Posteruption chemical evolution of a volcanic caldera lake: Karymsky Lake, Kamchatka
he 1996 short-lived subaqueous eruption at the Karymsky caldera lake suddenly changed the composition of the lake water. The lake, with a surface area of ~10 km2 and a volume of ~0.5 km3, became acidic, increased its salinity to ~1000 mg/kg, and became dominated by SO42− and Ca2+. Since the eruption...
| Published in: | Geophysical Research Letters |
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| Main Authors: | , , , |
| Other Authors: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
2013
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| Subjects: | |
| Online Access: | http://hdl.handle.net/11391/1188680 https://doi.org/10.1002/grl.50961 |
| Summary: | he 1996 short-lived subaqueous eruption at the Karymsky caldera lake suddenly changed the composition of the lake water. The lake, with a surface area of ~10 km2 and a volume of ~0.5 km3, became acidic, increased its salinity to ~1000 mg/kg, and became dominated by SO42− and Ca2+. Since the eruption, the lake chemistry has evolved in a predictable manner described by simple box model. As a result of dilution by incoming SO4-Ca-Mg-poor water, SO4, Ca, and Mg concentrations follow a simple exponential decrease with a characteristic time close to the residence time of the lake. Na, K, and Cl decrease relatively significantly slower, indicating a continuing input of these constituents into the lake that was initiated during the eruption. Thus, the dynamics of two groups of lake water solutes can be predicted by a simple box model for water and solute mass balance. |
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