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An Apparatus for Investigation of the Distribution of Movement with Depth in Shallow Soil Layers

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Publisher’s version / Version de l'éditeur: Building Research Note, 39, p. 10, 1962-10-01

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An Apparatus for Investigation of the Distribution of Movement with

Depth in Shallow Soil Layers

Williams, P. J.

https://publications-cnrc.canada.ca/fra/droits

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AN APPARATUS FOR INVESTIGATION

OF T m

DISTRIBUTION

OF

MOVEMENT WITH DEPTH

IN

SHALLOW SOIL LAYERS

by

P

.

J

.

W i l l i a m s

T h i s note describes the construction and operation

of

an

instrument for measuring soil movements

in

a

layer extending from the

ground surface to

a

depth of 2 t o 3 m. It w a s designed for investigation of the d o w n alope movements (solUluction), e s sentially due to frost action that frequently occur in Arctic and sub-Arctic areas.

Recent publications discuss observations on the occurrence and nature of these movements

(1,2,3),

and certain considerations relevant

to experhental investigations of this type (4). PREPARATION

OF

APPARATUS

Portable battery-operated resistance bridge, (e,g, Tinsley, modified type

4907x1.

Polyethylene tubing

-

5/8 in. *i.

d.,

3/4 in. *om

d.

For each probe

One spring steel strip, 15 cm. x

1.2

cm., shaped a = shown

in

Fig. 1,

Approx.

0.035 in,* thickness.

Two single strand, straight wire, resistance strain gauges ( e . g . Baldwin S , R ,

-

4, Type A-12-2,

R e sistance

-

61

ohms approximately), Contact cement.

2 to 3 rn. four-conductor [gauge 22) cable, f l e s b l e . 4 spade lugs,

4 Dimensions are given in inches when theae are commonly used in c o m e r cial de scription.

(4)

G l a e s tube - 15 or 16 mm. i. d.

Polyethylene tubing

-

1/4 in. i , d.

*,

318 in. o. d.

*

Pr o ~ o r t ions

Epoxy Compound:

Components Obtainable from

F i e l d Preparations

H y s o l (Canada) Ltd.

,

P.

0.

Box

53,

Stn.

R,

Toronto 1 7 , Ontario. Thiokol Liquid Polymer 3 Nagaltuck Chemical Co..

Elrnira, O n t a r i o .

Activator DMP 30 ( R o b and Haas)

A length o f the polyethylene tubing (518 in. i. d, ) i s inserted in the ground, The lower end i e heat sealed before ineertion and the upper end closed with a rubber stopper. During insertion the tube is held straight by inserting a wooden rod.

Construction

of

Probe (Fig. la)

The probe is used to measure curvatures of the tube. W h e n

i n s e r t e d into the tube the prabe takes up the s a m e curvature, Strains

e e t up in the metal strip are measured by the strain gauges, and provide a measure

of

thie curvature ( s e e a180 (41).

Electrical resistance strain gauges operate on the p r i n c i p l e

that the change in resistance of a w i r e on undergoing strain is approximately

proportional to the strain. A s in the prabe, two gauges are commonly u s e d in most applications, t h e i r resistance usually being measured in a form of wheatstone b r i d g e circuit ( F i g . lb). B y using two gauges e r r o r s due to

temperature change a r e avoided. W i t h the two gauges as arranged in the probe,

the reading8 obtained represent mice the strain in the strip. In practice

i t is not usually necessary to c o n s i d e r the curvature/strain/resistance

relationship, since the probe is calibrated d i r e c t l y f o r curvature in t e r m s of bridge reading. The Tinsley bridge mentioned above is moderately priced

and in combination with the S R 4 gauges specified has proved satisfactory.

M o s t commercially produced battery-operated bridges for s t r a i n gauge

*

D i m e n s i o n s a r e given in inches w h e n these are commonly used in

(5)

reading would probably be satisfactory. It is necessary that the bridge range be appropriate f o r tke resistance changes developed in the gauges used, for a l l likely. curvatures of the probe.

A pair of gauges must be selected, which, when connected acrose the bridge terminals, permit a zero reading. (In the case of the Tinsley B r i d g e , modified 4?07X, there w i l l be a slight difference in resi5- tance between the t w o gaziges.) Tke gauges are carefully mounted one on

each s i d e of the cleaned s t r i p with the contact cement, The leads are s o l d e r e d ta the canduetor cable, Sleeving covers the junction and the bared conductor.

It is important that t b e s l e e v i l g is loose and does not g r i p the l e a d wire. The

two ends of the sleeving are closed w i t h a small dab of Vaseline. Tape is

w o m d around the narrower part af the strip and the conductor cables.

The polyethylene tubing ( 114 in, i. d. ) is passed over the con- ductor cable,

and

pressed ever the narrower part of the strip. It is con-

stricted if necessary by a w i r e binding.

