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Humidity in Canadian buildings Hutcheon, N. B.
CANAI Ser TH1 B92 no. l g c . 2
BIJXI31FL
IW
CkNf-DIAR BUILDIN'ESby
N.B. Hutcheon
( A talk
sf-ven
at the Canadian Chapters Confe-r e n c e ,
ASHAE, T o r o n t o , February14,
1955.
)7 . J > ,.-
-h * :,+ ,.% . C
-
rm e materials o f which a house
is
made m a gnormzlly c o n t a i n 2500 pounds o f w a t e r , T h e a i r contained
in the house a t any one time nil1 amount t o abollt
750
poundsof
which about5
pounds w i l l be w a t e r vaTour, The maintenance of t9is relatively s m a l l w a t e r content of the a i r at t h e properl e v e l c a n b e v e r y i m ~ o r t a n t since
it
may determine not only thel e v e l of moisture c o n t e n t of" furnishings, and of m u c h of t h e
house structure
itself,
b u t a l s o r a t e s o f e v ~ l o r a t i o n or of moisture u p t a k e w h i c h m a y affect y e o p l e as well a s m a t e r i a l s ,Excessive mofsture l e v e l s mag l e a d to r a p i d d e t e r i o r a t i o n or other faulty s e ~ v i c e f r o m many m a t e r i a l s .
Tke human
body i s a d a p t a b l e t o changing moisture conditions over a fairly wide range without serious ill effectson
health, while under the same conditions manymaterials e x h i b i t undesirable characteristics, The regula-
tion
of m o i s t w e l e v e l s in the air will often be more readilyj u s t i f i e d
on
t h e b a s i s of the responseo f
materials thanof
people,
In
some cases the absolute level of w a t e r c o n t e n tis of concern while in o t h e r s
it
is the r e l a t i v e l e v e l , usually expressed as r e l a t i v ehumidity, which
becomesof
h p o r t a n c e .
In
view of these complications, a b r i e f r e v i e wof the p r o p e r t i e s of w a t e r vapour
in
air i sin
o r d e r , before proceeding to f u r t h e r d i s c u s s i o n of humidity,P r o p e r t i e s
of
Water-
Vapourin
AirWater
vapourin
a i ris
a gas w " n i c h occupiesa l l the
space, along w i t h the air present,I n
many ways the water vapour c a n act independently of the a i r , since in g e n e r a l i t s properties do not depend on the presence of the a i r ,I t
exerts i t s o x m vapour pressure and c a n move about throughair
in a space,or
move through materials under differences in i t s ownvanour pressure, independently o f
the
a i r ,However,
when the air is moved suddenlyo r
is h e a t e d o r c o o l e d , the w a t e rvapour
present is s i m i l a r l y a f f e c t e d , s o t h a t
it
i~ u s u a l l y necessaryto consider it a s a p a r t of an air-vapour r n l x t u r e .
Some of t h e characteristics
of
water v a p o u r ,and
particularly t h e changes in properties of a m i x t u r e
of
a i r and water v a p o w can best be presented by a sinple p l o t ofwater vapour c o n t e n t of t5c ~ i r a ~ h i n s t t e n p e r a t u r e , a s
shown
in
F i g u r e1.
On
t h ev e r t i c a l
s c a l eis
shownt h e
v a n o u rc o n t e n t
a s a p ~ r c e n t a 5 ebg
w e i z h tof
t % e r d i e i ~ h tof
dr:: a l r p r e s e n t . Thel i r n i t f n : ? cp
a n t i t i e s r.rhich c a n be h e l d st anyc l v e n t e m p e r a - t u r e z r e
shown by
t h e heavyline nlarked
'saturation".
A t
7 5 ' ~ ~
f o r example, t h e ueter vapour c o n t e n tis
1.9
p e r cent. A t49'
( p o i n tD )
t h e w a t e r vapour required f o r saturztian i s 0.7 ner cent r d h i l eat
2 0 ~ ( ~ o i n tF)
o n l y 0.2per cent i s required.
