Enfoque químico del deterioro y biodeterioro de rocas calcáreas conformantes de monumentos patrimoniales de importancia histórica y cultural

Enfoque químico del deterioro y biodeterioro de rocas calcáreas conformantes de monumentos patrimoniales de importancia histórica y cultural

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... Ver más

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Luna Azul

1909-2474

Barbosa López, Aida Liliana

Tatis Castro, Roy David

UNIVERSIDAD DE CALDAS

2013-01-01

247

284

Colombia

meteorización de piedra

corrosión pétrea

monumentos históricos de piedra

biodeterioro

Deterioro

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spelling Enfoque químico del deterioro y biodeterioro de rocas calcáreas conformantes de monumentos patrimoniales de importancia histórica y cultural
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Universidad de Caldas
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Artículo de revista
Núm. 36 , Año 2013 : Enero - Junio
36
meteorización de piedra
corrosión pétrea
monumentos históricos de piedra
biodeterioro
Deterioro
Barbosa López, Aida Liliana
Tatis Castro, Roy David
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. 
Bede, E. (2000). Characterization of surface morphology of carbonate stone and its effect on surface uptake of so2. Elsevier proceedings of the 9th international congress on deterioration and conservation of stone.303,304.
Al-Algha, M. R. (2006). Weathering of building stones and its relationship to the sustainable management of the aggregate resources in Gaza strip, Palestine. Building and environment, 41(5), 680, 681.
Benavente, D.; García del Cura, M. A.; García-Guinea, J.; Sánchez-Moral, S. y Ordóñez, S. (2004). Role of pore structure in salt cristallization in unsaturated porousstone. Journal of crystal growth, 260, 532.
Coussy, O. (2006). Deformation and stress from in-pore drying-induced crystallization of salt. Journal of mechanics and physics of solids, 54, 1518, 1526.
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. y Crispim, C. (2005). Cyanobacteria and biodeterioration of cultural heritage: a review. Microbial ecology, 49, 1.
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.
Flatt, R. J. (2002). Salt damage in porous materials: how high supersaturations are generated. Journal of crystal growth, 242, 435, 437.
Fernandes, P. (2006). Applied microbiology and biotechnology in the conservation of stone cultural heritage materials. Applied microbiology and biotechnology, 73, 292.
Espinosa-Marzal, R. y Scherer, G. W. (2010). Advances in understanding damage by salt crystallization. Accounts of chemical research, 43, 897-900.
Doehne, E. y Price, C. (2010). Stone conservation, anoverview of current research. The getty trust publications, 2,15. Espinosa, R. M.; Franke, L. y Deckelmann, G. (2008). Predicting efflorescence and subflorescences of salts. Matter. res. soc. symp. proc., 1047.
Doehne, E. (2002). Salt weathering:a selective review.Geological society, London, special publications, 205,51-56.
De los Ríos, A.; Cámara, B.; García del Cura, M.; Rico, V.; Galván, V. y Ascaso, C. (2009). Deteriorating effects of lichen and microbial colonization of carbonate building rocks in the Romanesque churches of Segovia (Spain). Science of the total environment, 407, 1127.
Crispim, C. A.; Gaylarde, C. C. y Gaylarde, P. M. (2004). Biofilms on church walls in Porto Alegre, rs, Brazil, with special attention to cyanobacteria. International biodeterioration and biodegradation, 54, 122.
Crispim, C. A. y Gaylarde, C. C. (2004). Cyanobacteria and biodeterioration of cultural heritage: a review. Microbial ecology, 49, 3.
Benavente, D.; Martínez-Martínez, J.; Cueto, N.; García del Cura, M. A. (2007). Salt weathering in dual-porosity building dolostones. Engineering geology, 94, 215, 216.
Crispim, A. C.; Gaylarde, M. P.; Gaylarde, C. C. y Brett, A. N. (2006). Deteriogenic cyanobacteria on historic buildings in Brazil detected by culture and molecular techniques. International biodeterioration and biodegradation, 57, 239, 240.
Publication
Colston, B. J.; Watt, D. S. y Munro, H. L. (2001). Environmentally-induced stone decay: the cumulative effects of crystallization-hydration cycles on a Lincolnshire oopelsparite limestone. Journal of cultural heritage, 4,304, 305.
Charola, A. E. y Ware, R. (2002). Acid deposition and the deterioration of stone: A brief review of a broad topic. Geological society, London, special publications, 205, 393-399.
Böke, H.; Göktürk, H. E.; Caner-Saltik, E. N. y Demirsi, Ş. (1999). Effect of airborne particle on SO2-calcite reaction. Applied surface science, 140, 70, 71, 74.
Bonazza, A.; Messina, P.; Sabbioni, C.; Grossi, C. M. y Brimblecombe, P. (2009). Mapping the impact of climate change on surface recession of carbonate buildings in Europe. Science of the total environment, 407, 2039,2040.
Borgia, G. C.; Camaiti, M.; Cerri, F.; Fantazzini, P. y Piacenti, F. (2000). Study of water penetration in rock materials by NMR tomography: hydrophobic treatmenteffects. Journal of cultural heritage, 1, 128.
Cataldo, R.; De Donno, A.; De Nunzio, G.; Leucci, G.; Nuzzo, L. y Siviero, S. (2005). Integrated methods for analysisof deterioration of cultural heritage: the Crypt of“Cattedrale di Otranto”.Journal of cultural heritage, 6,31.
Cardell, C.; Delalieux, F.; Roumpopoulos, K.; Moropoulou, A.; Auger, F. y Van Grieken, R. (2003). Salt-induced decay in calcareous stone monuments and buildings in a marine environment in sw France.Construction and building materials, 17, 165.
Cardell, C.; Benavente, D. y Rodríguez-Gordillo, J., (2008). Weathering of limestone building material by mixed sulfate solutions. Characterization of stone microstructure, reaction products and decay forms. Materials characterization, 59, 1371.
Camaiti, M.; Bugani, S.; Bernardi, E.; Morselli, L. y Matteini, M. (2007). Effect of atmospheric NOx on biocalcarenite coated with different conservation products. Applied geochemistry, 22, 1248.
