effect of hydrostatic pressure upon the relaxation of ... · preted as the effect of hydrostatic...

6
JOURNAL OF RE SEARCH of the National Bureau of Standa rds-A. Physics and Chemistry Vol. 65A, No. 4, July-August 1961 Effect of Hydrostatic Pressure Upon the Relaxation of Birefringence in Amorphous Solids Roy M. Waxler and Leason H. Adams ( March 28, 1961) A s tud y was made of the e ff ect of hy dr ostat ic press ur e up on the relaxat ion of bire- fringence in two commercial plast ics which were glasslike in na ture. The birefringence was introduc ed in to t he materials by loading in uniaxi al compres sion, and the d ecay of b irefrin- ge nce with ti me was meas ur ed using a pola rimeter. The rate at which the optical p ath- difference di sapp eared was great ly inhibit ed by the hydro stat ic pressur e, a nd a press ur e of 10,000 bars was fo und to be sufficie nt to sto p t he re lease comp lete ly. The results are int er- prete d as t h e e ff ect of h ydrostat ic press ur e upon the mobility of the mate rials. Some experi- men ts ,,-ere co ndu cted to d ete rmine the eff ect of te mp e ra t ur e up on the relaxatio n, th at t he eff ects of press ur e and tempe rat ur e might be co mp ared. 1. Introduction When an amorphous solid is subjected to a uni - axial str ess, i t be comes bir efringent, and the s ub se- qu ent de cay of this birefringence is associa ted with a rel axation of the str ess. This ph enomenon is attrib- uted to fl ow in the m aterial. Th e relaxation of internal stress in glass as a function of tempera t ur e was investiga ted some years ago by Adams and Williamson [1] 1 in their work on annealin g. In ves- tigations by Lillie [2] and Isard and Douglas [3] give evidence that in the annealing of sili cate glasses, th e release is accomplished essen tially by viscous flow. Regardl ess of the mechanism by which the stress is released, the influence of hydro static pr essur e upon this mobility is of general int erest in solid state physics. Th e hy drostati c pressure of itself do es not introdu ce any double refra ction into the material , as will be shown. 2. Measurement of Optical Path-Difference In m eas Ul'in g opti cal pa th-difference it is custom- ary to use a B abinet compens ator or a g raduat ed quartz wedg e, which instrum ents afford a sen sitivit y of about ± 5 mIL. A pol arim eter developed by Goran- son and Adams [4] affords a sensiti vity of ± 0.0 5mlL, and th e measur e ments may be made easily. 2 Plan e- polarized light is rotated through an angle equal to one-half the phase lag produ ced by double refraction in the specimen by this inst nun ent. Since the meas- ur ement s were of angul ar displa cement , it was found to be conveni ent and ad equ ate to express th e optical path-difference as phase lag in the sp ecimen in degrees, this valu e being twice the measured valu e of the rotation . Th e inst rum ent is equipped with a graduat ed quartz wedge used in determining th e multi - pIes of 36 0 0 when the phase lag in the sp ecimen ex - ceeds one whole wavelength . A high pr ess ur e mercury arc lamp was lI sed with optical fil ters to isol ate the green lin e of 5461A. 1 J' igul' CS in brackets indicate tile litorature referenccs at tile end of this paper. 2 1:11 e authors are indebted to the GeophYSical Laboratory of the Caruegie In- stitute of Washington for the Joan of this instrument . 3. Pressure Apparatus Th e app arat us and techniques for hydro st ati c pr essur es hav e been descnb ed 111 d etail by Weir [5]. Briefly, a heavy-walled pressur e vessel has a smooth bore which contains a light petroleum di stillate. By means of a hydraulic pre ss, a leak- proof pist on is forced into the bor e of the vessel thereb y compressing the liquid and gen erating hydro static pressure. The apparatus is designed for pressur es up to 10 ,000 bars, and the press ur e is m easUl'ed internally b y mean s of a m angan in pressur e gage to a pr ecision of bar . 4. Choi ce of Material and Method of Intr oducing Optical Path Differ ence It was convenient to select a glass such as glu cose, or poly bu tyl metha crylate, that would ann eal around room temperature. It was planned to intro du ce doubl e refraction into a specimen by plunging it into a bath at low te mp eratur e, and then to observe the rel axation at room temperature. Some poly- bu tyl me thacr yl ate was polymerized and molded into block s. The dimensions of these blocks were redu ced to nf X 71'6 X % in. to permi t them to enter the bore of the pressur e vessel. The amount of double refra ction introdu ced into one of these small specimens by quenching varied markedly so that was impossible to find an area with sufficient um- formi ty to allow a good measurement. Considering the difficulti es with temperature- induced photoelastic eff ects, a m et hod was so ught that would introduce in to a specimen a uniform bir efringence that would decay with time. It has been found in early work on pboto elastic str ess analysis [6] that when a transparent 121astic l oaded and the load held constant over a period of t Ull e, the optical path difference caused by the s tr ess does not remain constant but inc reases with t ime. Likewise, when the load is removed, the optical pa th difference do es not go to zero immediately bu t decays gradually. Th ese effe cts are shown very roughl y for allyl 283

