Contrasting weathering and climate regimes in forested and cleared sandstone temples of the Angkor region |
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| Authors: | Marie‐Françoise André Olivier Voldoire Erwan Roussel Franck Vautier Bruno Phalip Hang Peou |
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| Institution: | 1. Laboratory of Physical and Environmental Geography – GEOLAB, CNRS/Blaise Pascal University, , Clermont‐Ferrand, France;2. Institut Universitaire de France, , Paris, France;3. Maison des Sciences de l'Homme, CNRS/Blaise Pascal University, , Clermont‐Ferrand, France;4. Centre of History ‘Spaces and Cultures’, Blaise Pascal University, , Clermont‐Ferrand, France;5. APSARA National Authority, , Siem Reap, Cambodia |
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| Abstract: | Comparative assessment of stone weathering intensities and bioclimatic conditions was conducted at four temples located in cleared and forested sites of the Angkor Park, based on similar protocols. Four thousand sculpted lotus petals carved in the same grey sandstone were categorized by using two customized scales of weathering intensity, and climate monitoring was conducted from December 2008 to November 2009. Whereas 70% of the sandstone lotus petals are almost completely destroyed by mechanical weathering in cleared areas, 74% of petals located in forested environments appear to be totally free of mechanical weathering and are only affected by superficial biochemical weathering. Ambient conditions are also contrasting, with the magnitude of the diurnal surface temperature and relative humidity ranges being three times higher at cleared sites than in wooded areas. As wetting–drying cycles are the driving force of sandstone decay at Angkor, causal links are suggested between weathering and climate regimes. In wooded areas, the microclimate is buffered by the forest and the associated lithobionts, which maintain constant humidity levels, reduce thermal stresses at the stone surface and induce a slow biochemical weathering regime. In cleared areas, direct exposure to sunshine and monsoon rains induces pronounced wetting–drying cycles conducive to swelling–shrinking movements and other potential processes, provoking the rapid mechanical decay of the sandstone. Even if local damage can be caused by tree roots, the forest cover and the associated lithobionts obviously play an overall protective role. Additionally, microtopographical factors related to architectural designs and post‐building events probably explain intra‐site and between site minor differences in the amount of sandstone decay, by influencing key factors such as the water residence time at the stone surface. Last, the contrasting weathering regimes in forested and cleared sites are but a trend, for besides overwhelming mechanical weathering, chemical weathering is also operative at cleared sites, as indicated by salt efflorescences and ferric oxidation. Copyright © 2012 John Wiley & Sons, Ltd. |
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| Keywords: | sandstone weathering cultural heritage deterioration Angkor temples microclimate bioprotection forest cover |
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