書誌事項
- タイトル別名
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- Occurrence and Quality of Groundwater in the Tunnels of the Rokko Mountain Area, Kinki District, Japan
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説明
Since 1960, several tunnels were excavated through the Rokko mountain area which is chiefly composed of granitic rocks. The routes of these tunnels are shown in Fig. 1.<BR>The geology and the occurrence of groundwater along each tunnels are shown in Fig. 2-5. So close relations were observed between the fault zones and the fountain of groundwaters, that the groundwater of this area is defined as fissurewater along the fault zone.<BR>The results of chemical analyses of the groundwaters and the surfacewaters in this area are shown in Table 1.2., and water qualities are also summarized in Fig. 6-9. Judging from these results, it is clear that the groundwater is chracterized by heigher alkalinity, heigher pH and being rich in F content than the surfacewater. But, on the other hand, the former is lower in hardness.<BR>No special abnormality of the water quality is recognized in the annual variation diagram (Fig. 10) which were measured at the Rokko tunnel from Apri1, 1967 to Februay, 1970.
収録刊行物
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- 応用地質
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応用地質 12 (1), 16-28, 1971
一般社団法人 日本応用地質学会
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詳細情報 詳細情報について
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- CRID
- 1390282679072101120
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- NII論文ID
- 110003335351
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- NII書誌ID
- AN00026635
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- ISSN
- 18840973
- 02867737
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- データソース種別
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- JaLC
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- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可