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海底声学原位测试声速提取技术研究
引用本文:李红星,陶春辉,刘财,邓显明,周建平,张金辉,顾春华,何拥华.海底声学原位测试声速提取技术研究[J].海洋科学进展,2007,25(4):474-479.
作者姓名:李红星  陶春辉  刘财  邓显明  周建平  张金辉  顾春华  何拥华
作者单位:1. 国家海洋局,第二海洋研究所,浙江,杭州,310012;国家海洋局,海底科学重点实验室,浙江,杭州,310012;吉林大学,地球探测科学与技术学院,吉林,长春,130026
2. 国家海洋局,第二海洋研究所,浙江,杭州,310012;国家海洋局,海底科学重点实验室,浙江,杭州,310012
基金项目:国家高技术研究发展计划——海底物理原位测试系统(2002AA615130、2005AA615040),国家自然科学基金资助项目——天山兴安岭和锡霍特断褶系地壳精细结构及其动力学意义(40574042),国家海洋局青年基金资助项目——基于小波分析的浅剖资料精细后处理技术研究(903-01)
摘    要:海底沉积物的声学声速特性是沉积物声学中的一个重要的研究方向。正确提取声学原位测量的声速对海底沉积物声学反演至关重要。分析了海底声学原位测试系统的输出子波特性,提出了基于子波提取的互相关双向极值声速提取法。在声速提取过程中,发现某些通道实测声波到达时会出现超出正常范围的异常。分析后认为异常通道的到达波相位出现180°反至现象。通过互相关数值的负极小值提取的声波到达时对互相关正极大值所获得的到达时曲线进行校正后提取声速,得到了正确的结果,说明了本方法的正确性。

关 键 词:海底声学原位测试系统  声速提取  互相关双向极值法  换能器源  海底沉积物声学特征
文章编号:1671-6647(2007)04-0474-06
修稿时间:2006-11-13

Study on Sound Speed Picking-up Technique by Geoacoustically Measuring In-situ Marine Sediment
LI Hong-xing,TAO Chun-hui,LIU Cai,DENG Xian-ming,ZHOU Jian-ping,ZHANG Jin-hui,GU Chun-hua,HE Yong-hua.Study on Sound Speed Picking-up Technique by Geoacoustically Measuring In-situ Marine Sediment[J].Advances in Marine Science,2007,25(4):474-479.
Authors:LI Hong-xing  TAO Chun-hui  LIU Cai  DENG Xian-ming  ZHOU Jian-ping  ZHANG Jin-hui  GU Chun-hua  HE Yong-hua
Institution:1. Second Institute of Oceanography, SOA , Hangzhou 310012, China; 2. Key Lab of Submarine Geosciences, SOA, Hangzhou 310012, China; 3. College of Geo-exploration Science and Technology, Jilin University, Changchun 130026, China
Abstract:The marine sediment acoustic characteristics are an important research direction in sediment acoustics,and the correct pick-up of in-situ marine sediment sound speed is of great importance to the marine sediment acoustics inversion.In this paper,the output wavelet characterisitics of in-situ marine sediment geoacoustic measuring system are analyzed,and a cross-correlation two-way extreme value sound speed picking-up method based on wavelet pick-up is then proposed.In the sound speed pick-up process,it is shown that the anomalies of measured sound wave arrival times for some channels occurred,and it is concluded that the arrival sound wave phases for the abnormal channels are reversed.The sound wave arrival time curve obtained by finding the cross-correlation positive maxima is rectified by the sound wave arrival times obtained by finding the cross-correlation negative minima to pick-up the sound speed,and correct results are obtained,which indicates the correctness of this method.
Keywords:in-situ marine sediment geoacoustic measuring system  sound speed pick-up  cross-correlation two-way extreme value method  source transducer  marine sediment acoustic characteristics
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