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Page 1: Effect of hydrostatic pressure upon the relaxation of ... · preted as the effect of hydrostatic pressure upon the mobility of the materials. ... for each test, ... 6. Calculation

JOURNAL OF RESEARCH of the National Bureau of Standards-A. Physics and Chemistry Vol. 65A, No. 4, July-August 196 1

Effect of Hydrostatic Pressure Upon the Relaxation of Birefringence in Amorphous Solids

Roy M. Waxler and Leason H. Adams

(March 28, 1961)

A study was made of the e ffect of hydrostatic pressure upon t he re laxation of bire­fringence in two co mmercia l plastics whi ch were g lasslike in nat ure. The birefrin gence was introduced in to t he materials by loading in uniaxial compression , a nd the decay of birefrin­gence with time was measured usin g a polarimeter. The rate at whi ch t he opt ica l path­difference disappeared was greatly inhibited by t he hydrostatic pressure, and a press ure of 10,000 ba rs was found to be sufficient to stop t he release completely . The resul ts are inter­preted as t h e effect of hydrostat ic pressure upon t he mobility of the materials. Some experi­ments ,,-ere co ndu cted to determ ine t he effect of temperat ure upon the relaxation, that t he effects of pressure a nd tempe rature migh t be co mpared.

1. Introduction

When an amorphous solid is subj ected to a uni­axial stress, i t becomes birefringent, and the subse­quent decay of this birefringence is associa ted with a relaxation of the str ess. This phenomenon is attrib­u ted to flow in the m aterial. The relaxation of internal stress in glass as a function of tempera ture was investigated some years ago by Adams and Williamson [1] 1 in their work on annealing. Inves­tigations by Lillie [2] and I sard and Douglas [3] give evidence that in the annealing of silicate glasses, the release is accomplished essen tially by viscous flow. R egardless of the mechanism by which the stress is released, the influence of hydrostatic pressure upon this mobility is of general interest in solid state physics. The hydrostatic pressure of itself does not introduce any double refraction into the material , as will be shown.

2 . Measurement of Optical Path-Difference

In m easUl'ing optical path-difference it is custom­ary to use a Babinet compensator or a graduated quartz wedge, which instruments afford a sensitivity of about ± 5 mIL. A polarimeter developed by Goran­son and Adams [4] affords a sensitivity of ± 0.05mlL, and the measurements may be made easily. 2 Plane­polarized light is rotated through an angle equal to one-half the phase lag produced by double refraction in th e specimen by this instnunent. Since the meas­urements were of angular displacement, it was found to be convenient and adequate to express the optical path-difference as phase lag in the specimen in degrees, this value being twice the measured value of the rotation. The instrument is equipped with a graduated quartz wedge u sed in determining the multi­pIes of 3600 when t he phase lag in the specimen ex­ceeds one whole wavelength. A high pressure mercury arc lamp was lIsed with optical fil ters to isolate the green line of 5461A.

1 J' igul'CS in brackets indicate tile litorature referenccs at tile end of this paper. 2 1:11e authors are indebted to the GeophYSical Laboratory of the Caruegie In­

stitute of Washington for the Joan of this instrument .

