Publisher’s version / Version de l'éditeur:
Vous avez des questions? Nous pouvons vous aider. Pour communiquer directement avec un auteur, consultez la
première page de la revue dans laquelle son article a été publié afin de trouver ses coordonnées. Si vous n’arrivez pas à les repérer, communiquez avec nous à PublicationsArchive-ArchivesPublications@nrc-cnrc.gc.ca.
Questions? Contact the NRC Publications Archive team at
PublicationsArchive-ArchivesPublications@nrc-cnrc.gc.ca. If you wish to email the authors directly, please see the first page of the publication for their contact information.
https://publications-cnrc.canada.ca/fra/droits
L’accès à ce site Web et l’utilisation de son contenu sont assujettis aux conditions présentées dans le site LISEZ CES CONDITIONS ATTENTIVEMENT AVANT D’UTILISER CE SITE WEB.
Internal Report (National Research Council of Canada. Division of Building Research), 1959-12-01
READ THESE TERMS AND CONDITIONS CAREFULLY BEFORE USING THIS WEBSITE.
https://nrc-publications.canada.ca/eng/copyright
NRC Publications Archive Record / Notice des Archives des publications du CNRC : https://nrc-publications.canada.ca/eng/view/object/?id=99ab0042-bca8-4242-8da1-a5d8ec0bf9e4 https://publications-cnrc.canada.ca/fra/voir/objet/?id=99ab0042-bca8-4242-8da1-a5d8ec0bf9e4
NRC Publications Archive
Archives des publications du CNRC
For the publisher’s version, please access the DOI link below./ Pour consulter la version de l’éditeur, utilisez le lien DOI ci-dessous.
https://doi.org/10.4224/20338101
Access and use of this website and the material on it are subject to the Terms and Conditions set forth at St. Lawrence Burns: radiant temperature of openings
NATIORAL RESEARCH COUNCIL CANADA
D I V I S I O N OF BirTLDING RESEARCH
ST. LAWRENCE BURNS
RADIANT TEMPERATURE O F OPEXINGS by D. G. S t e p h e n s o n R e p o r t N o . 156 o f t h e D i v i s i o n o f B u i l d i n g R e s e a r c h OTTAWA December 1959
The circumstance:; t h a t l e d t o t h e c a r r y i n g o u t of f i r e t e s t s on e i g h t b u i ' l d i n g s i n t h e p r o j e c t lcnown a s t h e S t . Lawrence Burns, a r l > l t h e o b j e c t i v e s a n d t h e ways i n which t h e s e were achicvtci a r e f u l l y d e s c r i b e d i n a
g e n e r a l r e p o r t . I t c o n s t i t u t e s t h e complete r e c o r d of t h e planning and e x e c u t i o n of t h e experiments, t o ~ e t h e r w i t h
a l l g e n e r a l inforniation. The d e t a i l s on each kind of
measurement made, i n c l u d i n g t h e r e s u l t s o b t a i n e d , a r e con- t a i n e d i n s e p a r a t e companion r e p o r t s of which t h i s i s one.
A l l t h e r e s u l t s a r e combined and a r e d i s c u s s e d and f i n a l c o n c l u s i o n s drawn i n a summary r e p o r t .
D u p l i c a t i o n h a s been avoided a s f a r a s p o s s i b l e , and i t w i l l be n e c e s s a r y t o r e f e r t o t h e g e n e r a l r e p o r t i n r e a d i n g any of t h e o t h e r r e p o r t s i n c l u d i n g t h i s one f o r any i n f o r m a t i o n which i s p e r t i n e n t t o more t h a n one of them. A l i s t i n g o f a l l r e p o r t s on t h e p r o j e c t f o l l o w s t h i s p r e f a c e .
