Humic acids in subsurface waters from the Southern Great Plain, Hungary
Subsurface water samples from different depths were analysed in the Southern part of the Great Hungarian Plain. Permanganate oxidizability and concentration of humic acid were measured. These data showed that there are humic and non-humic organic material in subsurface waters of different ages. The...
Elmentve itt :
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Dokumentumtípus: | Cikk |
Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1985
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Sorozat: | Acta mineralogica-petrographica
27 |
Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
Tárgyszavak: | |
Online Access: | http://acta.bibl.u-szeged.hu/24737 |
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001 | acta24737 | ||
005 | 20220726112124.0 | ||
008 | 161017s1985 hu o 0|| eng d | ||
022 | |a 0365-8066 | ||
040 | |a SZTE Egyetemi Kiadványok Repozitórium |b hun | ||
041 | |a eng | ||
100 | 1 | |a Varsányi Irén | |
245 | 1 | 0 | |a Humic acids in subsurface waters from the Southern Great Plain, Hungary |h [elektronikus dokumentum] / |c Varsányi Irén |
260 | |a University of Szeged, Department of Mineralogy, Geochemistry and Petrology |b Szeged |c 1985 | ||
300 | |a 165-170 | ||
490 | 0 | |a Acta mineralogica-petrographica |v 27 | |
520 | 3 | |a Subsurface water samples from different depths were analysed in the Southern part of the Great Hungarian Plain. Permanganate oxidizability and concentration of humic acid were measured. These data showed that there are humic and non-humic organic material in subsurface waters of different ages. The proportion of this organic materials is characteristic on the age of the waters. On the basis of this proportion can be concluded the reaction of organic matarials taking place in waters after burial. | |
650 | 4 | |a Természettudományok | |
650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
695 | |a Kőzettan, Ásványtan, Földtan | ||
856 | 4 | 0 | |u http://acta.bibl.u-szeged.hu/24737/1/mineralogica_027_165-170.pdf |z Dokumentum-elérés |