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Updated: May 23, 2025

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Seawater Sampling and Collection
Published on: June 17, 2009
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水质地质异质性对韩国济州火山岛的淡水和盐水相互作用的影响,韩国
Chang-Seong Koh1, Eun-Hee Koh1, Won-Bae Park1
1Jeju Groundwater Research Center, Jeju Research Institute, Jeju City, Republic of Korea.
Ground water
|March 10, 2025
概括
济州岛的水文地质异质性
科学领域:
- 地球科学 地球科学 地球科学
- 水文地质学 水文地质学
- 火山学 火山学是一门学科.
背景情况:
- 济州岛的沿海含水层系统表现出水地质异质性.
- 了解淡盐水过渡区 (FSTZ) 对沿海含水层管理至关重要.
研究的目的:
- 为了研究FSTZ的形状和潮对济州东部沿海含水层的淡盐水相互作用的影响.
- 开发火山沿海含水层的概念性水文地质模型.
主要方法:
- 来自钻井核心的地质日志的分析.
- 对于特定导电性 (SC) 和温度配置文件的地球物理记录.
- 时间序列分析地下水位和多深度SC数据.
主要成果:
- 在状石层中观察到一个尖的FSTZ,而在岩层中则出现了一个类似阶梯的FSTZ.
- 潮对地下水位的影响与距离海岸的距离相关.
- SC数据显示,受地质结构影响的潮变化的反应取决于深度.
结论:
- 水地质异质性,特别是火山结构,如石和岩,显著控制了FSTZ的发展和淡盐水的动态.
- 状石层中的管道流促进了快速的淡水排放和利的FSTZ.
- 层层的岩结构导致边界流,阶段式的FSTZ,以及明显的潮-SC关系.
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