51. The influence of building orientation on climate weathering cycles in Staffordshire, UK
- Author
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David P. Halsey, David E. Searle, David J. Mitchell, and Karl Macnaughton
- Subjects
Geography ,West midlands ,Humidity ,Weathering ,Physical geography ,Spall ,Tower ,Archaeology ,Case hardening - Abstract
Publisher Summary Climate or meteorological induced cycles are associated with weathering processes of building stone for a long time. Freeze-thaw cycles have severe effects on stone disintegration. Other cycles such as heating-cooling and wetting- drying creates similar stresses in stone. During certain synoptic conditions, building orientation has a great influence on climatic extremes of different facades. The use of sensors and data loggers has opened up the potential for in-depth investigations of general climatic monitoring of the exterior of buildings and effect of cyclic changes in temperature and moisture on stone. The chapter describes the study conducted to evaluate the frequency of heating-cooling, wetting-drying, and freeze-thaw cycles on the four cardinal faces of the tower of Lichfield Cathedral, Staffordshire, UK by using temperature and humidity sensors located on them.. It focuses on the assessment of the influence of orientation of building on the frequency of climatic cycles. The west and south faces have the highest frequency, whereas the north and east have the lowest values, with the north having the least. These could be loosely termed the “maritime” and “continental” faces, respectively. In a parallel study of 30 sandstone churches in the West Midlands, the occurrences of 18 forms of weathering were recorded. Granular disintegration, spalling, multiple flaking, total case hardened stone, and total autotrophic stone were found to be the greatest on the north; and relief weathering and total blackened stone were the greatest on south and west aspects.
- Published
- 2000
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