If
at n temperature o f7 r ° F
t h e r e i s lessthan
1,9
p e r cent o f water vapour p r e s e n t , the air-vapourm i x t u r e i s s e i d t o be g a r t i a l l y saturated, T!le d e g r e e of ssturation c a n be expressed
in
t a m s o f r e l a t i v e humiditg.Cn
t h e v e r t i c a lline
r e p r e s e n t i n g7 5 O ~
a number of points can be l o c a t e d which correspond to the percentages of w a t e rvapour p r e s e n t at v a r f o u s values of r e l a t i v e humidity. This c a n be extended t o o t h e r t e m p e r a t u r e s t o permit the construction of t h e c u r v e d l i n e s on t h e c h a r t s%ewing r e l a t i v e
humidity.
Un h s a t l n z or cooling
an
air-vapourmixture
withoutc h a n g t n g t h e w a t e r c o n t e n t , the percentage o f water p r e -
sent will obviously remain c o n s t a n t , and t h e s e processes
c a n be represented b y h o r i z o n t a l l i n e s on t h e c h a r t . Three processes t y p i c a l of cnndftfons which arise at times in
b u i l d i n g s a r e shown, e n d w i l l bs discussed.
D a m ~ n e s s in Basements
T'ne c o n d i t i o n s in a damp basement
on
a h u d d d a yIn
sm-ner might be represented by p a i n t A, c o r r e s p o n f i n gto
100
p e r cent relative humidity a t75'.
At
t h i s conditionm o l d s
will f o ~ m ,
w o o d will s w e l l and clothing and o t h e r ~ r t i c l e s w i l l be ('amp.If,
however,
heat 5 s addedt o
tke n i xt o
r a i s e i t s temper2ture t o y o 0 , t h e r e s u l t i n g
" n r o c e s s t '
can be r e p r e s e n t e d Sy t h e lLne A I3on
t h e c h e r t . The finalcondition, represented bg point B, shows t h a t t h e r e l z t i v e
h u m i d i t y w i l l - b e o n l y 62 per cent, Clothes w i l l now dry, a n d wood
will
s h r i n k t o a mare n o m a l condition. A d d i n g h e a t ist h u s one w a g of' curing dampness
In
b a s e m e n t s a l t h o u g hin
summer t; he c u r e m a y be l e s s acceptable
t h a n
thea i l m e n t .
Point
C
represents a coAm-3n c o n d i t i o n in modern C a n a d i a n homesi n
winter: 40 p e r c e n t r e l a t i v e h u m i d i t y at75'.
The windows u r f a c e s ,
however, may be only at4q0,
T h i sw
;.ndow s u r f a c e , as shown by t h e process l i n e CI),
Thetenperzture
o f
1 1 9 ~
at N!IIC~ Kqis air-vapour m i x t u r e ,if
cooled, becomes s a t u r a t e d , is k n o w n a s
i-t;s
d e w - ~ o i n tA.
:
r
e
If
the windowsurf
sce is colder then the dew-p o i n t of
tth
eair v a p o wrnixtme in contzlct
w i t hit,
condensatian r , r i l l o c c u r ,
?or
t?le e x a i ~ ? l e represented bythe
process C
D E,
the a i r in contact rdth the w i n d o w surface at 3 2 O c2n o n l y r e t a f n0 - 3 7
p e r c e n t moisture, w h r e a s t h e r ew a s
0.74
per c e n t present i n i t i a l l y , and condensation on t h e w i n d o w surfacemust
occur,If
the v i n d a w surface l a above32'
the condensation w i l l appear as dew; if below 32',it w i l l
appear a s frost,
The s w f s c e s a? nost cannon materials have
an
af_Cinitg f o r r ; a t c r m o l e c c l ~ s . i ! o l e c u l ~ r f o r c e s ora t t r z c t - i o n ~ \ l f l lh o l d w a t e r molecules to the surface,
The
thickness of t h e w a t e r f L h 2ornied, and t h e r e f o r e t h e m o u n t
of
water h e l din
equilibrium ractl? the surroundcling atmosphere is r ~ v - g h 1 ~ p r o p o r t i o n a l to r e l z t i v ehmiei
