Humic acid as an indicator of subsurface water movements

Concentration of humic acids and their E4/Ee ratio in shallow groundwater, deeper subsurface water and thermal water samples were determined. Humic acids were isolated from several samples' and their С and H contents were also measured. The E4/E„ and H/C ratios of humic acids differ to each oth...

Teljes leírás

Elmentve itt :
Bibliográfiai részletek
Szerzők: Varsányi Irén
Bertalan Balogi M.
Dokumentumtípus: Cikk
Megjelent: University of Szeged, Department of Mineralogy, Geochemistry and Petrology Szeged 1985
Sorozat:Acta mineralogica-petrographica 27
Kulcsszavak:Kőzettan, Ásványtan, Földtan
Tárgyszavak:
Online Access:http://acta.bibl.u-szeged.hu/24738
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260 |a University of Szeged, Department of Mineralogy, Geochemistry and Petrology  |b Szeged  |c 1985 
300 |a 171-174 
490 0 |a Acta mineralogica-petrographica  |v 27 
520 3 |a Concentration of humic acids and their E4/Ee ratio in shallow groundwater, deeper subsurface water and thermal water samples were determined. Humic acids were isolated from several samples' and their С and H contents were also measured. The E4/E„ and H/C ratios of humic acids differ to each other in shallow ground- and in thermal waters. The Ed/Ee ratio of humic acids in deeper Pleistocene waters of less CI" content is similar to that of the shallow groundwaters and those of higher CI" content is similar to that of the thermal waters. The E4/E„ ratio shows an upward migration of deep waters along fault line, where this migration was supposed on the basis of the higher CI" concentration of waters. 
650 4 |a Természettudományok 
650 4 |a Föld- és kapcsolódó környezettudományok 
695 |a Kőzettan, Ásványtan, Földtan 
700 0 2 |a Bertalan Balogi M.  |e aut 
856 4 0 |u http://acta.bibl.u-szeged.hu/24738/1/mineralogica_027_171-174.pdf  |z Dokumentum-elérés