Silicon in ultrafresh groundwater

A case study of the Imandra Lake catchment, the Kola Peninsula

Natalia V. Guseva, Yuliya G. Kopylova, Daria A. Vorobeva, Albina A. Khvashchevskaya, Zinaida A. Evtyugina

Research output: Contribution to journalConference article

Abstract

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.

Original languageEnglish
Article number01018
JournalE3S Web of Conferences
Volume98
DOIs
Publication statusPublished - 7 Jun 2019
Event16th International Symposium on Water-Rock Interaction, WRI 2019 and 13th International Symposium on Applied Isotope Geochemistry, 1st IAGC International Conference - Tomsk, Russian Federation
Duration: 21 Jul 201926 Jul 2019

Fingerprint

Catchments
silicon
Lakes
Groundwater
catchment
Silicon
groundwater
lake
water-rock interaction
Water
water
oxide
Rocks
water exchange
hydroxide
magnesium
potassium
aluminum
cation
Silicon oxides

ASJC Scopus subject areas

  • Environmental Science(all)
  • Energy(all)
  • Earth and Planetary Sciences(all)

Cite this

Silicon in ultrafresh groundwater : A case study of the Imandra Lake catchment, the Kola Peninsula. / Guseva, Natalia V.; Kopylova, Yuliya G.; Vorobeva, Daria A.; Khvashchevskaya, Albina A.; Evtyugina, Zinaida A.

In: E3S Web of Conferences, Vol. 98, 01018, 07.06.2019.

Research output: Contribution to journalConference article

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