Testing General Relativity with Atom Interferometry Savas - - PowerPoint PPT Presentation

testing general relativity with atom interferometry
SMART_READER_LITE
LIVE PREVIEW

Testing General Relativity with Atom Interferometry Savas - - PowerPoint PPT Presentation

Testing General Relativity with Atom Interferometry Savas Dimopoulos with Peter Graham Jason Hogan Mark Kasevich Testing Large Distance GR Cosmological Constant Problem suggests Our understanding of GR is incomplete (unless there are ~10 500


slide-1
SLIDE 1
slide-2
SLIDE 2

Testing General Relativity with Atom Interferometry

Savas Dimopoulos

with

Peter Graham Jason Hogan Mark Kasevich

slide-3
SLIDE 3

Testing Large Distance GR

Our understanding of GR is incomplete

CCP+DM inspired proposals for IR modifications:

Damour-Polyakov DGP ADDG (non-locality) Ghost condensation ... MOND Beckenstein ... Brans-Dicke Bimetric ...

Cosmological Constant Problem suggests

(unless there are ~10500 universes!)

slide-4
SLIDE 4

Precision long distance tests

QED:

10 digit accuracy

g-2, EDMs, etc

Principle of Equivalence tested to 3×10-13 most other tests ~ 10-3 to 10-5

time delay (Cassini tracking) light deflection (VLBI) perihelion shift Nordtvedt effect 10-5 10-3 10-3 10-3 Lense-Thirring (GPB)

GR:

slide-5
SLIDE 5

Precision GR tests mostly use: Can we study GR using atoms over short distances (meters)? Planets and photons over astronomical distances

slide-6
SLIDE 6

Precision GR tests mostly use: Can we study GR using atoms over short distances (meters)? Planets and photons over astronomical distances

Yes, thanks to the tremendous advances in Atom Interferometry

  • Unprecedented Precision

(see Nobel Lectures ’97, ’01, ’05 )

  • Several control variables (v, t, ω, h)

We are at crossroads where atoms may compete with astrophysical tests of GR

slide-7
SLIDE 7

Atom Interferometry

can measure minute forces

Galileo Current Future

∼ 10−11g

∼ 10−17g

∼ g

An old idea

A.Peters

slide-8
SLIDE 8

Atom Interferometry

can measure minute forces

Galileo Current Future

∼ 10−11g

∼ 10−17g

∼ g dv dt = −∇φ + GR

φ = GN Me Re

An old idea

A.Peters

slide-9
SLIDE 9

Outline

  • Post Newtonian General Relativity
  • Atom Interferometry
  • Preliminary estimates
slide-10
SLIDE 10

Post-Newtonian Approximation

Expansion in potential and velocity

Atom velocity:

φ = GNMearth Rearth ∼ 1 2 × 10−9

Small Numbers

Earth’s potential: height Rearth ∼ 10 m 6 × 106 m ∼ 1 6 × 10−5 Gradient:

vatoms ∼ 10 m sec ∼ 3 × 10−8

slide-11
SLIDE 11

Particle equation of motion

d v dt = −∇(φ + 2φ2 + ψ) −∂ ζ ∂t + v × (∇ × ζ) +3 v ∂φ ∂t + 4 v( v · ∇)φ − v2∇φ

Newtonian Gravitational Potential Kinetic Energy Gravitational Potential Rotational Energy Gravitational Potential