3 . Pressure Apparatus

The apparatus and techniques for o?tain~ng hig~ hydrostatic pressures have been descnbed 111 detail by Weir [5]. Briefly, a heavy-walled pressure vessel has a smooth bore which contains a light petroleum distillate. By means of a hydraulic press, a leak­proof piston is forced into the bore of the vessel thereby compressing t he liquid and generating hydrostatic pressure. The apparatus is designed for pressures up to 10 ,000 bars, and the pressure is measUl'ed internally by means of a manganin pressure gage to a precision of ±}~ bar.

4. Choice of Material and Method of Introducing Optical Path Difference

It was convenient to select a glass such as glucose, or polybutyl methacrylate, that would anneal around room temperature. It was planned to introdu ce double refraction into a specimen by plunging it into a bath at low temperature, and then to observe the relaxation at room temperature. Some poly­butyl methacrylate was polymerized and molded in to blocks. The dimensions of these blocks were reduced to nf X 71'6 X % in. to permi t them to enter the bore of the pressure vessel. The amount of double refraction introduced into one of these small specimens by quenching varied markedly so that ~t was impossible to find an area with sufficient um­formi ty to allow a good measurement.

Considering the difficulties with temperature­induced photoelastic effects, a method was sought that would introduce in to a specimen a uniform birefringence that would decay with time. It has been found in early work on pbotoelastic stress analysis [6] that when a transparent 121astic i~ loaded and the load held constant over a period of tUll e, the optical path difference caused by the stress does not remain constant but increases with time. Likewise, when the load is removed , the optical path difference does not go to zero immediately but decays gradually. These effects are shown very roughly for allyl

283

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16

14

7 t Rm UNDER LOAD

.< 12 '

~ IO

! '" 6

o I I I 1 I

RECOVERY

o 200 400 600 600 1000 1200 1400 1600 1800 2000 2200 2400 TIME ,min

FIGU RE 1. Biref1'ingence in a specimen of allyl diglycol carbo­nale when loaded to 350 kg jcm2 for 960 minutes and then unloaded.

diglycol carbonate in figure 1, where a specimen in the form of a block 1 % X Yt6 X % in. was loaded length­wise in uniaAial compression. Allyl diglycol carbonate is widely used in stress analysis, having a stress­optical coefficient of 26.5 brewsters, where 1 brew­ster= 10- 13 (cm)2/dyne. It is available in large clear sheets that give excellent transmission of light in the visible region.

A small loading mechanism which has been de­scribed previously [7] was employed to insure a uniform and uniaxial compression of the specimen. This device was modified for the present work, so that instead of using suspended weights, the load was applied by means of a testing machine. A specimen of allyl diglycol carbonate with the same dimensions as used previously was loaded to 350 kg/cm2, and the platens of the testing machine were then held in this fixed spatial position for a period of 16 hr. Upon removing the residual load, measure­ment of the specimen in the polarimeter showed that there was a phase lag of about 720°, or two wave­lengths of the 5461 A line. This residual phase lag reduced to about 20 percent of its original value in the course of a day, and when a plot was made of the phase lag in the specimen versus time, the points fell on a smooth curve.

Change in birefringence under load was also observed in commercial polymethyl methacrylate. Like allyl diglycol carbonate, this material is avail­able in large, clear sheets, and affords excellent transmission in the visible region of the spectrum. However, polymethyl methacrylate has a much smaller stress-optical coefficient (about 3.75 brew­sters). A specimen of this plastic, with the same dimensions as used previously, was loaded in uniaxial compression to 700 kg/cm2, and the platens of the testing machine were then held in this fixed spatial position for a period of 16 hr. Upon removal of the residual load, the specimen exhibited a residual phase lag corresponding to three-quarters of a wavelength of mercury green light, and this lag gradually reduced to about 20 percent of its original value in the course of a day.

For both allyl diglycol carbonate and polymethyl methacrylate, X-ray diffraction patterns obtained from a Geiger counter diffractometer showed the presence of broad peaks typical of amorphous materials .