Tho p a r t i c i p a t i o n of t h e B r i t i s h J o i n t F i r e
Research Organization i n t h e experiment, t h e i n t e r e s t and s u p p o r t of t h e Federal C i v i l Defence a u t h o r i t i e s , t h e a s s i s t a n c e of t h e O n t a r i o F i r e Marshal and h i s s t a f f , and f i n a l l y t h e complete c o - o p e r a t i o n and v e r y c o n s i d e r a b l e a s s i s t a n c e extended by t h e Hydro-Xlectric Power Commission of O n t a r i o a r e a l l g r a t e f u l l y acknowledged. I t i s
a
p l e a s u r e a l s o t o be a b l e t o r e c o r d t h e s p e c i a l c o n t r i b u t i o n made by members of t h e s t a f f of t h e F i r e S e c t i o n who worked l o n g h o u r s , o f t e n under t r y i n g f i e l d c o n d i t i o n s and a t g r e a t p e r s o n a l inconvenience, t o meet t h e many d e a d l i n e s and t o complete t h e p r o j e c t i n a most s a t i s f a c t o r y manner.
The a u t h o r of t h i s r e p o r t i s D r . D. G. Stepheneon, r e s e a r c h o f f i c e r w i t h t h e B u i l d i n g S e r v i c e s S e c t i o n of
t h i s D i v i s i o n , who a s s i s t e d t h e F i r e S e c t i o n i n t h i s p r o j e c t by a r r a n g i n g f o r and a n a l y s i n g t h e r e a d i n g s of r a d i a n t temperature of window openings.
Ottawa
REPORTS ON THE ST. LA~"lRBIlTCE BURRS
-
--
Sub-Tit13 Author
General Report G. 1.V. S h o r t e r
Smoke and Sowid Nea s u r e n e n t s G. Williams-Leir
Temperature Idea surement s G. JJ!illiams-Leir
Radiometer Measurements J . H . McGuire
V e n t i l a t i o n Rate Measurements J . H . I~IcGuire Resis-tance Thermometer
Measurements J . H . McGuire
Radiant Temperature of Openings D. G. Stephenson
Gas A n a l y s i s J . R . J u t r a s
Summary R e p o r t G. W. S h o r t e r and
S T . LA!O3ENCE BURNS R A D I A N T
TEMPERATURE
OF OPENINGSD.G.
Stephenson S i n c e a b u r n i n g b u i l d i n g can i g n i t e n e i g h b o w i n g s t r u c t u r e s i f t h e r a d i a t i o n r e a c h i n g t h e exposed s u r f a c e 8 i s s u f f i c i e n t l y i n t e n s e , b u i l d i n g codes u s u a l l y s p e c i f y a minimum s e p a r a t i o n between b u i l d i n g s . I t i s p o s s l b l e t o c a l c u l a t e t h e s e p a r a t i o n which i s r e q u i r e d t o p r e v e n t f i r e s p r e a d by r a d i a t i o n i f t h e f o l l o w i n g d a t a a r e a v a i l a b l e : 1. The i n t e n s i t y of t h e r a d i a t i o n e m i t t e d by a b u r n i n g b u i l d i n g ;2. The r a d i a n t energy f l u x which w i l l i g n i t e t h e exposed wooden p a r t s of a n a d j a c e n t b u i l d i n g .
I A q u i t e complete I n v e s t i g a t i o n of "The I n i t i o n of
Wood by ~ a d i a 1 ; l o n " was made by Lawson a n d Simms
7
l 9 5 2 ) , b u t v e r y few measurements of tho r a d i a t i o n e m i t t e d by a burning b u i l d i n g have been r e p o r t e d . Whon c a l c u l a t i n g t h e e n e r g y whiah may be t r a n s f e r r e d by r a d i a t i o n i t i s common t o assume t h a t t h e openings i n t h e s h e l l of a b u r n i n g b u i l d i n g r a d i a t e a 3b l a c k b o d i e s a t 1000°C. The v a r i a t i o n i n r a d i a t i o n i n t e n s i t
%
w i t h time i s normally n o t t a k e n i n t o a c c o u n t , i . e . , t h e 1000 Ci n t e n s i t y i s assumed t o e x i s t long enough f o r t h e exposed s u r f a u e s t o come t o a n e q u i l i b r i u m t e m p e r a t u r e . The S t . Lawrence b u r n s p r o v i d e d a n u s u s u a l o p p o r t u n i t y t o o b t a i n f i e l d measurements of the r a d i a t i o n e m i t t e d b y different t y p e s of b u r n i n g b u i l d i n g s a t v a r i o u s s t a g e s i n t h e development of a f i r e . A r e p r e s e n t a t i v e of t h e J o i n t F i r e Research O r g a n i z a t i o n ( G r e a t ~ r i t a i n ) measured t h e t o t a l r a d i a t i o n i n o i d e n t on a s u r f a c e l o c a t e d