φ ψ ζ

“scalar potential” “vector potential”

slide-12
SLIDE 12

Non-abelian gravity

d v dt = −∇(φ + 2φ2 + ψ)−∂ ζ ∂t + v × (∇ × ζ) +3 v ∂φ ∂t + 4 v( v · ∇)φ − v2∇φ

In empty space ∇2φ = 4πGNρ = 0

Newton Einstein

∇2δφ = (∇φ)2 ∼ ∇2φ2

⇒ δφ ∼ φ2

∇ · g =

= ⇒ “∇ · g = 0”

slide-13
SLIDE 13

Non-abelian gravity

d v dt = −∇(φ + 2φ2 + ψ)−∂ ζ ∂t + v × (∇ × ζ) +3 v ∂φ ∂t + 4 v( v · ∇)φ − v2∇φ

In empty space ∇2φ = 4πGNρ = 0

Newton Einstein

∇2δφ = (∇φ)2 ∼ ∇2φ2

⇒ δφ ∼ φ2

∇ · g =

= ⇒ “∇ · g = 0”

Effect ∼ 10−9g

  • nly gradient measurable → 10−15g
slide-14
SLIDE 14

“Kinetic Energy Gravitates”

d v dt = −∇(φ + 2φ2 + ψ)−∂ ζ ∂t + v × (∇ × ζ) +3 v ∂φ ∂t + 4 v( v · ∇)φ − v2∇φ

Effect ∼ v2

atomsg

− v2∇φ + 4 v( v · ∇)φ

∼ 10−15g

slide-15
SLIDE 15

General Relativity effects on equation of motion

d v dt = −∇(φ + 2φ2 + ψ)−∂ ζ ∂t + v × (∇ × ζ) +3 v ∂φ ∂t + 4 v( v · ∇)φ − v2∇φ

slide-16
SLIDE 16

General Relativity effects on equation of motion

d v dt = −∇(φ + 2φ2 + ψ)−∂ ζ ∂t + v × (∇ × ζ) +3 v ∂φ ∂t + 4 v( v · ∇)φ − v2∇φ

1 10−9

slide-17
SLIDE 17

General Relativity effects on equation of motion

d v dt = −∇(φ + 2φ2 + ψ)−∂ ζ ∂t + v × (∇ × ζ) +3 v ∂φ ∂t + 4 v( v · ∇)φ − v2∇φ

10−15

1 10−9

slide-18
SLIDE 18

General Relativity effects on equation of motion

d v dt = −∇(φ + 2φ2 + ψ)−∂ ζ ∂t + v × (∇ × ζ) +3 v ∂φ ∂t + 4 v( v · ∇)φ − v2∇φ

10−15

10−13

∼ 0

1 10−9

slide-19
SLIDE 19

General Relativity effects on equation of motion

d v dt = −∇(φ + 2φ2 + ψ)−∂ ζ ∂t + v × (∇ × ζ) +3 v ∂φ ∂t + 4 v( v · ∇)φ − v2∇φ

10−15

10−13

∼ 0

10−15

∼ 0

1 10−9

slide-20
SLIDE 20

General Relativity effects on equation of motion

d v dt = −∇(φ + 2φ2 + ψ)−∂ ζ ∂t + v × (∇ × ζ) +3 v ∂φ ∂t + 4 v( v · ∇)φ − v2∇φ

Can these terms be measured in the lab?

10−15

10−13

∼ 0

10−15

∼ 0

1 10−9

slide-21
SLIDE 21

Light Interferometry

accurate measurement of

beamsplitter mirror mirror beamsplitter

  • utput

ports

∆L L ∼ λ L ×(phase resolution)

x y

slide-22
SLIDE 22

similar to light interferometer but arms are separated in space-time instead of space-space

r T 2T t

  • utput

ports mirror mirror beamsplitter beamsplitter

Atom Interferometry

slide-23
SLIDE 23

similar to light interferometer but arms are separated in space-time instead of space-space

r T 2T t

  • utput

ports mirror mirror beamsplitter beamsplitter

Atom Interferometry

slide-24
SLIDE 24

similar to light interferometer but arms are separated in space-time instead of space-space

r T 2T t

  • utput

ports mirror mirror beamsplitter beamsplitter

Atom Interferometry

slide-25
SLIDE 25

similar to light interferometer but arms are separated in space-time instead of space-space

r T 2T t

  • utput

ports mirror mirror beamsplitter beamsplitter

Atom Interferometry

slide-26
SLIDE 26

similar to light interferometer but arms are separated in space-time instead of space-space

r T 2T t

  • utput

ports mirror mirror beamsplitter beamsplitter

Atom Interferometry

slide-27
SLIDE 27

use lasers as beamsplitters and mirrors

r T 2T t

Atom Interferometry

slide-28
SLIDE 28

Atom Interferometry

slow atoms fall more under gravity and the interferometer can be as long as 1 sec ~ earth-moon distance!

