Why pore size is important in the deterioration of porous stones used in the built heritage

作者: David Benavente

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参考文章(4)
Michael Steiger, A. Elena Charola, Katja Sterflinger, Weathering and Deterioration Stone in Architecture. pp. 227- 316 ,(2011) , 10.1007/978-3-642-14475-2_4
S. Cuezva, A. Fernandez-Cortes, D. Benavente, P. Serrano-Ortiz, A.S. Kowalski, S. Sanchez-Moral, Short-term CO2(g) exchange between a shallow karstic cavity and the external atmosphere during summer: Role of the surface soil layer Atmospheric Environment. ,vol. 45, pp. 1418- 1427 ,(2011) , 10.1016/J.ATMOSENV.2010.12.023
M. Ángeles García-del-Cura, David Benavente, Javier Martínez-Martínez, Nora Cueto, Sedimentary structures and physical properties of travertine and carbonate tufa building stone Construction and Building Materials. ,vol. 28, pp. 456- 467 ,(2012) , 10.1016/J.CONBUILDMAT.2011.08.042
D. Benavente, N. Cueto, J. Martínez-Martínez, M. A. García del Cura, J. C. Cañaveras, The influence of petrophysical properties on the salt weathering of porous building rocks Environmental Earth Sciences. ,vol. 52, pp. 215- 224 ,(2007) , 10.1007/S00254-006-0475-Y