Title: Cosmic Conclusions
1Cosmic Conclusions
David Gerstle LArTPC Yale University
Undergraduate
2Outline
- How do we get a particles/m2/s number?
- Detector location information
- J(gtE) (m2 s sr)-1
- Angular distribution
- Math
- The numbers
- What does that number mean for a given detector
size and live-time? - Are these numbers accurate?
- How does the muon flux and track length affect
us? - Conclusions and further questions
3Effect of Detector Location
- The two values associated with a location which
most affect the flux are the atmospheric depth
(g/cm2) and geomagnetic cutoff (GV). - Greater the atmospheric depth, lower the flux.
The depth is intimately related to the altitude. - Greater the geomagnetic cutoff value, lower the
flux. GCV is the least value of kinetic energy
divided by charge a primary cosmic ray must have
to get through the Earths magnetic field. It is
closely related to latitude (for the geomagnetic
field varies with latitude). - Soudan 990 g/cm2 at 400m altitude 1.0 GV at
47N.
4Need a J(E) (m2 s sr)-1 and Angular
Distribution
- J(E) is the vertical flux of particles above an
energy E. - What value of E should we use?
- 0.3 GeV/c muons travel 1m in LAr.
- As this 1m is (probably) the shielding LAr we
will end up having, 0.3 GeV/c (0.2 GeV KE) is a
good value for E. - 0.5 GeV is the lower limit of photon events of
interest for a detector which is in a beam I
used this value for photons. - Generally accepted to be cosn?
- J(E)cosn?, admittedly, is a poor model for the
shape of J(E,?). - However, the area (with respect to d?) under
J(E)cosn? is very close to the area under
J(E,?), so I have used J(E)cosn?. - Even though they have different shapes,
J(E)cosn? is a fine approximation for how we are
using it.
5Math
J(E)
- Horizontal Surface
- Vertical Surface
Formula used in spreadsheet
6Numbers I Use
n
muon J(gt0.3 GeV/c) (m2 s sr)-1 8.87E01 2.16
muon Kranshaar (1949) 53N, 1.6 GV, 259m Kranshaar (1949) 53N, 1.6 GV, 259m Crooks Rastin (1972) 53N, gt0.35 GeV/c
photon J(gt0.5 GeV) (m2 s sr)-1 9.02E-01 3
photon Pugacheva et al., (1973) and Palmatier (1952) Pugacheva et al., (1973) and Palmatier (1952) Kameda (1960), Beuermann and Wibberenz (1968)
Photon values are adjusted from photon data
Note a factor of 100 between muon and photon
flux FOR THESE values of E
- Recall Soudan 990 g/cm2 at 400m altitude
1.0 GV at 47N. - All citations were found within Grieder, P.K.F.
Cosmic Rays at Earth. Amsterdam Elsevier
Science, 2001. A spectacular book.
7Results for gt0.3 GeV/c muons and gt0.5 GeV photons
Time bin (s) Diameter (m) Height (m)
2.00E-03 35 35
Horizontal (m2 s)-1 Horizontal s-1 Vertical (m2 s)-1 Vertical s-1 TOTAL s-1 TOTAL
muon 1.34E02 1.29E05 3.25E01 1.25E05 2.54E05 5.08E02
photon 1.13E00 1.09E03 2.40E-01 9.24E02 2.01E03 4.03E00
- Recall that Horizontal means through a
horizontal surface and similarly for Vertical. - Note that as photon energy increases, the flux
rapidly decreases using a smaller value of E in
J(gtE) will significantly increase the total
photon flux.
8Are these Muon Numbers Accurate?
- PDG quotes a muon integral flux through a
horizontal surface as being 1 (cm2 min)-1
170 (m2 s)-1 - I calculated 130 (m2 s)-1 for Egt0.3 GeV/c.
- The difference is accounted for by recognizing
PDG to have used Emin effectively 0 in J(gtE).
Linear Scale
0.3 Gev/c
9Are these Photon Results Accurate?
- It is key that we know what E value to use
because the curve is so steep.
dN/dE
J(gtE)
10How does the muon flux affect us?
- Yellow curve is Horizontal and Teal curve is
Vertical N(gtE)x(p), where x(p) is the path
length of a muon in LAr (from a dE/dx
calculation). - Nhor(gt0.3 GeV/c)x(gtp) 1800 particle meters per
meter2 per second. - Nvert(gt0.3 GeV/c)x(gtp) 450 particle meters per
meter2 per second. - 35m by 35m cylindrical detector and 2 millisecond
drift-time yields 7000 particle meters during
each live-time.
11Conclusions and further Questions
- All calculations were done in Excel the file is
in the LArTPC DocDB 160 CosmicConclusions.xls - We might consider buying a copy of Mr. Grieders
250 book. - Need to determine the effect of these numbers on
the data acquisition system. - These data are with respect to a Soudan, MN
detectorshould we consider another surface
location? - Lower latitude and altitude would reduce flux.
- Is there reason to use a different value for E in
J(gtE) for muons and/or photons? - Do we need to accurately model the shape of
J(E,?)? - Can we mathematically model the effect of the
geomagnetic cutoff? Do we need to?