American Journal of Geophysics, Geochemistry and Geosystems
Articles Information
American Journal of Geophysics, Geochemistry and Geosystems, Vol.7, No.3, Sep. 2021, Pub. Date: Aug. 30, 2021
Geotechnical Study of the Dikes on the Left Bank of the Ikopa River in Antananarivo, Madagascar
Pages: 126-130 Views: 1231 Downloads: 260
Authors
[01] Fabrice Mario Rahajanaharimamonjy, Laboratory of Mineral Chemistry, Faculty of Science, University of Antananarivo, Antananarivo, Madagascar.
[02] Bruno Razanamparany, Laboratory of Mineral Chemistry, Faculty of Science, University of Antananarivo, Antananarivo, Madagascar.
[03] Andrianirina Randriantsimbazafy, Department of Building and Public Works, Antananarivo Polytechnic School, University of Antananarivo, Antananarivo, Madagascar.
[04] Koto-Te-Nyiwa Ngbolua, Department of Biology, Faculty of Science, University of Kinshasa, Kinshasa, Democratic Republic of the Congo.
[05] Robijaona Rahelivololoniaina Baholy, Process Engineering and Industrial, Agricultural and Food Systems, University of Antananarivo, Antananarivo, Madagascar.
Abstract
The objective of this study is to reduce the risk of flooding in the capital of Madagascar from the study of the left bank of IKOPA which is often broken during the periods of floods of this river. In order to carry out this work, two hand auger drillings at 8.00 m depth with a pressure test every meter were carried out. In both drillings, a permeability test of the Lefranc type (NF P 94-132) was carried out. At point RGT1, the site consists of a micaceous yellowish clayey silt with a limiting pressure varying from 0.11 to 0.18MPa, blackish peaty clay with a limiting pressure varying from 0.23 to 0.24 MPa, fine slightly grey clayey sand with a limiting pressure varying from 0.52 to 1.24 MPa, the permeability coefficient (KL) is 8.20 10-5m/s. At RGT2, the site consists of brown, reddish to yellowish micaceous clayey silt with limiting pressure ranging from 0.06 to 0.10MPa, yellowish micaceous silty clay to blackish peaty clay with limiting pressure ranging from 0.17 to 0.24 MPa, gray fine sand with limiting pressure ranging from 0.11 to 0.70 MPa. The coefficient of permeability (KL) is 5.30 10-5m/s. The results are not consistent with the overall stability of the bank. Thus, it does not resist during the flood, by this fact, the principle of embankment construction should be controlled to avoid the breach of this bank.
Keywords
Flooding, Permeability Coefficient, Survey, Soil, Madagascar, Indian Ocean
References
[01] Rakotomahanina, M. E. R., Ratiarison, M. A. A., Razanajatovo, M. M., & Rabemanotrona, M. (2005) The climatology of rain in Madagascar.
[02] State of the Environment Report Madagascar (2012). Atmosphere, Air and Climate Change. Ministry of Environment and Forests / General Secretariat / Directorate General of Environment / Directorate of Integration of the Environmental Dimension (D.I.E.D.) / Environmental Communication for Behaviour Change Service.
[03] Kuriqi, A., Ardiçlioglu, M., & Muceku, Y. (2016). Investigation of seepage effect on river dike’s stability under steady state and transient conditions. Pollack Periodica, 11 (2), 87-104.
[04] Boubchir, A. M. (2007). Flood risks and land use in the Thore (Labruguière and Mazamet region). University of Toulouse Le Mirail. 73p.
[05] Duret L.. (1977). Estimation of flood flow in Madagascar, Mediterranean Agricultural Techniques.
[06] Dauphine, A. & Damienne, P. (2007). Resilience: a concept for risk management. Annals of Geography, 654, 115-125.
[07] Benjamin G. (2004). Predetermination of flood flows in small torrential watersheds. Doctoral thesis from the University of Montpellier II; 376p.
[08] Guillier, F. (2017). Evaluation of the vulnerability to floods: Experimental method applied to Flood Prevention Action Programs. University of Paris-East. 531p.
[09] Apipa. (2010). Flooding of the Antananarivo plain by the floods of the Ikopa and its tributaries, 90p.
[10] Apipa, (2010). Study of the evacuation of floods in the downstream part of the plain of Antananarivo, 90p.
[11] Genetay, E., & Mehdizadeh, R. (2018) Quantification of the uncertainty on the Menard pressure modulus due to human measurement errors, calculated according to the standard NF P 94-110-1.
[12] Clarke, BG & Menard. (1996). pressure meter test in ground investigation. part 1- site operations. Proceedings of the Institution of Civil Engineers-Geotechnical Engineering, 119 (2), 96-108.
[13] Zubair, M. (2014). Geotechnical characterization by pressure meter and laboratory tests for alluvial soils (PhD thesis, University of Engineering and Technology, Lahore).
[14] Masoud, Z. (2014). Geotechnical characterization by pressuremeter and laboratory tests for alluvial soils (PhD thesis, lahore university of engineering and technology, Pakistan).
[15] Chapuis, RP, Soulié, M. & Sayegh, G. (1990). Laboratory modeling of field permeability tests in cased boreholes. Canadian Geotechnical Journal, 27 (5), 647-658.
[16] Dhouib, A., Shahrour, I., & Lafhaj Lefranc, Z. (1998) Permeability test: theoretical analysis and practical interpretation.
[17] Chapuis, RP. (1999). Variable head borehole permeability testing of compacted clay liners and covers. Canadian Geotechnical Journal, 36 (1), 39-51.
[18] Vinceslas, G., Ferber, V., Rozier, E. H., Flahaut, R., & Fauchard, C. (2008). Instrumentation of an embankment in a flood zone: Example of the experimental embankment of the CER. Bulletin des laboratoires des ponts et chaussées, (272), pp-89.
[19] Cassan, M. (2005). On-site permeability tests in soil investigation. Press des Ponts.
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