概括
地下化水显示和之间的线性关系,由页岩过海水和淡水解释. 矿物反应,比如dolomitization,也会给这些水添加.
科学领域:
- 地质化学 地质化学
- 水文地质学 水文地质学
- 沉积地质学的地质学
背景情况:
- 地下水的化学成分受到岩石构成的相互作用的影响.
- 了解像和化物这样的溶解离子的起源对于解释水文地质过程至关重要.
研究的目的:
- 为了解释在地下化水中观察到的和化物之间的线性关系.
- 确定控制这些水的化学成分的主要机制.
主要方法:
- 使用日志图谱分析 (Ca++) 和 (Br-) 度之间的关系.
- 解释水岩相互作用,包括超过和矿物反应.
主要成果:
- 在地下化水中,log Ca++和log Br-之间发现了线性相关性.
- 作为一个关键的过程,确定了原始海水和入的淡水的页岩超过.
- 与沉积矿物质的多洛米化和其他反应为溶液提供额外的Ca ++.
结论:
- 地下化水的化学演变是物理 (超) 和化学 (矿物反应) 过程的结果.
- 页岩超过在缩某些离子方面发挥着重要作用.
- 矿物沉积物的相互作用,特别是多洛米化,是重要的二次来源.
相关概念视频
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