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Acoustic Gas Thermometry Roberto M. Gavioso 1 st June 2017 28th Meeting of the Consultative Committee for Thermometry (CCT) CCT/17-29

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Page 1: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

Acoustic Gas Thermometry

Roberto M. Gavioso

1st June 2017

28th Meeting of the Consultative Committee for Thermometry (CCT)

CCT/17-29

Page 2: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

outline Acoustic Gas Thermometry

hystorical development

• development of theory: Laplace was finally right

• wide ranging applications of acoustic gas thermometry ...

• ... including primary temperature standards

ongoing work and future perspectives

• extending the temperature range of primary acoustic thermometers

• alternatives for dissemination: simplification of primary methods

• practical acoustic thermometers

results

• determinations of the molar gas constant R and the

Boltzmann constant k

• determinations of T-T90

milestones along a successful road

• theory and practice of a sphere

• son et lumiere: advantages of the new SI

Page 3: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

1627 - Francis Bacon

gedanken experiment To try exactly the time wherein sound is propagated

[..] let a man stand in a steeple, with a candle, veiled; and let

another man stand a mile off: then let the person in the steeple

strike a bell and at the same instant withdraw the veil; the other, at

a distance, may measure the time between the light seen and the

sound heard, for light is propagated instantaneously*

*Or what comes very near thereto, for in the space of seven or

eight minutes it is thought by some to travel from the sun to the

earth.

transient method 1635 - Pierre Gassendi

478 m/s

Marin Mersenne 1636

448 m/s

Cogitata Physico

Mathematica

steady-state method

Benedicam Dominum, Benedicam Dominum Benedicam Dominum

1656 - Viviani, Borelli

360 m/s

1708 - Derham, Flansted, Halley

348 m/s

at 20 °C, 1 atm, 50% relative humidity

speed of sound in air

344 m/s

Sylva Sylvarum 1627

Page 4: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

2 1

p

S V

cpc

c

1687 Newton

1816 Laplace

2 1=

T

pc

2 4

pc

1727 Euler

Newton (isothermal)

T = const

Laplace (adiabatic)

S = const

dQ = 0

wavelength mean free pathl

1S

p

1T

p

Page 5: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

21 S

S

cp

1

Sp

1S

S

V

V p

0 50 100 150 200 250 300 350 4000

200

400

600

800

1000

1200

1400

1600

Tc

isothermal speed of sound

liquid water

water vapor

sp

ee

d o

f so

un

d / m

s-1

Temperature / °C

adiabatic speed of sound

liquid water

water vapor

21L s

S

pc

K

2

T

S

pc

G

longitudinal waves

shear waves

bulk modulus

shear modulus

versatility of Laplace equation

Page 6: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

1965 - 1975 up to 20000 K He: 300 K - 2000 K, 2 MPa 1962

Page 7: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

sonic anemometry (& thermometry)

2 MT u

R

sonic temperature

w' T '

sonic kinematic heat flux

turbulent heat flux

sonic anemometers are sensors that are able to estimate wind speed vector

by measuring the influence of local wind speed on the transmission of

ultrasound signals between pairs of emitters and receivers that configure

acoustic paths. This estimation is normally assigned to the geometric center

of acoustic path midpoints

sonic anemometers are used to evaluate the turbulent heat flux from the sonic

kinematic heat flux (or “temperature flux”), i.e. the covariance of the vertical wind

velocity w and the sonic temperature T the vertical wind velocity w and the

speed of sound c being simultaneously measured by the anemometer, and the

speed of sound being then corrected for the effect of the crosswind

Page 8: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

Acoustic Thermometry of Ocean Climate (ATOC) precision 50 ms – accuracy 0.1 s ≈ 0.05 K

3.3 kW at 57 Hz 206 dB

1994

Page 9: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

2015

abstract: measuring temperature changes of the deep oceans, important for determining the oceanic heat content and its impact on the Earth’s

climate evolution, is typically done using free-drifting profiling oceanographic floats with limited global coverage. Acoustic thermometry provides

an alternative and complementary remote sensing methodology for monitoring fine temperature variations of the deep ocean over long distances

between a few underwater sources and receivers. We demonstrate a simpler, totally passive (i.e., without deploying any active sources)

modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing

hydroacoustic stations of the International Monitoring System. We suggest that passive acoustic thermometry could improve global monitoring of

deep-ocean temperature variations through implementation using a global network of hydrophone arrays

