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DETERMINATION OF SEDIMENTARY RATE IN ESTUARY AND COAST BY ~(228)Th TECHNIQUE
作者姓名:康兴伦  顾德隆  张经  朱校斌  施伟  康建海  秦晓光
作者单位:KANG Xing lun,Teh Lung Ku,ZHANG Jing,ZHU Xiao binSHI Wei,KANG Jian hai,QIN Xiao guang (Institute of Oceanology,Chinese Academy of Sciences,Qingdao 266071,China
基金项目:ContributionNo.4 1 5 5fromtheInstituteofOceanology,ChineseAcademyofSciences.    Project 4 95 76 2 99supportedbyNSFC .
摘    要:INTRODUCTIONTheHuangheRiverwellknownworldwideforitshighsedimentdischargeisChina’ssecondlargestriver,whoserunoffismainlysuppliedbyprecipitationovertheupperreaches.However,thematerialfromsoilerosionintheLoessPlateauinthemiddlereachesisamajorcontributort…


DETERMINATION OF SEDIMENTARY RATE IN ESTUARY AND COAST BY ~(228)Th TECHNIQUE
KANG Xing lun,Teh Lung Ku,ZHANG Jing,ZHU Xiao binSHI Wei,KANG Jian hai,QIN Xiao guang.DETERMINATION OF SEDIMENTARY RATE IN ESTUARY AND COAST BY ~(228)Th TECHNIQUE[J].Chinese Journal of Oceanology and Limnology,2001(4).
Authors:KANG Xing lun  Teh Lung Ku  ZHANG Jing  ZHU Xiao binSHI Wei  KANG Jian hai  QIN Xiao guang
Abstract:Analysis of 232 Th, 230 Th , and 228 Th in sediments showed that there was an excess of 228 Th over that supported by the parents 232 Th or 228 Ra in sediments in many regions. This excess 228 Th with a half life of 1.91 years can be used for dating purpose over a time period of the order of a decade, so average sedimentary rates in the Yalujiang River Estuary, and in the Huanghe River Estuary and its adjacent Laizhou Bay can be obtained from decreases in the excess 228 Th activity as a function of depth in sediment.
Keywords:activity  excess  sedimentary rate  estuary  Laizhou Bay
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