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In hydrology, brine is a form of salt water, namely, water with relatively high concentration of salt (usually sodium chloride). The brine cropping out at the surface as saltwater springs are known as "licks" or "salines".〔(【引用サイトリンク】url=http://www.dnr.state.oh.us/Portals/10/pdf/GeoFacts/geof07.pdf )〕 The contents of dissolved solids in groundwater vary highly from one location to another on Earth, both in terms of specific constituents (e.g. halite, anhydrite, carbonates, gypsum, fluoride-salts, organic halides, and sulfate-salts) and regarding the concentration level. Using one of several classification of groundwater based on Total Dissolved Solids, brine is water containing more than 100,000 mg/L TDS.〔(【引用サイトリンク】url=http://www.igrac.net/dynamics/modules/SFIL0100/view.php?fil_Id=135 )〕 Brine is commonly produced during well completion operations, particularly after the hydraulic fracturing of a well. == See also == * Brine pool * Brine treatment * Brinicle * Salinity * Sea salt * Seawater 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Brine (hydrology)」の詳細全文を読む スポンサード リンク
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