(A) Locations of the two hydroacoustic stations (red

dots) near Ascension and Wake Islands.. (B)

Zoomed-in schematic of the hydrophone array

configurations for the Ascension and Wake Island

sites, which both have a similar layout. Each

hydroacoustic station consists of a northern and

southern triangle array of three hydrophones (or

triad), with each triangle side equal to approximately

2 km. The distance L between triad centers is equal

to 126 km and 132 km for the Ascension and Wake

Island stations, respectively.

(C) Noise cross-correlation waveforms, averaged

over three different years, obtained between all 9

pairwise combinations of the elements of the north

and south triads for the Wake Island. (D) Same as

C, but for Ascension Island. The beams shown by

dashed lines in A are centered on the lines joining

the centers of the south and north triads of each

hydroacoustic station (yellow line) and which

intersect the Polar regions where potential ice noise

sources contributing to the coherent arrivals shown

in C-D are located (18b).

Page 10: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

ideal gas assumptions:

• the molecules of the gas are indistinguishable, small, hard spheres

• collisions are elastic and motion is frictionless (no energy loss)

• Newton's laws apply

• average distance between molecules is much larger than molecular size

• the molecules constantly move in random directions with a distribution of speeds

• there are no attractive or repulsive forces between the molecules

22

02

rmsvu

0 5 3 monoatomic gas 2 2

0 0 0 0

1

3rms

S

p kT RTu T v

m M

squared mean

molecular speed molar mass molecular mass

1873

Alfred Marshall Mayer

Koenig flame

manometer (1862) Wheatstone revolving mirror

(1834)

ambient to 1000 °C

kTmvrms

2

3

2

1 2 mean

kinetic energy p RT Mideal gas

equation of state

Page 11: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

1979 273.16 K

8.4 ppmru R

1965

2 K ÷ 20 K

repeatabilty 3 mK

[..] We felt that experimental determination of

isotherms from measurements of the speed of

sound in helium gas as a function of pressure was

a promising approach. The concept of deriving

values of absolute temperature from speed-of-

sound measurements is not of recent origin. Lord

Rayleigh recognized the possibility of such an

experiment in 1878 in observations on a

communication from A. M. Mayer [..].

[..] Since gas thermometry is the method which has

been most widely used for achieving temperature

values that approach values on the thermodynamic

scale, the technique was given serious

consideration. But precise gas thermometry is a very

painstaking undertaking, especially at low

temperatures, where certain difficulties are

intensifled [..]

Page 12: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

thermal viscous shell ducts

2 N

N

au f f f f f

z

-23 -1 -1

A 1.380 651 3 0.000 002 5 10 J mol Kk R N (1.8 ppm)

1988

1979 - 1988

bulk thermal viscous ducts Ng g g g g

Page 13: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

22

2 sound

0 20

B B Blight

frequencyenergy mass velocity masstemperature lim

frequencypc

k k k

ac

ac

2 ,, ,

a p Tu p T f p T

z

mw

mw

2 ,, ,

a p Tc p T f p T

z

ac mw

acmw

, ,

, ,

u p T f p T z

c p T zf p T

1986

Page 14: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

1999

217 K to 303 K

2

20TPW TPW

,lim

,p

u p TT

T u p T

Page 15: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

2000

90 K to 300 K

Page 16: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

2003

303 K, 430 K, 505 K

Page 17: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

2004 234 K to 380 K

Page 18: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

18

8 1 10f

f

precision

improved frequency measurement

6 < 1 10f

f

accuracy

2004

Page 19: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

2006 77 K to 273 K

Page 20: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

2007

271 K to 552 K

Page 21: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

2008 -2011 iMERA- Plus Research Project

Determination of the Boltzmann constant

for the redefinition of the kelvin

coordinator J. Fischer

on-lathe interferometry

Page 22: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

23 1

2 2rmskT mv

composition

(including isotopes)

of test gases

liquid He cold trap

heated getter

mass spectrometry

6 3 4 60.03 10 He He 1 10 60.25 10M M

helium argon

2010

Ar 0 1 ppmru M .

