Experimental Study Of Evolution Of Aqueous Sio2 In The Mineral Water In Basalt Beds Of Jingyu County, China

PROCEEDINGS OF THE FOURTEENTH INTERNATIONAL SYMPOSIUM ON WATER-ROCK INTERACTION, WRI 14(2013)

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摘要
The mineral water in Jingyu County, Jilin Province of China, was selected as the research target. Laboratory water-basalt interaction experiments were conducted to investigate the concentrations and rate of release of aqueous SiO2, a characteristic component in the mineral water from this region. Results show that the release of SiO2 from water-rock interactions conform to a log-log curve law. In 155-day experiments, the amount of SiO2 released from the basalt powder is 138-196 mg/kg, and that from basalt blocks is lower at 46.2-62.6 mg/kg. The pH values tend to be neutral. The electrical conductivity of aqueous solutions tends to increase gradually. The release rate of SiO2 is basically constant at about 0.04-0.14 mg/kg.d after 155 days. The released silica concentrations and rates are functions of rock texture, rock surface area, and reaction time. (C) 2013 The Authors. Published by Elsevier B.V. Selection and/or peer-review under responsibility of Organizing and Scientific Committee of WRI 14-2013
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关键词
basalt,mineral water,HSiO3-,genesis,characteristic component
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