A piece of allyl diglycol carbonate which showed no evidence of double refraction when examined in polarized light was placed in the pressure bomb and subjected to a pressure of 10,000 bars for a period of 10 min. The pressure was then released, and the specimen, upon removal from the bomb, still showed no sign of double refraction after temperature equilib­rium had been established. The result of this ex­periment was taken as verification of the statement in the introduction that hydrostatic pressure of itself does not introduce any double refraction into an amorphous solid.

Since the relaxation curve for allyl diglycol car­bonate was not closely reproducible for specimens treated in the same way, it was decided to load a specimen double the usual length, one half to be placed in the pressure bomb at elevated pressure, and the other half to be used as a reference specimen at atmospheric pressure. Upon removal from the loading apparatus, examination in polarized light showed that the optical path-difference in each half was the same.

5 . Experimental Procedure

The above approach was followed in an experiment where the pressure bomb was raised to 10,000 bars, this pressure being selected because a large effect was sought. Making allowances for the time spent in raising and lowering the pressure in the bomb, the results of the experiment indicated that there was no relaxation of the specimen at all during the time it was under the pressure of 10,000 bars. This initial experiment was followed by similar ones using pres­sures of 2,100 bars, 1,000 bars, and 500 bars, and it could be seen, qualitatively, that the relaxation pro­ceeded at a greater rate at each succeedingly lower pressure.

To ascertain that this inhibiting of the relaxation was not unique for allyl diglycol carbonate, two ex­periments of a similar nature were conducted with polymethyl methacrylate at pressures of 2,000 bars and 1,000 bars. It was necessary to enclose a poly­methyl methacrylate specimen in a polyethylene bag in order to protect it from attack by the petroleum fraction used in the pressure bomb. The results of the experiments agreed qualitatively with earlier results, that the relaxation proceeded at a greater rate at lower pressure. Since the relaxation curves for polymethyl methacrylate had been found to be reproducible at atmospheric pressure, it was not necessary to have an individual reference specimen for each test, as with allyl diglycol carbonate.

All these experiments on both plastics were con­ducted at a temperature of 24 °e.

6. Calculation of Relative Mobilities

In studying the relaxation of each amorphous solid,

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an empirical relationship between the variables was sought for greater convenience in handling the data. It was found that the data could be fitted very well to the equation

d</>= _A</>1 dt

(1)

where </> represents the phase lag in a specimen , t represents the time, and A is a constant for a given temperature and pressure. Integrating equation (1) one obtains

1 1 </>3- </>~=3At, (2)

</>0 being the initial phase lag in the specimen. It can be seen that by plotting the reciprocal cubed of phase lag versus time that a straight line results. Further­more, knowing the t ime and amount of phase lag in the specimen when it was put into the pressure bomb, and the time and amount of phase lag when it was removed, it was possible to infer the rate of the relaxation under pressure. This is shown in figure 2 for allyl diglycol carbonate subj ected to a pressure of 1,000 bars.

It was asswned that the constant, 3A, was a measure of the tendency to flow in the material, or of its mobility in the most general sense. The ratio of the slopes of the two straight lin es shown in figure 2 was taken as an expression of the mobility at elevated pressure relative to the mobility at atmos­pheric pressure ; i.e., the relative mobility was taken as ApjAo where 3Ao and 3Ap are respectively the slopes at atmospheric pressure and at elevated pres­sure. The data for each experimen t were treated in this manner, and relative mobilities were calculated in each case.

7 . A New Experimental Method

There were several objections to making measure­ments in the foregoing manner: (1) Only a rough estimate could be made of the time that a specimen was affected by the pressure, because 10 min would elapse in bringing the bomb up to pressure, and

. IZXlO- '

.10

~ :5 .06

if .06 :3

~ .O~

.01

I BAR

1000 BIRS I BAR

O ~~-L~~~~-L~~~-L~~~~-L~~~ o " ~ ~ ~ ~ ~ m m ~ • ~ m

IIME. min

about th.e same time would elapse in releasing the pressure; (2) it was known that there was a tempera­ture rise due to adiabatic compression, and a lowering of temperature due to adiabatic expansion; (3) one could see that the fourth power relationship for the relaxation (eq 1) held at atmospheric pressure, but there was no assurance that the same law applied while a specimen was under pressure.

