Second virial coefficient of from - NIST · 2011. 7. 18. · JOURNAL OF RESEARCH of the Notional Bu...

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JOURNAL OF RESEARCH of the Notional Bu reau of Standa rds - A. Ph ysics and Chemistry Vol. 72A, No. 2, March- April 1968 Second Virial Coefficient of He 4 in the Temperature Range from 2 to 20 oK Marjorie E, Boyd, Sigurd y, larsen, and Harmon Plumb Institute for Basic Standards, National Bureau of Standards, Washington, D. C. 20234 ( December 7, 1967) We p reliminary values for Ihe seco nd viria l coeffic ient of He' in the te mp eratu re range from 2 to 20 K. 1 h ey wele de rI ved from rece nt so und ve lOC It y meas ur e m e nt s in Ih e gas made by Plumb a nd Cata la nd uSIn g a n ultra sonIc Int erfe rometer. Key Word s: He', low te mp era tur e, seco nd viri a l. In thi s c ommuni ca ti on we pr ese nt valu es for the seco nd vi rial coe ffi cient of He 4 in the tempe ratur e ran ge from 2 to 20 oK. Th ey were derived from rece nt so und velocit y measurements in the gas mad e by Plumb a nd Ca taland using an ultr aso ni c interferom- eter [1] .1 Our valu es for the virials must be consid- ered as prelimin ary s in ce the me thod for determining them from so und velocity data pl aces such stringent de mand s on th e numerical accuracy of the l atter that it.will be n ecessa ry to ac c umul ate a much larger body of dat a than is now ava il ab le to ac hi eve more exact virials. H owever, th e pr oblem of discre pan ci es existing betw ee n various provisional te mp e ratur e scales below 20 oK is c urr e ntly of strong int er es t [2] and contrib- utes a note of ur gency to the probl em of obtai nin g new meas ured values of th e second virial coe ffi cient in thi s t e mp e ratur e ran ge. C urr e ntl y, th e o nl y va lu es ava il a bl e are obtained e ith er by extrapolating upw ard from th e PVT data of Keller [3] in the 2 to 4 oK region, by relying on a very few point s obtained by Keeso m and Walstra [4] mor e than twe nt y years ago, or by us in g th eo re ti c al calculations ba sed on ass umed inter- mol ecu l ar potential function s. We thus be li eve that o ur values, although th ey mu st be r ega rd ed as te nt a- tiv e, are probably the b es t now available and may therefore prove useful as guid es to ward resulvin <f th e inte rn a ti onal temperature · scale difficulties. meas ur ements of sou nd velocity isotherms wh ic h should enable more accurate and re li ab le valu es to be determined are now in progr ess in this laboratory. Isothe rm s of the spee d of so und as a function of pr ess ur e were obtained [1 1 at pressures low e noua h that the isoth er ms could be re pr ese nt ed by a rel at ionship, W' 1=C( l +a p) , where W is th e so und 1 Figures in . br ac kets indicate the lit eratu re referen ces at the end of this I}aper. 155 veloc it y. C RT/M , a nd Ca is the s lor e of th e iso- th e rm o Th e coefficient a is related to the seco nd virial coefficient B by [51 the e quation a(T) = (RT) - I [2B TB ' TlB"] 3 15 where th e pnmes denote differe ntiation with respect to T, the te mp e ratur e. To o btain the seco nd virial from the a 's it is thu s necessa ry to ass ume a fu nctional form for B(T) with coefficients to be det erm ined, differe ntiat e it twice, and det erm ine the cons tant s by leas t squares fittin g of the data for a(T). This approxi- mation of B by an arb itr ar il y chose n ex press ion intro- du ces a stro ng un ce rtainty in th e r es ults in ad dition to the un certainti es involved in dete rminin g the a's from the isoth er ms. Many exper im e ntali sts hav e u se d th e form B = a + bi T , and recent experience of two of th e authors (MEB and SYL) [6J in fittin g results of an accurate phase-shift ca lculation of B fo r He 4 , using a Lennard-Jon es potential with deBoer param eters, indi- ca t es th at this is a r easo nabl e form in the t empera tur'e range of this d ata. H owever, c urvatur e as a fun ction of liT does b eco me in cr eas in gly a pp are nt for the L-J vi rials at about 20 OK, as well as at the low T end. Using, then, B = a. + bi T we find th e res ults shown in t ab le 1. An id ea of the accuracy ma y be o bt a in e d by both observing the c hanges in th e res ults when fittin g to different te mp e rature ranges se parat ely and by noting th e effec t of addin g additional terms in th e functional form for B. Of th ese two t ypes of changes the first is th e l east se rious in its e ff ec ts on th e re sults. Co mparin g the virials obtained when fittin g th e mi ddl e te mp e ratur e range to those obtain ed fittin g the high and low ranges separately we find them to differ by

