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The geoecological impact of eruptions on Karymskii Volcano and Tokareva crater, Eastern Kamchatka: The 1996-2008 observations

机译:火山喷发对堪培加东部卡林斯基火山和Tokareva火山口的地球生态影响:1996-2008年观测

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This paper considers the geoecological impacts of eruptions on Karymskii Volcano and the Tokareva crater for the 1996-2008 period, which resulted in changes in (a) the relief around these edifices, (b) the discharge and composition of water in the Karymskii River and other streams in the area, and (c) the discharge and composition of gases in thermal springs. It was found that the concentration of CH_4 previously had been abnormally high in free gases that emanate from the new Piipovskii Springs and an explanation is provided of the decrease in their concentration over time. We detected variations in the radon activity, OARn (Bq/m~3), in free gases that are released in the Karymskii caldera hydrothermal occurrences; the variations are consistent with those in the eruptive activity of Karymskii Volcano in 2005-2006. We describe permafrost rocks in the Karymskii caldera that favor the generation of a cryolithic zone.
机译:本文考虑了喷发对Karymskii火山和Tokareva火山口在1996-2008年期间的地质生态影响,这些变化导致(a)这些建筑物周围的浮雕,(b)Karymskii河和该区域的其他气流,以及(c)温泉中气体的排放和组成。发现新的Piipovskii Springs散发的游离气体中CH_4的浓度以前异常高,并提供了其浓度随时间降低的解释。我们检测到在Karymskii破火山口热液事件中释放的自由气体中don活度OARn(Bq / m〜3)的变化;这些变化与2005-2006年卡林斯基火山的喷发活动一致。我们描述了Karymskii破火山口中的冻土岩石,它们有利于形成冰晶岩带。

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