Literature DB >> 28053436

ITS-90 Density of Water Formulation for Volumetric Standards Calibration.

Frank E Jones1, Georgia L Harris2.   

Abstract

A new formulation of the density of air-saturated water as a function of temperature on the 1990 International Temperature Scale (ITS-90) is presented. Also, a new equation for calculating isothermal compressibility as a function of temperature on ITS-90 was developed. The equations are to be used to calculate the density of water, in the temperature range 5 to 40 °C on ITS-90, used in the gravimetric determination of the volume of volumetric standards.

Entities:  

Keywords:  ITS-90; air-saturated water; calibration; density of water; isothermal compressibility; volumetric standards

Year:  1992        PMID: 28053436      PMCID: PMC4909168          DOI: 10.6028/jres.097.013

Source DB:  PubMed          Journal:  J Res Natl Inst Stand Technol        ISSN: 1044-677X


1. Introduction

In the gravimetric determination of the volume (calibration) of volumetric standards, water is used as the calibrating fluid. The volume is calculated from the mass and density of the water. In many quarters, the formulation of Wagenbreth and Blanke [1] is used to calculate the density of water. In this paper, a new formulation of the density of water (based primarily on the work of Kell [2]) as a function of temperature on the 1990 International Temperature Scale is presented.

2. Kelt’s Formulations

2.1 Density of Water

In 1975, Kell [2] published a new formulation for the density of air-free water at a pressure of 101.325 kPa (1 atmosphere) valid from 0 to 150 °C “that is in improved agreement with most data sets.” The Kell formulation is where t is temperature in °C on the 1968 International Practical Temperature Scale (IPTS-68).

2.2 Isothermal Compressibility

Kell also developed equations for calculation of the isothermal compressibility, κ, of air-free water [2]. In the temperature range 0 to 100 °C on IPTS-68, the equation can be expressed as where κ is isothermal compressibility in (kPa)−1.

3. New Formulations

3.1 Density of Air-Free Water

In the present work, the Kell calculated values of ρ were fitted over the temperature range 5 to 40 °C on the new 1990 International Temperature Scale (ITS-90) [3] to an equation quartic in temperature. The equation is In contrast with the Kell equation, a term in t is not necessary due at least in part to the fact that the 0 to 4 °C region, in which ρ increases with increasing temperature, has been excluded. Equation (3) applies to air-free water. Values of the density of air-free water were calculated for temperatures (ITS-90, t90) between 4.999 and 39.990 °C using Eq. (3) and compared with corresponding Kell values. The estimate of the standard deviation (SD) of the difference was 0.00034 kg m−3. The ratio of SD to the mean value of density was 3.4 × 10−7, which is negligible.

3.2 Conversion of IPTS-68 to ITS-90

A very simple equation relating ITS-90 temperature, t90 to IPTS-68 temperature, t68, has been used in the present work to generate values of t90 for the development of Eq. (3). The equation for the temperature range 0 to 40 °C is In the temperature range 0 to 100 °C the equation is

3.3 Change in Density of Water with Air Saturation

Bignell [4] measured the change in the density of water with air saturation for 80 points in the range of 4 to 20 °C. He fitted the points to develop the equation where Δρ is in kg m−3. There is no need to adjust for temperature scale. Bignell concluded that “there is probably not much need to extend the work to higher temperatures because the effect diminishes and the accuracy of density metrology at these temperatures would not warrant a more accurately known correction.”

3.4 Density of Air-Saturated Water on ITS-90

Equation (5) was added to Eq. (3) to produce an equation to be used to calculate the density, ρas, of air-saturated water in the temperature range 5 to 40 °C on ITS-90: The uncertainty in the density of air-saturated water for an uncertainty in temperature of 1 °C is approximately 210 ppm or 0.21 kg m−3 at 20 °C.

3.5 Isothermal Compressibility

The thermal compressibility data used by Kell have been fitted against temperature on ITS-90 for the temperature range 5 to 40 °C. The resulting equation is where κ is thermal compressibility in (kPa)−1. The estimate of standard deviation (SD) of the residual, calculated κ–data κ, is 2.1 × l0−11 (kPa)−1; the ratio of SD to the midrange value of κ is 4.6 × l0−5, which is negligible for present purposes. It is not necessary to make a correction to κ for air saturation. The value of the isothermal compressibility of water is approximately 46.5 parts per million (ppm)/atmosphere at 20 °C. At locations where the atmospheric pressure is significantly different from 1 atmosphere (101.325 kPa), a correction for compressibility calculated using Eq. (7) should be made. For example, at Boulder, CO, the correction for compressibility is approximately −8 ppm at 20 °C.

