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Technical Note (National Research Council of Canada. Division of Building Research), 1958-06-01
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Eden, W. J.
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r1.t1
NATIONAL RESEARCH COUNCIL OF CANADAセᆪLNM
DIVISION OF BUILDING RESEARCH'fE
C
1HIN ][ CAlL
NOT FOR PUBLICATION
NOTJE
No.
252
FOR INTERNAL USE
PREPARED BY VI.J. Eden CHECKED BY CBC APPROVED BY NBH
PREPARED FOR Mza. C.P. Harford, City Englneer,
Prinoe George, B.C. June
1958
SUBJECT Soil Tempezaature Installation at Prinoe George, B.C.
SUN:rf.t.ARY•
This report desoribes the instrumentntion supplied to the City of Prince George to measure solI temperatures around water mains. The
installation was made in November
1957
under the direotion or イセN C.P. lrnrford, City Engineer. Instzauctions are given for carrying out and reoording the observations.SOIL T8?tPD:HA'1'fTHE iNnセセtNA|llG|tion AT PRINCE GEORGE, B.e.
by
"N.J. Eden
To ョsLGjZエセエ in the study of problems w:i.th frozen water
nervlce in Prince George, B.C., セ・ Division of Building
Rosearch agreed to supply the neoessary ゥョウエイオキセョエ。エゥッョ to
ᄋセ。ウオイ・ soil temperatures In Prince George. This roport
describes sn installation @sde in the fall of
1957
underthe direction of
7r.
C.P. Barford, City eョセゥョ・・イN Instruotionsar Biven for making end recording the observations.
For the City of Prince George. the reoorda \ul1 be
used to determine the thermal recime of the soil surrounding
「ャセゥ・、 water servioes. For the Division, records will be
obtained for t 1e セ・ョ・イ。ャ study of soil temperatures as
reI ted to ッャャイセエゥ」 oonditions.
The thermooouple oircuit was prefabricated in the
Division's laboratories in Ottawa and shipped to Prince George
for installation in Hovembezt 1957. A potentiometer beoame
available 1n January
1958
and was shipped to Prince George sothat tomperatuI'o records began at that date. The Installation
The site chosen for the installation was one of エLセ
ウセイNァ・ウエ・、 by the City of Prinoe George. It is lenown as the
"Central Station" located on h。イー・セ Street on Lot
8, BLK55,
nC937.
The installation consisted of tl1rea strines ofthermo-couples, on over the water main, one at tho cnntre of a
Anow-cleared streot and the third in ,round were a normal
snow fall セSs allowed to sect nulate. T e soil oonditions were
unlforl:1, oonsisting of sandy gravel, grading from 2 in. SiZ8
to flne sand. Figure 1 is a site plan of the installation
prep red from informs'l;ion received 'rom the city.
Strine No.1 was lonated 12 ft from the 11strmTIent hut
provided by too city undor a snow-covered surface. It oonsisted
of
6
thermooouples pIa oed at depths of 1, 2.3, 5.
7 and セo ft.'11 e second s·tring t"/SS s1 tua ted under the centre of J,Jarper
streov. The ウエiGセョァ had 10 thermocouples at the follOWing depths:
2
-over the water main, had 10 thermooouplos at 2, .3,
h,
5, 6,
7, 8,
9
and 10 ft plus 1 thermooouple used to measure thetornpero ture near the wator ma in. rl!he thermooouples were
tapod to a 2- by 2-in. wooden post to maintain the correot spaoing.
The instrument hut was an
8-
by 8-ft wooden ウィ・ャエ・セand provision was made for heating the hut when readings
V:Tero belng taken.
lJ.'he Clrouit
Figure 2 is a cirouit 、ゥ。エセ。ュ for the Prince George
installation Which consisted of several elemonts. There
were three thernooouple strings aaoh terminating in a
jlJnotion box sealed \'7i th a bi tu:minous sealing oompound. From
the junction box a oopper lead wire from each thermocouple
エッイセゥョ。エ・、 in the rotary switoh. One constantan load, 」ッセュョ
to all the thermooouples in the string, エ・イyセNョ。エ。、 in tho
reference junction. The copper member of the referenoe junction
was lod through the switch to the potentiometer.
