摘要
Theprincipleofthespatialcorrelationcharacteristicsofsea-bottombackscatteringwasexpounded.TheKirchhoffmodelisintroducedtosimulatesea-bottombackscatteringandthespatialcorrelationiscalculated.Somesedimentcharacteristicparameters,suchastheratioofsedimentmassdensitytowatermassdensity,theratioofsedimentsoundspeedtowatersoundspeed,theattenuationcoefficientofsoundwaves,thestrengthandexponentofseabottominterfaceroughnessspectrum,areconsideredwhilesimulatingandtheirinfluencesonspatialcorrelationareanalyzed.Byestablishingtheexpressionsofthesedimentcharacteristicparameterswiththelogarithmicsedimentgrainsize,thevariationtendencyofthespatialcorrelationversusthelogarithmicsedimentgrainsizeisobtained.Thewidthofthemajorlobeofthespatialcorrelationfunctionnarrowsasthelogarithmicsedimentgrainsizeincreases.Thecomparisonsbetweensimulateddataandin-situdatacollectedinOctober2007haveproventhattheirspatialcorrelationfunctionwaveformsagreewellunderthesamesedimentcharacteristics.
出版日期
2012年03月13日（中国期刊网平台首次上网日期，不代表论文的发表时间）
