phys 5326 – lecture #11

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Monday, Feb. 24, 2003 Dr. Jae Yu. PHYS 5326 – Lecture #11. Brief Review of sin 2 q W measurement Neutrino Oscillation Measurements Solar neutrinos Atmospheric neutrinos A lecture on neutrino mass (Dr. Sydney Meshkov from CalTech). Next makeup class is Friday, Mar. 14, 1-2:30pm, rm 200. - PowerPoint PPT Presentation

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Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

1

PHYS 5326 – Lecture #11Monday, Feb. 24, 2003

Dr. Jae Yu

1. Brief Review of sin2W measurement

2. Neutrino Oscillation Measurements1. Solar neutrinos2. Atmospheric neutrinos

3. A lecture on neutrino mass (Dr. Sydney Meshkov from CalTech)

•Next makeup class is Friday, Mar. 14, 1-2:30pm, rm 200.

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

2

How is sin2W measured?

• Cross section ratios between NC and CC proportional to sin2W

• Llewellyn Smith Formula:

)(CC

)(CC

W4

W22

)(CC

)(NC)(

σ

σ1θsin

95

θsin21

ρσ

σR

WEMweak QIcoupling 2)3( sin)3(weakIcoupling

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

3

SM Global Fits with New ResultsWithout NuTeV dof=20.5/14: P=11.4%With NuTeV dof=29.7/15: P=1.3%Confidence level in upper Mhiggs limit weakens slightly.

LEP EWWG: http://www.cern.ch/LEPEWWG

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

4

Tree-level Parameters: and sin2W(on-shell)

• Either sin2W(on-shell) or 0 could agree with SM but both agreeing

simultaneously is unlikely

150GeV

Mln0.00032

50GeV

175GeVM0.00022θδsin

H

2

22tshell)(On

W2

0.0400.9983ρ

0.00310.2265θsin

0

W2

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

5

• R can be expressed in terms of quark couplings:

Model Independent Analysis

2R

2L-

--

grgR 1

XN

XN

Where

2

1

XνNσ

XNνσr

Paschos-Wolfenstein formula can be expressed as

2R

2L

νν

W22

νCC

νCC

νNC

νNC gg

r1

rRRθsin

2

σσ

σσR

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

6

Model Independent Analysis

Difficult to explain the disagreement with SM by:Parton Distribution Function or LO vs NLO or Electroweak Radiative Correction: large MHiggs

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

7

Linking sin2W with Higgs through Mtop vs MW

150GeVM

ln0.0003250GeV

175GeVM0.00022θδsin H

2

22tshell)(On

W2

One-loop correction to sin2W

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

8

Oscillation Probability• Substituting the energies into the wave function:

E

tmiE

mpitt 2expcossin2exp22

121

where and .22

21

2 mmm pE

• Since the ’s move at the speed of light, t=x/c, where x is the distance to the source of .

• The probability for with energy E oscillates to e at the distance L from the source becomes

E

LmP e

222 27.1

sin2sin

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

9

Why is Neutrino Oscillation Important?• Neutrinos are one of the fundamental constituents in nature

– Three weak eigenstates based on SM• Left handed particles and right handed anti-particles only

– Violates parity Why only neutrinos?– Is it because of its masslessness?

• SM based on massless neutrinos• Mass eigenstates of neutrinos makes flavors to mix• SM in trouble…• Many experimental results showing definitive evidences of

neutrino oscillation– SNO giving 5 sigma results

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

10

Sources for Oscillation Experiments• Must have some way of knowing the flux

– Why?• Natural Sources

– Solar neutrinos– Atmospheric neutrinos

• Manmade Sources– Nuclear Reactor– Accelerator

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

11

Oscillation Detectors• The most important factor is the energy of neutrinos

and its products from interactions• Good particle ID is crucial• Detectors using natural sources

– Deep under ground to minimize cosmic ray background– Use Cerenkov light from secondary interactions of

neutrinose + e e+X: electron gives out Cerenkov light CC interactions, resulting in muons with Cerenkov light

• Detectors using accelerator made neutrinos– Look very much like normal neutrino detectors

• Need to increase statistics

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

12

Solar Neutrinos• Result from nuclear fusion process in the Sun• Primary reactions and the neutrino energy from

them are:

eLieBe 77

158B

0.867Be

1.44pep

0.42pp

E End point (MeV)ReactionName

eeDpp

eDpep

eeHeB 48 2

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

13

Solar Neutrino Energy Spectrum

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

14

Comparison of Theory and Experiments

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

15

Sudbery Neutrino Observatory (SNO)•Sudbery mine, Canada•6800 ft underground•12 m diameter acrylic vessel•1000 tons of D2O•9600 PMT’s

Elastic Scattering

Neutral Current

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

16

SNO e Event Display

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

17

Solar Neutrino Flux

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

18

SNO First Results

0.35

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

19

Atmospheric Neutrinos• Neutrinos resulting from the atmospheric

interactions of cosmic ray particles to e is about 2 to 1– He, p, etc + N ,K, etc

e+e+

– This reaction gives 2 and 1 e

• Expected flux ratio between and e is 2 to 1• Form a double ratio for the measurement

The

Exp

NN

NN

R

e

e

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

20

Super Kamiokande•Kamioka zinc mine, Japan• 1000m underground•40 m (d) x 40m(h) SS•50,000 tons of ultra pure H2O•11200(inner)+1800(outer) 50cm PMT’s•Originally for proton decay experiment•Accident in Nov. 2001, destroyed 7000 PMT’s•Dec. 2002 resume data taking

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

21

Atmospheric Neutrino Oscillations

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

22

Super-K Atmospheric Neutrino Results

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

23

Super-K Event Displays

Stopping 3

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

24

Other Experimental Results

Soudan 2 experiment

Macro experiment

Monday, Feb. 24, 2003 PHYS 5326, Spring 2003Jae Yu

25

Accelerator Based Experiments• Mostly from accelerators• Long and Short baseline experiments

– Long baseline: Detectors located far away from the source, assisted by a similar detector at a very short distance (eg. MINOS: 370km, K2K: 250km, etc)

• Compare the near detector with the far detector, taking into account angular dispersion

– Short baseline: Detectors located at a close distance to the source

• Need to know flux well

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