By W. M. Edmunds, W. M. Edmunds, C. J. Milne
In lots of coastal parts of Europe the influence of reduced sea degrees for a lot of the previous 100,000 years has ended in the emplacement of unpolluted groundwater assets to depths of more than are happening within the smooth period. The papers provided learn the prevalence of palaeowaters in Europe from the Baltic to the Atlantic, the palaeoclimatic and geological controls on their emplacement, in addition to geochemical and geophysical thoughts for his or her evaluate. The conflicts for coping with those assets in hugely populated sector of Europe is mentioned. Readership: Quaternary Scientists, Hydrogeologists and Groundwater administration pros. additionally of curiosity to lecturers attracted to Palaeoclimate reports and Coastal technological know-how. compatible for submit Graduate path paintings on worldwide switch, environmental technology and hydrogeology.
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Extra info for Palaeowaters in Coastal Europe: Evolution of Groundwater since the Late Pleistocene (2001)(en)(310
CLARK, I. & FRITZ, P. 1997. Environmental Isotopes in Hydrogeology. Lewis Publishers, Boca Raton. GROUNDWATER STATE. 1994. Estonian Geological Survey, Tallinn. JOELEHT. A. 1998. Geothermal studies of the Precambrian basement and Phanerozoic sedimentary cover in Estonia and in Finland. PhD thesis, University of Tartu. KLEMAN, J. & BORGSTROM, I. 1994. Glacial land forms indicative of partly frozen bed. Journal of Glaciology, 40, 225-264. LOOSLI, H. , BARBECOT, F. ET AL 2001. Isotopic methods and their hydrogeo- chemical context in the investigation of palaeowaters.
2, Table 1) a flow log runs in a well that is fully screened in the Ribe Formation, showing that the entire aquifer thickness contributes to flow. Groundwater samples obtained from the bottom, middle and top of the aquifer showed no significant differences in groundwater quality and age (Buckley et al 2001). At the Fjand site (site 3, Fig. 1) the geophysical logs were especially helpful in defining important flow zones and mixing of waters from different aquifers due to short-circuiting wells. Vertical flow in and around the casing of poorly constructed and damaged wells results in the mixing of groundwaters of different ages at Fjand, leading to invasion of modern waters from the surficial aquifer, as well as Early Holocene waters from the deepest aquifer, into a thin aquifer at c.
LEIJNSE, A.. PUNKARI, M. & VAN WEERT, F. H. A. 1996. The impact of glaciation on the groundwater regime on Northwest Europe. Global and Planetary Change, 12,397,413. CLARK, I. & FRITZ, P. 1997. Environmental Isotopes in Hydrogeology. Lewis Publishers, Boca Raton. GROUNDWATER STATE. 1994. Estonian Geological Survey, Tallinn. JOELEHT. A. 1998. Geothermal studies of the Precambrian basement and Phanerozoic sedimentary cover in Estonia and in Finland. PhD thesis, University of Tartu. KLEMAN, J. & BORGSTROM, I.
Palaeowaters in Coastal Europe: Evolution of Groundwater since the Late Pleistocene (2001)(en)(310 by W. M. Edmunds, W. M. Edmunds, C. J. Milne