| MENG JINSHENG,GUAN DINGHUA.ESTIMATION OF THE ATTENUATION OF SOUND IN MARINE SEDIMENTS BY NORMALLY-INCIDENT PULSES[J].Acta Oceanologica Sinica,1985,(4):503-509 |
| ESTIMATION OF THE ATTENUATION OF SOUND IN MARINE SEDIMENTS BY NORMALLY-INCIDENT PULSES |
| ESTIMATION OF THE ATTENUATION OF SOUND IN MARINE SEDIMENTS BY NORMALLY-INCIDENT PULSES |
| 投稿时间:1984-05-05 修订日期:1985-01-08 |
| DOI: |
| 中文关键词: |
| 英文关键词: |
| 基金项目: |
|
| 摘要点击次数: 843 |
| 全文下载次数: 597 |
| 中文摘要: |
| A method of remote sensing of attenuation coefficient of sound wave in marine sediments is proposed in this paper.Under certain conditions the echo envelope has an exponential decay EXP(-βCt).When the frequency is high enough,the exponential decay would be the dominant factor in the shape of the echo envelope.Therefore,the attenuation coefficient can be estimated from the envelope.The echo as a function of time is deduced on the basis of a small-scale layering model of marine sediments.The deduction can be regarded as a description of the mechanism of the volume-scattering of high-frequency sound in marine sediment.Experiments at sea are described,and the results are given. |
| 英文摘要: |
| A method of remote sensing of attenuation coefficient of sound wave in marine sediments is proposed in this paper.Under certain conditions the echo envelope has an exponential decay EXP(-βCt).When the frequency is high enough,the exponential decay would be the dominant factor in the shape of the echo envelope.Therefore,the attenuation coefficient can be estimated from the envelope.The echo as a function of time is deduced on the basis of a small-scale layering model of marine sediments.The deduction can be regarded as a description of the mechanism of the volume-scattering of high-frequency sound in marine sediment.Experiments at sea are described,and the results are given. |
|
查看全文
查看/发表评论 下载PDF阅读器 |
| 关闭 |