ty,
D a t a on the m o i s t w e contefits
o f
varSolrs commonrnzt e r i a l s
in equilibrium w i t ht h e
atmosphere a t v a r i o u sr e l a t i v e h m i d i t i e s a r e availzhle. Wood, far e x a m r ~ l e , ~ a i T 1
have a m o i z t w e c o n t e n t o f
5
p e rcent
by w e i g h t at 2 C p a r cent~ e l ~ t i v e
humldTty. T b j s increases to10
p e r centat
50 p e r c e n t r e l a t T v e humidity, and to 30 p e r c e n t z t r e l a t i v ehumidities v e r y
c l o s e
to 1CQ pep cent.It
w i l l o f coursec c n t a i n oven more water thsn L l i s
when
f u l l y saturated. Plost p l ~ n t a n daninal
aroducts ex.hib5.t similar ~ r o p ~ r t i e s * IuIascnrymaterials a l s o ~E!TF: on
water
f r o mt h e
a i r ,Significant dimensional changes t a k e p l a c e
in
many
m o t c r i a l s u s e d in buildings with changein
r r ~ o i s t w econ t e n t . Again, wood providez a r ~ ~ e l l - k n o w n example,
It
exhibits s'lrFnBa,ges o f a b c c t 0,1? 2 , and
4
p e r cent in the Scngitudinal, r a d i a land
tangential directTans respeetive-ly
on a change f'.'rcnair-dry
at12
to 15
p e r c e n t moisturec ~ n t e n t
to oven-dry. Simillar ex?ansions trike p l z c e rfxcn ther n c i s t w e content 5s r c ~ { ~ a r e d . . Most w o o d . - r i b r e products,
including
papers,w113
exhibit n o T s t u r e c > ~ n n s i a n consistent w i t h the b a s i c ~ . - o o d properties t o a degree dependento n
thef i k re orientation 2nd srrnncement, A l r ~ o s t all y l a n t and a n i m a l products exhibit similar
expansion
and contractionw i t h changes
Zn
m o i s t u r e c o n t e n t , Less g e n e r a lly
recognizsd are the d h ~ n s i o n a l ckanges w h i c h can occur ir? - ~ l r : , ~ ' : ~ y m a t e r i a l s a s aresult
of changes in r n o i s t ~ z e c c - - ' --_>,
- -
wateris
eitheran
essentialor
a c o n t r i b u t o r yf a c t o r
in
a l m o s tall
c a s e s o fbrezkdown
of building m a t e r i a l s resulting from chemicalchanges
such as t h e rusting o fs t e e l ,
p h y s i c a l changes such as the palling of
mascnry
by frosta c t i o n , 07 b i o l o g i c a l processes such as t h e
r o t t i n g
o f p l a n tand
animal
products,In
all c a s e s these e f f e c t s a r eninin5zed or eliminated if a l o w l e v e l of moisture
content
c a n be maintained,
X f f e c t s
of
R e l a t i v e Humidityupon
PeopleThere
is, curlnusly
enough, little concZusivee v i d e n c e t o show
that
eltherhigh
o rlow
r e l a t i v ehumidities
a r e of t h e m s e l v e s d e t r i m e n t a l t o the h e a l t h of normalgeople,
It
may be predicted, from the known p r o p e r t i e s of 1 - ~ a t e r , t h a t l o w humLditieswdlL
l e a d t o dry !lair and skinand to i n c ~ e a s e d e v a p o r a t f o n r a t e s f r o m t h e membranes of
t h e resniratory system, and t h a t h i g h h u ~ i d i t i e s will
wro2uce
t h e oppositeeffect,
Evzporation from t h es w f
aceof
t h e body is one of + 5 e rnechanf sms emnloyed by thehuman body to regulate i t s tem~erature.
If,
however,
thee v a p o r a t i r n r a t e tends t o be e i t h e r high o r low b1. v i r t u e
of low or
high
humidLty of the surroundinga l r
the Codyi s a b l e
to
make caapensating adjustments w i t h o u t , as f a ras is known, any ill efzects under normal conditions. EvLdence on Yne e f f e c t s of krumtdity upon the
s p r e a d of air-borne bacteria is also inconclusive.
