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南黄海中部海底沉积物原位声速与物理性质相关关系
引用本文:阚光明,苏元峰,李官保,刘保华,孟祥梅.南黄海中部海底沉积物原位声速与物理性质相关关系[J].海洋学报,2013,35(3):166-171.
作者姓名:阚光明  苏元峰  李官保  刘保华  孟祥梅
作者单位:国家海洋局第一海洋研究所, 山东 青岛 266061;国家海洋局海洋沉积与环境地质重点实验室, 山东 青岛 266061;国家海洋局第一海洋研究所, 山东 青岛 266061;国家海洋局海洋沉积与环境地质重点实验室, 山东 青岛 266061;国家海洋局第一海洋研究所, 山东 青岛 266061;国家海洋局海洋沉积与环境地质重点实验室, 山东 青岛 266061;国家深海基地管理中心, 山东 青岛 266061;国家海洋局第一海洋研究所, 山东 青岛 266061;国家海洋局海洋沉积与环境地质重点实验室, 山东 青岛 266061
基金项目:国家自然科学基金资助项目(41106061);国家海洋局青年基金资助项目(2012318)。
摘    要:基于在南黄海中部获得的海底沉积物原位声速数据,分析讨论了原位声速与密度、含水量、孔隙比、孔隙度等沉积物物理性质参数的相关关系。通过回归分析建立了海底沉积物原位声速预测方程。结果表明,原位声速与上述物理参数之间具有良好的相关性,相关系数r均大于0.93。对比分析了原位声速预测方程与甲板声速预测方程的差异,两者最小相差15.8 m/s,最大相差31.3 m/s,平均差值约为22.6 m/s。将原位声速预测方程与其他研究者建立的声速预测方程进行了对比,结果表明不同声速预测方程存在明显差异,初步分析了存在差异的原因。

关 键 词:沉积物声速  原位测量  物理性质  声速预测方程  南黄海

The correlations between in-situ sound speeds and physical parameters of seafloor sediments in the middle area of the southern Huanghai Sea
KAN Guangming,SU Yuanfeng,LI Guanbao,LIU Baohua and MENG Xiangmei.The correlations between in-situ sound speeds and physical parameters of seafloor sediments in the middle area of the southern Huanghai Sea[J].Acta Oceanologica Sinica (in Chinese),2013,35(3):166-171.
Authors:KAN Guangming  SU Yuanfeng  LI Guanbao  LIU Baohua and MENG Xiangmei
Institution:First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China;Key Laboratory of State Oceanic Administration for Marine Sedimentology and Environmental Geology, State Oceanic Administration, Qingdao 266061, Chnia;First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China;Key Laboratory of State Oceanic Administration for Marine Sedimentology and Environmental Geology, State Oceanic Administration, Qingdao 266061, Chnia;First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China;Key Laboratory of State Oceanic Administration for Marine Sedimentology and Environmental Geology, State Oceanic Administration, Qingdao 266061, Chnia;National Deep Sea Center, State Oceanic Administration, Qingdao 266061, Chnia;First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China;Key Laboratory of State Oceanic Administration for Marine Sedimentology and Environmental Geology, State Oceanic Administration, Qingdao 266061, Chnia
Abstract:Based on the sound speeds of seafloor sediments measured in-situ in the middle area of the southern Huanghai Sea, the correlations between the in-situ sound speeds and the physical parameters of seafloor sediments such as density, moisture content, porosity ratio and percent porosity are analyzed.The predicting equations of the in-situ sound speeds are established by means of a regression analysis.The result shows that there are good correlations between the in-situ sound speeds and the physical parameters with the coefficients r>0.95.The comparison between the predicting equations of the in situ sound speeds and those established based on the sound speeds measured in laboratory on board indicates that their average deviation is 22.6 m/s with a minimum of 15.8 m/s and a maximum of 31.3 m/s.The comparison between the predicting equations of the in-situ sound speeds and those developed by other authors demonstrates a distinct difference among the different predicting equations of sound speeds, and the reasons are discussed
Keywords:sound speed of seafloor sediment  in situ measurements  physical properties  predicting equations of sound speed  the southern Huanghai Sea
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