Evidence for dilution of deep, confined ground water by vertical recharge of isotopically heavy Pleistocene water
Journal Article
·
· Geology; (USA)
- Syracuse Univ. NY (USA)
New analyses of the isotopic composition of water, {sup 14}C-dating of dissolved inorganic carbon, and order-of-magnitude Darcy calculations suggest that a dilute body of water, trending north-south in the Cambrian-Ordovician aquifer of Iowa, was emplaced as vertical recharge of Pleistocene-age water from the base of the Des Moines lobe of late Wisconsin time. The recharge occurred through more than 300 m of overlaying Silurian to Mississippian age rocks. The {delta}{sup 18}O values range from {minus}10{per thousand} to {minus}9{per thousand} for the dilute water body and are consistent with a mixture of Des Moines lobe meltwater and precipitation found today in the north-central US. These results suggest that (1) the climate at the end of the last glaciation was mild and (2) a ground-water stable isotope signature similar to that of modern precipitation in an aquifers recharge area is not a priori evidence for relatively recent recharge.
- OSTI ID:
- 5541798
- Journal Information:
- Geology; (USA), Journal Name: Geology; (USA) Vol. 19:5; ISSN GLGYB; ISSN 0091-7613
- Country of Publication:
- United States
- Language:
- English
Similar Records
Sulfur isotope evidence for regional recharge of saline water during continental glaciation, north-central United States
sup 18 O/ sup 16 O and sup 13 C/ sup 12 C in lower Paleozoic articulate brachiopods: Implications for the isotopic composition of seawater
Geochemistry of the Cambrian-Ordovician aquifer system in the northern midwest, United States
Journal Article
·
Wed Oct 31 23:00:00 EST 1990
· Geology; (USA)
·
OSTI ID:5796857
sup 18 O/ sup 16 O and sup 13 C/ sup 12 C in lower Paleozoic articulate brachiopods: Implications for the isotopic composition of seawater
Journal Article
·
Tue Dec 31 23:00:00 EST 1991
· Geochimica et Cosmochimica Acta; (United States)
·
OSTI ID:7049641
Geochemistry of the Cambrian-Ordovician aquifer system in the northern midwest, United States
Book
·
Sat Dec 31 23:00:00 EST 1988
·
OSTI ID:5711928
Related Subjects
58 GEOSCIENCES
580000* -- Geosciences
AGE ESTIMATION
AQUIFERS
BETA DECAY RADIOISOTOPES
BETA-MINUS DECAY RADIOISOTOPES
CAMBRIAN PERIOD
CARBON 14
CARBON ISOTOPES
CARBONIFEROUS PERIOD
CENOZOIC ERA
CLIMATES
DEVELOPED COUNTRIES
EVEN-EVEN NUCLEI
FEDERAL REGION VII
GEOLOGIC AGES
GEOLOGIC HISTORY
GLACIERS
GROUND WATER
HYDROGEN COMPOUNDS
HYDROLOGY
IOWA
ISOTOPE DATING
ISOTOPE RATIO
ISOTOPES
LIGHT NUCLEI
MATTER
MIXING
NORTH AMERICA
NUCLEI
ORDOVICIAN PERIOD
ORGANIC MATTER
OXYGEN 18
OXYGEN COMPOUNDS
OXYGEN ISOTOPES
PALEOZOIC ERA
PLEISTOCENE EPOCH
QUATERNARY PERIOD
RADIOISOTOPES
RECHARGE
SILURIAN PERIOD
STABLE ISOTOPES
USA
WATER
YEARS LIVING RADIOISOTOPES
580000* -- Geosciences
AGE ESTIMATION
AQUIFERS
BETA DECAY RADIOISOTOPES
BETA-MINUS DECAY RADIOISOTOPES
CAMBRIAN PERIOD
CARBON 14
CARBON ISOTOPES
CARBONIFEROUS PERIOD
CENOZOIC ERA
CLIMATES
DEVELOPED COUNTRIES
EVEN-EVEN NUCLEI
FEDERAL REGION VII
GEOLOGIC AGES
GEOLOGIC HISTORY
GLACIERS
GROUND WATER
HYDROGEN COMPOUNDS
HYDROLOGY
IOWA
ISOTOPE DATING
ISOTOPE RATIO
ISOTOPES
LIGHT NUCLEI
MATTER
MIXING
NORTH AMERICA
NUCLEI
ORDOVICIAN PERIOD
ORGANIC MATTER
OXYGEN 18
OXYGEN COMPOUNDS
OXYGEN ISOTOPES
PALEOZOIC ERA
PLEISTOCENE EPOCH
QUATERNARY PERIOD
RADIOISOTOPES
RECHARGE
SILURIAN PERIOD
STABLE ISOTOPES
USA
WATER
YEARS LIVING RADIOISOTOPES