a
known d i s t a n c e from t h e b u r n i n g b u i l d i n g . To supplement h i s r e s u l t s i t was d e c i d e d t o measure t h e e q u i v a l e n t b l a c k body t e m p e r a t u r e of a wlndowi n
t h e room where t h e f i r e s t a r t e d . These r a d i a n t t e m p e r a t u r e measurements a r e t h e s u b j e c t of t h i s r e p o r t .D e s c r i p t i o n of A p p a r ~ t u s and
---
ProcedureA t h e r m o p i l e r a d i o m e t e r d e s i g n e d by Linke and F e u s s n e r and manufactured by P m J o K i p p and Zonen of D e l f t was u s e d
a s
t h e r a d i a t i o n s e n s i n g devico. Tho i n s t r u m e n t was m o d i f i e d by r e p l a c i n g one of t h e 1/2-bil;- d i a m e t e r g l a s s f i l t e r s by a double w a l l e d s c r e e n w i t h a 114-in. d i a m e t e r h o l e a t i t s c e n t r e . With t h i s a p e r t u r e t h e i n s t r ~ ~ r n e n t oould be l o c a t e d up t o 20 f t from a n openlng 2 f t wide a n d s t i l l have t h e opening c o m p l e t e l y f i l l t h e f i e l d of view of t h o i n s t r u m e n t eThe e l e c t r o m o t i v e f o r c e g e n e r a t e d by t h e r a d i o m e t e r thermo- p i l e was r e c o r d e d by a s e l f - b a l a n c i n g p o t e n t i o m e t e r s t r i p - a h a r t r e c o r d e r , The r e c o r d e r had a r a n g e from
-5
t o + 5 m i l l i v o l t s a n d a o h a r t speed of 1 i n . p e r minute, A 5 - m i l l i v o l t b i a s v o l t a g e was p u t i n s e r i e s w i t h t h e p o t e n t i o m e t e r i n p u t s o t h a t t h e e f f e c t i v e range was from 0 t o +10 m i l l i v o l t s .The r a d i o m e t e r was s e t on a s u r v e y o r ' s t r i p o d a b o u t
5
f t above t h e ground. The t r i p o d was l o c a t e d d i r e c t l y i n f r o n t of and 2 0 f t from a window of t h e room i n which t h e f i r e waa s t a r t e d . To e n s u r e t h a t t h e i n s t r u m e n t was a c c u r a t e l y s i g h t e d on t h e c e n t r e of t h e window t h e f o l l o w i n g p r o c e d u r e was f o l l o w e d :I* A 250-watt i n f r a - r e d lamp was a t t a c h e d a t t h e c e n t r e of t h e window.
2 e The r a d i o m e t e r o u t p u t was c o n n e c t e d t o a d-c a m p l i f i e r w i t h a n o u t p u t m e t e r whioh s e r v e d a s a galvanometer,
3.
The r a d i o m e t e r was s i g h t e d on t h e lamp u s i n g the peep s i g h t which i s a t t a c h e d t o t h e b a r r e l of t h e i n s t r u m e n t .4
.
The f i n e s i g h t i n g w a s done by a d j u s t i n g t h e a z i m u t h a n d e l e v a t i o n t o g i v e a maximum o u t p u t from t h e t h e r m o p i l e . W i t h a 250-watt lamp a t 2 0 f t t h e r a d i o m e t e r i s v e r y s e n s i t i v e t o a n g l e , The p r o c e d u r e d u r i n g a b u r n was a s f o l l o w s : 1. The i n s t r u m e n t was s e t up o n t h e t r i p o d a t l e a s t a n hour b e f o r e t h e b u r n s t a r t e d ,2. The s i g h t i n g was done a s d e s c r i b e d and t h e r a d i o m e t e r o u t p u t was t h e n c o n n e c t e d t o t h e r e c o r d i n g potentiome t e r m The p o l a r i t y of t h e c o n n e c t i o n was checked t o make s u r e t h a t i n c r e a s i n g r a d i a t i o n c a u s e d an o n - s c a l e
3.