The エィ・セョッ」ッオーャ・ウ were made of 20-gauGe
copper-oonstantan duplex wire; each member was covered by polyvinyl
chloride, and the two leads were enoased in cotton impregnated
with asphalt. Qセ・ thermocouple points were proteoted by
plastic tubing and were dipped in glyptol enamel. The duplex
TIire terminated in a metal junotion box in whioh the .oopper membors were connected to 20-gauge pvo-covered copper lead
wire. The constantan members met at a cornmon po5.nt and viera
led to the referenoe junction by a single 20-gauge constantan oonduotor.
The refer'enoe junction consisted of a therm.ocouple
immersed In a thermos flask filled with crushed ice and VIa ter to m."l:Lntain a temperature of .32°F.
'J.'he switch \'laS a 28-point rotary type )·iian.ufactnred by
Lewis Engineering Corporation. It is the セAー・ often used by
tho Division in thermocouple circuits. Table I lists the
owi toh point numbers corresponding to the various ther:'l1oooupleo.
Before being shipped.f. the oj.rouit assem'bly was c}10clwd
and found to be accurato to "loP. The potentiometer キセウ a
Rubicon portable model reading in mill! vol ts; ins't;ructions for
its ャjァLセ r{ere inoluded when the instrument was delivered. One
prccautlon should be taken wlth tLls instrument - it must NOll'
- 3
-TABLE I
セカャゥ tah point Thermooouple string Depth below Remarks
No. No. surfaoe
li't. 1 1 1 2 1 2
セ
1 3 Under snow 15
coverセ
17
1 107
2 1 8 2 2 9 2a
Under oentre 10 2 line of 11 2l
street 12 2il
27
2 8ゥセ
29
2 1017
3
2 183
a
19
:3 203
セ
Over water 213
main 223
7
セ。
;;
8:3
9セV
,
103
On6
in water main at7-ft
depthffhe oircuit diagram in Fig. 2 indicates the oorrAot
v!iring for obtaining temperatures above
32°F.
['or readings below the freezing point it is necessary to interchanGe theIe ads to the potentiometer. Reading the Potentiometer, iI
To obtain readings, the potentiometer should bo placed
on a solId level base. It: should be switohed on at loast
5
minutos be foro any readings are taken. When 。、NQオウエゥョ{セ the
:i.nstrumcnt tho f:irst step is to centre the galvanmnetor. Course adjustment is made by turn:1.nc; the galvanometer knob.r:.tne
ad,ju.stment is made by slid:I.ng the etohed glass plate nntil the
-4-The next step is to balance the instrument. against the standard cell. This is dono by turning the resistanoe knobs Rl and R2 as direoted in the manufaoturer's instructions. The balance of the instrwnent ahould be checked frequently while the
readings are being made.
The emf's of the th armoo ouple9 are de termlned by
pressing on the emf button. This button Should not be depressed oontinuously otherwise Q slight error is introduoed.
The millivolt readings obtained are converted to temperatures by using thq conversion table appended to this
report. .
Troatment of Records
It has been found that seasonal variations in soil temperatures extend to e depth of about 20 ft. Daily
variations extend to a depth of about 2 1/2 ft. To assess the magnitude of seasonal wave, temperatures need only be takon at intervals of 2 weeks or 1 month. The daily wave, it it is to be studied in detail, requires frequent readings. To overoome the daily variations it is suggested that readings be taken at the same time of day at eaoh interval.
