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Basic Physical and Chemical Factors

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Hydrogeology

Abstract

Water never exists in a chemically pure form in nature because it dissolves substances, transports them and then deposits some of them elsewhere. This leads not only to redistribution of substances in the groundwater conducting layers, but also to the formation of secondary rocks and possibly to the salinization of groundwater and soils. Here, the chemical composition of the water (and thus its quality) depends on its physical and physical-chemical properties. The understanding of such processes and of the respective water quality regimes enables conclusions to be drawn on the origin and the movement of the groundwater, the availability for industrial and domestic use, the environmental influences and options for the remediation of harmful impacts. On the other hand, the composition of some mineral and medicinal waters can give them therapeutic characteristics in health care.

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References

  • Carmi I, Gat JR (1994) Estimating the turnover time of groundwater reservoirs by the helium-3/tritium method in the era of declining atmospheric tritium levels: opportunities and limitations in the time bracket 1990–2000. Isr J Earth Sci 43:249–253

    Google Scholar 

  • Clark ID, Fritz P (1997) Environmental isotopes in hydrogeology. Lewis, Boca Raton, p 328

    Google Scholar 

  • Cook PG, Solomon DK (1997) Recent advances in dating young groundwater: chlorofluorocarbons, 3H/3He and 85Kr. J Hydrol 191:245–265

    Article  Google Scholar 

  • Drost W, Moser H, Neumaier F, Rauert W (1972) Isotopenmethoden in der Grundwasserkunde. Informationsheft des Büros Eurisotop Monographie 16(61):178

    Google Scholar 

  • Ekwurzel B, Schlosser P, Smethie WM Jr, Plummer LN, Busenberg E, Michel RL, Weppernig R, Stute M (1994) Dating of shallow groundwater: comparison of the transient tracers 3He/3H, chlorofluorocarbons, and 85Kr. Water Res 30(6):1639–1708

    Google Scholar 

  • Geyh MA (1988) Methoden der Umweltisotope. In: Schneider H (ed) Die Wassererschließung. Essen, Vulkan-Verl, pp 339–353

    Google Scholar 

  • Geyh MA (2000) Groundwater: saturated and unsaturated zone. In: Mook W (ed) Environmental isotopes in the hydrological cycle. Principles and applications – technical documents in hydrology, vol 39(IV). UNESCO, Paris, p 196

    Google Scholar 

  • Hsieh ST, Lauder GV (2004) Running on water: three-dimensional force generation by basilisk lizards. PNAS 101:16784–16788

    Article  Google Scholar 

  • International Atomic Energy Agency (1987) Studies on sulfur isotope variations in nature. UNESCO-IAEA, Vienna, p 124

    Google Scholar 

  • International Atomic Energy Agency (2005) Use of chlorofluorocarbons in hydrology – a guidebook. UNESCO-IAEA, Vienna, p 277

    Google Scholar 

  • Mattheß G, Frimmel FH, Hirsch P, Schulz HD, Usdowski E (1992) Progress in Hydrogeochemistry. Springer, Berlin, p 544

    Book  Google Scholar 

  • Mook WG (2000) Introduction to isotope hydrology. Theory methods review. In: Mook WG (ed) Environmental isotops in the hydrological cycle. Principles and applications. IHP-V technical documents in hydrology, 39(1). UNESCO, Paris, p 280

    Google Scholar 

  • Moser H, Rauert W (1980) Isotopenmethoden in der Hydrologie. In: Mattheß G (ed) Lehrbuch der Hydrogeologie, vol 8. Borntraeger, Stuttgart, p 400

    Google Scholar 

  • Roether W (1970) Tritium und Kohlenstoff-14 im Wasserkreislauf. Z Dt Geol Ges Sonderh. Hydrogeologie-Hydrogeochemie: 183–192

    Google Scholar 

  • Stober I (1994) Die physikalischen Eigenschaften von Wasser und Gestein, ihre Tiefenabhängigkeit und Folgerungen für die Praxis – unter besonderer Berücksichtigung des kristallinen Grundgebirges. Beitr Z Hydrogeol 45:105–132

    Google Scholar 

  • Yurtsever Y (2000) Modelling. In: Mook WG (ed) Environmental isotops in the hydrological cycle. Principles and applications. IHP-V technical documents in hydrology, vol 39(6). UNESCO-IAEA, Paris, p 127.

    Google Scholar 

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Hölting, B., Coldewey, W.G. (2019). Basic Physical and Chemical Factors. In: Hydrogeology. Springer Textbooks in Earth Sciences, Geography and Environment. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-56375-5_10

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