珠江三角洲及其邻近的架子地下水系统的演变自代晚期以来
Chong Sheng1, Jiu Jimmy Jiao1,2,3, Jinpeng Zhang4
1Department of Earth Sciences, The University of Hong Kong, Hong Kong, China.
Science advances
|April 10, 2024
概括
在珍珠河三角洲内陆盐水和海上淡地下水共存. 古地质模型显示,这是由于地质时间的海水入侵和低淡水形成交替而发生的.
科学领域:
- 水文地质学 水文地质学
- 古气候学 古气候学
- 地质化学 地质化学
背景情况:
- 地下水系统通常假定陆上是淡水,海上是盐水.
- 这项研究调查了珍珠河三角洲含水层系统内陆盐水和新鲜的海上地下水的反直觉共存.
研究的目的:
- 探索内陆架设置中的地下水系统的形成机制和演变.
- 解决有关同一含水层内对比的地下水类型共存的知识差距.
主要方法:
- 进行了广泛的实地研究,以确定地下水的盐分分布.
- 复杂的古水文地质模型模拟地下水系统的演变.
- 分析古气候变化及其对地下水系统的影响.
主要成果:
- 在珍珠河三角洲,内陆盐水和海上新鲜地下水的共存.
- 在普莱斯托时代晚期发现的新鲜地下水形成在海上低.
- 通过全新世纪的过渡确定盐水地下水的形成古海水入侵内陆.
结论:
- 陆地和海上地下水系统在地质时间尺度上呈现交替变化.
- 地下水系统在响应古气候变化时呈现出歇斯底里,显著滞后.
- 古气候强迫对当今的地下水系统有剩余的影响.
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