Prom エセBャゥウ installation. the Division requires sufficient reoords to draw up a graph showing the monthly variations of
temperature vl1th depth. An example of this type of graph 18 ウィッセセ in Fig. 6 of "Ground Temperature Illvestigations in Canada" by d.B. Crawford and R.F. Legget .. Engineering jッセョ。ャL Vol. ャセッ
No.3,
Naroh1957
セ (Research Paper No.33
of the Division ofBuilding Re3aarohJ. To onllect infor@Stlon on the goneral problem of frozen water mains, additional records suoh as the water エ・ュー・イ。エエセ・ウL rates of flow and the depth of frost
enoountered in winter exoavation would be helpful. It is believed that the meteorologioal records obtained from Prince George Airport by the d・セ。イエュ・ョエ of Transport will be adequate for c orrela tion purposes. The fOI'"'AJ' supplied by Mr. G.W. Jonea
of the Engineering Dapartment, City of Prinoe George, if oompleted, will supply very acceptable infornmtion for the Division's records.
APPEnDIX 101
• - il11111"01
t Conver 1 TenD. of セGBカ Temp .. of r.cv _ r . . . セ-
セ10
-.4tR
セァ
KNPVセN11
-.L!.
!+.
o
r,c:
< cIセ12
MNセRS37
+.107
iR
- .1..\.02
-.3
81
38
+.129セV
+.15°
11
-.360
+.172
1)
-.340
41
+.193
17
-.319
42
+.21[)18
-.298
tta
+.2i
8
19
••27
6
+.200
20
-.25
J'g
+.2a1
21
MNRセセ
+.3°3
22
-.2
セヲイセ
+.32
5
セセ
-.193
KNSセMW-.171
49
+.3 9
セセ
-.15°
50
+·ili
O-.128
51....
2
27....107
52
KNセMSアN28
•• 08ft§a
+.11.57
29
-.06
セ+.479
30-.043
セァ
+.5°0
)1 -.021+.r)23
3
2-.000
57
KNUセU
セセ
+.02258
+.5
7
+.043
g6
+.589
+.612
GROUND SURFACE
セOセL
SWITCH-#17 2' 3' ,.. -19 4' 20 5' SWITCH #26 21 6'_ /
22 7 23' 8' ,,/セ 24 9' 6" WATER 25 10" MAIN STRING NO. 3--
3' t 4' L E A D - I Y 10 II s' CABLE 12 6' /3 7' 14 S' 15 9' 16 10' STR I NG NO. 2 6 10' STRING NO. I 4 5' 5 7' DEPTH OF THERMOCOUPLEセセ
jQ_O|GMセセセセ
SWITCH#, I' SWITCH#7 I' 2 2' 2' 3PROFILES OF THERMOCOUPLE STRINGS
HARPER
ST LEAD IN CABLE 6" ASBESTOS CEMENT WATER MAIN N -t-66' I f-o. - - - - MMMMNNZNNNNNNZNNNNMMMMMMセNi I III
I I ST RING NO. 3J
Ii W I セャ STRING N O . 2 : : , .JihセtヲMMMZMMMMMMB[Mセ」イMMセZZ
セMM -- __ MMセ IIセZ
a:: APPROX./:1
0..1
TRAVELLED III
PORTION. II I GRAVEL SURFACE II
I I6
I
ST R I NG NO. I Iw iセ ...JI .
ll. o a:: Q.SITE PLAN
SCALE /": 20'-0" (CITY OWNED) 'LOT 8 BLK 55 OL 937FIGURE
SOIL TEMPERATURE
MEASUREMENT AT
CENTRAL STATION
e
e
j 1 0 - 1 POTENT I.DMETER , 1 0 + Ie
セ STRING NO. ILJ
SELECTOR SWI TCHセ
セMMMMMMMMMMMゥェセMセセセセセ]]]]]]セ]]]セLMMMMMMMMMMML
I IU
t-セ
i '
i
I,
:
'I
I
I
J
REFERENCE JUNCTIONi :',
!
'II
' - - - / : I
I
: '
I
r - - - _ - - - - , ;
'I
!
III
LEGEND I
I
セi
COPPER LEAD WIRE
!
I
セ
CONSTANTAN WIRE
FIGURE
2
STRING NO.2