Transcript of Second virial coefficient of from - NIST · 2011. 7. 18. · JOURNAL OF RESEARCH of the Notional Bu...

Page 1: Second virial coefficient of from - NIST · 2011. 7. 18. · JOURNAL OF RESEARCH of the Notional Bu reau of Standards - A. Physics and Chemistry Vol. 72A, No. 2, March-April 1968

JOURNAL OF RESEARCH of the Notional Bu reau of Standa rds - A. Physics and Chemistry

Vol. 72A, No. 2, March- April 1968

Second Virial Coefficient of He4 in the Temperature Range

from 2 to 20 oK

Marjorie E, Boyd, Sigurd y, larsen, and Harmon Plumb

Institute for Basic Standards, National Bureau of Standards, Washington, D.C. 20234

(December 7, 1967)

We pre~e nt p re limin a ry values for Ihe second viria l coeffic ie nt of He' in the te mpe ra tu re range from 2 to 20 K. 1 hey wel e derI ved fro m rece nt sound ve lOC Ity meas ure me nt s in Ihe gas made by Plumb a nd Catala nd uSIng a n ultrasonIc Int erfe ro meter.

Key Words: He', low te mperature , second viri a l.

In thi s communi cati on we prese nt valu es for the second vi rial coe ffi cie nt of He4 in the te mpe rature range from 2 to 20 oK. They we re derived from rece nt so und velocity measurements in the gas made by Plumb a nd Catala nd using an ultraso ni c inte rfe rom ­eter [1] .1 Our values for the virial s mu s t be co ns id ­ered as pre limin ary s in ce the method for de te rminin g th e m from so und velocity data places such stringent de mands on th e num e rical accuracy of the latter that it.will be necessary to acc umula te a mu ch larger body of data than is now ava il able to achi eve more exact virials.

However, the problem of disc repan c ies ex isting be twee n various provis ional te mperature scales be low 20 oK is curre ntly of stron g inte res t [2] and contr ib­utes a note of urge ncy to the proble m of obtai nin g new meas ured values of the second virial coe ffi c ient in thi s t emperature range. C urre ntl y, th e onl y va lu es ava il able are obtained either by ex tra pola ting upward from th e PVT data of Kelle r [3] in the 2 to 4 oK region, by relying on a very few points obtained by Keeso m and Walstra [4] more than twenty years ago, or by us in g theore ti c al calculation s based on ass um ed inter­molecu lar potential function s. We thus beli eve that our values, although they must be regarded as te nta­tive, are probably the bes t now available a nd may therefore prove useful as guides toward r esulvin <f the intern a tional temperature · scale difficulti es. Fu~th er meas ure ments of sound velocity iso therm s wh ich should e nable more accurate a nd re li ab le values to be de te rmined are now in progress in thi s labor atory.

Iso th erms of the s peed of sound as a function of pressure were obtained [1 1 at pressures low e nouah th a t th e isotherms could be re presented by a lin e~r relations hip , W'1=C( l +ap) , where W is the sound

1 Figures in . brackets indicate the lit erature refe rences at the end of thi s I}aper.

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veloc it y. C = ~ RT/M , a nd Ca is the slore of th e iso­

th e rm o Th e coefficie nt a is re lated to the second virial coefficient B by [51 the equation

a(T) = (RT) - I [2B +± TB ' +± TlB"] 3 15

where th e pnmes de note d iffere ntiation with respect to T, the te mperature. To obtain the seco nd virial from the a 's it is thus necessary to ass ume a fu nctio nal form for B(T) with coefficie nts to be de term ine d , differentiate it twice , and de termine the co nstants by leas t squares fittin g of the data for a(T). This approxi­mation of B by an arbitrarily chose n expression intro­du ces a strong uncertainty in the res ults in addition to the un certainties involved in de te rmining the a's from th e isotherms.

