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Moisture transport throughbuilding material
DifussionCapillary elevationHygroscopySurface condensationAtmospheric water
Diffusion
moisture move from a centre of high concentrationto low to achieve an equilibrium concentration
CapillaryCapillary attractionattraction
relatedrelated to to thethe surfacesurface tensiontension ofof waterwater
CapillaryCapillary attractionattraction
In In practicepractice::
•• mmateriaterialsals withwith biggerbigger poros poros absorbabsorb waterwater quicklyquickly, , butbutthethe highhigh isis lowlow
•• smallsmall pporousorous materimaterialsals absorbabsorb waterwater slowlyslowly, , butbut veryveryhighhigh
•• meanmean diameterdiameter ofof porousporous in in masonrymasonry 1010--5m,5m,itit correspondscorresponds toto highhigh ofof capillarycapillary actionaction1,49m1,49m
Surface condensationthermalthermal bridgesbridges ((surfacesurface moisturemoisture isis higherhigher thenthen interstitialinterstitial))
Hygroscopicity
hygroscopichygroscopic saltssalts (e.g.(e.g.calciumcalciumchloride)chloride) trytry to to achieveachieve equilibriumequilibriumwithwith theirtheir surroundingssurroundings by by takingtakingupup oror releasingreleasing moisturemoisture
Gravity-hydrostatic pressure
in in basementbasement wherewhere thethe waterwater table table isis wellwell aboveabovebasementbasement floorfloor levellevel
AtmosphericAtmospheric waterwaterWindWind presurepresure rainrain waterwater
forcingforcing thethe moisturemoisture to to enterenter thethe materialmaterial
MoistureMoisture analyseranalyserFullyFully automaticautomatic, , dryingdrying untiluntil constantconstant weightweight
Maximum Maximum weightweight capacitycapacity 45g45g
MoistureMoisture analysisanalysisgravimetricgravimetric methodmethod –– laboratorylaboratory testingtesting