Chemical-physical and dissolved gases in Etnean groundwater: data from Cherubino (S65) spring (Santa Maria di Licodia- CT)

Abstract: Groundwater chemical-physical data in the spring (Cherubino fountain – Santa Maria di Licodia, CT) located southwest of the Etna volcano (Gen 2009-Dec 2018), belonging to the Etna geochemical surveillance network (named S65) of the Istituto Nazionale di Geofisica e Vulcanologia (INGV). Data have been acquired by a water station equipped with multiparameter sensors. Dissolved CO2 (CO2c) has been re-calculated by mean of an algorithm (De Gregorio et al. 2011) using the raw data (CO2_0 and CO2_1).

Other Description: Federico C., Longo M., D'Alessandro W., Bellomo S., Bonfanti S., Brusca L., (2017), “Hydrological versus volcanic processes affecting fluid circulation at Mt. Etna: Inferences from 10 years of observations at the volcanic aquifer.” Chemical Geology, Volume (452): 71-84

摘要：本数据集涵盖埃特纳火山（Etna volcano）西南侧的凯鲁比诺泉（Cherubino fountain，位于圣玛丽亚迪利科迪亚，卡塔尼亚省，CT）2009年1月至2018年12月的地下水理化数据，该站点隶属于意大利国家地球物理与火山学研究所（Istituto Nazionale di Geofisica e Vulcanologia, INGV）搭建的埃特纳地球化学监测网络（命名为S65）。数据由搭载多参数传感器的水文站采集。溶解态二氧化碳（CO₂c）已借助算法（De Gregorio等，2011），利用原始数据（CO₂_0与CO₂_1）重新计算得到。

其他说明：Federico C.、Longo M.、D'Alessandro W.、Bellomo S.、Bonfanti S.、Brusca L.（2017），《影响埃特纳火山流体循环的水文与火山过程——基于火山含水层10年观测的推断》，《化学地质》（Chemical Geology），第452卷：71-84页。