scholarly journals The Hydrogeochemical Characteristic of Mineral Water Associated with Water-rock Interaction in Jingyu County, China

2017 ◽  
Vol 17 ◽  
pp. 726-729 ◽  
Author(s):  
Qian Zhang ◽  
Xiujuan Liang ◽  
Changlai Xiao
Keyword(s):  
Mineral Water ◽  
Rock Interaction ◽  
Hydrogeochemical Characteristic ◽  
Water Rock Interaction

Groundwater anomaly related to the 2018 Hokkaido Eastern Iburi earthquake in Northern Japan

2020 ◽  
Author(s):  
Yuji Sano ◽  
Takanori Kagoshima ◽  
Naoto Takahata ◽  
Kotaro Shirai ◽  
Jin-Oh Park ◽  
...  
Keyword(s):  
Mineral Water ◽  
Seismic Event ◽  
Rock Interaction ◽  
Carbonate Concentration ◽  
C Value ◽  
D Values ◽  
Isotopic Variations ◽  
Bottled Mineral Water ◽  
Water Rock Interaction ◽  
Northern Japan

<p>In order to study groundwater anomaly related to the 2018 Hokkaido Eastern earthquake (Mw6.6) occurred on 6<sup>th</sup> September, we have measured δD and δ<sup>18</sup>O values of commercial bottled mineral water at two sites in Iburi region, Hokkaido, Northern Japan from June 2015 to May 2019. At the Uenae site, 21km west of the epicenter, both δD and δ<sup>18</sup>O values are constant from June 2015 to February 2018. Then these values have decreased substantially from April 2018 to December 2018 with significant fluctuations. These variations may be attributable to a mixing of groundwater with light δD and δ<sup>18</sup>O values. At the Eniwa site 34km northwest of the epicenter, δD values have decreased slightly and monotonically, while δ<sup>18</sup>O values are constant from June 2016 to October 2018. Observed isotopic variations of the Uenae site are different from those found at the 2016 Tottori earthquake where the δ<sup>18</sup>O value of groundwater increased a couple of months before the seismic event, while the δD value was constant. These data were attributable to water-rock interaction in the aquifer. Thus, the mechanism of groundwater isotopic anomaly may be different between Tottori and Hokkaido earthquakes. In addition to the M6.7 earthquake, CO<sub>2</sub> injection by CCS project at Tomakomai, 13km southwest of the Uene site may be another factor to induce such variations. In order to evaluate the environmental impact of CO<sub>2</sub> injection, we should measure total carbonate concentration and δ<sup>13</sup>C value of carbonate at both sites. Then we will discuss mechanism of groundwater anomaly.</p>

scholarly journals Recharge of natural mineral water Jingyu County, northeastern China

2019 ◽  
Vol 98 ◽  
pp. 01032
Author(s):  
Xiujuan Liang ◽  
Hui Tian ◽  
Changlai Xiao ◽  
Mingqian Li ◽  
Ying Sun ◽  
...  
Keyword(s):  
Stable Isotope ◽  
Mineral Water ◽  
Atmospheric Precipitation ◽  
Northeastern China ◽  
Average Residence Time ◽  
Rock Interaction ◽  
Natural Mineral ◽  
Natural Mineral Water ◽  
Basaltic Aquifer ◽  
Water Rock Interaction

A light stable isotope investigation of the source of natural mineral water in Jingyu County indicates an origin predominantly from atmospheric precipitation. As water-rock interaction occurs in the runoff process, SiO2 in the basaltic aquifer is dissolved, forming a metasilicate-type mineral water. The average residence time of natural mineral water in the stratum is 20 to 56 years.

scholarly journals Sources of metasilicate in mineral water of Jingyu County, northeastern China

2019 ◽  
Vol 98 ◽  
pp. 01052
Author(s):  
Changlai Xiao ◽  
Yajie Yuan ◽  
Xiujuan Liang ◽  
Weifei Yang ◽  
Ying Sun
Keyword(s):  
Release Rate ◽  
Mineral Water ◽  
Northeastern China ◽  
The Other ◽  
Changbai Mountains ◽  
Rock Interaction ◽  
Immersion Experiment ◽  
Hydrolysis Of ◽  
Water Rock Interaction

