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Climate change, Climate change, ‘‘greeninggreening’’ of ofmasonry and implications formasonry and implications for
the decay of built heritagethe decay of built heritageand new buildand new build
Prof. B.J. Smith, Dr H.A Viles,Dr N.L. Betts, Dr J.J. McAlister,
Prof. P.A.M. Basheer,Prof A.S. Whiteley
Climate Change and Stone Decay:Climate Change and Stone Decay:A UK PerspectiveA UK Perspective
Many presumptions regarding salt-inducedMany presumptions regarding salt-induceddecay in the UK come from studies ofdecay in the UK come from studies oflimestones limestones in the comparatively dry southeastin the comparatively dry southeast
Explanations and preferred conservationExplanations and preferred conservationstrategies are based upon similar, stablestrategies are based upon similar, stableconditions and responses prevailing across theconditions and responses prevailing across therest of the UKrest of the UK
Sandstone Decay by Salt ActionSandstone Decay by Salt Action
Premised on periodic wetting followed by thorough dryingPremised on periodic wetting followed by thorough drying
Shallow wetting related to migration of a Shallow wetting related to migration of a ‘‘wetting frontwetting front’’
Wetting/drying facilitates surface and near-surface saltWetting/drying facilitates surface and near-surface saltaccumulation depending on drying rateaccumulation depending on drying rate
Leads to granular Leads to granular disaggregation disaggregation and/or contourand/or contourscalingscaling
Assumptions have influenced the design of standardAssumptions have influenced the design of standarddurability testsdurability tests
ContourContourScalingScalingandandGypsumGypsum
Climate Change and the Northwest UKClimate Change and the Northwest UK
Rainfall consistently increases in total amount and frequency towards theRainfall consistently increases in total amount and frequency towards thenorthwest northwest –– Belfast c. 200 rain days per annum Belfast c. 200 rain days per annum
Future scenarios for the northwest predict significant changeFuture scenarios for the northwest predict significant change
Increased uncertainty in day-to-day weather conditionsIncreased uncertainty in day-to-day weather conditions
Wetter, warmer and longer wintersWetter, warmer and longer winters
Could suggest increased time-of-wetness for exposed stoneworkCould suggest increased time-of-wetness for exposed stonework
Could result in increased chemical weathering of stonework in theCould result in increased chemical weathering of stonework in thenorthwest (northwest (Viles Viles 2002)2002)
Dryer conditions in the southeast of the UK could increase the significanceDryer conditions in the southeast of the UK could increase the significanceof salt crystallisation (of salt crystallisation (Viles Viles 2002)2002)
Predicted Rainfall ChangePredicted Rainfall Changefor the British Islesfor the British Isles
Source: Fealy and Sweeney, 2007
Regional Climate Change Scenarios: Temperature
Source: Fealy and Sweeney,2007
Regional Climate Change Scenarios: Rainfall
Climate Change ImplicationsClimate Change Implicationsfor Stoneworkfor Stonework
Prolonged and presumably more deeply penetratingProlonged and presumably more deeply penetratingwinter wetness alters a major control on stone decaywinter wetness alters a major control on stone decayprocessesprocesses
Should affect salt penetration and zones of concentrationShould affect salt penetration and zones of concentration
Could influence patterns of biological colonisation,Could influence patterns of biological colonisation,especially if wetness is combined with warmth and theespecially if wetness is combined with warmth and theabsence of frostabsence of frost
History of Atmospheric Pollution andHistory of Atmospheric Pollution andStone Decay in Belfast: Origins of theStone Decay in Belfast: Origins of theprojectproject
High concentrations of sulphates, particulates and marine aerosolsHigh concentrations of sulphates, particulates and marine aerosols
