On the problem of variability in the chemical composition of mud–volcanic waters: Evidence from the Yuzhno-Sakhalinsk mud volcano
On the problem of variability in the chemical composition of mud–volcanic waters: Evidence from the Yuzhno-Sakhalinsk mud volcano
复制标题
关于泥火山水化学成分变异性的问题：来自南萨哈林斯克泥火山的证据
DOI：
10.1134/s1819714017010031
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发表时间：
2017
影响因子：
0.8
通讯作者：
V. Ershov
中科院分区：
文献类型：
--
作者：
V. Ershov
考虑了2010-2014年对尤日诺-萨哈林斯克泥火山的水文地球化学观测结果。泥火山沃茨样品的化学分析是在不同的分析中心进行的，这类似于不同研究人员获得火山水化学数据的常见情况。结果表明，泥火山沃茨的化学成分在时间和空间上（对于火山的不同狮鹫）是相对稳定的。这使我们能够确定水文地球化学指标的特征范围。对于每一年的观测，Na，Mg，Ca，K和HCO 3浓度的变异系数大多在10 - 30%之间。然而，单个样品中分析的浓度可能彼此显著不同。这些自然变化可能是水化学数据解释中的错误来源。此外，有必要说明泥火山沃茨作为分析化学调查对象的具体情况。
The results of hydrogeochemical observations on the Yuzhno-Sakhalinsk mud volcano in 2010–2014 are considered. The chemical analysis of samples of mud–volcanic waters was carried out at various analytical centers, which is similar to the common situation where hydrochemical data for a volcano are obtained by different researchers. It is shown that the chemical composition of the mud–volcanic waters is relatively stable in time and space (for different gryphons of the volcano). This allows us to determine the characteristic range of hydrogeochemical indicators. For each year of observations, the coefficients of variation for the concentrations of Na, Mg, Ca, K, and HCO3mostly range from 10 to 30%. However, the concentrations analyzed in individual samples may differ significantly from each other. These natural variations are a likely source of errors in the interpretation of hydrochemical data. In addition, it is necessary to account for the specifics of mud–volcanic waters as an object of analytical chemical investigations.
影响因子：
5
作者：
GIGGENBACH, WF
通讯作者：
GIGGENBACH, WF