These considerations made it desirable to ob erve the relaxation while a specimen was under pressure. Fortunately, for this purpose, it was possible to utilize a pressure vessel equipped with glass windows 3

[8]. The windows were supported by hardened stainless steel plugs, the contacting faces being ground optically flat. The combination of window and supporting steel plug made a Bridgman seal [9} according to a design proposed by Poulter [10} . The vessel was capable of supporting pressures up to 1,500 bars, and had been built 'with a surrounding oil bath for temperature control.

In .order to observe relaxation under pressure, the polarllneter of Goranson and Adams was disas­sembled and remounted on a large optical bench. The pressure vessel was placed at such a position in the optical train that it enclosed tbe specimen. As a safety measure against possible failure of the win­dow, a total reflection prism was placed in the optical train immediately after the specimen , so that the light beam was turned through 90 0 • The light beam then passed through the quarter-wave plate and analyzer which were placed at right angles to the rest of the optical train (fig. 3) . With this arrangement, the reflection of the polarized light had no effect upon the measurement of phase lag in the specimen beyond changing the zero point in taking readings.

Photoelastic effects caused by hydrostatic pressure were observed in the glass windows of the vessel, and these effects increased in magnitude with in­creasing pressure. A black cross typical of a radial distribution of stress appeared when the windows were examined between crossed polaroids with white light. With the aid of a sensitive red tint plate,

• This pressure vessel was kindly loaned b y Dr. R. E. Gibson, D irector of tbe Appli~d Physics Laboratory of the Jobns Hopkins University .

ME RCUIIY ARCl AM1'

Oil BATH

~COLLIMATING GREEN LENS FI LTER . , PRE SSURE

_. . -8 --[S3--IT_._.-: 0 ___ ..!I!~B~ TO TALREfLECIiON POLARIZER D- SPECIMEN ~ PRISM

,.;., OUAR TER - WAVE T PL ATE ,

~ AN AlYZER

, 17' EYE

FIGURE 2. The reciprocal cubed of phase lag in allyl diglyeol carbonate as a function of time, showing the effect of a hydro-static pressure of 1,000 bars in comparison with that of 1 bar, FIGURE 3. Arrangement of optical system to measure optical the plot at 1,000 bars being inferred. path-difference.

285

_____ .J'

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it was estimated that at a pressure of 1,000 bars, the optical path-difference varied from zero at the center of the aperture to about 50 m,« at the edge. This maximum was reduced to about 25 m,u by plac­ing a diaphragm at the wi.nd~w. Using the pol~r­imeter with monochromatIc hght produced an In­tegrated effect of this variation so th~t it was slightly more difficult to make a photometnc match at tho higher pressures.

The pressure in the bomb was measured by means of a calibrated Bourdon gage to the nearest 7 bars. A mercury contact thermoregulator held the tem­perature in the oil bath surrounding the bomb to within ± 0.02 00.

:Measurements were then made of relaxation while a specimen was under hydrostatic pressur.e, and the results of a typical experiment are shown 111 figure 4. The specimen was first. allowed to .relax at atmos­pheric pressure for a penod o~ 120 m111, and then ~he hydrostatic pressure was applIed and held for a penod of 240 min.

The reciprocal cubed of phase lag was plotted ao-ainst time in minutes and it can be seen from figure 4 b that the fourth power relationship for relaxation (1) really holds at el~vated.prcssure. The irreg~­larities in the points ImmedIately ~fter char:ges ~n pressure are attributable to assocIated, a.dlabatlC temperature changes. The slope of the straIgl.l tIme which represents the parameter, 3Ap , was found , therefore from direct measurements rather than by determining the slope by i.nfere!1ce, as had bee ,~ done before a pressure bomb wIth wmdows was avall~ble. The parameter, 3AQ, was found f.rom t~e slope oj the straight line in the first , l~O-mIn penod, when the specimen was at atmosphenc pressure, and t he rela­ti ve mo bili ty was calcula ted .

Experiments at 24 °0 were conducted on allyl dio-Iycol carbonate at pressures of 162, 430, and 869 ba~·s . Relative mobilities were calculated and these data were combined with data obtained by the old method of estimating the relaxation under pressure (see fig. 2). The relative mobilities versus pressure at 24 °0 are shown in figure 5 for both allyl diglycol carbonate and polymethyl methacrylate.

