概括
深海水可能不和碳酸. 增加的压力显著提高碳酸的和度,影响海洋性,因为有机体溶解.
科学领域:
- 地质化学 地质化学
- 海洋学 海洋学 海洋学
背景情况:
- 碳酸和度对于海洋碳酸系统至关重要.
- 海洋压力随着深度而显著变化,可能会影响化学平衡.
研究的目的:
- 为了研究水静压对碳酸的和度的影响.
- 评估对深海化学和性的影响.
主要方法:
- 在不同压力 (1和1000大气压) 的溶液中平衡阿拉贡石卵石.
- 在不同的压力条件下测量碳酸的和度.
主要成果:
- 与1大气相比,碳酸的和度在1000大气中增加了大约2.7倍.
- 这种取决于压力的和表明深海水可能不和.
结论:
- 对于碳酸来说,深海水可能不和.
- 沉没的石灰质生物的溶解可能会增加深海环境中的海洋性.
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