概括
加拉帕戈斯山丘上的热水喷口释放了富含和缺乏的液体. 这表明-的交换反应,并透露流体通过沉积物和山丘的上游速度.
科学领域:
- 地质化学 地质化学
- 海洋地质学海洋地质学
- 水热系统 水热系统
背景情况:
- 加拉帕戈斯山丘水热场位于加拉帕戈斯扩散中心的侧面.
- 海水通过地下玄武岩循环,可能改变其化学成分.
研究的目的:
- 为了研究加拉帕戈斯山丘水热场沉积物孔水的化学成分.
- 了解控制这种独特的热水系统中离子度的过程.
- 为了确定流体通过沉积物和热水上升的速度.
主要方法:
- 从核心样本中分析沉积物孔水化学.
- 和离子梯度的解释.
- 基于化学数据的流体流程建模.
主要成果:
- 在沉积物孔水中观察到高离子和低离子度.
- 有证据表明,海水和玄武岩之间存在-交换反应.
- 非线性离子梯度表明明显的上升速度:在海底沉积物中每年约1厘米,在热水中每年约20厘米.
结论:
- 观察到的离子异常归因于玄武岩-海水交换反应.
- 流体上升的速度在海底沉积物和活跃的热水之间有很大差异.
- 这项研究提供了关于中洋山脊上热水流体循环的动态的见解.
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