| 海底沉积物孔隙度与声速的关系 |
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| 引用本文： | 唐永禄.海底沉积物孔隙度与声速的关系[J].海洋学报,1998,20(6):39-43. |
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| 作者姓名： | 唐永禄 |
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| 作者单位： | 中国科学院声学研究所南海研究站, 海口 570105 |
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| 摘 要： | 给出大陆架海底沉积层中声速(压缩波)Vp依赖于沉积物孔隙度n的一个新的经验公式,该公式当n=100时,Vp=V0,V0为海底水声速.公式的计算值与我国周边大陆架测量值吻合较好,并将其结果与国内外成果作了对比讨论.
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| 关 键 词： | 海底沉积物 物理参量 声速 |
| 收稿时间： | 1997/3/21 0:00:00 |
| 修稿时间： | 1997/7/14 0:00:00 |
The Relationship between porosity of sea bed sediment and sound velocity |
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| Tang Yonglu.The Relationship between porosity of sea bed sediment and sound velocity[J].Acta Oceanologica Sinica (in Chinese),1998,20(6):39-43. |
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| Authors: | Tang Yonglu |
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| Institution: | Research Station of South China Sea, Chinese Academy of Sciences, Haikou 570105 |
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| Abstract: | A new experiential formula of the relationship between the sound velocity Vp Ccompressional wave)in the sea-floor sediments of the continental shelf and its porosity n is given.When n=100,Vp=V0,V0 is sound velocity of sea water closed to sea bed.Experimental results on continental shelf of China neighborhood obtained by this formula are better than those of other formulae. |
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| Keywords: | Sea bed sediment physical parameters sound velocity |
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