University of Heidelberg - Department of Physics and Astronomy - Institute of Environmental Physics

Groundwater and Paleoclimate

Members and associates
Instruments
    Noble gas mass spectrometer (VG5400)
    He isotope mass spectrometer (MM3000)
    Radiometric tritium lab
    SF6 gas chromatograph
    Rn α-detector

Isotopes
    3H
    3, 4He
    20, 22Ne
    36, 40Ar
    84Kr
    132Xe
    222Rn

Topics
    Age dating of young waters
      Ground and surface waters with ages less than 50 yr are dated by the 3H-3He and SF6 methods, in order to study processes such as vertical mixing in lakes, groundwater recharge, or the spreading of contaminants in aquifers
    Noble gas paleotemperatures
      Dissolved noble gas concentrations in groundwater enable the determination of paleo-recharge temperatures, which are used to reconstruct the late pleistocene temperature history. A new project explores the potential of fluid inclusions in speleothems as an archive for this proxy.

Examples
    Groundwater ages in the Odenwald region. Ages ranges for the different geological units and zones of mixing with deeper groundwater are shown.
    Noble gas paleotemperature record from the North China Plain. A glacial - interglacial temperature change of 4 - 6°C is found.

Lectures