With t h e r a d i o m e t e r s h u t t e r c l o s e d t h e b i a s v o l t a g e i n the i n p u t c i r c u i t was a d j u s t e d t o give a r e c o r d e r r e a d i n g of z e r o on the c h a r t ,4.
The s h u t t e r was r e p l a c e d by t h e1/4-in.
diameter a p e r t u r e .5.
A t the o f f i c i a l s t a r t of t h e t e s t t h e r e c o r d e r c h a r t f e e d was s t a r t e d and t h e n t h e r e c o r d e r was l e f t unattended.6.
The o p e r a t o r went t o t h e r a d i o m e t e r and s t a y e d t h e r e d u r i n g t h e remainder of t h e t e a t . He r e a d and reoorded t h e radiometer temperature a t 1/2-min i n t e r v a l s andrecorded o b s e r v a t i o n s of t h e p r o g r e s s of t h e f i r e , gag., when t h e g l a s s broke, when t h e flames s t a r t e d coming out of t h e window, e t o .
7.
The radiometer was removed when t h e o p e r a t o r thought i t might be damaged by t h e c o l l a p s e ofa
w a l l o r when t h e h e a t was s o i n t e n s et h a t he could no l o n g e r s t a y by t h e instrument
A. C a l i b r a t i o n
The radiometer was purchased a s a l a b o r a t o r y s t a n d a r d which could be used t o c a l i b r a t e s o l a r r a d i a t i o n r e c o r d e r s .
A s soon a s i t waa r e c e i v e d i t was checked a g a i n s t t h e S i l v e r Disk Pyrheliometer No.
14
which i s t h e s t a n d a r d used bythe
Meteorological Branch of t h e Department of Transport. The oomparison was made on a c l e a r day u s i n g t h e sun a s a source. The average of many comparisons i n d i c a t e d t h a t t h e f a c t o r f o r t h i s i n s t r u m e n t i s
t
=
instrument temperature O C T h i s i s based on t h e I n t e r n a t i o n a l s c a l e of1956,
which g i v e s r a d i a t i o n v a l u e s 2 p e r c e n t lower t h a n does t h e1913
s o a l e . T h i s o a l i b r a t i o n was determined f o r t h e s t a n d a r d a p e r t u r e , n o t t h e s m a l l one. To o b t a i n t h e f a c t o r f o r t h e reduced a p e r t u r e , t h e r a d i o m e t e r was s e t up i n f r o n t of a g a s - f i r e d r a d i a t i o n p a n e land' the thermopile o u t p u t was reaorded a s t h e two a p e r t u r e 8 were a l t e r n a t e d . The r a t i o of out u t w i t h small a p e r t u r e t o
f:
o u t p u t w i t h l a r g e a p e r t u r e was 0.2 0. This i s a l s o t h e r a t i o of t h e s o l i d angle of view f o r the two a p e r t u r e s . The s o l i d a n g l e of view f o r t h e s t a n d a r d a p e r t u r e i s given by t h e i n s t r u - ment manufacturer a s W = ?f/125. Thus t h e angle f o r the reduced a p e r t u r e i s 0.260
x
,
71'/480.125
The r a d i a t i o n from a burning b u i l d i n g h a s a peak i n t e n s i t y a t wavelengths between 2 and
2.5
microns, whereas s o l a r r a d i a t i o nh a s i t s peak i n t e n s i t y a t about 0.5 micron. It was decided t o check t h e radiometer c a l i b r a t i o n f o r long wavelength r a d i a t i o n s l n c e t h e i n s t r u m e n t had only been c a l i b r a t e d w i t h s o l a r r a d i a t i o n . The D i v i s i o n does n o t have a h i g h temperature f u r n a c e which i s s u i t a b l e f o r c a l i b r a t i n g a radiometer i n t h e 2.5-micron range, s o t h a t a blaok body a t 100°C (10-micron wavelength) was used.
