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首页> 外文会议>International Conference on Earth Science, Mineral, and Energy >Brackishwater in the Jambakan area: Where did they come from? (geoelectric and geohydrology analysis)
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Brackishwater in the Jambakan area: Where did they come from? (geoelectric and geohydrology analysis)

机译：吉宾山区的Brackishwater：他们来自哪里？ （电气电和地析液分析）

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摘要

Jambakan is a village in Bayat District, Klaten Regency, Central Java Province, Indonesia. Brackishwater exists in the aquifers of study area, even though the location is ±30 km apart from the sea. In light of this, scientific discussion on where this water comes from is deemed necessary. The groundwater quality analysis at the local wells, detected brackishwater existence in shallow aquifers at the depths of 5-8 m. The geoelectrical method using the Schlumberger and dipole-dipole electrode configurations screened for any aquifers vertically and horizontally. The results showed that aquifers were distributed discontinuously, for which they were interpreted as fan alluvial deposits in shallow seas or molasses accumulations on the land. The interpretation also revealed that the brackishwater resulted from contacts with minerals in seawater sediments that composed the aquifers in this village.
机译：jambakan是印度尼西亚中爪哇省克拉滕地区的巴特特区的一个村庄。 淡淡淡的学习区的含水层存在，即使位置除了海外的位置±30公里。 鉴于此，科学讨论被认为是必要的。 局部井的地下水质量分析，在5-8米的深度检测到浅含水层中的淡咸水存在。 使用钢板和偶极偶极电极配置的电气测电料垂直和水平筛选任何含水层。 结果表明，含水层不连续分布，它们被解释为浅海或糖蜜积累的风扇冲积沉积物。 解释还揭示了咸水潜水员与海水沉积物中的矿物接触，这些沉积物在这个村庄组成了含水层。

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