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The town of Lixus is the most important archaeological site on the Moroccan Atlantic coast. It is essentially built, from at least 12 centuries BC, by rocks of sedimentary origin. A preliminary diagnosis allowed us to identify the main factors of the physico-chemical degradation observed on the buildings of the monument. The interest of the conservation of this archaeological richness requires an intervention of safeguard, which will go beyond the operation of protection of its perimeter to another desired action of development of its tourist and cultural purposes. The objective of this work mainly concerns a comparative study of the petro-physical characteristics of the sandstones sampled at various levels of the geological formation located to the northwest of the Lixus site, as a substitute stone, which will be used for any eventual rehabilitation operation. On the basis of the definition of the main causes of pathologies observed at the level of the site, the realization of these categories of action are first carried out by an experimental simulation of accelerated aging by "imbibition-drying" cycling. Then the call for petrographic analyzes where the thin sections revealed the mineralogical composition, the proportion of the figured elements and the nature of the bonding phase of the rocks tested; then the chemical characterization carried out by XRF fluorescence (X-Ray Fluorescence) and the quantification of the carbonated fraction by calcimetry. Also and with the help of geotechnical tests, in particular the determination of the porosity, the density and the hydric density as well as the uniaxial compressive strength (RC) and the rebound index (hardness by sclerometer). The confrontation of all the results obtained reveal a valid estimate of the potential for durability and compatibility in the sense of homogeneity with the material to be replaced, in view of their significant mineralogical composition in terms of sufficient quantity of silica and calcite. The tests used allowed the refinement of the discriminating mechanical parameters, they highlighted the relationships between the mechanical resistance and the physical properties of this replacement stone, particularly the high mechanical resistance (50.1–74.9 MPa), the absolute density values (2.54–2.68) and the rebound index (30–34) significant, which evolve inversely proportional to the low porosity values (1.7–2.20). However, all these recorded results have qualified this rock as a resistant lithology according to the classification adopted by the International Society of Rock Mechanics (ISRM), recommended for any possible renovation of Lixus.
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124--136
Opis fizyczny
Bibliogr. 21 poz., rys., tab.
Twórcy
autor
- Geosciences Laboratory, Department of Geology, Ibn Tofail University, Av. de L’Université, Kenitra, Morocco
autor
- Geosciences Laboratory, Department of Geology, Ibn Tofail University, Av. de L’Université, Kenitra, Morocco
autor
- Natural Resources and Environment Department, Hassan II Agronomic and Veterinary Institute, PO Box 6202, Rabat, Morocco
autor
- Natural Resources and Environment Department, Hassan II Agronomic and Veterinary Institute, PO Box 6202, Rabat, Morocco
autor
- Geosciences Laboratory, Department of Geology, Ibn Tofail University, Av. de L’Université, Kenitra, Morocco
autor
- Geosciences Laboratory, Department of Geology, Ibn Tofail University, Av. de L’Université, Kenitra, Morocco
autor
- Geosciences Laboratory, Department of Geology, Ibn Tofail University, Av. de L’Université, Kenitra, Morocco
- LR3G, Department of Geology, Abdelmalek Essaadi University, Avenue Khenifra, Tétouan 93000, Morocco
autor
- Geosciences of Applications Laboratory, Hassan II University of Casablanca, Casablanca 20000, Morocco
autor
- Geosciences of Applications Laboratory, Hassan II University of Casablanca, Casablanca 20000, Morocco
autor
- Geosciences Laboratory, Department of Geology, Ibn Tofail University, Av. de L’Université, Kenitra, Morocco
Bibliografia
- 1. Abdelkhaliki L. 1997. Tectono-sedimentary evolution of gravity deposits in the Prerif internal and the unit from habit (Rif external western, Morocco): bet in square in the basins pre-pit neogenes. 3rd cycle thesis. Univ. Mohamed V. Rabat, 176.
- 2. Adil S., Aberkane M. 1993a. Contribution at the study from training coastal plio-quaternaries of Larache (North-Western Morocco) 14the IAS Regional Meeting Of Sedimentology. Marrakesh: 27–29 April, 1993.
- 3. Akerraz A., El Khayari A. 2000. Archaeological surveys in the Lixus region. Preliminary results. Africa _ romana, 13, 1646–1668.
- 4. Beck K. 2006. Study of the water properties and weathering mechanisms of high porosity limestone (PhD thesis, University of Orléans).
- 5. Beck K., Muzahim A.M., Rozenbaum O. 2006. Stones of historical monuments: characterization and mechanisms alteration from freestone.
- 6. Bouzubaa N., Dekayir At. 2013. Characterization and origin from materials used in the construction of the Roman mosaic of the ocean god from the archaeological site of Lixus (Morocco).
- 7. Dessandier D. 1995. Study of the porous medium and fluid transfer properties of Touraine white tufa. Application to the durability of stones in work (Ph.D. thesis, University of Tours), 210.
- 8. Dott R.L. 1964. Graywacke and Matrix. What Approach of Immature Sandstone Classification, Journal of Sedimentary Petrology, 34, 625–632.
- 9. De La Martinière H.M.P. 1890. Research on the location of the town of Lixus. Bulletin of the Committee for Historical and Scientific Works, 134–148.
- 10. El Gharbaoui M. 1981. The Earth and the man in the Peninsula Tingitane. Study on the man and the middle natural in the rif western. work Inst. se, Series Geology you Geography physical, 15, 439.
- 11. Jeanette D. 1992. Transfers capillaries in the rocks” Necks doctoral European – Sciences and materials of cultural heritage, Ravello-Florence.
- 12. Hassini H. 2005. About the so-called Hellenistic enclosure of Lixus. Nouv Archéol Patrim, 6, 9.
- 13. Asbery L., et al. 2007. Integrated study of the degradation of Roman and Islamic historic monuments in the city of Rabat (Morocco): proposals for sustainable solutions for prevention and restoration.
- 14.Montalban C.L. 1927. Graphic album of the explorations of Lixus, Junta Central de Monumentos, Larache.
- 15. Ousha H. 2018. The alteration from rocks of construction from landmarks historical of lixus in the North-West of Morocco and Luz in the South of Portugal (Algarve western).
- 16. Ouacha H., Ben Moussa A., Baghdad B., Simão J., Taleb A., Dalimi M. 2016. Inventory of the Flora populating the historical monuments of Lixus, European Journal of Scientific Research, 142(3).
- 17. Ouacha H., Ben Moussa A., Simão J. 2013. The salt crystallization weathering of building rocks of the Archaeological sites Calcarenites of north-western Morocco (Lixus, Banasa and Thamusida), European Scientific Journal, 9(18), 282–290.
- 18. Ponsich M. 1981. Lixus: the temple district. Antiquities Museum.
- 19. Snoussi M. 1982. Geochemistry and mineralogy from sediment purposes of the estuary from Lukkos. Contribution at the study of one ecosystem estuarine. Thesis of 3rd cycle, Univ.
- 20. Tejera De Leon J. 1993. The Neogene foreland basins of the western outer Rif linked to the Jebha - Arbaoua transformant. (Morocco). Thesis es Sci, Univ. from Pau and the Atour countries, 83, 323.
- 21. Tissot C. 1877. Research on the geography of Mauretania Tingitane.
Uwagi
Opracowanie rekordu ze środków MEiN, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2022-2023).
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Bibliografia
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