Predominance of building sandstonesPredominance of building sandstones
Rapid soiling of new and replacement stoneRapid soiling of new and replacement stone
Frequent surface Frequent surface disaggregation disaggregation and contour scaling of sandstonesand contour scaling of sandstones
Widespread formation of Widespread formation of indurated indurated iron coatingsiron coatings
History of ill-thought-out interventionHistory of ill-thought-out intervention
Anecdotal evidence of increased Anecdotal evidence of increased ‘‘greeninggreening’’ of buildings, independent of of buildings, independent ofinterventionintervention
Pollution overPollution overBelfastBelfast
Soiling: SevenSoiling: SevenYears afterYears afterCleaningCleaning
AnecdotalAnecdotalevidence forevidence forincreasedincreasedgreening ofgreening ofsandstonesandstone
St MarkSt Mark’’s Church, Belfasts Church, BelfastMay 1999 & October 2001May 1999 & October 2001
RESEARCH FINDINGSRESEARCH FINDINGSExposure Trials 1:Exposure Trials 1:Late 1980s, Early 1990sLate 1980s, Early 1990s
Number of exposure sites across BelfastNumber of exposure sites across Belfast
Rapid growth of gypsum crusts on shelteredRapid growth of gypsum crusts on shelteredsamplessamples
Samples exposed to Samples exposed to rainwashrainwash, crust-free, crust-free
SHELTERED PORTLAND:SHELTERED PORTLAND:Belfast - 1 yearBelfast - 1 year
SHELTERED PORTLAND:SHELTERED PORTLAND:Belfast - 1 yearBelfast - 1 year
RESEARCH FINDINGSRESEARCH FINDINGSExposure Trials 2:Exposure Trials 2:Late 1990sLate 1990s
Trials repeated at same sites as 10 years previouslyTrials repeated at same sites as 10 years previously
Continued gypsum crust development on sheltered samples -Continued gypsum crust development on sheltered samples -possibly less rapidpossibly less rapid
Extensive biological colonisation of Extensive biological colonisation of rainwashed rainwashed samplessamples
Marked reduction in permeability associated with colonisationMarked reduction in permeability associated with colonisation
Coincided with period of above normal rainfall amount andCoincided with period of above normal rainfall amount andfrequency during winter monthsfrequency during winter months
Exposure Trial: City HallExposure Trial: City Hall
Microbial Community on Microbial Community on DunhouseDunhouseSandstone Exposed at Belfast Sandstone Exposed at Belfast HarbourHarbourfor 2 yearsfor 2 years
Fungal Fungal Hyphae Hyphae and Algal Cells/Filamentsand Algal Cells/Filamentson Dumfries Sandstone Exposed aton Dumfries Sandstone Exposed atNorth Belfast for 2 yearsNorth Belfast for 2 years
Mucilage Binding Coal Mucilage Binding Coal Flyash Flyash totoDunhouse Dunhouse Sandstone Exposed atSandstone Exposed atBelfast Belfast Harbour Harbour for 2 yearsfor 2 years
Reduction in Permeability due to BiologicalReduction in Permeability due to BiologicalColonisationColonisation, , Dunhouse Dunhouse SandstoneSandstoneExposed at Belfast Exposed at Belfast Harbour Harbour for 2 yearsfor 2 years
Rainfall Patterns for Exposure TrialRainfall Patterns for Exposure Trial
RESEARCH FINDINGSRESEARCH FINDINGSSalt Related Decay 1:Salt Related Decay 1:St MatthewSt Matthew’’s Churchs Church
Extreme decay of quartz sandstone in the low-lying, pollutedExtreme decay of quartz sandstone in the low-lying, polluteddocks area of Belfastdocks area of Belfast
Characterised by rapid retreat of individual blocksCharacterised by rapid retreat of individual blocks
The need for site-specific conservation identifiedThe need for site-specific conservation identified
Research into the diagnosis of decay processes and controlsResearch into the diagnosis of decay processes and controlsrequiredrequired
Removal of complete blocks of sandstone permittedRemoval of complete blocks of sandstone permitted
Rapid RetreatRapid Retreatof Individualof IndividualBlocksBlocks
RESEARCH FINDINGSRESEARCH FINDINGSSalt Related Decay 2:Salt Related Decay 2:Results from AnalysesResults from Analyses
Two- and three-dimensional salt distributions by within completeTwo- and three-dimensional salt distributions by within completeblocks by IC and AASblocks by IC and AAS