3.6 Compressibility-Corrected Water Density Equation

The expression for the density of air-saturated water, ρasc, at an ambient pressure of P kPa is where ρas is calculated using Eq. (6) and κ is calculated using Eq. (7).

4. Tables

Table 1 is a tabulation of values of the density of air-saturated water using Eq. (6). Table 2 is a tabulation of the values of the density of air-free water calculated using Eq. (3). Table 3 is a tabulation of values of air-free water calculated using the formulation of Wagenbreth and Blanke [1], this table has been included in this paper for purposes of comparison.
Table 1

Density of air-saturated water (g/cm3)from Eq. (6) using Kell [2] data

t(°C)0.00.10.20.30.40.50.60.70.80.9
  50.9999610.9999590.9999570.9999550.9999530.9999500.9999480.9999450.9999420.999939
  60.9999360.9999330.9999300.9999260.9999220.9999190.9999150.9999110.9999060.999902
  70.9998970.9998930.9998880.9998830.9998780.9998720.9998670.9998610.9998560.999850
  80.9998440.9998380.9998320.9998250.9998190.9998120.9998050.9997980.9997910.999784
  90.9997770.9997690.9997610.9997540.9997460.9997380.9997300.9997210.9997130.999704
100.9996950.9996870.9996780.9996690.9996590.9996500.9996400.9996310.9996210.999611
110.9996010.9995910.9995810.9995700.9995600.9995490.9995380.9995270.9995160.999505
120.9994940.9994820.9994710.9994590.9994470.9994350.9994230.9994110.9993980.999386
130.9993730.9993610.9993480.9993350.9993220.9993090.9992950.9992820.9992680.999255
140.9992410.9992270.9992130.9991990.9991840.9991700.9991560.9991410.9991260.999111
150.9990960.9990810.9990660.9990510.9990350.9990190.9990040.9989880.9989720.998956
160.9989400.9989230.9989070.9988910.9988740.9988570.9988400.9988230.9988060.998789
170.9987720.9987540.9987370.9987190.9987010.9986830.9986650.9986470.9986290.998611
180.9985920.9985740.9985550.9985360.9985170.9984990.9984790.9984600.9984410.998421
190.9984020.9983820.9983630.9983430.9983230.9983030.9982830.9982620.9982420.998221
200.9982010.9981800.9981590.9981380.9981170.9980960.9980750.9980540.9980320.998011
210.9979890.9979670.9979450.9979240.9979010.9978790.9978570.9978350.9978120.997790
220.9977670.9977440.9977210.9976980.9976750.9976520.9976290.9976060.9975820.997559
230.9975350.9975110.9974870.9974630.9974390.9974150.9973910.9973660.9973420.997317
240.9972930.9972680.9972430.9972180.9971930.9971680.9971430.9971180.9970920.997067
250.9970410.9970150.9969900.9969640.9969380.9969120.9968850.9968590.9968330.996806
260.9967800.9967530.9967260.9967000.9966730.9966460.9966190.9965910.9965640.996537
270.9965090.9964820.9964540.9964260.9963990.9963710.9963430.9963140.9962860.996258
280.9962300.9962010.9961730.9961440.9961150.9960860.9960570.9960280.9959990.995970
290.9959410.9959120.9958820.9958530.9958230.9957930.9957640.9957340.9957040.995674
300.9956430.9956130.9955830.9955530.9955220.9954910.9954610.9954300.9953990.995368
310.9953370.9953060.9952750.9952440.9952120.9951810.9951490.9951180.9950860.995054
320.9950230.9949910.9949590.9949270.9948940.9948620.9948300.9947970.9947650.994732
330.9946990.9946670.9946340.9946010.9945680.9945350.9945020.9944680.9944350.994402
340.9943680.9943340.9943010.9942670.9942330.9941990.9941650.9941310.9940970.994063
350.9940280.9939940.9939600.9939250.9938900.9938560.9938210.9937860.9937510.993716
360.9936810.9936460.9936100.9935750.9935390.9935040.9934680.9934330.9933970.993361
370.9933250.9932890.9932530.9932170.9931810.9931440.9931080.9930710.9930350.992998
380.9929620.9929250.9928880.9928510.9928140.9927770.9927400.9927020.9926650.992628
390.9925900.9925530.9925150.9924770.9924390.9924010.9923630.9923250.9922870.992249
Table 2

