why is it so hard to measure the strength of gravity?

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Why is it so hard to measure the Why is it so hard to measure the strength of gravity? strength of gravity? Stephen M. Merkowitz NASA/GSFC March 8, 2007

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Page 1: Why is it so hard to measure the strength of gravity?

Why is it so hard to measure the Why is it so hard to measure the strength of gravity?strength of gravity?

Stephen M. Merkowitz

NASA/GSFC

March 8, 2007

Page 2: Why is it so hard to measure the strength of gravity?

2G UMD - 3/8/07

Newton’s Law of GravityNewton’s Law of Gravity

• What is the quantity of matter?

• What is the distance dependence?

• What is the strength of gravity?FG = G

Mmr2

“there is a power of gravity pertaining to all bodies, proportional to the several quantities of matter which they obtain... the force of gravity towards the several particles of any body is inversely as the square of the distances of places from the particles” - Isaac Newton

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3G UMD - 3/8/07

What is the quantity of matter?What is the quantity of matter?

Inertial mass = Gravitational mass?Equivalence Principle Tests

Lunar Laser Ranging Torsion Pendulum Tests

Page 4: Why is it so hard to measure the strength of gravity?

4G UMD - 3/8/07

What is the distance dependence?What is the distance dependence?

Inverse Square Law Tests

Page 5: Why is it so hard to measure the strength of gravity?

5G UMD - 3/8/07

What is the strength of gravity?What is the strength of gravity?

• G is a fundamental physical constant

• Planetary motion - used to weight the planets and the sun

• Hydrostatic equilibrium for stars

• Planck scale

• May play a central role in unification at high energies (short distances)

• Fundamental constant in metrology?

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6G UMD - 3/8/07

Why is it so hard to measure the strength of gravity?Why is it so hard to measure the strength of gravity?

• Absolute measurement dependent on mass, length, & time.

• Gravitational interaction ~1000 times smaller than electromagnetic interaction.

• Gravitational force cannot be shielded.

• G has no known dependence on another fundamental constants.

• Measuring instrument of choice, torsion pendulum, is subject to a variety of parasitic couplings and systematic effects.

Page 7: Why is it so hard to measure the strength of gravity?

7G UMD - 3/8/07

Henry Cavendish (1798)Henry Cavendish (1798)

Density of Earth = 5.448 x Density of Water

Cornu & Baille (1873) used G as scale factor

“Experiments to determine the density of the Earth”

G = (6.754 ± 0.05) × 10−11Nm2 /kg2

I. Falconer, Measur. Sci. Tech. 10, 470 (1999).

G =3g

4π R⊕ρ⊕

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8G UMD - 3/8/07

Cavendish ExperimentCavendish Experiment

“As the force with which the balls are attracted by these weights is excessively minute, not more than 1/50 000 000 of their weight, it is plain, that a very minute disturbing force will be sufficient to destroy the success of the experiment” - Henry Cavendish

Apparatus by John Michell

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9G UMD - 3/8/07

G MeasurementsG MeasurementsG

·1011

(m3 /k

g/s2 )

Page 10: Why is it so hard to measure the strength of gravity?

10G UMD - 3/8/07

Measurement ErrorMeasurement Error

Uncertainty of G has increased only by about an order of magnitude per century!

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11G UMD - 3/8/07

1998 Relative Situation1998 Relative Situation

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12G UMD - 3/8/07

The Big G ControversyThe Big G Controversy

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13G UMD - 3/8/07

NBS G MeasurementNBS G Measurement

Source PPMPosition of large masses 10Mass of large masses 1Length of small mass 22Thickness of small mass 36Density of small mass 6Moment of inertia of mirror 23Frequency difference 40Total 64