Gypsum concentration in the near surface zone linked to contourGypsum concentration in the near surface zone linked to contourscalingscaling
Sodium, Magnesium and Chloride distributed throughout blocks, butSodium, Magnesium and Chloride distributed throughout blocks, butconcentrated in concentrated in ‘‘hot spotshot spots’’
Lack of correlation between Sodium, Magnesium and Chloride mightLack of correlation between Sodium, Magnesium and Chloride mightimply imply ‘‘saltsalt’’ dispersion by ion diffusion dispersion by ion diffusion
Ion diffusion may have implications for other alteration processes,Ion diffusion may have implications for other alteration processes,including iron migrationincluding iron migration
Gypsum Distribution withGypsum Distribution withDepthDepth
NaNa++ Mg Mg++++ & & ClCl-- DistributionDistributionwith Depthwith Depth
RESEARCH FINDINGSRESEARCH FINDINGSSalt Related Decay 3:Salt Related Decay 3:Experimental ResultsExperimental Results
Modelling block retreat: the importance ofModelling block retreat: the importance ofof deep saltsof deep salts
Assessing the feasibility of ion diffusionAssessing the feasibility of ion diffusion
Salt andSalt andMoisture FlowsMoisture Flows
Decay Patterns & SurfaceDecay Patterns & SurfaceChemistryChemistry
DiffusionDiffusionCoefficientCoefficient
SUMMARY 1SUMMARY 1Possible Changes in the Nature ofPossible Changes in the Nature ofSalt-Related Stone DecaySalt-Related Stone Decay
Prolonged saturation of complete stone blocksProlonged saturation of complete stone blocks
Irregular and possibly incomplete surface drying for much of yearIrregular and possibly incomplete surface drying for much of year
Deeper penetration of salts (especially those of high mobility)Deeper penetration of salts (especially those of high mobility)
Movement of salt through stone by ion diffusion rather than in solutionMovement of salt through stone by ion diffusion rather than in solution
Presence of a store of Presence of a store of ‘‘deep salt' that may facilitate continued retreat ofdeep salt' that may facilitate continued retreat ofindividual blocks following initial individual blocks following initial delamination delamination or removal of surface layersor removal of surface layersduring conservationduring conservation
Visual Visual disamenitydisamenity
SUMMARY 2SUMMARY 2Possible Effects of Increased BiologicalPossible Effects of Increased BiologicalColonisation of Rainwashed StoneworkColonisation of Rainwashed Stonework
Active biological decay, both chemical and physicalActive biological decay, both chemical and physical
Decrease in surface porosity/permeabilityDecrease in surface porosity/permeability
Continued wetting of stone by frequent rainfall andContinued wetting of stone by frequent rainfall andcondensationcondensation
Prolonged saturation following reduced evaporationProlonged saturation following reduced evaporation
Facilitation of dust deposition and the formation of complexFacilitation of dust deposition and the formation of complexbio-mineralogic bio-mineralogic crustscrusts
Implications for Stone ConservationImplications for Stone Conservation
Avoid actions that further promote biological colonisation:Avoid actions that further promote biological colonisation: Chemical cleaningChemical cleaning Increased atmospheric nitrogenIncreased atmospheric nitrogen
Need to appreciate changing patterns of soiling:Need to appreciate changing patterns of soiling: Greening of exposed surfaces instead of gypsum crusts in sheltered areasGreening of exposed surfaces instead of gypsum crusts in sheltered areas
Avoid ad hoc interventionAvoid ad hoc intervention
Surface dressing alone may activate deep saltsSurface dressing alone may activate deep salts
Consider alternative intervention:Consider alternative intervention: BiocidesBiocides Water repellentsWater repellents Requires new protocols for application in a Requires new protocols for application in a ‘‘wetter worldwetter world’’
Greening after ChemicalGreening after ChemicalCleaningCleaning
AggressiveAggressiveCleaning ofCleaning ofGreenedGreenedStoneworkStonework