Many experim e ntali s t s hav e u se d th e form B = a + bi T, and recent experience of two of the authors (MEB and SYL) [6J in fittin g results of an accurate phase-shift calculation of B fo r He4 , using a Le nn ard-Jones potential with deBoer parameters, indi ­cates that this is a reasonable form in the temperatur'e range of thi s data. However, c urvature as a fun ction of l i T does beco me in c reas ingly a pparent for the L-J vi rial s a t abo ut 20 OK, as well as at th e low T end.

Usin g, then, B = a. + biT we find th e res ults show n in tab le 1. An idea of the accuracy may be obta ine d by both observing the changes in the res ults when fittin g to diffe re nt temperature ranges separately and by noting the effect of addin g additional terms in the functional form for B. Of these two types of cha nges the first is the least se rious in its e ffec ts on the res ults. Co mparing the virials obtained when fittin g the middle te mperature range to those obtained fittin g the high and low ranges separately we find them to differ by

Page 2: Second virial coefficient of from - NIST · 2011. 7. 18. · JOURNAL OF RESEARCH of the Notional Bu reau of Standards - A. Physics and Chemistry Vol. 72A, No. 2, March-April 1968

TABLE 1. Second virial coefficient of He4 from 2 to 20 oK

Range fitted Derived formula for B

2-10 oK (21.28 ± 0.46) - (449.2±3.2)/T

(19 .6± 1.1) - (422 ± 17) /T -(69±42)

T' (24.4±2.3) - (459.9 ± 8.3) /T - (0 .18±0.13)T

11-20 oK (17.00± 0.20) - (379.1 ± 5.0)/T

(14.30±0.71) - (246±34) /T (1223 ± 314)

T' (22.6 ± 1.3) - (446 ± 25)/T- (O. lll ± 0.026) T

4-16 oK (19.43±0.24) - (430.3±3.1)/T

(17.60±0.39) - (378± ll) /T- (23~ ±47)

(23.40±0.73) - (455.1 ±4.8)/T- (0.131 ± 0.024)T

amounts varying from about 7 cm3/mol at 2 oK down to about 0.1 at 20 oK.

Introduction of another term in the expression for B, can , depending on the particular form , lead to dras­tically differing results, even though the standard deviations (0" a) for the fitting of 0' are similar. This is illustrated in table 1. Thus it would appear that the fitting of more complicated expressions for B than the simple 2-constant function used here cannot be jus­tified unless either more extensive data are available or a strong theoretical justification of a particular functional form for B(T) can be made.

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B calculated from derived formula (cm3 /mol) era

2°K 4 °K 10 oK 16 oK 20 oK

1.30 -203.3 -91.0 -23.64 .. ... ... .. .... . .. " ... . .. ....

1.19 -209. -90.0 -23.3 ... ... . ...... .. ..... ..... . .. .

1.23 -205.9 -91.3 -23.4 ....... ...... . . . .......... .. .

0.25 -20.91 -6.69 -1.96 ..... . ... . .... .. .. ... .. . ...

.15 .. ... . .. .. .. .. .. .. ... ...... -22.5 -5.8 - 1.1

.15 . . . . . . . . . . . . . . ... . .. . . . .... -23.1 -7.1 -1.9

.73 -195.8 . -88.2 -23.60 -7.46 -2.08

.42 -230. -91.6 -22.6 -6.9 -1.9

.39 -204.5 -90.9 -23.42 -7.14 -1.98

References [11 H. Plumb and G. Cataland, Metrologia 2, 127 (1966). [2] Meeting of Advisory Committee on Thermometry to Interna·

tional Committee on Weights and Measures, Gaithersburg, Md. , and Ottawa, Canada, Sept. 6-14, 1967.

[3J W. E. Keller, Phys. Rev. 97, 1 (1955). [4] W. H. Keesom and W. K. Walstra, Physica 13, 225 (1947). '­[51 A. Van Itterbeek and W. H. Keesom, Commun. Kamerlingh

Onnes. Lab., Leiden No. 216c; Proc. Koninkl. Ned. Akad. Wetenschap. 34, 988 (1931).

[6] S. Y. Larsen, M. E. Boyd and J. E. Kilpatrick, to be published.

(Paper 72A2-491)