Equilibrium-nonequilibrium state of groundwater with rock-forming minerals in theYuncheng basin, Northern China

Abstract

The paper presents the results of investigation of equilibrium states in the groundwater-carbonate and aluminosilicate mineral systems of theYuncheng basin.The chemical equilibrium analysis of the groundwater samples show that the water-rock system is characterized by an equilibrium-nonequilibrium state. The main cause of the state is the interaction of water with primary alumiosilicate minerals (anorthite, albite, muscovite, K-feldspar) that results in formation of secondary minerals (clays, montmorillonite, hydromica). The secondary minerals are in equilibrium with groundwater at the present time of the system evolution.

Original language	English
Title of host publication	Water-Rock Interaction - Proceedings of the 12th International Symposium on Water-Rock Interaction, WRI-12
Pages	957-959
Number of pages	3
Volume	2
Publication status	Published - 2007
Event	12th International Symposium on Water-Rock Interaction, WRI-12 - Kunming, China Duration: 31 Jul 2007 → 4 Aug 2007

Other

Other	12th International Symposium on Water-Rock Interaction, WRI-12
Country	China
City	Kunming
Period	31.7.07 → 4.8.07

ASJC Scopus subject areas

Geochemistry and Petrology
Water Science and Technology

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Equilibrium-nonequilibrium state of groundwater with rock-forming minerals in theYuncheng basin, Northern China. / Gorlushko, A. S.; Shvartsev, S. L.; Li, Y.

Water-Rock Interaction - Proceedings of the 12th International Symposium on Water-Rock Interaction, WRI-12. Vol. 2 2007. p. 957-959.

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution

Gorlushko, AS, Shvartsev, SL & Li, Y 2007, Equilibrium-nonequilibrium state of groundwater with rock-forming minerals in theYuncheng basin, Northern China. in Water-Rock Interaction - Proceedings of the 12th International Symposium on Water-Rock Interaction, WRI-12. vol. 2, pp. 957-959, 12th International Symposium on Water-Rock Interaction, WRI-12, Kunming, China, 31.7.07.

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abstract = "The paper presents the results of investigation of equilibrium states in the groundwater-carbonate and aluminosilicate mineral systems of theYuncheng basin.The chemical equilibrium analysis of the groundwater samples show that the water-rock system is characterized by an equilibrium-nonequilibrium state. The main cause of the state is the interaction of water with primary alumiosilicate minerals (anorthite, albite, muscovite, K-feldspar) that results in formation of secondary minerals (clays, montmorillonite, hydromica). The secondary minerals are in equilibrium with groundwater at the present time of the system evolution.",

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year = "2007",

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N2 - The paper presents the results of investigation of equilibrium states in the groundwater-carbonate and aluminosilicate mineral systems of theYuncheng basin.The chemical equilibrium analysis of the groundwater samples show that the water-rock system is characterized by an equilibrium-nonequilibrium state. The main cause of the state is the interaction of water with primary alumiosilicate minerals (anorthite, albite, muscovite, K-feldspar) that results in formation of secondary minerals (clays, montmorillonite, hydromica). The secondary minerals are in equilibrium with groundwater at the present time of the system evolution.

AB - The paper presents the results of investigation of equilibrium states in the groundwater-carbonate and aluminosilicate mineral systems of theYuncheng basin.The chemical equilibrium analysis of the groundwater samples show that the water-rock system is characterized by an equilibrium-nonequilibrium state. The main cause of the state is the interaction of water with primary alumiosilicate minerals (anorthite, albite, muscovite, K-feldspar) that results in formation of secondary minerals (clays, montmorillonite, hydromica). The secondary minerals are in equilibrium with groundwater at the present time of the system evolution.

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BT - Water-Rock Interaction - Proceedings of the 12th International Symposium on Water-Rock Interaction, WRI-12

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