.031 X 10-'

.018

.014 -

~ .010 -

~

;:: .016 ~

.011 I BAR -

.008

.0 04

1.0 "-o

0.9

0.8

• AllYL OIGLYCOl CARBON ATE o POLY- METHYL METHICRYlITE

0.7

o

). 0.6

>

~ 0.4

0.1

O~~~~~~~~ o u _ ~ 4~ ~ ~ ~ _ _ 1=

PRESSURE. BARS

FIGURE 5. Relative mobility as afunction of pressure at 24°C.

8 . Effect of Temperature

In order to gain some conception of the relative effects of temperature and pressure upon the re­laxation of allyl diglycol carbonate, additional ex­periments were conducted at 20 °0 and 30 . °0. The observations were made, as nearly as pOSSIble, at pressures of 200, 500, and1 ,QOO bars,a fres hly ?ut specimen being used each tIme. When r~lative mobilities were calculated from the data, It was found that a straight line represented the relat.ion­ship l / (relative mobility) versus pressure at a gIven temperature, and this is shown in figure 6. The data for all the relative mobilities resulting from change in pressure are given in table 1.

30 'C

80 J 110 160 100 140 180 310 360 400 440 480 0 =--I~OO-...J.l;-O - 3;'-0 -4~00-...J.50-0 - 6'-00- 7:"-:00- --'80-:-0 --::9:-:-00 ---:1=000:--::110::-0 --::"100

TIME, min 0 PRESSURE . BARS FIGURE 4. Th e reciprocal cubed of phase lag in allyl digl ycol

carbonate as a function o.f time, showing the effect of a hydro­static pressw'e o.f 430 bars in comparison with that o.f 1 bar.

FIGURE 6. ( Relative mobility) - l in allyl diglycol carbonate as a .function o.f pressure at 3 temperatw·es .

286

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T ABLE 1. Dependence of Telative mobility upon preSSUTe at constant temperature

Tempera- Pressure Relative Material ture bars mobility

A.IAo ----

°0

{ 1 LOOO

Allyl diglycol carbonate ___________ _______ 20 223 0.357

397 . 198 941 .115

1 LO(\() 162 0.427 4311 .193

24 500 .203 869 . 107

l,OM .0746 2,100 .0364

la, 000 0.0

{ 1 1. 000

30 204 0.405 601 .145 853 . 117

{ I LOoo Polymethyl meth.cry!"te _________________ 24 1, 000 0.230

2, 000 . 0403

One experiment was conducted a L atmospheric pressure t o determine Lbe value or 3 A [or the sam e specimen or allyl diglycol carbonate at 20, 24, and 30 °e. Usil1g the slope or the straight line at 20 °e as a basis, r elative mobilities were determined , and they appeared to vary exponel1tially with tempera­ture accord ing to the equation

1.1 -

1.0

0.9 -

~ 0.8

) ~ 0.7

::::; ~ 0.6 -

~ 0.5 -

'" x 10.4

0.3 -

0.1

0.1 -

11 14 16 18 TEMPEArURE, 'C

30 31 34 36

A o Log -A = 0.1068-2_120

20 (3) F lGURE 7. E.O·ect of tem pemt1lre upon the relative mobility of

allyl diglycol cm'bonate at atmospheric preSSUl'e.

where Ao is the mobility at t he given temperature, 0, and A 20 is the mobility at 20 °e. This r elation­ship is shown in figure 7, a nd the data are shown in table 2.

9 . Discussion

As can be scen in figure 5, the flow in amorphoLls solids is very ensitive to the effect o[ hydrostatic pressure and even the comparatively low pressure of 162 bars is sufficient to reduce the rela tive mobility or allyl diglycol carbonate to less than haH its valuc at atmospheric pressure. The effec t becomes less pronounced at higher pressures , bnt a pressure or 10 ,000 bars is sufficient to inhibit the flow completely. The effect in polymethyl methacrylate is comparable, but not as great as in allyl diglycol carbonate.

