{"title":"EXPERIMENTAL STUDY ON THE EROSION RATE OF NATURALLY DEPOSITED COHESIVE SEDIMENT ON RIVER BEDS","authors":"K. Nishimori, M. Sekine, T. Higuchi, Toshio Akagi","doi":"10.2208/PROHE.52.541","DOIUrl":null,"url":null,"abstract":"The erosion rate of naturally deposited cohesive sediment on river beds was investigated experimentally. In this study, we tried to establish reasonably the preparation procedure of a test sample which has almost same property of deposited cohesive sediment in an actual field of each river. After some detailed investigations about the preparation of test sample, a series of experiments were conducted in a laboratory flume in a same manner as that of our previous work. As a result of this erosion experiments, it was found that the measured data has the same tendency as that obtained by previous work.","PeriodicalId":11343,"journal":{"name":"Doboku Gakkai Ronbunshuu B","volume":"76 1","pages":"541-546"},"PeriodicalIF":0.0000,"publicationDate":"2008-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Doboku Gakkai Ronbunshuu B","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2208/PROHE.52.541","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
Abstract
The erosion rate of naturally deposited cohesive sediment on river beds was investigated experimentally. In this study, we tried to establish reasonably the preparation procedure of a test sample which has almost same property of deposited cohesive sediment in an actual field of each river. After some detailed investigations about the preparation of test sample, a series of experiments were conducted in a laboratory flume in a same manner as that of our previous work. As a result of this erosion experiments, it was found that the measured data has the same tendency as that obtained by previous work.