| 南黄海海水中悬浮体跃层及底部浑水层 |
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| 引用本文： | 李凡,徐善民,姜秀珩,宋怀龙.南黄海海水中悬浮体跃层及底部浑水层[J].海洋科学,1991,15(5):42-46. |
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| 作者姓名： | 李凡 徐善民 姜秀珩 宋怀龙 |
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| 作者单位： | 中国科学院海洋研究所，中国科学院海洋研究所，中国科学院海洋研究所，中国科学院海洋研究所 青岛 266071，青岛 266071，青岛 266071，青岛 266071 |
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| 摘 要： | 南黄海海水中悬浮体含量垂向分布中常见有跃层现象,它们是在海浪和潮流综合作用下,由海底表层沉积物的再悬浮产生的。南黄海冷水团促进了浑水层和悬浮体跃层的发育。 浑水层能够改变光、声波在海水中传播的性质,增大海水的浮力,增强对海底的侵蚀力。
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| 关 键 词： | 南黄海 海水 悬浮体 跃层 浑水层 |
| 收稿时间： | 8/2/1990 12:00:00 AM |
SUSPENDED-CLINE AND LOWER TURBID WATER IN SEAWATER IN THE SOUTE YELLOW SEA |
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| Li Fan,Xu Shanmin,Jiang Xiuhang and Song Huailong.SUSPENDED-CLINE AND LOWER TURBID WATER IN SEAWATER IN THE SOUTE YELLOW SEA[J].Marine Sciences,1991,15(5):42-46. |
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| Authors: | Li Fan Xu Shanmin Jiang Xiuhang and Song Huailong |
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| Abstract: | Suspended-cline and lower turbid water always present in vertical distribution of suspended matter in sea water in the South Yellow Sea. They had been seen in data not only in the South Yellow Sea, but also in other sea areas, such as continental shelf and slope water off the north-eastern U. S.. They are formed by fesuspension of bottom sediments under influence of water and tidal current. In addition, South Cold Water Mass promote develope of the suspended-cline and lower turbid water.Turbid water can change propagative properties of the light and acoustic wave, increase buoyancy of sea water and strengthen erosive activity to sea floor. |
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| Keywords: | Suspended-cline Turbid water |
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