The glaas t u b i ~ g is placed vertically in a clamp, The strip

is placed in the tube with its ehd caught in a small groove previously c o t

diametrically in a cork, closing the lower end of the glaes tube. The atrip is 3eld vertical by a split cork which holds the polyethylene tubing aboz~t 1 c m beyond its junction with the metal strip. Before finally placing

the

split ,

cork in position the epoxy-polymer-accelerator mix is poured in to f i l l the

g l a s s tube. After it h a s set, the glass is shattered and completely removed. T p e probe may be sanded smooth and to exact size; i t must not be excessively

strained, and ca3 be carried in a protective tube. Marks a r e made at inter- vals of 3 , 7 5 c m on the polyethylene tubing ( 114 in. i . d. ) and n u m b e r e d con-

secutively. "1" is coincident with the top

of

the probe. A s t r a i g h t line

(!'guide line") i a marked down the length of the tubing.

CALIBRATTOV

O F

PROBE

(1) A 1- to 2-m length of polyethylene tubing is fixed f i r m l y ,

without k i n k i ~ g but with two or more curves. At least 10 crn at one end

s.clo::ld be straight. A Sine continu.ous w i t h this part of the tube, serves

as the X axis, f o r the determination of y ordinates f o r points down the t u b e . It is helpful i f the tube is so arranged that i t does not cross the

X

axis. It car be very satisfactorily held izl a bed of plaster of par is, which

prevents movement or d i s tortian.

( 2 ) b-itervals of 1 5 cm are marked on the tube and t\e y ordinales

(6)

( 3 ) A table is prepared ( F i g . 3) to give the angles

#

;

# 2 ;

0

e t c . corresponding to the curvature at each point down the tube ( F i g . 2).

In compiling the table the following steps are taken (care should be taken t o

follow the arrangement illustrated by the example in Fig, 5 ) ;

the tube.

c) Divide by

A

(corresponding to length of probe

=

1 5 ) to obtain

8

sin +8 ; gin

+

; sin

+

e t c ,

0 8 1 92; . .

.

d) Read angle

+.

; + 8 2 ; e t c . from table^.

e ) The required angles

+

0 ;

+l;

+2; etc. are obtained from

+ S O

4

-

baa:

0a2

-

+B1; e t c *

(4) The shunt on the bridge is s e t so that the galvanometez needle is centred? with "per cent resistance change" reading 0. Readings

a r e obtained with the probe for intervals of one probe length ( 1 5 c m ) down

the tube, i. e . at each marked point.

( 5 ) F o u r probe readings at each point are made as follows:

Two series of readings progressing down the tube and two p r o g r e s ~ i n g up

the tube, taking c a s e to maintain similar orientation of the probe guide l i n e .

The 'averages f o r the readings for each point are calculated. It is e s s e n t i a l that the midpoint of the probe coincides with the points marked on the tube.

t

The average probe reading at each point is then plotted against t h e corres-

ponding angle

9

in the table ( F i g . 3 ) .

( 6 ) Individual points deviate considerably f r o m the straight-

l i n e relationship a s s u m e d to exist between angle

+

and the probe reading.

A m u c h larger n u m b e r of points can be obtained by repeating procedures

2 t e 5, for additional s e t s of paints marked (and values of y) on the same

tube.

*

This procedure prepares t h e T i n s l c y b r i d g e , such that the readizlg

obtained for the s t r h i g h t position of the probe in question w i l l be 0. Other t y p e s of b r i d g e may require a slightly d i f f e r e n t p r o c e d u r e to achieve this.

(7)

PROCEDURE FOR OBSERVATIONS

IN

FIELD

*( 1) S e t s h u n t s o that galvanometer needle is centred, with "per cent resistance change" reading 0 .

( 2 ) Place probe in top of tube and record orientation of guide line. Then determine ( b y gentle bending), and

record

whethex probe w i l l read eve for convex upslope, or convex downslope, curvature of tube.

(3) R e c o r d readings : read probe at consecutive positions down tube, at intervals equal t o one quarter of probe length (use markings

on lead cable). Position

No. 1

is that position where upper end of probe l a level with top of tube. Take care that the guide line rernaine roughly

oriented in the same way as the probe is moved down the tube,

For tubes apparently curved, take four s e t s

of

readings ( F i g . 4): take a s e t of readings proceeding down the tube and a s e t as the probe is being withdrawn; then remove the p,robe completely, turn through

18O0, and take two further s e t s of readings. These should have, in general, opposite sign to that of the f i r e t t w o s e t s .

(43 Measure amount of tube exposed above ground surface.

It occasionally happens that in pas sing through a straight past

of

the tube at some depth the probe rotates through 1806. This is detected as the probe moves into a more curved part of the tube, by the sign of the readings differing from that expected from other determinations on the same tube. This difficulty can be overcome by guiding the lead cable very care- fully as the probe is pushed into the tube.