Cornfort, as o p p o s e d
to
h e a l t h ,is
a subjective reaction. P e o p l ea r e
c o m f o r t a b l eor
uncomfortable ifthey
t h i n k they a r e .
It
seems r e a s o n a b l e t o assuxathct
drynesso f t h e hair, s k i n , and nasal passages ~ e s u l t i n g f r o m
low
humidity,
or
a wetness of t h e s k i n resulting f r o m h i g hhumidifv
a r e
i n v o l v e din
s e n s a t i o n so f
discomfort attribut- ed to extremes of humidity,It
may be n o t e d , however, t h a t conditions w3icha r e
normal
t o one p e r s o n may be abnormal, and t h e r e r o r e uncomfortable 50 anather,The
well-known
ASSAE Comfort C h a r t which has beenin
use f o r many y e a r s i n d t c a t e s t h a t a s the r e l a t i v ehumidity
f s increased, t h e temperature o f t h e air*must
belowerg8 t o p r o v i d e t'ls same comfort sensation.
A
temperature of74
F
at
10 p e r cent r e l a t i v e humiditsi s
shown to p r o v i d e t h e szme c o m f o r t a s a t e ~ e r a t u r e o f 7 0 w i t h a r e l a t i v e3 m i d i t y
of
50 p e r c e n t .It
has
been a ~ g u e d t h a t humidifying a house w i l l result in a s a v i n g inf u e l
since t h e temnperatwe can beloprered r ~ i t h o u t s a c r - i f ice
in
c o m f o r t , C ~ l c u l a t i o n w i l l s y o w , however, t h a twith
normal r a t e s o f a i r l e a k a g ein
houses tbe
e x t r a
r u e 1
r e q u i r e d to e v a ~ o r a t e t h e w a t e r for humidification w i l lusually
offset t h e szzving t o be made by t h e t e m p e r a t u r ereduction
p e ~ r n i t t e dby
the
comfort c h a r t ,A
research papep p r e s e n t e d r e c e n t l y before theASHAE
r e p o r t s no change in sensations of' comfort over therange of r e l a t i v e humidity f r o m 30 to 80 p e r cent, at l e a s t
f o r c o n L 5 t i o n s at tqhich no free
sweat in^
occurs. Thisi n d i c a t e s t h a t the influence of r e l a t i v e humidity may
be
over- emphasized by the Comfort Chart, The b a s i s f o r the ComfortC h a r t is
shortly
to be re-examined through an e x t e n s i v e r e s e a r c h program,It
haslong
been recognized thaithe
r e l a t i v ehumidities
in
Canodian
buildin~s h e a t e ? to comforttemperatures a r e u s u a l l y quite
low
in
w i n t e r , The o u t s i d ea i r
I-fhich e n t e r s a bui.1 ding in w i n t e r has a l o w moisture c o n t e n t , and when h e s t e d provides low r e l a t i v e humidity unless substzntial quantities o f w a t e r a r e e v ~ p o r a t e dwithin the b u i l d i n g , This mzy be v e r i f i e d by r e f e r e n c e to t h e process shown by the line
F
G
of Figure 1, whichshews % h o t a i r from outside at 2 0 ' ~ and 100 p e r c e n t r e l a t i v e
humidity
r ~ i l lwhen
h e a t e d to75%'
have only 12 p e r cent r e l a t i v e :mrnidity. The m o t s t w e c o n t e n twill
haveto
beincreazee f r o m 0,2 to
0,74
p e r cent to p r o v i d e40
per cent r ~ l a t i v ehumidity,
The r e l a t i v e humidity
w i t h i n
a b u i l d i n g w 5 l Zdepend cn t h e moisture c o n t e n t of t h e outside a i r , the
v e n t i l a t i o n
r a t e ,
the rate at w h i c h moisture i s l o s tt h r o u g h t h e building enclosure and the rate at w h i c h m o i s t - u r e is s u p p l i e d to the air within t h e b u i l d i n g ,
These
f a c t o r s m a y v a r y widely from one caseto
another,The average January temperature in Vancouver is