2015

Ar 0 6 ppmru M .

june 2017 Ar 0 4 ppmru M .

Page 23: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

The new kelvin 31 August 2015 Page 23 of 48

Thermodynamics vs. ITS

0.1

1

10

100

1000

10000

100000

1900 1920 1940 1960 1980 2000 2020

Rel

ativ

e er

ror

or r

epro

duci

bili

ty, p

pm

Year

Boltzmann's constant

Temperature scales

Metrologia Boltzmann Special Issue 2015, R. White and J. Fischer Figure 1: Relative uncertainty in the value of Boltzmann’s constant. Also shown is the relative reproducibility of the practical temperature scales, in the vicinity of 100 C.

Page 24: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

determinations of k with AGT and other methods 2017 (yesterday)

AGT with cylindrical cavities

Johnson noise thermometry (JNT)

60 59 10ru k .

60 70 10ru k .

61 95 10ru k . 62 10ru k

67 5 10ru k .

Page 25: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

25 50 75 100

-7.5

-5.0

-2.5

0.0

2.5

WG4 u(WG4)

PTB - DCGT 2015 - (C1 - He)

PTB - DCGT 2015 - (C1, C2 - He, Ne)

LNE-CNAM - AGT 2015

LNE-CNAM - AGT 2006

UCL - AGT 2000

NRC - RIGT 2017

(T-T

90)

/ m

K

Temperature / K

100 150 200 250 300 350 400-10

-8

-6

-4

-2

0

2

4

6

8

10

NPL - AGT 2015

NPL - AGT 2016

INRiM - AGT 2016

VNIIFTRI - AGT 2017

NIM - AGT 2017

LNE - AGT 2015

(T-T

90)

/ m

K

Temperature / K

2012 - 2017 AGT data

2012 - 2015 EMRP Research Project

Implementing the new kelvin - InK

coordinator G. Machin

Page 26: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

coordinator G. Machin

2016 -2019 EMRP Research Project

Implementing the new kelvin 2 - InK2

T-T90 by Acoustic Gas Thermometry (AGT) between 430 K and 933 K

Inconel pressure

vessel 1 MPa @

1000 K

Page 27: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

Benefits

• 2-stage pulse-tube cryostat no LHe

• 2 thermal shields and 2 vacuum chambers

• minimum temperature < 4 K

• same calorimeter for T and T90 realization

• houses a larger number of CSPRTs

• provides good stability especially

in ranges 30 K – 77 K and

150 K – 234 K

Risks and drawbacks

• vibrations could affect measurements

• complex design, needed long realization

time

coordinator G. Machin

2016 -2019 EMRP Research Project

Implementing the new kelvin 2 - InK2

T-T90 by Acoustic Gas Thermometry between 5 K and 200 K

Page 28: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

extending the temperature range of primary thermometers

The cold valve The prototype sphere

The Cryogenic Current Comparator

Amplification and its shield

AGT at T < 4 K

Page 29: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

8 cm

16 cm

22 c

m

termination of acoustic and microwave waveguides

• material: copper; shape: triaxial ellipsoid; interrnal radius: 4 cm; interrnal volume: 260

cm3; thick wall to minimize shell coupling; the cavity is designed to be vacuum- and

pressure tight

• excitation of acoustic and microwave resonances by waveguides

• embedded thermometer wells for cSPRTs and long-stem SPRTs

• working gas: helium (calculable properties) purity maintained by a getter

• temperature range of initial tests: 230 K to 430 K;

• aimed accuracy: ± 5 ppm

2 2 2

0 1 2 , , ... u p T u p T A T p A T p

measured calculable for He

alternatives for dissemination: simplification of primary methods

Page 30: Acoustic Gas Thermometry - BIPM - BIPM · modality for acoustic thermometry of the deep oceans (for depths of ~ 500–1500 m), using only ambient noise recorded by two existing hydroacoustic

assembled

calibration zone with

Peltiers

Microphone and Loudspeaker in stabilised zone