水层和沿海海洋之间的水交换中的季节性振荡
Holly A Michael1, Ann E Mulligan, Charles F Harvey
1Department of Civil and Environmental Engineering, MIT, Cambridge, Massachusetts 02139, USA.
Nature
|August 27, 2005
概括
海底地下水排放会将盐水释放到沿海地区. 由于内陆水表变化导致的淡水-盐水界面的季节性变化,解释了这种盐水排放及其时间.
科学领域:
- *沿海水文地质学和海洋学.
- *地球化学和环境科学.
背景情况:
- *海底地下水排放 (SGD) 是陆地和海洋水进入沿海地表水的重要途径.
- * SGD为沿海海洋提供营养,污染物和微量元素.
- *观察到的盐水排放和地化学痕迹表明与内陆充电周期的断开,表明时间滞后.
研究的目的:
- * 调查控制性海底地下水排放的机制.
- * 为了解释内陆充电和海水中的盐水排放之间观察到的时间间隔.
- * 为了证明季节性水文循环与沿海水库盐水系统之间的联系.
主要方法:
- * 在马萨诸塞州瓦科伊特湾 (Waquoit Bay) 实地测量了水力梯度和海上流动.
- * 开发和应用一个通用的沿海地下水系统模型.
- *分析淡水-盐水界面动态,以应对水表波动.
主要成果:
- *淡水和盐水界面的季节性变化解释了大量的盐水排放.
- *海水在冬季被吸入含水层 (接口向陆地移动),夏季被排放 (接口向海移动).
- * 盐水排放落后于季节性内陆充电周期.
结论:
- *内陆的季节性水文循环与沿海水层的盐水地下水系统直接相关.
- * 淡水-盐水界面的运动是季节性盐水SGD的关键驱动因素.
- * 这种机制表明,沿海水域的化学物质装载具有显著的季节性.
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