~ S ' F
w h i l e t h a tfor
O t t a w a is +10'~.The
correspondingo u t d o o r r e l a t i v e hwnZdPties a r e about;
the sane,
88
p e r cent,at each l o c a t i o n . However, when outtioar ~ . i r at t h ~ s e c o n d i t i o n s
i s
mimed t o7S0F
t3eresulting
humidity f o rOttewa
is onlyr.$
per c e n t while t h a t f o r Vancouver is 25 per cent,In
manyp u b l i c buildings h a v i n p high v e n t i l a t i o n r a t e s and l o w rates of moisture s u p ~ l y , the relative humidities produced w i l l . be
c l o s e t o
these
values,'d?um the
v e n t i l a t i o n r a t eIs
at t h e m i n i m w l l r e q u i r e d of10
c f a p e r person, the r n o i s t u r erate
r e s u l t
in
'nuruictitics s f60
r?sr c e n tfop
I ~ c n c o c v e r 2nd1;s
n e r cent
f o r 0ttal:x.It
rngy bbe n o t e d t h a t n ~ b l i c b u i l d i n g sin
Vancouver may n o t r e q u - i r e huvidiflcatlon even ir_ w i n t e r , an2 thath ~ ~ i d i k s s s n a y ~ i s e at times a b o v c 50 g e r c e n t at m o d e r a t e
to low ventilation r a t e s ,
In
d w e l l i n g s thc situ2tioa i s s o m m h a t d i f f e r e n tt h a n in
~ u b l i c bxildings s i n c e ventilation rates a r efrequenklg reduces to a nlinimwn
in
o r d e r to conserve fueland t h e r e are substantial sources of m c i s t u r e . T h e a v e r a g e Canaciian dr.relling + r i l l '.lcLrc a transmission h e a t l o s s of
about
0.04
Btu
p e r cubic T o o t o f b u i l d i n g v c l - m e per degreeternperatme d i f f e r e n c e
between
indoors and outdoors, Vent-i l a t i o n (or infiltrstian) w i l l add to t h i s to the extent
45
p e r cent for e a c h h o u r l y air change. The s p a c e p r o v i d e d per o c c u p a n twill
f o r manyhouses
be a b o u t 2000 c u b i c feet, andthe hourly air change reqcired
f o r
v e n t i l a t i o nat
the acceptedm i n i m u x o f 10 cfm p e r p e r s o n w i l l be cnly 0 . 3 , Tne advantages
in
fuel economy o f reducing the v e n t i l a - t i o nr a t e
a r e a p p a r e n t ,It
has
been d e t e r ~ ~ i n e d t h a t the a v e r a g e familyof
f o u r w f L l produce by i t s a c t i v i t i e s w i t h i n a house about0 , 7 pounds of w a t e r vapour p e r h o u r normally, b u t t h e t this
fireg r i s o t o a s much a s 2 pounds p E r h o w on w a s h days,
These q u a n t i t i e s may be used to calculate t h e v e n t i l a t i o n
r a t c s at r~r'nricln
40
per cent r e l a t i v e humidity will b e m a i n t a i n e dw i t h i n
the
?tousefor
t h e a v e r z ~ ; eJanuary
c o n d i t i o n s at Vancouver 2nd at O t t a w a .It
i s f o u n d thatfar
Vancocver the ventilationr e t e must
b e 0.40 2S.r c h a n f ~ e c per hour nc.rmz!llg, a ~ d 1.1on
wash days and for O t t a : . ~ a t h e r a t e s
must
be 0.25 and 0,F.S a i rchanges p e r h o w . Since o n l y
0.3 air
changes p e r hour arer e q u i r e d f o r f r e s h c s s
it
may b e concluded! t h a t many houses a r e a d e c j u a t e l ~ 1 1 a ~ 1 i d . i f fed by norrrlal mcist-ure soEpcesw i t h i n t h e house,
Tf
t h e v e n t i l a t i o n r a t e s a r eminimum,
Ondays on which exceptional
amounts o f
r n c i s t w e are r e l e a s e d within t h e houseit
may be necessary t o i n c r e a s ethe ventilation r a t s
fnr above t h e ninimm to p r e v e n t t h e r e l a t i v e humidity
from
-
rising above 40 per cent,