r T 2T t

slide-29
SLIDE 29

Raman Transition

1,p 2,pk Ω1 Ω2

ke f f = ω1 +ω2 ∼ 1 eV ωef f = ω1 −ω2 ∼ 10−5 eV

kef f

ω1 ω2 ω2

slide-30
SLIDE 30

Raman Transition

pulse is a beamsplitter pulse is a mirror

π

π/2

1,p 2,pk Ω1 Ω2

Π

  • 2

Π 3 Π

  • 2

2 Π t Rabi1 1

  • 2

1 , c12 c22 1,p 2,pk

ψ = c1|1, p+c2|2, p+k

slide-31
SLIDE 31

AI Phase Shifts

Total phase difference comes from three sources:

∆φtot = ∆φpropagation + ∆φlaser + ∆φseparation

slide-32
SLIDE 32

Propagation Phase

integral taken over each arm of interferometer

r T 2T t

∆φtot = ∆φpropagation + ∆φlaser + ∆φseparation φpropagation =

  • mdτ =
  • Ldt =
  • pµdxµ
slide-33
SLIDE 33

Laser Phase

  • ut|Hint|in = out|
  • µ·

E0ei

x|in

the laser imparts a phase to the atom just as a mirror or beamsplitter imparts a phase to light

∆φtot = ∆φpropagation + ∆φlaser + ∆φseparation φlaser =

  • vertices

(phase of laser)

slide-34
SLIDE 34

Separation Phase

r T 2T t

∆xµ

∆φseparation =

  • ∆xµ pνdxν
slide-35
SLIDE 35

Measuring Gravity

a constant gravitational field produces a phase shift:

r T 2T t

φpropagation = 1 2mv2 − mgh

  • dt

∆φpropagation = mg × (area) = mg × k mT × T

∆φtot = kgT 2 ∼ 108 radians

slide-36
SLIDE 36

Gravity Phases

                                                     

GkMT 2 R2

e

  • 1. × 108

− 2GkMT 3vL

R3

e

−2. × 103 − GMT 2ω

R2

e

−1. × 103

GMT 2ωA R2

e

  • 1. × 103

7G2kM 2T 4 6R5

e

1.16667 × 102

3GkMT 2vL R2

e

  • 3. × 101

− 3G2kM2T 3

R4

e

−3. − Gk2MT 3

mR3

e

−1.

7GkMT 4v2

L

2R4

e

3.5 × 10-2

2GMT 3ωvL R3

e

  • 2. × 10-2

− 2GMT 3vLωA

R3

e

−2. × 10-2

3Gk2MT 2 2mR2

e

1.5 × 10-2

G2kM 2T 2 R3

e

  • 1. × 10-2

− 11G2kM 2T 5vL

2R6

e

−5.5 × 10-3 − 7G2M 2T 4ω

6R5

e

−1.16667 × 10-3

7G2M 2T 4ωA 6R5

e

1.16667 × 10-3 − 8GkMT 3v2

L

R3

e

−8. × 10-4 − 3GMT 2ωvL

R2

e

−3. × 10-4

35G2kM 2T 4vL 2R5

e

1.75 × 10-4

5GkMT 2v2

L

R2

e

  • 5. × 10-6

− 11G2k2M 2T 5

4mR6

e

−2.75 × 10-6 − 15G2kM 2T 3vL

R4

e

−1.5 × 10-6

slide-37
SLIDE 37

Gravity Phases

non-relativistic constant g NR gravity gradient

                                                     

GkMT 2 R2

e

  • 1. × 108

− 2GkMT 3vL

R3

e

−2. × 103 − GMT 2ω

R2

e

−1. × 103

GMT 2ωA R2

e

  • 1. × 103

7G2kM 2T 4 6R5

e

1.16667 × 102

3GkMT 2vL R2

e

  • 3. × 101

− 3G2kM2T 3

R4

e

−3. − Gk2MT 3

mR3

e

−1.

