摘要
分析了造成波浪衰减几种力学机制,并针对不同模型海底底床下的波浪衰减,以及有限深底床和无限深底床的波浪衰减进行了计算比较,认为造成波浪衰减的力学机制直接和底床砂质的性质相关.
The several mechanisms of wave damping are treated analytically on the different models, and compared finite depth seabed with infinite depth seabed as well. It is found that the mechanism is related to properties of soil directly.
出处
《地球物理学进展》
CSCD
2001年第3期47-52,共6页
Progress in Geophysics
基金
国家自然科学基金项目(19602021)