摘要
吉林省靖宇县四海泉矿泉水赋存在第四系下更新统军舰山组玄武岩中,为偏硅酸矿泉水,偏硅酸质量浓度达38.1 mg/L。矿泉水清澈透明,无臭和味,色度<5无异色,浑浊度0.1/NTU,阳离子钠质量浓度为5.86 mg/L,钙离子质量浓度14.82 mg/L,镁离子质量浓度6.36 mg/L,可溶性总固体为168 mg/L,水化学类型为重碳酸钙型水。水质达到了《饮用天然矿泉水》规范标准要求。
Sihaiquan natural mineral water occurs in the basalt of Junjianshan Formation, lower pleistocene, Quaternary ,which belongs to metasilicate mineral water, metasilicate concentration reached 38.1mg/L. Mineral water is clear, no odor and unusual taste, chromaticity＆lt;5, without unusual color , turbidity 0.1/NTU, sodium cation concentration is 5.86 mg/L, calcium ion mass concentration of 14.82 mg/L, magnesium ion mass concentration of 6.36 mg/L, total soluble solids is 168 mg/L, hydrochemical type is heavy calcium carbonate type . Water quality has reached the＆quot;drinking natural mineral water＆quot;standard requirements.
出处
《吉林地质》
2014年第4期84-86,共3页
Jilin Geology
关键词
偏硅酸型矿泉水
玄武岩
勘查评价
metasilicate mineral water
basalt
exploration and evaluation