The r e s u l t s a r e given i n Appendix A. T h i s t e s t showed t h a t the c a l i b r a t i o n c o n s t a n t f o r t h e i n f r a - r e d r a d i a t i o n i s s l i g h t l y h i g h e r t h a n t h a t f o r the s o l a r spectrum. The f a o t o r a p p r o p r i a t e f o r s o h r r a d i a t i o n was used $or c a l o u l a t i n g the r a d i a n t temperature of t h e burning b u i l d i n g s .
B.
C a l c u l a t i o n of Radiant Temperature from Radiometer Output The normal r a d i a t i o n i n t e n s i t y from a b l a c k body a t T o Kelvin i e&
-
I n
-
'r
Langley/min S t e r a d i a nwhere 4.
=
81.3
xlom1*
The r a d i a t i o n i n u i d e n t on the thermopile when t h e radiometer f i e l d of view i s completely f i l l e d by' a r a d i a t o r a t
To
Kelvin i s In times t h e s o l i d a n g l e of t h e f i e l d of view,Thus
i n c i d e n t r a d i a t i o n
=
W e ?
.a
0-A
Langle y/minand t h e r a d i a t i o n e m i t t e d by t h e radiometer w i t h i n t h i s same s o l i d angle i s
M r . Bernard ~ r u l 6 , Xssaarch Technician w i t h B u i l d i n g S e r v i c e s S e c t i o n was l a r g e l y r e s p o n s i b l e f o r t h e o p e r a t i o n of t h e i n s t r u m e n t a t i o n
i n
t h e f dt'lr:i and provided v a l u e d a s s i s t a n c e .GROUND FLOOR = PORCH ROOF - J PORCH RAILING ,/ NOTES :
1. ALL WALLS a CEILINGS OF PLASTER
1 INSTRUMENTATION IN BASEMENT WEST CORNER 12
n
lzi CLOSED BEDROOM LEGEND : --4 JHERMOCOUPL ESA
b
& RESISTANCE THERMOMETER
0
RADIOMETERS / 0 ' - 2 "x 8 '-3 " El OPEN BEDROOM 8 ' - 0 / / '- 5 " @ THERMOP/L E RADIOMETER \ L7 GAS COLLECTORS " 'b DOWN A SMOKE METERSb l
0 BEDROOM BEDROOM 10'-2"x 10'-6" 8 ' . 0 ' ' ~ 1 0 ' . ~ ' ' A N E M O M E T E R 0-
5 10=
1 F E E TSASH REMOVED BEFORE F/RE
NOTES:
I . ALL WALLS 8 CEILINGS OF FIBREBOARD EXCEPT
- IN BEDROOMS, WALLS 8 CEILINGS OF PLASTER
- IN KI TCHEN
.
WAINSCOT OF WOO02 INSTRUMENTATION WEST CORNER LEGEND - a THERMOCOUPLES RESISTANCE THERMOMETER
0
RADIOMETERS @ THERMOPILE RADIOMETER n GAS COLLECTORS C\ SMOKE METERS---COVERED WITH
/
PLASTERBOARD GROUND FLOOR . . I5'0"L
. 3 0 S P _ , : I NOTES :I ALL WALLS a CEILINGS OF FIBREBOA RD
L-
2 6 ' - 0 " FIRST FLOOR I i l 2. IN BASEMENT WEST CORNER .f
LEGEND : 4 THERMOCOUPLES-
-% RESISTANCE THERMOMETER KITCHEN B DINING ROOM 18'-2"x 9'10" 5 2 . LIVING ROOM .*---
t--4
i0
RADIOMETERS @ THERMOPILE RADIOMETER 9 ' - l / ' x 18'-2" GAS COLLECTORS 10 O - A F E E T 6 -UP CRIBFIGURE 3
-
BUILDING No. 3-
TWO-
STOREY SOLID BRICK DWELLING\ COVERED WfTH PLASTERBOARD DINING ROOM 1 4 ' - 1 0 " r 1 5 ' - 5 " SASH
