资源描述:
《浙江朱家尖岛砾石海滩沉积物分布及形态特征》由会员上传分享,免费在线阅读,更多相关内容在行业资料-天天文库。
1、南京大学学报(自然科学)第40卷第6期Vol.40,No.6JOURNALOFNANJINGUNIVERSITY2004年11月Nov.,2004(NATURALSCIENCES)X浙江朱家尖岛砾石海滩沉积物分布及形态特征XX王爱军,高抒,杨(南京大学海岸与海岛教育部重点实验室,南京,210093)摘要:砾石海滩是波浪作用下形成的海岸地貌类型.在浙江朱家尖岛的大乌石塘和小乌石塘两处口袋状砾石滩,采集了砾石滩不同部位的沉积物样品.根据样品的粒度分析和颗粒形态分析,发现砾石滩沉积物粒度参数及砾石形态参数在横向和纵向上的分布特征为
2、:横向上,砾石平均粒径由陆向海递减,分选变好,扁长度及杆状程度由砾石堤顶部向海递增,球度以潮间带为最低;纵向上,大乌石塘砾石粒径由湾顶向南北两个方向递减,分选变好,球度降低,杆状程度提高,而小乌石塘砾石粒径由海滩南部向北递减,分选先变好再变差,球度减小,扁长度及杆状程度提高.小乌石塘海滩顶部砾石对应的水深为5m、周期为10s临界起动轨迹流速和临界波高分别为3.28m/s和4.84m,大乌石塘的临界起动轨迹流速、临界波高分别为3.17m/s和4.69m.砾石形态参数和平均粒径的变率分析表明,小乌石塘在横向上的磨蚀作用的效应略强
3、于搬运作用,而在纵向上却略弱于搬运作用;大乌石塘的海滩砾石主要发生磨蚀作用,在横向上的搬运作用非常微弱,而在纵向上其效应略弱于磨蚀作用.关键词:砾石海滩,粒度特征,砾石形态,朱家尖中图分类号:P737.23SedimentDistributionandShapeCharacteristicsofGravelBeaches,ZhujiajianIsland,ZhejiangProvinceWangAi-Jun,GaoShu,YangYang(MinistryofEducation,KeyLaboratoryforCoastan
4、dIslandDevelopment,NanjingUniversity,Nanjing,210093,China)Abstract:Gravelbeachesareformedwherethecoastisdominatedbywaveswithsufficientgravelsupply.Onthebasisofanalysesofthegravelsamplescollectedfromtwopocketgravellybeaches(knownas“BigCobbleDike”and“SmallCobbleDike”
5、,respectively)atZhujiajianIslandofftheZhejiangcoast,thegrainsizeparameters(mean,sortingcoefficient,skewnessandkurtosis)andshapeparameters(sphericityandroundness)ofthegravelshavedistinctdistributionpatterns.Intheonshore-offshoredirection,thegravelsbecomesmallerinsiz
6、eandbettersortedtowardsthesea-withanincreaseinthepercentageofprolateandrodshapedgravels:thesphericityofgravelsisthelowestinthemiddleinter-tidalzone.Alongshore,attheBigCobbleDikethegravelsizeisthelargestinthemiddlesectionofthebeach,andthematerialbecomesbettersortedt
7、owardthenorthandthesouth,withaX基金项目:国家杰出青年科学基金(49725612)收稿日期:2003-11-10XX通讯联系人,E-mail:ajwang7708@sohu.com©1994-2008ChinaAcademicJournalElectronicPublishingHouse.Allrightsreserved.http://www.cnki.net·748·南京大学学报(自然科学)第40卷decreaseinsphericityandanincreaseinthepercenta
8、geofrod-shapedgravelsinthesamedirection.AttheSmallCobbleDike,thegravelsizedecreasesfromthesouthtowardsthenorth;inthesamedirection,thesoringbecome