Camuffo, D. (1998). Microclimate for cultural heritage. Developments in atmospheric science 23 Elsevier science b.v. 12, 13.
Deterioration
Abstract: Stony monuments declared as cultural world heritage are deteriorated through the years because of physical, chemical and environmental agents which depend largely on their geographic location. Among these agents are: gust of, winds that wear away the stone eroding it; rainy seasons which bring dissolved salts and cause corrosion because of their chemical reaction with the calcareous material matrix which solubilizes Luna Azul ISSN 1909-2474 No. 36, enero - junio 2013 ©Universidad de Caldas 247 calcium carbonate which is their main component; because of solar radiation all through the year stones lose their color; high humidity allows plants and living forms to grow. Anthropogenic activities which are not environmentally friendly are other important factor: vehicle gas emissions, for example, deteriorate greatly old stone monuments because they are highly corrosive acids. This way, optimal conditions are created for fungi, algae, bacteria, lichens and plants which are invasive and colonizing to live on the stone surface and cause biodeterioration. Since metabolisms of these species involve consumption of inorganic substrates that are present in the stones, they become another factor affecting monument’s durability, stability, and aesthetic appearance.
Chemical approach to the deterioration and biodegradation of calcareous rocks that make up heritage monuments of historical and cultural importance
biodeterioration
cultural world heritage stony monuments
stone corrosion
stone weathering
Journal article
1909-2474
247
284
https://revistasojs.ucaldas.edu.co/index.php/lunazul/article/download/1667/1584
https://revistasojs.ucaldas.edu.co/index.php/lunazul/article/view/1667
2013-01-01T00:00:00Z
2013-01-01
2013-01-01T00:00:00Z
institution UNIVERSIDAD DE CALDAS
thumbnail https://nuevo.metarevistas.org/UNIVERSIDADDECALDAS/logo.png
country_str Colombia
collection Luna Azul
title Enfoque químico del deterioro y biodeterioro de rocas calcáreas conformantes de monumentos patrimoniales de importancia histórica y cultural
spellingShingle Enfoque químico del deterioro y biodeterioro de rocas calcáreas conformantes de monumentos patrimoniales de importancia histórica y cultural
Barbosa López, Aida Liliana
Tatis Castro, Roy David
meteorización de piedra
corrosión pétrea
monumentos históricos de piedra
biodeterioro
Deterioro
Deterioration
biodeterioration
cultural world heritage stony monuments
stone corrosion
stone weathering
title_short Enfoque químico del deterioro y biodeterioro de rocas calcáreas conformantes de monumentos patrimoniales de importancia histórica y cultural
title_full Enfoque químico del deterioro y biodeterioro de rocas calcáreas conformantes de monumentos patrimoniales de importancia histórica y cultural
title_fullStr Enfoque químico del deterioro y biodeterioro de rocas calcáreas conformantes de monumentos patrimoniales de importancia histórica y cultural
title_full_unstemmed Enfoque químico del deterioro y biodeterioro de rocas calcáreas conformantes de monumentos patrimoniales de importancia histórica y cultural
title_sort enfoque químico del deterioro y biodeterioro de rocas calcáreas conformantes de monumentos patrimoniales de importancia histórica y cultural
title_eng Chemical approach to the deterioration and biodegradation of calcareous rocks that make up heritage monuments of historical and cultural importance
description 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. 
description_eng Abstract: Stony monuments declared as cultural world heritage are deteriorated through the years because of physical, chemical and environmental agents which depend largely on their geographic location. Among these agents are: gust of, winds that wear away the stone eroding it; rainy seasons which bring dissolved salts and cause corrosion because of their chemical reaction with the calcareous material matrix which solubilizes Luna Azul ISSN 1909-2474 No. 36, enero - junio 2013 ©Universidad de Caldas 247 calcium carbonate which is their main component; because of solar radiation all through the year stones lose their color; high humidity allows plants and living forms to grow. Anthropogenic activities which are not environmentally friendly are other important factor: vehicle gas emissions, for example, deteriorate greatly old stone monuments because they are highly corrosive acids. This way, optimal conditions are created for fungi, algae, bacteria, lichens and plants which are invasive and colonizing to live on the stone surface and cause biodeterioration. Since metabolisms of these species involve consumption of inorganic substrates that are present in the stones, they become another factor affecting monument’s durability, stability, and aesthetic appearance.
author Barbosa López, Aida Liliana
Tatis Castro, Roy David
author_facet Barbosa López, Aida Liliana
Tatis Castro, Roy David
topicspa_str_mv meteorización de piedra
corrosión pétrea
monumentos históricos de piedra
biodeterioro
Deterioro
topic meteorización de piedra
corrosión pétrea
monumentos históricos de piedra
biodeterioro
Deterioro
Deterioration
biodeterioration
cultural world heritage stony monuments
stone corrosion
stone weathering
topic_facet meteorización de piedra
corrosión pétrea
monumentos históricos de piedra
biodeterioro
Deterioro
Deterioration
biodeterioration
cultural world heritage stony monuments
stone corrosion
stone weathering
citationissue 36
citationedition Núm. 36 , Año 2013 : Enero - Junio
publisher Universidad de Caldas
ispartofjournal Luna Azul
source https://revistasojs.ucaldas.edu.co/index.php/lunazul/article/view/1667
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Luna Azul - 2015
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