在2016年熊本地震之前和之后,热水中的深层流体
Fumiaki Tsunomori1, Noritoshi Morikawa2, Masaaki Takahashi2
1Geochemical Research Center, Graduate School of Science, The University of Tokyo, 7-3-1 Hongo, Bunkyo, 113-0033, Tokyo, Japan.
Ground water
|February 6, 2024
概括
贵族气体和同位素分析显示,KUM和OTN含水层的深层流体供应稳定,ASO只有深层气体,不受2016年熊本地震的影响.
科学领域:
- 地质化学 地质化学
- 同位素水文学 同位素水文学
- 环境科学 环境科学
背景情况:
- 了解流体来源及其稳定性对于含水层管理至关重要.
- 2016年熊本地震提供了一个自然实验,以评估对水文地质系统的地震影响.
研究的目的:
- 调查供应给KUM,OTN和ASO含水层的流体的来源和稳定性.
- 为了确定2016年熊本地震对这些含水层系统的影响.
主要方法:
- 对贵重气体 (He,Ne) 度和同位素比率 (3He/4He) 的分析.
- 测量氧- (δD-δ18O) 和/ (Li/Cl) 同位素的比率.
- 长期 (2013-2021) 监测离子组成和流体化学.
主要成果:
- 稳定的3He/4He比率表明,所有地点的深层气体供应都是一致的.
- 4He/20Ne比率表明KUM和OTN的表面流体贡献减少,但在ASO稳定.
- δD-δ18O和Li/Cl关系证实了KUM和OTN的稳定深水供应,以及所有地点的稳定充电.
- 在监测参数中没有检测到2016年熊本地震的地震影响.
结论:
- KUM和OTN含水层从熊本地区下方接收持续的深层流体供应.
- ASO水层主要由深沉的天然气供应.
- 水库流体供应动态保持稳定,并没有受到2016年熊本地震或其余震的影响.
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