April 2002
June 2002
Test WallTest WallSt MatthewSt Matthew’’ssChurchChurch
Test Wall after 4 monthsTest Wall after 4 months
Treated and UntreatedTreated and UntreatedTest WallTest Wall
CONCLUSIONSCONCLUSIONS
The high rainfall totals and rainfall frequency in Belfast provide an insight intoThe high rainfall totals and rainfall frequency in Belfast provide an insight intothe possible consequences of increased time-of-wetness for stoneworkthe possible consequences of increased time-of-wetness for stonework
Research has suggested the need to rethink assumptions concerningResearch has suggested the need to rethink assumptions concerningpatterns and controls on salt related decay in patterns and controls on salt related decay in ‘‘wetwet’’ environments environments
Stone response to increased time-ofStone response to increased time-of––wetness is complex, with manywetness is complex, with manyfeedbacks operating. The effects of which are complicated by changingfeedbacks operating. The effects of which are complicated by changingpollution regimes: less pollution regimes: less suplhursuplhur, increased localised nitrogen, different, increased localised nitrogen, differentparticulatesparticulates
Conservators should assess alternative approaches to building management,Conservators should assess alternative approaches to building management,including a more flexible approach to preventative strategiesincluding a more flexible approach to preventative strategies
The New ProjectThe New Project
Aim The overall aim is to understand how periods
of prolonged, deep-seated wetness impact onthe ‘greening’, deterioration and potentialconservation of sandstone masonry, throughan interdisciplinary study linking civilengineering, geomorphology, climatology andenvironmental microbiology with architectsand conservators.
Objectives 1Objectives 1
1. To understand the current greening of sandstone walls typical ofthat found across the NW UK today and its relationship to climate, airquality and micro-environmental conditions. (Smith, McAlister andViles)
2. To monitor the moisture contents of sandstone test walls to quantify‘time of wetness’ (both at the surface and at depth) in the west ofNorthern Ireland and its relationship to greening. (Basheer & Viles)
3. To relate wetness regimes in sandstone walls to existing climaticconditions. (Basheer, Betts & Smith)
4. To determine future wetness regimes in sandstone walls throughstatistically downscaling climate projections and utilising links betweenwetness and climatic parameters discovered in objective 3. (Smith &Betts)
Objectives 2Objectives 2
5. To investigate the relationship between moisture levels and iondiffusion of key anions and cations within sandstone blocks and theirpotential significance for sandstone deterioration. (McAlister andBasheer)
6. To investigate the links between greening (algal colonisation) ofsandstone blocks and moisture regimes and deterioration and todevelop and test new conceptual models of sandstone deterioration
under wetter, ‘greener’ conditions. (Viles, Smith and Whiteley) 7. To devise practical advice for building with sandstone and
managing the greening and deterioration of existing sandstone wallsunder wet conditions. (Smith, Basheer, Betts, McAlister, Viles &Whiteley)
Programme stagesProgramme stages
PROGRAMME STAGE 1: Field survey and sampling of sandstone walls,Belfast (Objective 1)
PROGRAMME STAGE 2: Construction and monitoring of test walls nearEnniskillen (Objectives 1-3)
PROGRAMME STAGE 3: Laboratory simulation of algal colonisation and itsimpact on moisture regimes and sandstone deterioration (Objective 6)
POGRAMME STAGE 4: Laboratory simulation of ion diffusion withinsandstone blocks under saturated conditions and its impact on sandstonedeterioration (Objective 5)
PROGRAMME STAGE 5: Linking current climate to moisture regimeswithin sandstone masonry walls and predicting future conditions(Objectives 3 and 4)
PROGRAMME STAGE 6: Developing practical guidance and advice forfuture use and management of sandstone masonry in NW UK (Objective 7)