Browsing ELibrary by Author "Aeschbach-Hertig W."
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Browsing ELibrary by Author "Aeschbach-Hertig W."
Now showing items 1-5 of 5
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Kipfer R.; Aeschbach-Hertig W.; Hofer M.; Hohmann R.; Imboden D.M.; Baur H.; Golubev V.; Klerkx J. (1996)Hydrothermal water enters Frolikha Bay, a well-known site of high geothermal heat flux in the northern part of Lake Baikal, at 400 m depth. On the basis of CTD profiles, the hydrothermal water is identified as forming an ...
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Holocher J.; Peeters F.; Aeschbach-Hertig W.; Hofer M.; Brennwald M.; Kinzelbach W.; Kipfer R. (2002)The formation of an excess of dissolved gas (''excess air'') in quasi-saturated media was studied by analyzing and interpreting dissolved noble gas concentrations in laboratory column experiments. Using quartz sand filled ...
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IMPROVING NOBLE GAS BASED PALEOCLIMATE RECONSTRUCTION AND GROUNDWATER DATING USING 20NE/22NE RATIOS Peeter F.; Aeschbach-Hertig W.; Holocher J.; Brennwald M.S.; Kipfer R.; Beyerle U. (2003)The interpretation of noble gas concentrations in groundwater with respect to recharge temperature and fractionated excess gas leads to different results on paleo-climatic conditions and on residence times depending on the ...
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Loosli H.H.; Aeschbach-Hertig W.; Barbecot F.; Blaser P.; Darling W.G.; Dever L.; Edmunds W.M.; Kipfer R.; Purtschert R.; Walraevens K. (2001)Isotope and geochemical techniques are the primary way in which the residence time, recharge conditions and subsequent evolution of palaeowaters can be determined. Isotopic species and noble gas concentrations are used as ...
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Kipfer R.; Aeschbach-Hertig W.; Peeters F.; Stute M. (2002)In contrast to most other fields of noble gas geochemistry that mostly regard atmospheric noble gases as 'contamination,' air-derived noble gases make up the far largest and hence most important contribution to the noble ...
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