The source of metasilicate in mineral water of Jingyu County. located in Changbai Mountains of northeastern China, was analysed through two groups of water-rock interaction experiments. One is a hydrolysis immersion experiment using basalt and the other is an immersion experiment utilizing a mixture of soil, scoria, and clastic basalt under the same conditions. Results indicate that the metasilicate in mineral water is mainly derived from the hydrolysis of silicates and silica in the basalt, scoria, and soil. In the first immersion experiment, the release of metasilicate is linear, with dissolved metasilicate increasing continuously through time at a stable release rate of about 0.01 mg/(kg·day). The second experiment indicates that the contribution of soil and scoria to metasilicate in mineral water is higher than that of clastic basalt under the same conditions.

87SR/86SR, δ18O AND NOBLE GASES AS TRACERS OF WATER-ROCK INTERACTION IN THE THEISTAREYKIR GEOTHERMAL FIELD

2020 ◽  
Author(s):  
Marie Haut-Labourdette ◽  
◽  
Daniele Pinti ◽  
André Poirier ◽  
Marion Saby ◽  
...  
Keyword(s):  
Noble Gases ◽  
Geothermal Field ◽  
Rock Interaction ◽  
Water Rock Interaction

scholarly journals Geochemical and isotopic evidence of groundwater salinization processes in the Essaouira region, north-west coast, Morocco

2021 ◽  
Vol 3 (7) ◽  
Author(s):  
Otman EL Mountassir ◽  
Mohammed Bahir ◽  
Driss Ouazar ◽  
Abdelghani Chehbouni ◽  
Paula M. Carreira
Keyword(s):  
Groundwater Recharge ◽  
West Coast ◽  
Exchange Process ◽  
Environmental Isotopes ◽  
Annual Rainfall ◽  
Groundwater Salinization ◽  
Rock Interaction ◽  
North West ◽  
The North ◽  
Water Rock Interaction

AbstractThe city of Essaouira is located along the north-west coast of Morocco, where groundwater is the main source of drinking, domestic and agricultural water. In recent decades, the salinity of groundwater has increased, which is why geochemical techniques and environmental isotopes have been used to determine the main sources of groundwater recharge and salinization. The hydrochemical study shows that for the years 1995, 2007, 2016 and 2019, the chemical composition of groundwater in the study area consists of HCO3–Ca–Mg, Cl–Ca–Mg, SO4–Ca and Cl–Na chemical facies. The results show that from 1995 to 2019, electrical conductivity increased and that could be explained by a decrease in annual rainfall in relation to climate change and water–rock interaction processes. Geochemical and environmental isotope data show that the main geochemical mechanisms controlling the hydrochemical evolution of groundwater in the Cenomanian–Turonian aquifer are the water–rock interaction and the cation exchange process. The diagram of δ2H = 8 * δ18O + 10 shows that the isotopic contents are close or above to the Global Meteoric Water Line, which suggests that the aquifer is recharged by precipitation of Atlantic origin. In conclusion, groundwater withdrawal should be well controlled to prevent groundwater salinization and further intrusion of seawater due to the lack of annual groundwater recharge in the Essaouira region.

scholarly journals Water–rock interaction and the concentrations of major, trace, and rare earth elements in hydrocarbon-associated produced waters of the United States

2021 ◽  
Author(s):  
Carleton R. Bern ◽  
Justin E. Birdwell ◽  
Aaron M. Jubb
Keyword(s):  
United States ◽  
Rare Earth ◽  
Rare Earth Elements ◽  
Water Chemistry ◽  
Produced Water ◽  
The United States ◽  
Rock Interaction ◽  
Produced Waters ◽  
Water Rock Interaction

Comparisons of hydrocarbon-produced waters from multiple basins and experiments using multiple shales illustrate water–rock interaction influence on produced water chemistry.

Modeling water-rock interaction in the surficial environment: The role of precursors, nucleation, and Ostwald ripening

1990 ◽  
Vol 84 (1-4) ◽  
pp. 322-325 ◽  
Author(s):  
C.I. Steefel ◽  
P. Van Capellen ◽  
K.L Nagy ◽  
A.C. Lasaga
Keyword(s):  
Ostwald Ripening ◽  
Rock Interaction ◽  
Water Rock Interaction
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