실내실험을 통한 수중 매립토의 다짐효과 분석

Experimental Study on Compaction Effect of Hydraulic Fill Soils

  • 이행우 (농림부 농촌진흥과) ;
  • 장병욱 (서울대학교 조경 지역시스템공학부) ;
  • 장웅희 (한국농촌공사 농어촌연구원) ;
  • 봉태호 (서울대학교 조경 지역시스템공학부)
  • Lee, Haeng-Woo (Regional Development & Rural Tourism Div., Ministry of Agriculture & Forestry) ;
  • Chang, Pyoung-Wuck (Dept. of Landscape Architecture & Rural System Engineering, Seoul National University) ;
  • Chang, Woong-Hee (Rural Research Institute, Korea Rural Community & Agriculture Corporation) ;
  • Bong, Tae-Ho (Dept. of Landscape Architecture & Rural System Engineering, Seoul National University)
  • 발행 : 2006.03.24

초록

A series of laboratory tests was carried out for analyzing compaction characteristics of hydraulic fill soils(or hydraulically filled soils). Hydraulic fill soils were settled down by the weight of soil particle itself in water and consolidated by the extraction of water from the soil structures. Water content and dry unit weight were observed as the depth of sedimentation and consolidation soil. It was found from the result that the optimum water content $(W_{cpt})$ of the maximum unit weight$(\gamma_{dmax})$ is higher than that of laboratory compaction test(KS F 2312 A method). It was due to difference in compaction energy and compaction effect between two methods. And the maximum dry unit of hydraulic fill soil is smaller than that of laboratory compaction test. Especially in terms of compaction effect, the maximum relative compaction degrees$(R_{cmax})$ of Seamangum dredged sand, river sand and mixed sand, half and half of dredged and river sands, were 85%, 91% and 86%, respectively. It means that the compaction effect can be $85\sim91%$ of the maximum unit weight in laboratory compaction test.

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