Abstract
Geology, hydrophysical properties, and mechanical behavior of two main varieties of ornamental stones in Algeria have been studied in detail. Travertines and onyx in western Algeria are summarized to two large layers, the Bouhanifia and the Ain Takbalat deposits. Their formation is related to the hydrothermalism following the great fault of Tafna. The travertine formed in water overflow while onyx is set up along the lines of outputs of the sewage of dissolved CaCo3. The results obtained show a good correlation between petrography and the mechanical behavior; the bedding planes and laminations of the travertines give a petrophysical anisotropy across the sample. Two types of mechanical testing: compressive and flexural strength were carried out either parallel or perpendicular to the veins. This test showed that mechanical behavior is guided by the nature, thickness, composition, and orientation of the veins.
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Angeles Garcia-del-Cura M, Benavente D, Martinez-Martinez J, Cueto N (2012) Sedimentary structures and physical properties of travertine and carbonate tufa building stone. Constr Build Mater 28:456–467
Anon (1999) Méthode d’essai sur la pierre naturelle – Détermination de la résistance à la compression simple. UNE-EN
Anon (2002) Méthode d’essai sur la pierre naturelle. Détermination de la résistance à la traction par flexion. UNE-EN 13161
Barruol G, Kern Z (1996) Seismic anisotropy and shear-wave splitting in lower crust und upper mantle rocks from the Ivrea zone experimental and calculated data. Phys Earth Planet Inter 95:175–194
Benavente D, Cultrone G, Gomez-Heras M (2008) The combined influence of mineralogical, hygric and thermal properties on the durability of porous building stones. Eur J Mineral 20:673–685
Bertoletti M (2002) In: Ungaro L, De Nuccio M (eds) Trapezoforo con protomo di pantera. I Marmi colorati della Roma imperiale, Venezia, pp 386–387
Chentout M, Alloul B, Dj B (2014) The relation between the petrographic, physico-mechanical properties and the use of some deposit paving in Algeria. Eng Geol Soc Territory. doi:10.1007/978-3-319-09048-1-61
Coca P, Rosique J (1992) Ciencia de materiales. Pirámide, Madrid
Çobanoglu I, Çelik SB (2008) Estimation of uniaxial compressive strength from point load strength, Schmidt harness and P-wave velocity. Bull Eng Geol Environ 67:491–498
Del Rio LM, Lopez F, Esteban FJ, Tejado JJ, Mota M, Gonzàlez I, San Emeterio JL, Ramos A (2006) Ultrasonic
Demirdag S (2009) The effect of using different polymer and cement based materials in pore filling applications on technical parameters of travertine stone. Constr Build Mater 23:522–530
Dubois C (1908) Études sur l’administration et l’exploitation des carrières marbres, porphyre, granit, etc. dans le monde romain, Paris
Erdoğan Y (2011) Engineering properties of Turkish travertines. Sci Res Essays 6(21):4551–4566
Goudie AS (2006) The Schmidt Hammer in geomorphological research. Prog Phys Geogr 30:703–718
Gnoli R (1988) Marmora Romana, 2nd edn. Rome
Gnoli R : Marchei MC, Sironi A (1997) Repertorio. In: Borghini G. (ed), Marmi antichi, Roma, pp 142–149
Gsell S (1895), Atlas archéologique de l’Algérie. Algiers and Paris
Haney MG, Shakoor A, (1994) The relationship between tensile and comprehensive strengths for selected sandstones as influenced by index properties and petrographic characteristic. Proc 7th IAEG Cong. Lisbon, Portugal, Vol 2: pp 493–500
Hatzor YH, Palchik V (1997) The influence of grain size and porosity on crack initiation stress and critical flaw length in dolomites. Int J Rock Mech Min Sci 34:805–816
Isık EC, Ozkahraman HT (2010) An economic solution to high quality travertine filling. Constr Build Mater 24:2619–2627
Jackson MD, Marra F, Hay RL, Cawood C, Winkler EM (2005) The judicious selection and preservation of tuff and travertine building stone in ancient Rome. Archaeometry 47:485–510
Jaeger JC, Cook NGW (1976) Fundamentals of rock mechanics, 2nd edn. Chapman and Hall, New York
Karpuz C, Paşamehmetoğlu AG (1997) Field characterization of weathered Ankara andesites. Eng Geol 46:1–17
Kahraman S (2001) A correlation between P-wave velocity, number of joints and Schmidt hammer rebound number. Int J Rock Mech Min Sci 38:729–733
Kahraman S (2007) The correlations between the saturated and dry P-wave velocity of rocks. Ultrasonics 46(4):341–348
Kahraman S, Yeken T (2008) Determination of physical properties of carbonate rocks from P-wave velocity. Bull Eng Geol Environ 67:277–281
Lazzarini L (2002) La determinazione della provenienza delle pietre decorative usate dai romani. In: De Nuccio M; Ungaro L (eds) : I marmi colorati della Roma imperiale, Venezia, pp 223–265.
