Characteristics of Beachrocks: A Review

被引:30
作者
Danjo T. [1 ,2 ]
Kawasaki S. [2 ]
机构
[1] Graduate School of Engineering, Hokkaido University, Sapporo, Hokkaido, 060-8628, Kita 13, Nishi 8, Kita-ku
[2] Hokkaido University, Sapporo, Hokkaido, 060-8628, Kita 13, Nishi 8, Kita-ku
基金
日本学术振兴会;
关键词
Beachrock; Bibliographical research; Calcium carbonate; Coastal sediment;
D O I
10.1007/s10706-013-9712-9
中图分类号
学科分类号
摘要
Beachrocks are calcareous rocks that have been quite recently formed and are found in the intertidal zone on sandy beaches. The authors are developing an artificial rock with self-healing capabilities that can be used in coastal areas to repair the infrastructure of coastal walls. Because beachrocks are formed naturally on beaches, they merit study as a model for artificial rocks. We conducted a bibliographical study in order to gather information about the characteristics of beachrocks, which may aid in the manufacturing of artificial rocks. This study investigated their geographic distribution, formative periods, physical properties, and origins. The study found that over 90 % of beachrocks are found between the latitudes 40°N and the Tropic of Capricorn, and that their formative periods range from 26,000 years to just a few decades ago. We also learned that the cement component of beachrocks mainly consists of either calcium carbonate or silica. The dynamic characteristics of these components have been studied in only three papers, which note that their uniaxial compression strength ranges from as low as 6.0 to 42.0 MPa. Since very limited data are available on beachrocks in Japan where the artificial rock technology will first be deployed, there is a need for collecting additional data on their mechanical properties, elemental composition ratios, and mineral content. © 2013 Springer Science+Business Media Dordrecht.
引用
收藏
页码:215 / 246
页数:31
相关论文
共 102 条
[71]  
Omoto K., Calibrated radiocarbon ages and isotope fractionations of beachrock samples collected from Okinawa Island, Kouri Island, Yagachi Island and Hamahiga Island, Southwest Japan, Proc Inst Nat Sci Nihon Univ, 44, pp. 1-17, (2009)
[72]  
Omoto K., Ito Y., Radiocarbon age and geomorphic development of Wakimisaki-beachrock designated as a natural monument by Nagasaki prefecture, Proc Gen Meet Assoc Jpn Geogr, 70, (2006)
[73]  
Psomiadis D., Tsourlos P., Albanakis K., Electrical resistivity tomography mapping of beachrocks: application to the island of Thassos (N. Greece), Environ Earth Sci, 59, 1, pp. 233-240, (2009)
[74]  
Ramsay P.J., 9000 years of sea-level change along the southern Africa coastline, Quat Int, 31, pp. 71-75, (1995)
[75]  
Ravisankar R., Rajalakshmi A., Gamma-ray spectroscopic and PIXE analysis of beach rock sample of south east coast of Tamilnadu, India, Int J PIXE, 17, 3-4, pp. 193-203, (2007)
[76]  
Rey D., Rubio B., Bernabu A.M., Vilas F., Formation, exposure, and evolution of a high-latitude beachrock in the intertidal zone of the Corrubedocomplex (Ria de Arousa, Galicia, NW Spain), Sediment Geol, 169, pp. 93-105, (2004)
[77]  
Russell R.J., Caribbean beach rock observation, Zeitschrift für Geomorphologie, 3, pp. 227-236, (1959)
[78]  
Sasajima S., Et al., Hosyanendaisokuteiho no kaihatu to kairyoniyoru koukosiryo no sokutei to hennnen, pp. 16-30, (1979)
[79]  
Sahayam J.D., Chandrasekar N., Kumar S.K., Rajamanickam G.V., Distribution of arsenic and mercury in subtropical coastal beachrock, Gulf of Mannar, India, J Earth Syst Sci, 119, 1, pp. 129-135, (2010)
[80]  
Schubert C., Valastro J.R.S., Quaternary geology of La Orchila Island, central Venezuelan offshore, Caribbean Sea, Geol Soc Am Bull, 87, pp. 1131-1142, (1976)