P R O C E D U R E F O R INTERPRETATION

OF

READINGS W H E R E

CURVATURE

O F

TU8E LS

OBSERVED ( F I G S . 4,5,6)

(1) The s i g m of the second pair of readings f o r each probe

position (under 'after rotation through 180") are reversed 2nd the algebraic a v e r a g e of the four r e a d i n g s is calculated.

>:: This procedure prepares tile T i n s l e y b r i d g e , scch t h a t the reading

o b t a i n e d f o r the straight position of the probe in question w i l l be 0. O t h e r

(8)

(2) Separate the list of average readings into four column^

as follows: starting with the deepest reading and proceeding upwards l i s t every fourth one ( e . g . l o t h , 6th, 2nd), thus making the first column

Then begin with t h e penultimate reading and proceed as before. Make third

and four th columns similarly (Fig.

5).

( 3 ) U s i n g the form of table shown (Fig. 61, compute x and y

coordinates as indicated, f o r the f i r s t column of figures,

In

the preparing of the table values for

9

a r e read from the calibration graph for the probe ueed. +s f o r any probe position is obtained by summing the values of t$ f o r all probe

p s s i t i ~ n s down to and including that probe position. x and y are obtained

i n

a

similar way by summing the values of cos

+,L

and sin

@,L

respectively. Preparation of this table can be regarded as the reveree of the process used in calibration ( F i g s . 2 and 3 ) .

(4) A second table is prepared f o r the second column of figures which is treated similarly, except that to the first angle

+,

is added

.

2 5 times

the first angle

+

obtained in the previous table (para. 3 above). Also to the f i r s t value

of

x i s added

.

25 times the probe length.

(5) The t h i r d and fourth columns are computed similarly, except that factors of

.

5 and . 7 5 respectively, are used, instead of - 2 5 .

The values of x and y from all four calculations are plotted on one graph, The third point f r o m the top represents the top of

the

tube. The

orientation of the curvature i n relation to the slope {i. e . convex or concave downslope) is given by the observation described on page 5 , paragraph (2). R E F E R E N C E S

1) W i l l i a m s , P.

J.

Some investigations into certain solifluction and patterned ground features in Norway. Geogr, Jour, V o l . CXXIII,

Pt.

I , M a r c h 1957.

2). 'Williams, P. 5. An investigation into processes occurring in solifluction.

Am. Jour

.

Sci. , Val. 257,

No.

7 , 1959, p. 481-490.

33 Vfilliarns, P.

S.

Quantitative investigations of soil movement in frozen

ground phenomena. B u l l , P e r i g l . (In P r e s s ) .

4) IVilliams,

P.

J. The direct recording of soliflucticrn movements. Am.

(9)

S T R A I N SENSITIVE W l R E OF S T R A I N GAUGE

3

5 -10 CM SPRING STEEL EPOXY COMPOUNO W l R E G R A D U A T E D C U T - A W A Y VIEW POLYETHYLENE CABLE CONTA1NING LEAD WIRES 0

-

GMS I0 SCALE

FIGURE

t

o

PROBE FOR

DETERMINATION

OF SHAPE

OF

BURIED

TUBE

LEGEND

s

= S H U N T

(ro

PERMIT INITIAL

ZERO READ/NG)

0 = VARIABLE RESISTANCE CALIBRATED FOR

" % STRAIN CHANGE"

G

= S T R A I N GAUGE

F I G U R E

I

b

GENERAL FORM

OF WHEATSTONE BRIDGE CIRCUIT ( A S USED IN T I N S L E Y M O D l F l E O 4 9 0 7 1 )

(10)

FIGURE

2

DIAGRAM

ILLUSTRATING

COMPUTATIONS

FOR

DETERMINING CURVATURE OF

GAL1

BRATION

TUBE

(11)

Figaxe 3

-

Determination of

+

for calibration tube

...

Probe

No.

...

-

Date

G

Points marked on cali- bration tube, 15 c m intervals 0 1 2 3

Shunt reading

...

Length

of

tube exposed above ground

...,...

c~~

reading convex upslope

...

...

downs lope

Y

0 0 . O ? 1. 51 5 . 9 6

Figure 4

-

Field readings

*Y

0,

O n 14' 4 " 51' 15" 10' Sin

+

8 2nd s e t

P r o b e position After Rotation through 180 a

.

3 I

Q

+

0"

14" $: 4" 37! + l o P 191 1 s t s e t 1st: s e t

0.07

1.44 t 4 . 4 5 ;' , 2nd e e t Column 4 . a 0 4 1 . 0 8 4 7 -2617 1

Figure 5

-

Computation of field observatione ( s t e p 1 )

Column 2 Colwnn 3

,

Probe position Average (fram

4 s e t s )

(12)

Figure

Figure  4  -  Field  readings

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