Silicon in ultrafresh groundwater: a case study of the Imandra Lake catchment, The Kola Peninsula; E3S Web of Conferences; Vol. 98 : 16th International Symposium on Water-Rock Interaction (WRI-16) and 13th International Symposium on Applied Isotope Geochemistry (1st IAGC International Conference)
| Parent link: | E3S Web of Conferences Vol. 98 : 16th International Symposium on Water-Rock Interaction (WRI-16) and 13th International Symposium on Applied Isotope Geochemistry (1st IAGC International Conference).— 2019.— [01018, 6 p.] |
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| Autor Corporativo: | |
| Outros autores: | , , , , |
| Summary: | Title screen The ultrafresh groundwater (with TDS values less than 200 mg/L) of the Imandra Lake catchment, Kola Peninsula, is from an intensive water exchange zone, where the water has a short period of contact with the rock. Therefore, the considered water is at the initial stages of the water–rock interaction. The water is saturated with respect to oxides and hydroxides of aluminium and iron. In the groundwater of the Imandra Lake catchment area, the silicon concentrations significantly exceed the concentrations of magnesium and especially potassium. Nevertheless, water is undersaturated with respect to with respect to silicon oxides. The shown enrichment of water with cations is explained by time of water-rock interaction. |
| Idioma: | inglés |
| Publicado: |
2019
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| Subjects: | |
| Acceso en liña: | https://doi.org/10.1051/e3sconf/20199801018 |
| Formato: | Electrónico Capítulo de libro |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=661665 |
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| 200 | 1 | |a Silicon in ultrafresh groundwater: a case study of the Imandra Lake catchment, The Kola Peninsula |f N. V. Guseva [et al.] | |
| 203 | |a Text |c electronic | ||
| 300 | |a Title screen | ||
| 320 | |a [References: 12 tit.] | ||
| 330 | |a The ultrafresh groundwater (with TDS values less than 200 mg/L) of the Imandra Lake catchment, Kola Peninsula, is from an intensive water exchange zone, where the water has a short period of contact with the rock. Therefore, the considered water is at the initial stages of the water–rock interaction. The water is saturated with respect to oxides and hydroxides of aluminium and iron. In the groundwater of the Imandra Lake catchment area, the silicon concentrations significantly exceed the concentrations of magnesium and especially potassium. Nevertheless, water is undersaturated with respect to with respect to silicon oxides. The shown enrichment of water with cations is explained by time of water-rock interaction. | ||
| 461 | |t E3S Web of Conferences | ||
| 463 | |t Vol. 98 : 16th International Symposium on Water-Rock Interaction (WRI-16) and 13th International Symposium on Applied Isotope Geochemistry (1st IAGC International Conference) |o Tomsk, Russia, July 21-26, 2019 |v [01018, 6 p.] |d 2019 | ||
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| 610 | 1 | |a Кольский полуостров | |
| 701 | 1 | |a Guseva |b N. V. |c hydrogeologist |c Professor of Tomsk Polytechnic University, Doctor of geological and mineralogical sciences |f 1984- |g Natalia Vladimirovna |3 (RuTPU)RU\TPU\pers\32200 |9 16200 | |
| 701 | 1 | |a Kopylova |b Yu. G. |c hydrogeologist |c Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences |f 1941- |g Yuliya Grigorievna |3 (RuTPU)RU\TPU\pers\33262 | |
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