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 |
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ASJC Scopus subject areas
- Geochemistry and Petrology
- Water Science and Technology
Cite this
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
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TY - GEN
T1 - Equilibrium-nonequilibrium state of groundwater with rock-forming minerals in theYuncheng basin, Northern China
AU - Gorlushko, A. S.
AU - Shvartsev, S. L.
AU - Li, Y.
PY - 2007
Y1 - 2007
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.
UR - http://www.scopus.com/inward/record.url?scp=84863290840&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84863290840&partnerID=8YFLogxK
M3 - Conference contribution
AN - SCOPUS:84863290840
SN - 9780415451383
VL - 2
SP - 957
EP - 959
BT - Water-Rock Interaction - Proceedings of the 12th International Symposium on Water-Rock Interaction, WRI-12
ER -