G. G. Luther and W. R. Towler, Phys. Rev. Lett. 48, 121 (1982).

G = (6.6726 ± 0.0005) × 10−11Nm2 /kg2

Time of swing methodω 2 = K f + Kg( ) I

Kg =d 2Udϕ 2

G =∆ ω 2( )I

kg

, kg = Kg G

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14G UMD - 3/8/07

Limitations of Time ofLimitations of Time of Swing MethodSwing Method

• Changes in environment

• Changing environmental mass distribution

• Uncertainty of pendulum mass distribution

• 1/f noise

• Anelastic fiber properties (Kuroda effect)

K. Kuroda, Phys. Rev. Lett., 75, 2796 (1995).S. Matsumura et al., Phys. Lett. A 244, 4 (1998).

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15G UMD - 3/8/07

University of Washington G MeasurementUniversity of Washington G Measurement

J. H. Gundlach and S. M. Merkowitz, Phys. Rev. Lett. 85, 2869 (2000)

G = (6.674255 ± 0.000092) × 10−11Nm2 /kg2

Source PPMPendulum Width 0.4Pendulum Thickness 4.0Attractor Diagonal 7.1Ball-bar Calibration 1.4Attractor Vertical 5.2Sphere Diameter 2.6Attractor Temperature 6.9Sphere Mass 0.4Air Humidity 0.5Remaining Twist 0.3Magnetic Field 0.6Rot. Temperature Grad. 0.4Time Base: 0.1Data Reduction 2.0Statistical Error 5.8Total 13.7

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16G UMD - 3/8/07

MethodMethod

• Start pendulum turntable at constant rate

• Turn on acceleration feedback so torsion fiber does not twist

– No Kuroda effect

– Angular acceleration transferred to turntable

– Angle encoding absolutely calibrated

• Attractor mass on different turntable rotating at constant difference speed pendulum, thin

vertical platevacuum chamber on a turntable

Attractor mass

Page 17: Why is it so hard to measure the strength of gravity?

17G UMD - 3/8/07

Signal periodic at twice per revolution

ϕπαϕα imm

mm

mm eQqm

IG

l

l

ll

lll

l∑∑∑+

−=

= +−==

1, 1214)(

rdrYrrq mm3*

pend )ˆ()( ll

l ∫= ρ

rdrYrrQ mm3)1(

source )ˆ()( ll

l+−∫= ρ

ϕπα 2sin5

1622

2222 Q

IqG−=

Biggest component is 22α

Gravitational acceleration of a torsion balanceGravitational acceleration of a torsion balance

Page 18: Why is it so hard to measure the strength of gravity?

18G UMD - 3/8/07

Thin Plate PendulumThin Plate Pendulum

α22 = −24π

5GQ22 sin2ϕ

α22 = −16π

5G

q22

IQ22 sin2ϕ

q22

I=

ρr r p( )Y22 θ p,φp( )rp

2d3rp∫ρ

r r p( )sin2θprp

2d3rp∫2D →

1532π

q22

I=

w2 − t2

w2 + t215

32πFinite thickness plate:

Page 19: Why is it so hard to measure the strength of gravity?

19G UMD - 3/8/07

Minimize other Minimize other gravity momentsgravity moments

αl2 l=odd vanish by symmetrical design of pendulum & source

α42 q42vanishes for rectangular plate with( )222

103 twh +=

Q42 vanishes for vertical sphere separation of

ρ32

=z

α62, α82 Small and calculable

Higher terms small, fall of as2−

l

Rr r=pendulum radius

R=attractor mass radius

z

ρ

Page 20: Why is it so hard to measure the strength of gravity?

20G UMD - 3/8/07

ApparatusApparatus

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Big G ApparatusBig G Apparatus

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Pendulum positionPendulum position

• 4 bounces off pendulum plate gives angle amplification of 8

• Insensitive to other rotations

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PendulumPendulum

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24G UMD - 3/8/07

Turntable ReadoutTurntable Readout

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25G UMD - 3/8/07

PendulumPendulum--Turntable FeedbackTurntable Feedback

Pendulum ControllerInner TT Motor

Constant Difference

∆ω

Outer TTMotor

Outer TTEncoder

Inner TTEncoder

RecordAngle

Fiber Autocollimator

Controller

Page 26: Why is it so hard to measure the strength of gravity?