T h e cases just considered a r e
for
a v e r a g e modernhouse:, t i g h t l y constructed, and u i t h a r e l a t i v e l y
low
v o l u m eper occ'llp~nt, Older, l a r g e r houses, multi-storey, h a v i n g =any
100s
e-Ti
thing ~ a i n C o i . ~ s , and 3 ~ o v i d i n g Large volume p e r o c c ~ p a n t w i l l have unavoidably I ~ i g h v e n t i l a t i o n r a t e s and may haverelatively small n a t u r a l m o i s t u r e sources, Rere, t h e extreme
low btwnid.ities may approach t h o s e c a l c u l a t e d f o r p u b l i c :
T o r Vancou-~er and
5;
p a x a cent f o r O t t a ~ * i a , and m a ybe
evenl o ~ ~ j e r
f o r
p e r i o d so f
extremel o w t
em>erature. Feglecting
n a t w a l m a i s t ~ r e c o u r c e s , .r: ~ u c h a s
9.6
gallcnsof
v:.raterp e r day w i l l have t o be,added t o rrtaintain
40
p e r cent relative humidity a t7s F
f o r
each 10,000 cubic f e e t oPb u i l d i n g v o l u ~ e
f o r
one a i r change p e r hour w i t h c u t d o a ~air
6
szturatcd at 20
F,
k n ~ r i l e houses
of
twenty o r g l r r e ! gears ago had v e r glow humidities unless humidifiers w e r e u s e d , it is p r o b a b l e
that
2 l a r g e p r o p o s t j o n of the h o u s ~ s constructed within the l a s t t c n y e a r s h a v e s-ficient humidity p r o v i d e d by natural. sources w l t h i n the house,Upper
Limits
of Bumidity in i J i n t e rL i m i t s a r e p l a c e d
on
t h e r e l e t i v e humidities v ~ h l c h c s n b e c r . r r i e d in Canadian b u i l d i n g sin
w i n t e r bythe
occurrence of condensation, The occurrence of v i s t b l e candens
at
ion on t h e room-side s ~ r f a c e sof
windows, walls,f l o o r s , and c e i l i n g s depends upon t h e co~binstion o r t h e
r e l a t i v i :
humidity
maintained a n d the extent of the cooling produced a t t h e surfaces in question. Visible condensntiona l t h o u g h cornyon cn v:indows in w i n t e r i s n o t a s t r c u b l ~ s o m e as c o n c e a l e d c o n d e n s a t i o n which can ~ C C U T in r o o f s , attic spaces, and in w a l l s , Water vapour can & i f f u s e through
i n t e r i o r finishes o f w a l l s and t h r o u g l ~ ceilings, or m a y be
carried by a i r l e a k a g e ,
until it
encounters cold surfacesand i s c o n d ~ n n c d , When the surfaces on w11ich t h i s condensa- tion occurs ere brlow
freezing
f o r l o n g p e r i o d s of t i m e t h econdensation
accumulates
as frost,It
is n o t impossible(in
the c o l d e r a r e a s o f ~ a n a d a ) , with p o o r v z p o u r c o n t r o l ina w a l l or ceiling t o c o l l e c t a s
much
as one pourad or frostp e r square foot of w a l l or roof a r e a ,
This
providesone
g a l l o n o f w a t e r p e r stu.d s p a c e
in
a frame w a l l , w h j ~ ? rr-aybe r e l e a s e d o-Jer a few h a w s upon a r i s e
in
-t;emper:-t!rrre.. There is l i t t l e p o i n t in attelrrpting to f o r c e t h er e l a t i v e humidity in a building zbove the paint at which visible ccndensotion begins to occur, s i n c e the moisture
added will be transferred t o t h e c o l d s u r f a c e s and % r i l l
accumulate
t h e r e . The u p p e r lirnfts imposed o n r e l a t i v e humidities if windornr c o n d e n s ~ t i o n i s t o be avoided a r eOutdoor
TemperatureSin@
e Illlndow Double WindowWind
Nu
Wind Wind N o WindIt
nay be n o t e dthat
