花崗岩地帯湧水の化学組成に関する一考察 A study on the chemical composition of ground waters from granitic areas

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Powdered granitic rocks were allowed to react with distilled water under various conditions to estimate the formation mechanism of natural waters from granitic area and to discuss on the factors influencing the chemical composition of the waters. The experimental results indicate that the chemical composition and pH of the waters are influenced by the kind of granitic rocks, the water/rock ratio and P<sub>CO<sub>2</sub></sub>. The alkaline ground waters may result from the reactions of granitic rocks with the waters having low P<sub>CO<sub>2</sub></sub>. The ground waters from granitic areas where CO<sub>2</sub> from underground occurs abundantly are neutral or weak acidic, and their major species are Na<sup>+</sup>, Ca<sup>2+</sup>, HCO<sub>3</sub><sup>-</sup>. The proportion of the components is nearly equal to that of the surface waters. The percolation time of ground waters in granitic areas was inferred to be relatively short because of the high permeability of water into granitic rocks and low content of dissolved species. Accordingly, the metastable alminosilicates produced during the incongruent dissolution of granitic rocks, may control the chemical composition and pH of the ground waters.

収録刊行物

  • 地球化学

    地球化学 14(2), 69-76, 1981

    一般社団法人日本地球化学会

被引用文献:  4件中 1-4件 を表示

各種コード

  • NII論文ID(NAID)
    110008679708
  • NII書誌ID(NCID)
    AN00141280
  • 本文言語コード
    JPN
  • 資料種別
    雑誌論文
  • ISSN
    0386-4073
  • NDL 記事登録ID
    2291467
  • NDL 刊行物分類
    ME34(水文学--陸水)
  • NDL 雑誌分類
    ZM41(科学技術--地球科学)
  • NDL 請求記号
    Z15-645
  • データ提供元
    CJP引用  NDL  NII-ELS  J-STAGE 
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