Density of air-free water (g/cm3) from Eq. (3) using Kell [2] data

t(°C)0.00.10.20.30.40.50.60.70.80.9
  50.9999650.9999630.9999610.9999590.9999570.9999540.9999520.9999490.9999460.999943
  60.9999400.9999370.9999340.9999300.9999260.9999230.9999190.9999140.9999100.999906
  70.9999010.9998960.9998920.9998870.9998810.9998760.9998710.9998650.9998600.999854
  80.9998480.9998420.9998350.9998290.9998220.9998160.9998090.9998020.9997950.999788
  90.9997800.9997730.9997650.9997570.9997490.9997410.9997330.9997250.9997160.999708
100.9996990.9996900.9996810.9996720.9996630.9996530.9996440.9996340.9996240.999615
110.9996040.9995940.9995840.9995740.9995630.9995520.9995410.9995310.9995190.999508
120.9994970.9994850.9994740.9994620.9994500.9994380.9994260.9994140.9994020.999389
130.9993770.9993640.9993510.9993380.9993250.9993120.9992990.9992850.9992720.999258
140.9992440.9992300.9992160.9992020.9991880.9991730.9991590.9991440.9991290.999114
150.9990990.9990840.9990690.9990530.9990380.9990220.9990070.9989910.9989750.998959
160.9989430.9989260.9989100.9988930.9988770.9988600.9988430.9988260.9988090.998792
170.9987740.9987570.9987390.9987220.9987040.9986860.9986680.9986500.9986320.998613
180.9985950.9985760.9985580.9985390.9985200.9985010.9984820.9984630.9984440.998424
190.9984050.9983850.9983650.9983450.9983250.9983050.9982850.9982650.9982440.998224
200.9982030.9981830.9981620.9981410.9981200.9980990.9980770.9980560.9980350.998013
210.9979910.9979700.9979480.9979260.9979040.9978820.9978590.9978370.9978150.997792
220.9977690.9977460.9977240.9977010.9976780.9976540.9976310.9976080.9975840.997561
230.9975370.9975130.9974890.9974650.9974410.9974170.9973930.9973690.9973440.997320
240.9972950.9972700.9972450.9972200.9971950.9971700.9971450.9971200.9970940.997069
250.9970430.9970170.9969920.9969660.9969400.9969140.9968870.9968610.9968350.996808
260.9967820.9967550.9967280.9967010.9966750.9966480.9966200.9965930.9965660.996539
270.9965110.9964830.9964560.9964280.9964000.9963720.9963440.9963160.9962880.996260
280.9962310.9962030.9961740.9961460.9961170.9960880.9960590.9960300.9960010.995972
290.9959420.9959130.9958840.9958540.9958240.9957950.9957650.9957350.9957050.995675
300.9956450.9956150.9955840.9955540.9955230.9954930.9954620.9954310.9954010.995370
310.9953390.9953070.9952760.9952450.9952140.9951820.9951510.9951190.9950870.995056
320.9950240.9949920.9949600.9949280.9948950.9948630.9948310.9947980.9947660.994733
330.9947010.9946680.9946350.9946020.9945690.9945360.9945030.9944690.9944360.994403
340.9943690.9943350.9943020.9942680.9942340.9942000.9941660.9941320.9940980.994064
350.9940290.9939950.9939600.9939260.9938910.9938560.9938220.9937870.9937520.993717
360.9936820.9936460.9936110.9935760.9935400.9935050.9934690.9934330.9933980.993362
370.9933260.9932900.9932540.9932170.9931810.9931450.9931080.9930720.9930350.992999
380.9929620.9929250.9928880.9928510.9928140.9927770.9927400.9927030.9926650.992628
390.9925900.9925530.9925150.9924780.9924400.9924020.9923640.9923260.9922880.992249
Table 3