At pressures below 1,000 bars a linear relationship appears to hold for l / (relative mobility) versus pres­sure for allyl diglycol carbonate as shown in figure 6. At higher pressures the r elationship ceases to be linear and, as tbe pressure increases, l / (relative mobility) increases rapidly. Since the slopes of the straight lines in figure 6 are nearly the same, it appears that the pressure dependence of l / (relative mobility) is not affected by temperature, at least not ovcr the range of pressure and temperature inves ti­gated.

If this variable, l / (relative mobility), or relative resistance to flow is considered, it is interesting to compare the results of the present investigation with

T ABLE 2. Dependence of l'elative mobility tlpOn temperature at atmospheric pressure

Pressure Tempera- R elative Logarithm of rflative

Material bars tUre mobility mobility A,IA,. Log A ,/A,.

°0

{ ?O 1.0 0.0 ldlyl diglycol carbonate ______ 1 24 2.56 . 409

30 11. 49 1.060

t hose of Bridgman [9] in his work on the viscosity of liquids under pressure. Bridgman poin ts out th a t t he viscosity of a liquid increases with pressure at a rapidly increasing rate. H e also shows that the r elative change of viscosity with temperature be comes markedly greater a t high pressure, wh ereas most temperatme effects become less a t high pres­sures. Bridgman comments on the large magniLude or the pressure effect, and the large variation from liquid to liquid, and these observations apply gen­erally to all the liquids studied , although wa LeI' is somewhat abnormal in its b ehavior, and shows th e effect of association at low temperatmes and pres­sures.

From Bridgman's tabulated data it can be secn that oleic acid showed an increase of fomfold in relative viscosity upon increasing the pressure from

287

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1 bar to 1,000 bars at 30 °C. Allyl diglycol car­bonate showed a ninefold increase in relative resist­ance to flow for the same pressure change at the same temperature. Of all the liquids investigated by Bridgman, oleic acid showed the greatest pressure dependence of relative viscosity for pressures up to 1,000 bars . Eugenol showed the greatest pressure dependence up to 12,000 bars, and Bridgman calcu­lated that this increase of pressure at 30 °C would increase the relative viscosity by 107 . Although measurements were made at a slightly lower tem­perature (24 °C), the relative resistance to flow of allyl diglycol carbonate became infinitely great at 10,000 bars.

The authors thank Charles E. Weir of the National Bureau of Standards for his advice and material assistance in conducting the experiments . Tho authors also thank the members of the Bureau's Structural Engineering Section for their cooperation and the use of their equipment.

(Paper 65A4- 112)

10 . References

[1) L . H . Adams and E . D. Williamson, The annealing of glass, J. Franklin Inst. 190, 597, 835 (1920).

[2) H . R. Lillie, St ress release in glass a phenomenon in­volving viscosity as a variable with time, J . Am. Ceram. Soc. 19,45 (1936).

[3] J. O. Isard and R. W. Douglas, The relaxa tion of stress in fused silica. P art 1. Experimental. , J . Soc. Glass T ech. 39, 61 T . (1955) . Part II. Theoret ical. , J . Soc. Glass T ech. 39, 83 T . (1955).

[4) R. W. Goranson and L. H . Ada ms, A method for the precise measurement of optical path-difference espe­cially in stressed glass, J. Franklin lnst . 216, 475 (1933).

[5) Charles E. Weir, High-pressure appara tus for compres­sibility studies and its application t o measurements on leather and collagen, J . Research NBS 45, 6 (1950) RP 2160.

[6) E . G. Coker and L. N. G . FiloD, A treat ise on photo­elasticity, pp. 263, 267, 275 (Univ. Press, Cambridge, 1931) .

[7) Roy M. Waxler and Albert Napolitano, Relative stress­optical coefficients of some National Bureau of Stand­ards optical glasses, J. Research NBS 59, 2 (1957) RP 2779.

[8) R. E. Gibson, The compressions of certain salts in water, glycol and methanol, J . Am. Chern. Soc. 59, 1521 (1937) .

[9) P. W. Bridgman, The physics of high pressure, pp. 32, 330 (G. Bell and Sons, Ltd. , London, 1931) .

[10) T . C. Poulter, Apparatus for optical studies a t high pressure, Phys. Rev. 40, 860 (1932).

288