7GkMT 4v2

L

2R4

e

3.5 × 10-2

2GMT 3ωvL R3

e

  • 2. × 10-2

− 2GMT 3vLωA

R3

e

−2. × 10-2

3Gk2MT 2 2mR2

e

1.5 × 10-2

G2kM 2T 2 R3

e

  • 1. × 10-2

− 11G2kM 2T 5vL

2R6

e

−5.5 × 10-3 − 7G2M 2T 4ω

6R5

e

−1.16667 × 10-3

7G2M 2T 4ωA 6R5

e

1.16667 × 10-3 − 8GkMT 3v2

L

R3

e

−8. × 10-4 − 3GMT 2ωvL

R2

e

−3. × 10-4

35G2kM 2T 4vL 2R5

e

1.75 × 10-4

5GkMT 2v2

L

R2

e

  • 5. × 10-6

− 11G2k2M 2T 5

4mR6

e

−2.75 × 10-6 − 15G2kM 2T 3vL

R4

e

−1.5 × 10-6

slide-38
SLIDE 38

Gravity Phases

non-relativistic constant g NR gravity gradient Doppler shift

                                                     

GkMT 2 R2

e

  • 1. × 108

− 2GkMT 3vL

R3

e

−2. × 103 − GMT 2ω

R2

e

−1. × 103

GMT 2ωA R2

e

  • 1. × 103

7G2kM 2T 4 6R5

e

1.16667 × 102

3GkMT 2vL R2

e

  • 3. × 101

− 3G2kM2T 3

R4

e

−3. − Gk2MT 3

mR3

e

−1.

7GkMT 4v2

L

2R4

e

3.5 × 10-2

2GMT 3ωvL R3

e

  • 2. × 10-2

− 2GMT 3vLωA

R3

e

−2. × 10-2

3Gk2MT 2 2mR2

e

1.5 × 10-2

G2kM 2T 2 R3

e

  • 1. × 10-2

− 11G2kM 2T 5vL

2R6

e

−5.5 × 10-3 − 7G2M 2T 4ω

6R5

e

−1.16667 × 10-3

7G2M 2T 4ωA 6R5

e

1.16667 × 10-3 − 8GkMT 3v2

L

R3

e

−8. × 10-4 − 3GMT 2ωvL

R2

e

−3. × 10-4

35G2kM 2T 4vL 2R5

e

1.75 × 10-4

5GkMT 2v2

L

R2

e

  • 5. × 10-6

− 11G2k2M 2T 5

4mR6

e

−2.75 × 10-6 − 15G2kM 2T 3vL

R4

e

−1.5 × 10-6

slide-39
SLIDE 39

Gravity Phases

non-relativistic constant g NR gravity gradient Doppler shift GR ∇φ2

                                                     

GkMT 2 R2

e

  • 1. × 108

− 2GkMT 3vL

R3

e

−2. × 103 − GMT 2ω

R2

e

−1. × 103

GMT 2ωA R2

e

  • 1. × 103

7G2kM 2T 4 6R5

e

1.16667 × 102

3GkMT 2vL R2

e

  • 3. × 101

− 3G2kM2T 3

R4

e

−3. − Gk2MT 3

mR3

e

−1.