double windows p r o v i d e higher i n s i d e surf ace temperatures m d t h e r e fo r e
permit hZgher humidities t o be carried,Houses
can now be reasonably w e l l constructed,w i t h i n s u l a t i o n , v a p o u r b a r r i e r s , and a t t i c ventilation, s o
t h a t
it
i s p o s s i b l e to c a r r y humidities u p to - h o s e produc- i n g window c o n d e n s a t i o n , w i t h o u t o t h e r m o i s t u r e dlf'f i c u l t i e s ,150st public and commercial b u i l d i n g s a r e net cons true t e d t o t h e same s t a n d a r d s o f I n s u l a t i o n and v a n o u r c o n t r a 1 as wood frame houses and cannot
t o l e r z t e
the same r e l a t i v ehumidities without difficulty, Indeed much contemporary
b u i l d i n g d e s i g n employfng much glass and m e t a l . in w a l l s
is accentable only if t h e
inside
r e l a t i v e h m d d i t i e sa r e
allowed- t o remain at a low l e v e l
in'
cold weather,The humidity in
o l d e r houses andin
most publicand cormnercial buildings
not
s p e c i a l l y designed f a r p r o p e rc o n t r o l of
w a t e r vapour s h o u l d p r o b a b l y not ~ x c e e d 20 p e r centa t temperatures below z e r o . F o r
ineoor
humidities ofSO
peycent a t sub-sera o u t s i d e temperature, insulation and vapour
b a r r i e r s
must
be used, Low r e s i s t a n c e h e a t p a t h s p r o v i d e dby metal
or
s o l i d masonry at columns, at t h e edges of f l o o r and r o o f s l a b s and arcund v.Jindowsm u s t
be avoided, orgiven
s p e c i a l treatment to e l h i n a t e cold
room-side
s u r f a c e s , Double windov~s a r e essential,Industrial
buildingssuch
a stextile mflls
inwhich
hwniditleso f
70
t o 80 p e r cent mustbe c a r r i e d r e q u i r e still g r e a t e r preczutions in design, Windows m a y h a v e to b e eliminated, s p e c l a l vapour barriers,
u s u a l l y a p p l i e d as the i n s i d e surf ace,
will
b e required,and
h e a t may have to be introduced a t c e r t a i n portions of the
structure
t o maintain adequately high surface temperatures,R o o f s
f o r
such conditicnspresent a
s p e c i a l problem.It i s
clear
that
m z n y problems and much expense a r einvolved when
Conclusion
While I t w o u l d be d e s i r a b l e t o a v o i d
htgh
m o i s t m e c c n t e n t s top r e v e n t
deteriorationof
t h e b u - i l d i n gstructure,
and a"t;ihe
same
t i m e to p r o v i d econstant humidity the
Fearround t o minixize
d i m e n s i o n a l and o t h e r chztngesin
m t e r i a l sand
ru~nizhlngs
witbin
a b u i l d i n g , thisis
d i f f i c u l t t o achieve mder C s n a d i m~ - 1 i n t e r
c o n d i ti
a n s . Evennoderat
ehumidities inside buildings can produce wetting by condensa-
t l o n
on
andin
the buildingstructure,
because o f the larget e m p e r a t u r e gradients w Z t h i n w a l l s in rdinter. T h e b e s t
answer
in
many c a s e s where higher humidities are not; necessary r i i L L b e to allow the humidities to f 2 l l t o l o w l e v e l s . Inthe case
of b u i l d i n g s having l a r g e moisture s o w c e s steps may have to be t a k e n t o ellmTnate water v a p o u r f r o m t h e n t oa v o i d condensation. Consideration should
z l w ~ y s
be
g i v e nto
t h e difficulties which m a g he c r e a t e din
any g i v e nb u i l d i n g b e f o r e humidification i s added. )ken
r e l a t i v e
humidities