节点文献
海底沉积物孔隙度与声速的关系
The Relationship between porosity of sea bed sediment and sound velocity
【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.
【Abstract】 ── A new experiential formula of the relationship between the sound velocity Vp (compressional wave ) in the sea-floor sediments of the continental shelf and its porosity n is given. When n= 100, Vp =V0, V0is 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.
- 【文献出处】 海洋学报(中文版) ,ACTA OCEANOLOGICA SINICA , 编辑部邮箱 ,1998年06期
- 【分类号】P736.213
- 【被引频次】59
- 【下载频次】256