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Tatis Castro, R. D., & Barbosa López, A. L. (2013). Enfoque químico del deterioro y biodeterioro de rocas calcáreas conformantes de monumentos patrimoniales de importancia histórica y cultural. Luna Azul, (36), 247–284. Recuperado a partir de https://revistasojs.ucaldas.edu.co/index.php/lunazul/article/view/1667
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Los monumentos pétreos declarados como patrimonio histórico son deteriorados a través del tiempo por efecto de agentes físicos, químicos y medioambientales. Estos últimos dependen en gran medida de la ubicación geográfica del inmueble, dichos agentes son: el régimen de vientos que desgasta la roca erosionándola; temporadas de lluvia que al contener sales disueltas causan corrosión por reacciones químicas de estas con la matriz del material calcáreo solubilizando el carbonato de calcio el cual es su principal componente; radiación solar durante todo el año causante de decoloramiento; humedad que permite el establecimiento de formas de vida. Las actividades antropogénicas que no son amigables con el ambiente son otro factor determinante, las emisiones de gases vehiculares por ejemplo, deterioran en gran medida los monumentos de piedra antiguos por ser agentes ácidos altamente corrosivos. Se crean así las condiciones para el establecimiento y proliferación de organismos vivos en la piedra tales como bacterias, algas, hongos, líquenes y plantas que por ser invasivos y colonizadores causan biodeterioro. Dado que los metabolismos de estas especies involucran el consumo de sustratos químicos orgánicos e inorgánicos presentes en la roca, son otro factor que va en detrimento de la estabilidad, durabilidad, y apariencia estética de la misma.
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Espinosa-Marzal, R. y Scherer, G. W. (2010). Advances in understanding damage by salt crystallization.
Accounts of chemical research, 43, 897-900.
Fernandes, P. (2006). Applied microbiology and biotechnology in the conservation of stone cultural heritage materials. Applied microbiology and biotechnology, 73, 292.
Flatt, R. J. (2002). Salt damage in porous materials: how high supersaturations are generated. Journal of crystal
growth, 242, 435, 437.
Flores, M.; Lorenzo, J. y Gómez-Alarcón, G., (1997). Algae and bacteria on historic monuments at Alcalá de
Henares, Spain. International biodeterioration and biodegradation, 40, 244.
Gaylarde, C. y Crispim, C. (2005). Cyanobacteria and biodeterioration of cultural heritage: a review. Microbial
ecology, 49, 1.
Gaylarde, C. y Gaylarde, P. (2005). A comparative study of the major microbial biomass of biofilms on exteriors
of buildings in Europe and Latin America. International biodeterioration and biodegradation, 55, 131-133.
Gaylarde, C.; Gaylarde, P. y Neilan, B. A. (2012). Endolithic phototrophs in built and natural stone. Current microbiology, 65, 183-8.
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damaged stone monuments. Atmospheric environment, 34, 4383.
Ghedini, N.; Sabbioni, C. y Pantani, M. (2003). Thermal analysis in cultural heritage safeguard: an application.
Thermochimica acta, 406, 105.
Giavarini, C.; Santarelli, M. L.; Natalini, R. y Freddi, F. (2008). A non-linear model of sulphation of porous
stones: numerical simulations and preliminary laboratory assessments. Journal of cultural heritage, 9,14, 15.
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