Density of air-free water (g/cm3) from formulation of Wagenbreth and Blanke [1]

t(°C)0.00.10.20.30.40.50.60.70.80.9
  50.9999640.9999620.9999600.9999580.9999560.9999540.9999510.9999490.9999460.999943
  60.9999400.9999370.9999330.9999300.9999260.9999220.9999180.9999140.9999100.999906
  70.9999010.9998960.9998920.9998870.9998810.9998760.9998710.9998650.9998600.999854
  80.9998480.9998420.9998350.9998290.9998220.9998160.9998090.9998020.9997950.999787
  90.9997800.9997730.9997650.9997570.9997490.9997410.9997330.9997250.9997160.999707
100.9996990.9996900.9996810.9996720.9996620.9996530.9996430.9996340.9996240.999614
110.9996040.9995940.9995830.9995730.9995620.9995520.9995410.9995300.9995190.999507
120.9994960.9994850.9994730.9994610.9994490.9994370.9994250.9994130.9994010.999388
130.9993760.9993630.9993500.9993370.9993240.9993110.9992970.9992840.9992700.999256
140.9992430.9992290.9992150.9992000.9991860.9991720.9991570.9991420.9991280.999113
150.9990980.9990830.9990670.9990520.9990360.9990210.9990050.9989890.9989730.998957
160.9989410.9989250.9989080.9988920.9988750.9988580.9988410.9988240.9988070.998790
170.9987730.9987550.9987380.9987200.9987020.9986840.9986660.9986480.9986300.998612
180.9985930.9985750.9985560.9985370.9985190.9985000.9984800.9984610.9984420.998422
190.9984030.9983830.9983640.9983440.9983240.9983040.9982840.9982630.9982430.998222
200.9982020.9981810.9981600.9981390.9981180.9980970.9980760.9980550.9980330.998012
210.9979900.9979680.9979470.9979250.9979030.9978810.9978580.9978360.9978140.997791
220.9977680.9977460.9977230.9977000.9976770.9976540.9976300.9976070.9975840.997560
230.9975360.9975130.9974890.9974650.9974410.9974170.9973920.9973680.9973440.997319
240.9972940.9972700.9972450.9972200.9971950.9971700.9971450.9971190.9970940.997068
250.9970430.9970170.9969910.9969660.9969400.9969130.9968870.9968610.9968350.996808
260.9967820.9967550.9967230.9967020.9966750.9966480.9966210.9965930.9965660.996539
270.9965110.9964840.9964560.9964280.9964010.9963730.9963450.9963160.9962880.996260
280.9962320.9962030.9961750.9961460.9961170.9960880.9960600.9960310.9960010.995972
290.9969430.9959140.9958840.9958550.9958250.9957950.9957650.9957360.9957060.995676
300.9956450.9956150.9955850.9955540.9955240.9954930.9954630.9954320.9954010.995370
310.9953390.9953080.9952770.9952460.9952140.9951830.9951510.9951200.9950880.995056
320.9950240.9949920.9949600.9949280.9948960.9948640.9948310.9947990.9947660.994734
330.9947010.9946680.9946350.9946020.9945690.9945360.9945030.9944700.9944360.994403
340.9943690.9943360.9943020.9942680.9942340.9942010.9941670.9941320.9940980.994064
350.9940300.9939950.9939610.9939260.9938910.9938570.9938220.9937870.9937520.993717
360.9936820.9936470.9936110.9935760.9935410.9935050.9934690.9934340.9933980.993362
370.9933260.9932900.9932540.9932180.9931820.9931460.9931090.9930730.9930360.993000
380.9929630.9929260.9928890.9928520.9928150.9927780.9927410.9927040.9926670.992629
390.9925920.9925540.9925170.9924790.9924420.9924040.9923660.9923280.9922900.992252
The units for water density in these tables are g/cm3, as a convenience to those who routinely use these units.

5. Summary

Equation (3) can be used to calculate the density of air-free water in the temperature range of 5 to 40 °C in ITS-90 at one atmosphere. Equation (6) can be used to calculate the density of air-saturated water in the same temperature range at one atmosphere. Equation (8) can be used to calculate the density of air-saturated water in the same temperature range at an ambient pressure of P kPa. The use of Eq. (6) for air-saturated water, and Eq. (8) where appropriate, is recommended for calculation of water density.
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