QuickTime™ and aH.264 decompressor

are needed to see this picture.

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27G UMD - 3/8/07

Signal SpectrumSignal Spectrum

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28G UMD - 3/8/07

Implosion of Kingdome 4 miles away

Bad DataBad Data

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29G UMD - 3/8/07

Fitting for GFitting for G

Finite pendulum thickness 1.0007857Pendulum attachment & imperfections 1.0000433Data averaging interval ( t=1s) 1.0000667Numeric derivative ( t=10s) 1.0134544

62 correction 0.999876782 correction 0.9999951

Magnetic damper torque 1.0000060

Acceleration Fit Corrections

α22 φ( )= −24π

5GQ22 sin2φ

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Attractor Mass MetrologyAttractor Mass Metrology

Laser

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31G UMD - 3/8/07

Attention to DetailsAttention to Details

• Attractor metrology

– Temperature corrected Q22before & after run showed good reproducibility (6.1 PPM).

– Q22 is temperature corrected with attractor temperature during run.

– Average over turntable & sphere imperfections using orthogonal configuration pairs.

• Attractor masses

– Direct equal arm balance measurement ±6mg.

– The air density (pressure,temperature,…) is recorded during runs and the displaced air mass is subtracted.

– Take 2 configurations with balls moved 90° on the turntable.

– Average out non-spherocity & density fluctuations of the balls by rotating.

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Other TestsOther Tests

• Various signal speeds

• Various inner turntable speeds

• Large magnetic fields

• Large rotating temperature gradients

• Various sampling times

• Data simulations

• Different sets of 4 spheres

• Linearity with 8 and 4 ball measurements

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G Data SetsG Data Sets

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Value for GValue for G

Quantity Measurementuncertainty

∆G/G(ppm)

Systematic Errors: Pendulum: Width 20µm 0.4 Thickness & Flatness 4.0µm 4.0 Attractor Masses: Diagonal 1.0µm 7.1 Ball-bar Calibration 0.2µm 1.4 Vertical 1.0µm 5.2 Sphere Diameter 1.5µm 2.6 Attractor Temperature 100mK 6.9 Sphere Mass 3.0mg 0.4 Air Humidity 0.5 Remaining Twist: 0.3 Magnetic Field: 0.6 Rot. Temperature Grad.: 0.4 Time Base: 10-7 0.1 Data Reduction: 2.0Statistical Error 5.8Total 13.7

G = (6.674255 ± 0.000092) × 10−11Nm2 /kg2

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2000 Status2000 StatusG

·1011

(m3 /k

g/s2 )

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36G UMD - 3/8/07

PTB ResolutionPTB Resolution• Fibreless torsion balance floated in

mercury.

• Angular deflection compensated electrostatically.

• AC and DC operation difficult to cross calibrate accuratly.

• Linearity errors between capacitance & angle due to dielectric layers.

• Additional capacitances identified.

W. Michaelis et al., Metrologia 41, L29 (2004).C. C. Speake et al., Phys. Lett. A 263, 219 (1999).W. Michaelis et al., Metrologia 32, 267 (1996).

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University of Zurich G MeasurementUniversity of Zurich G Measurement

S. Schlamminger et al., Phys. Rev. Lett. 89, 161102 (2002)S. Schlamminger et al., Phys. Rev. D 74, 082001 (2006)

G = (6.674252 ± 0.000124) × 10−11Nm2 /kg2

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38G UMD - 3/8/07

2002 Value Adjustment2002 Value AdjustmentG

·1011

(m3 /k

g/s2 )

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39G UMD - 3/8/07

ConclusionsConclusions

• Big G controversy appears to be resolved.

• Recent measured values are converging.

• Rate of precision improvement appears to be increasing.

• Precision gap with other fundamental constantans narrowing.