7GkMT 4v2

L

2R4

e

3.5 × 10-2

2GMT 3ωvL R3

e

  • 2. × 10-2

− 2GMT 3vLωA

R3

e

−2. × 10-2

3Gk2MT 2 2mR2

e

1.5 × 10-2

G2kM 2T 2 R3

e

  • 1. × 10-2

− 11G2kM 2T 5vL

2R6

e

−5.5 × 10-3 − 7G2M 2T 4ω

6R5

e

−1.16667 × 10-3

7G2M 2T 4ωA 6R5

e

1.16667 × 10-3 − 8GkMT 3v2

L

R3

e

−8. × 10-4 − 3GMT 2ωvL

R2

e

−3. × 10-4

35G2kM 2T 4vL 2R5

e

1.75 × 10-4

5GkMT 2v2

L

R2

e

  • 5. × 10-6

− 11G2k2M 2T 5

4mR6

e

−2.75 × 10-6 − 15G2kM 2T 3vL

R4

e

−1.5 × 10-6

slide-40
SLIDE 40

Gravity Phases

non-relativistic constant g NR gravity gradient Doppler shift GR ∇φ2 GR −

v2∇φ + 4 v( v · ∇)φ

                                                     

GkMT 2 R2

e

  • 1. × 108

− 2GkMT 3vL

R3

e

−2. × 103 − GMT 2ω

R2

e

−1. × 103

GMT 2ωA R2

e

  • 1. × 103

7G2kM 2T 4 6R5

e

1.16667 × 102

3GkMT 2vL R2

e

  • 3. × 101

− 3G2kM2T 3

R4

e

−3. − Gk2MT 3

mR3

e

−1.

7GkMT 4v2

L

2R4

e

3.5 × 10-2

2GMT 3ωvL R3

e

  • 2. × 10-2

− 2GMT 3vLωA

R3

e

−2. × 10-2

3Gk2MT 2 2mR2

e

1.5 × 10-2

G2kM 2T 2 R3

e

  • 1. × 10-2

− 11G2kM 2T 5vL

2R6

e

−5.5 × 10-3 − 7G2M 2T 4ω

6R5

e

−1.16667 × 10-3

7G2M 2T 4ωA 6R5

e

1.16667 × 10-3 − 8GkMT 3v2

L

R3

e

−8. × 10-4 − 3GMT 2ωvL

R2

e

−3. × 10-4

35G2kM 2T 4vL 2R5

e

1.75 × 10-4

5GkMT 2v2

L

R2

e

  • 5. × 10-6

− 11G2k2M 2T 5

4mR6

e

−2.75 × 10-6 − 15G2kM 2T 3vL

R4

e

−1.5 × 10-6

slide-41
SLIDE 41

Gravity Phases

non-relativistic constant g NR gravity gradient Doppler shift GR ∇φ2 GR −

v2∇φ + 4 v( v · ∇)φ

                                                     

GkMT 2 R2

e

  • 1. × 108

− 2GkMT 3vL

R3

e

−2. × 103 − GMT 2ω

R2

e

−1. × 103

GMT 2ωA R2

e

  • 1. × 103

7G2kM 2T 4 6R5

e

1.16667 × 102

3GkMT 2vL R2

e

  • 3. × 101

− 3G2kM2T 3

R4

e

−3. − Gk2MT 3

mR3

e

−1.

7GkMT 4v2

L

2R4

e

3.5 × 10-2

2GMT 3ωvL R3

e

  • 2. × 10-2

− 2GMT 3vLωA

R3

e

−2. × 10-2

3Gk2MT 2 2mR2

e

1.5 × 10-2

G2kM 2T 2 R3

e

  • 1. × 10-2

− 11G2kM 2T 5vL

2R6

e

−5.5 × 10-3 − 7G2M 2T 4ω

6R5

e

−1.16667 × 10-3

7G2M 2T 4ωA 6R5

e

1.16667 × 10-3 − 8GkMT 3v2

L

R3

e

−8. × 10-4 − 3GMT 2ωvL

R2

e

−3. × 10-4

35G2kM 2T 4vL 2R5

e

1.75 × 10-4

5GkMT 2v2

L

R2

e

  • 5. × 10-6

− 11G2k2M 2T 5

4mR6

e

−2.75 × 10-6 − 15G2kM 2T 3vL

R4

e

−1.5 × 10-6

GR ∇φ2

slide-42
SLIDE 42

Gravity Phases

GR terms doppler shift experimentally controllable parameters are:

108 −2×103 10−2 3×101 5×10−6 10−6

kgT 2

−2 kgT 2 vLT Re

−15 kgT 2 vLT Re φ

3 kgT 2 vL

kgT 2 φ

5 kgT 2 v2

L

k, vL, T

slide-43
SLIDE 43

Gravity Phases

same scalings, measure with gradient experimentally controllable parameters are:

108 −2×103 10−2 3×101 5×10−6 10−6

kgT 2

−2 kgT 2 vLT Re

−15 kgT 2 vLT Re φ

3 kgT 2 vL

kgT 2 φ

5 kgT 2 v2

L

k, vL, T

slide-44
SLIDE 44

Gravity Phases

experimentally controllable parameters are:

108 −2×103 10−2 3×101 5×10−6 10−6

kgT 2

−2 kgT 2 vLT Re

−15 kgT 2 vLT Re φ

3 kgT 2 vL

kgT 2 φ

5 kgT 2 v2

L

k, vL, T

same scalings

“∇ · g = 0”

slide-45
SLIDE 45

Gravity Phases

unique scaling experimentally controllable parameters are:

108 −2×103 10−2 3×101 5×10−6 10−6

kgT 2

−2 kgT 2 vLT Re

−15 kgT 2 vLT Re φ

3 kgT 2 vL

kgT 2 φ

5 kgT 2 v2

L

k, vL, T

slide-46
SLIDE 46

Atomic Interferometer

10 m atom drop tower. 10 m

currently under construction at Stanford

slide-47
SLIDE 47

Atomic Equivalence Principle Test

10 m 10 m atom drop tower.

slide-48
SLIDE 48

Atomic Equivalence Principle Test

10 m 10 m atom drop tower.

Co-falling 85Rb and 87Rb ensembles

Will reach accuracy ∼ 10−16 Compared to Lunar Laser Ranging ∼ 3 × 10−13

slide-49
SLIDE 49

Atomic Equivalence Principle Test

10 m 10 m atom drop tower.

Co-falling 85Rb and 87Rb ensembles

Will reach accuracy ∼ 10−16 Compared to Lunar Laser Ranging ∼ 3 × 10−13 Then will test PN GR

slide-50
SLIDE 50

Other equivalence principle measurements

Atomic Equivalence Principle Test at Stanford 10-15 g 2008 MICROSCOPE 10-15 g 2011 Galileo Galilei 10-17 g launch 2009? STEP 10-17 g ?

slide-51
SLIDE 51

Can we measure H ?

Pioneer anomaly ? Radio ranging of Pioneer ↔ Laser ranging of atoms BUT equivalence principle says only tides measurable

R ∼ H2

way too small and Riemann

slide-52
SLIDE 52

Can we measure H ?

Pioneer anomaly ? Radio ranging of Pioneer ↔ Laser ranging of atoms BUT equivalence principle says only tides measurable

R ∼ H2

way too small Similarly DM is not measurable

10−17g

level, and causes the earth not to be an inertial frame But, Sun’s radiation pressure is measurable at the and Riemann

slide-53
SLIDE 53

GR Experimentation

1916 - 1920 Precession of Mercury and light bending 1920 - 1960 Hibernation 1960 - Now Golden Era, many astronomical tests New epoch? High precision atom interferometry allows for greater control and ability to isolate and study individual effects in GR such as 3-graviton coupling and gravitation of kinetic energy

slide-54
SLIDE 54

Good to Go!

slide-55
SLIDE 55