983 .
[42] J. Andrews,et al. 234U/238U activity ratios of dissolved uranium in groundwaters from a jurassic limestone aquifer in England , 1982 .
[43] F. Mackenzie,et al. Evolution of sedimentary rocks , 1971 .
[44] N. J. Lusczynski,et al. Hydrology of Brookhaven National Laboratory and vicinity, Suffolk County, New York , 1968 .