I I
REMOVED GROUND FLOOR NOTES :I. ALL WALLS 8 CEILINGS OF PLASTER 2 INSTRUMEN TATION IN BASEMENT SOUTH CORNER LEGEND: --o THERMOCOUPL ES
RESISTANCE THERMOhtE TER
0
RADIOMETERS@ THERMOPILE RAOIOME TER GAS COLL ECTORS
a
SMOKE METERSF E E T
FIGURE 4
-
BUILDING NO. 4-
TWO-
STOREY WOOD FRAME DWELLING WITH CLAPBOARD EXTERIOR AND BRICK INFILLING! - DOOP L EFT QPEh
\
NOTES :
-- --
J
FIRST FLOOR
I. ALL WALLS 8 CEILINGS OF PRESSED PAPERBOARD 2. INSTRUMEN PA TION IN BASEMENT LEGEND : 4 r m o c o u P L ~ s
-% RESISTANCE PHERMOME TER
0
RADIOMETERS@ THERMOPILE RADIOME PER
GAS COLLECTORS SMOKE METERS
O I p
F E E T
FIGURE 5 -BUILDING No. 5 - T W O
-
S T O R E Y WOOD F R A M E DWELLING W I T H> _i
IllU
4
+I->
" U~ '..4
STAGE (3'- 6" ABOVE FLOOR)I'I
-
6
:
NOTE : CEILING a WALLS OF-a.-.
.*
. 1- 1 1 1 STEEL POSTS1
WAINSCOT PLASTER WOOD LEGEND: 4 THERMOCOUPLES RESISTANCE THERMOMETERS ANEMOMETERS0
RADIOMETERS@
THERMOPIL E RADIOMETER GROUND FLOOR 0-
5 10 FEETFIGURE 6
-
BUILDING NO. 6-
T W O-
S T O R E Y SOLID BRICKGROUND FLOOR
I
N O T E S :
/. ALL WALLS B CEILiNGS
OF PL AS r m
2. INS TRUMEN TA TION
IN BASEMENT SOUTH CORNER LEGEND :
-
THERMOCOUPLES % RESISTANCE THERMOMETER0
RADIOMETERS8
THERMOPILE RADIOMETER GAS COLLECTORS SMOKE METERS -F E E T F I R S T F L O O RNOTE :
-
WALLS OF PLASTER CEILING OF WOOD LEGEND : --o THERMOCOUPLES& RESISTANCE THERMOMETERS ANEMOMETERS
0
RADIOMETERS THERMOPILE RADIOMETER GROUND FLOOR 0-
5 10 F E E TFIGURE 8
-
BUILDING
NO. 8
-
TWO
-
STOREY SOLID
BRICK
B L D G . No. 4 B L D G . No. 7
FIGLIRE 9 RECORDER CHARTS FOR BURNS OF HOUSES WITH INCOMBUSTIBLE LININGS
BLDG. No. 3 815 1 :I. 8 4 8 S 4 6
1 . 1
BJF 8 4 0 8 1 9 800, B e 1 8 6 6 ~r 871 1 B 7 P 1 B O B 1 808 7.e B L D G . No. 2F I G U R E 10 RECORDER C H A R T S FOR BURNS O F HOUSES W I T H C O M B U S T I B L E L I N I N G S
COMMUNITY HALL AULTSVILLE
FIGURE I!
BLDG. No. 5
RECORDER C H A R T S FOR BURNS No. 5 , 6 ,
8
A P P E N D I X A
CHECK ON R A D I OhEiTER C A L I B R A T I O N A T LONG VJAVELENGTHS
The r a d i o m e t e r was s i g h t e d i n t o a c o n i c a l b l a c k body which was m a i n t a i n e d a t 100°C by condensing steam a t atmospherio p r e s s u r e , A, Data f o r s m a l l a p e r t u r e : - T
=
373'
K e l v i n C a l c u l a t i o n :B.
Data f o r s t a n d a r d a p e r t u r e : C a l c u l a t i o n :125
x
0.092 mv=
B1.3 x
0.01158 = 12,22 Langle y/minThe good agreement between t h e v a l u e s of K found f o r the s m a l l and t h e s t a n d a r d a p e r t u r e s i s c o n f i r m a t i o n of t h e a c c u r a a y of the s o l i d angle r a t i o .