Lazzarini L (2009) The distribution and re-use of the colored marbles in the Roman Empire. In: Y. Maniatis (ed.), ASMOSIA VII: Bulletin de Correspondance Hellénique, supplement 51: pp 459–484
Molina E, Cultrone G, Sebastián E, Alonso FJ, Carrizo L, Gisbert J, Buj O (2013) The pore system of sedimentary rocks as a key factor in the durability of building materials. Eng Geol 118:110–121
Murat Y, Hurriyet A (2013) Modeling uniaxial compressive strength of building stones using non-destructive test results as neural networks input parameters. Constr Build Mater 47:1010–1019
NF P94-411 (2002) Détermination de la vitesse de propagation des ondes ultrasonore au laboratoire- Méthode par transparence
Pentecost A, Viles HA (1994) A review and reassessment of travertine classification. Geogr Phys Quaternaire 48:305–314
Playfair RL (1895) Handbook for Travellers in Algeria and Tunis, London
Přikryl R (2001) Some microstructural aspects of strength variation in rocks. Int J Rock Mech Min Sci 38:671–682
Sabatakakis N, Koukis G, Tsiambaos G, Papanakli S (2008) Index properties and strength variations controlled by microstructure for sedimentary rocks. Eng Geol 97:80–90
Sanders JE, Friedman GM (1967) Origin and occurrence of limestones. In: Chilingar GV, Bissel HJ, Fairbridge RW (eds) Carbonate rocks, Developments in sedimentology, vol 9A. Elsevier, Amsterdam, pp 169–265
Tawab AM (1970) Marbre et pierre ornementales oranaise étude géologique (BET – SONAREM)
Török A (2006) Influence of fabric on the physical properties of limestones. In: Kourkoulis SK (ed) Fracture and failure of natural building stones. Springer, Dordrecht, pp 487–495
Török Á, Vásárhelyi B (2010) The influence of fabric and water content on selected rock mechanical parameters of travertine, examples from Hungary. Eng Geol 115:237–245
Tsiambaos G, Sabatakakis N (2004) Considerations on strength of intact sedimentary rocks. Eng Geol 72:261–273
Vazquez P, Alonso FJ, Carriz L, Molina E, Cultrone G, Blanco M, Zamora I (2013) Evaluation of the petrophysical properties of sedimentary building stones in order to establish quality criteria. Constr Build Mater 41:868–878
Winkler EM (1997) Stone in architecture: properties, durability, 3rd edn. Springer, Berlin
Wong RHC, Chau KT, Wang P (1996) Microcracking and grain size effect in Yeun Long marbles. Int J Rock Mech Min Sci Geomech 33:479–485
Yagiz S (2006) Overview on geo-mechanical assessments of Denizli travertines in Turkey. Book of abstracts. In: 10th International association for engineering geology congress, Nottingham, pp 384
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Chentout, M., Alloul, B., Rezouk, A. et al. Experimental study to evaluate the effect of travertine structure on the physical and mechanical properties of the material. Arab J Geosci 8, 8975–8985 (2015). https://doi.org/10.1007/s12517-015-1910-8
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DOI: https://doi.org/10.1007/s12517-015-1910-8