Chemical and isotopic evidence for hydrogeochemical processes occurring in the Lincolnshire Limestone
- 26 March 2003
- journal article
- Published by Elsevier
- Vol. 121 (1-4) , 293-320
- https://doi.org/10.1016/0022-1694(90)90237-r
Abstract
No abstract availableKeywords
This publication has 27 references indexed in Scilit:
- Stable carbon isotope ratios and the existence of a gas phase in the evolution of carbonate ground watersPublished by Elsevier ,2003
- The Lincolnshire Limestone — Hydrogeochemical evolution over a ten-year periodPublished by Elsevier ,2003
- The age of groundwater in the Lincolnshire Limestone, England and its relevance to the flow mechanismPublished by Elsevier ,2003
- Precipitation of dissolved carbonate species from natural waters for δ13C analysis — A critical appraisalChemical Geology: Isotope Geoscience section, 1990
- Bacterial metabolism and the δ13C composition of ground water, Floridan aquifer system, South CarolinaGeology, 1988
- 234U/238U activity ratios of dissolved uranium in groundwaters from a jurassic limestone aquifer in EnglandEarth and Planetary Science Letters, 1982
- The occurrence and origin of methane in some groundwater flow systemsCanadian Journal of Earth Sciences, 1981
- A diffusion exchange model for solute movement in fissured porous rockQuarterly Journal of Engineering Geology, 1981
- The effect of climate on the chemistry of carbonate groundwaterWater Resources Research, 1975
- Isotopic standards for carbon and oxygen and correction factors for mass-spectrometric analysis of carbon dioxideGeochimica et Cosmochimica Acta, 1957