| 摘要: |
| 黄海夏季深层冷水(简称黄海冷水), 又称为黄海冷水团, 已为海洋物理学家进行过较多的研究。该水域化学研究开展较晚，近年来顾宏堪首先报道了黄海夏季溶解氧垂直分布最大值与黄海冷水密切相关。黄海冷水与其它水团一样，理、化、生物等特性是相互关联的统一体。遗憾的是，迄今尚未见到有关于此的多学科综合性的研究报道。
本文根据1959年海洋调查资料，对黄海冷水域主断面水文化学要素的垂直分布特性进行了研究，并讨论了该冷水形成及诸参数变化的原因。 |
| 关键词: 黄海冷水域 水化学要素 垂直分布 |
| DOI： |
| 分类号: |
| 基金项目:中国科学院海洋研究所调查研究报告第1008号 |
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| THE VERTICAL DISTRIBUTION OF THE CHEMICAL FACTORS IN THE YELLOW SEA COLD WATER |
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Diao Huanxiang, Shen Zhiliang
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Institute of Oceanology, Academia Sinica
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| Abstract: |
| This paper shows that the Yellow Sea (summer) Cold?water is formed from winter by the conservative property of the temperature in the deep water. The vertical distribution of various physic-chemical parameters in winter are in uniform condition. In summer, the vertical distribution of σt, P04-P and SiO3-Si increases with the depth and the maximum value of O2 and pH appears near the lower limit of thermocline. Causes of variation of various parameters are also discussed. |
| Key words: THE VERTICAL DISTRIBUTION CHEMICAL FACTORS THE YELLOW SEA COLD WATER |
