MICRO-STRUCTURES AND THE FUNDAMENTAL ENGINEERING PROPERTIES OF THE BEACH CALCARENITE IN SOUTH CHINA SEA
ZHU Changqi1,2,ZHOU Bin2,3,LIU Haifeng2
(1. Faculty of Engineering,China University of Geosciences,Wuhan,Hubei 430074,China;2. State Key Laboratory of Geomechanics and Geotechnical Engineering,Institute of Rock and Soil Mechanics,Chinese Academy of Sciences,Wuhan,Hubei 430071,China;3. General Contraction Company of CCTEB,Wuhan,Hubei 430064,China )
Abstract:The beach calcarenite is a sedimentary rock deposited at tidal beaches of coral reefs in South China Sea. It is consisted of coral sands that predominantly cemented by the carbonite calcium materials under tropical or sub-tropical marine environments. The beach calcarenites are also deposited in some of the coastal areas in Southern China. The research on the geotechnical engineering properties of beach calcarenites has a significant theoretical and practical impact on the safeguarding of our marine sovereignty and the development of defense facilities in the area. This paper studies beach calcarenite samples that collected from different locations in the South China Sea and the coastal area by using both micro and marco structure study measures. The objective of these studies is to establish the major parameters that control the mechanical strength of the beach calcarenite as well as to provide necessary theoretical guidelines for the further researches. The results indicate that,the beach calcarenite is characterized by the low unit weight,high porosity,and large permeability. The degree of cementation of the beach calcarenite is in between weak and medium. The measured uniaxial compressive strength under the air-dry condition varies from 2.02 to 19.39 MPa. It is evident that the saturation of beach calcarenite samples will reduce its uniaxial compressive strength with a softening coefficient varying from 0.45 and 0.96. In general,a smaller softening coefficient in the beach calcarenite sample correlates with a weak cementation. The tested tensile strength of beach calcarenite samples under the air-dry condition is between 0.62 and 2.52 MPa with a ratio of compressive to tensile strength varying from 3.08 and 9.14. The range of compressive to tensile strength of beach calcarenite samples is lower than that of rock samples from land origin,which is between 8 and 12. The differences in the compressive to tensile strength ratio might reflect the differences in the sedimentary conditions of different rock samples. The correlation analyses of parameters indicate that the unit weight and the cementation are major parameters affecting the compressive strength of beach calcarenite samples. Stronger cementation in samples results in a higher strength. Both porosity and grain size in samples are secondary parameters with an insignificant effect on the compressive strength of the beach calcarenite.
朱长歧1,2,周 斌2,3,刘海峰2. 南海海滩岩的细观结构及其基本物理力学性质研究[J]. 岩石力学与工程学报, 2015, 34(04): 683-693.
ZHU Changqi1,2,ZHOU Bin2,3,LIU Haifeng2. MICRO-STRUCTURES AND THE FUNDAMENTAL ENGINEERING PROPERTIES OF THE BEACH CALCARENITE IN SOUTH CHINA SEA. , 2015, 34(04): 683-693.
[1] 张明书. 关于海滩岩几个问题的初步研究[J]. 海洋地质与第四纪地质,1985,5(2):105–112.(ZHANG Mingshu. On problems of beachrock[J]. Marine Geology and Quaternary Geology,1985,5(2):105–112.(in Chinese))
[2] 孙金龙,徐辉龙. 中国的海滩岩研究与进展[J]. 热带海洋学报,2009,128(2):103–108.(SUN Jinlong,XU Huilong. Advances of beach rock research in China[J]. Journal of Tropical Oceanography,2009,128(2):103–108.(in Chinese))
[3] 李毓英. 南沙群岛太平岛地质概况[J]. 地质论评,1948,8(3):333–339.(LI Yuying. The geology survey on Taiping reef island in South China Sea[J]. Geology Review,1948,8(3):333–339.(in Chinese))
[4] 吴桑云,王文海.山东半岛海滩岩的特征及意义[J]. 黄渤海海洋,1995,13(1):19–23.(WU Sangyun,WANG Wenhai. On the characteristics of beach rock in Shandong peninsula and its geological significances. Journal of Oceanography of Huanghai and Bohai Sea,1995,13(1):19–23.(in Chinese))
[5] RUBBERT L F. The natural history of crystalline calcium carbonate:effect of magnesium content and salinity[J]. J. Sediment Petrol,1974,44(1):40–53.
[6] GIVEN R K,WILKINSON B H. Kinetic control of morphology,composition and mineralogy of abiotic sedimentary carbonates[J]. J. Sediment Petrol,1985,55(1):109–119.
[7] FOOKES P G,HIGGINBOTTOM I E. The classification and description of near-shore carbonate sediments for engineering purposes[J]. Géotechnique,1975,25(2):406–411.
[8] CARTER J P,JOHNSTON I W,FAHEY M,et al. Triaxial testing of North Rankin calcarenite[C]// Engineering for Calcareous Sediments:Proceeding of the International Conference on Calcareous Sediments,Perth,Australia(eds R.J. Jewell and M.S. Khorshid),Balkema,Rotterdam,1988,2:515-530.
[9] CLARK A R,WALKER B F. A proposed scheme for the classification and nomenclature for use in the engineering description of Middle Eastern sedimentary rocks[J]. Géotechnique,1977,27(1):93–99.
[10] LEROUEIL S,VAUGHAN P R. The general and congruent effort of structure in nature soils and weak rocks[J]. Geotechnique,1990,40(3):467–488.
[11] LAGIOIA R,NOVA R. An experimental and theoretical study of the behaviour of a calcarenite in triaxial compression[J]. Geotechnique,1995,45(4):633–648.
[12] AIREY D W. Triaxial testing of a naturally cemented soil[J]. Journal of Geotechnical Engineering,ASCE,1993,119,GT9:1 379–1 398.
[13] COOP M R,ATKINSON J H. The mechanics of cemented carbonate sands[J]. Geotechnique,1993,43(1):53–67.
[14] KUCHARSKI E,PRICE G,LI H,et al. Engineering properties of CIPS cemented calcareous sand[C]// Proceedings of the International Geological Congress,Beijing,China:1996:92–97.
[15] 赵焕庭,宋朝景,余克服,等. 西沙群岛永兴岛和石岛的自然与开发[J]. 海洋通报,1994,(10):13(5):44–56.(ZHAO Huanting,SONG Chaojing,YU Kefu,et al. Nature and development of Yongxing island and Shi island of xisha islands[J]. Marine Science Bulletin,1994,(10):13(5):44–56.(in Chinese))
[16] 中华人民共和国国家标准(GB/T 50266–2013). 工程岩体试验方法标准[S]. 中华人民共和国住房和城乡建设部,中华人民共和国国家质量监督检查检疫总局. 北京:中华计划出版社,2013.