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STATUS OF THE ABSORPTION LENGTH MEASUREMENT ANTARES collaboration meeting Clermont-Ferrand (France), May 17th-20th 1 H Yepes, JdD Zornoza, J Zuñiga, C.

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Presentation on theme: "STATUS OF THE ABSORPTION LENGTH MEASUREMENT ANTARES collaboration meeting Clermont-Ferrand (France), May 17th-20th 1 H Yepes, JdD Zornoza, J Zuñiga, C."— Presentation transcript:

1 STATUS OF THE ABSORPTION LENGTH MEASUREMENT ANTARES collaboration meeting Clermont-Ferrand (France), May 17th-20th 1 H Yepes, JdD Zornoza, J Zuñiga, C Bigongiari, J Ruiz IFIC (CSIC – Universidad de Valencia)

2 THE EXPERIMENTAL PROCEDURE (REMINDER) NEW TREATMENT OF ERRORS: DATA FITTING EXTRACTION OF ABSORPTION LENGTH CONCLUSIONS AND OUTLOOK OUTLINEOUTLINE ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 2

3 EXPONENTIAL FIT 1. THE EXPERIMENTAL SETUP: One single top LED of the lowest optical beacon in the line flashes to the upper storeys, then the signal hits can be plotted and fitted by means of an exponential function, once quality cuts are applied. The collected hits are a convolution of: Physics: Absorption length ( L abs ) Scattering ( L sca and  =  (  )) Detector: OB – OM relative orientation OM efficiency ARS token ring dead time Charge resolution To minimize the effects of the detector: Only OMs in the same line are considered. Consider only the region (R min, R max ) where signal < spe but well above background THE EXPERIMENTAL PROCEDURE ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th F2 3

4 N noise T max T min Nsignal 2. TIME DISTRIBUTION: Determine the peak  Gaussian fit Choose a fixed time window [T min, T max ] and select the hits: T min = T peak – 3  T max = T peak + 1000 ns Calculate their overall charge Q hits and N hits. 3. NOISE CONTRIBUTION: Fit a constant in the [-1000, -50] ns range (B level ) and substract the noise contribution (Q noise, N noise ): N signal = N hits(tot) – N noise = N tot – B level (T min - T max ) NOISE LEVEL THE EXPERIMENTAL PROCEDURE ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 4

5 4. CHARGE LOSSES: Some hits are lost due to the electronic dead time from the readout of the ARSs. Effect related to R min. Consider only the region where the probability to get more than one photoelectron is negligible (i.e. < 1 %). 5. PMT EFFICIENCY CORRECTION BY NOISE: Assume that the N noise ~  PMT Normalize PMTs signal to their own noise (hits or charge): THE EXPERIMENTAL PROCEDURE ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 5

6 6.NOISE FLUCTUATIONS: To avoid noise fluctuations at large distances, signal greater than the noise is required  Maximum distance to fit R max. 7.MEASUREMENT OF ERRORS: The estimation of statistical and dispersion errors are being carefully studied for the data:  Each storey provides 3 intensity measurements.  These measurements are not treated independently, correlated errors can be obtained. 8.LOW EFFICIENCY OMs CLEANING: Low efficiency OMs are removed. Checked from noise plots  Compute hits projections, fit a Gaussian and consider only OMs between (  +3 ,  -3  ). 9.THE BACKGROUND “FLATNESS”: Efficiency correction by noise is affected by noise fluctuations along the line  A “flat” level noise along the line required. THE EXPERIMENTAL PROCEDURE ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 6

7 Then the variable follows Student’s t distribution: with ν = n–1 degrees of freedom Therefore the error is taken to be: σ = t ∙ s/√n In order to have 68.27% errors, the one-side tail of the cumulative Student function must be 84.13% and thus t= 1.32 (for n=3) or t=1.83 (for n=2). If only one OM in the storey do not use that storey in the fit. NEW TREATMENT OF ERRORS: DATA FITTING ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 7 Each storey provides 3 intensity measurements (3 OMs). Assume these measurements are independent and gaussian distributed (check this hypothesis later with results). Assign one signal intensity per storey computed as the average of the 3 OMs – OM signal extraction as before: subtract background, correct by efficiency, discard bad OMs Compute error by means of Student’s t (this is the usual treatment for the estimation of the mean and standard deviation of a gaussian distribution when none of the two parameters are known): NEW TREATMENT OF ERRORS:

8 NEW TREATMENT OF ERRORS: DATA FITTING ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 8 SOME NEW FIT EXAMPLES (t-STUDENT TEST): Some errors give low - high values for  .  ↓,  2 ↑, forces to fit for this point, deforming the tendency. L2 L12

9 NEW TREATMENT OF ERRORS: DATA FITTING ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 9 TRANSMISSION LENGTH RESULTS: Blue UV Blue UV

10 NEW TREATMENT OF ERRORS: DATA FITTING ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 10 TRANSMISSION LENGTH RESULTS: Blue UV Blue UV

11 NEW TREATMENT OF ERRORS: DATA FITTING ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 11 The mean value of the distribution of the L errors from the fits shows a good agreement with the RMS of the transmission length distribution (Blue: 3.0m vs 2.4m, UV: 2.1 vs. 1.1): = 470 nm = 400 nm

12 NEW TREATMENT OF ERRORS: DATA FITTING ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 12 Blue  = 470 nm) Student’s t error values Entries 29 L ± RMS[m] 55.1±3.0 Average σ fit (RMS) [m] 2.4 (0.9) Mean Prob (  2 ) (RMS) 0.66 RMS Prob (  2 ) 0.36 Entries with Prob (  2 ) < 1% 1 UV ( = 400 nm) Student’s t error values Entries 13 L ± RMS[m] 38.1±2.1 Mean σ fit (RMS) [m] 1.1 (0.6) Mean Prob (  2 ) 0.61 RMS Prob (  2 ) 0.31 Entries with Prob (  2 ) < 1% 0 Reasonable fit probabilities Variability of L ~6% (RMS/L): RMS of L in agreement with average σ fit : 3.0 m vs 2.4 m Change of L with time not much larger than statistical Somewhat high probabilities: cluster close to 1 and Mean Prob (  2 ) = 0.66 (should be 0.5) RMS Prob (  2 )=0.36 (should be 1/√12=0.29) Good fit probabilities Variability of L around 6% (RMS/L): RMS of L distribution in agreement with average σ fit :2.1 m vs. 1.1 m Small cluster at high probabilities: Mean Prob (  2 ) = 0.6 (should be 0.5) RMS Prob (  2 )=0.31 (should be 1/√12=0.29) What errors would give a flat Prob (  2 ) (assuming they are the same at all distances) for the blue runs? Answer: 5% relative errors FITTING TRANSMISSION LENGTH: RESULTS

13 NEW TREATMENT OF ERRORS: DATA FITTING ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th EQUAL ERROR ASSIGNMENT FOR ALL THE EXPERIMENTAL POINTS (σ/x = 0.05): 13 Blue UV Blue UV

14 NEW TREATMENT OF ERRORS: DATA FITTING ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th EQUAL ERROR ASSIGNMENT FOR ALL THE EXPERIMENTAL POINTS (σ/x = 0.05): 14 Blue UV Blue UV

15 NEW TREATMENT OF ERRORS: DATA FITTING ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th For an equal error assignment (5 %), once again good agreement with the RMS of the transmission length distribution: = 470 nm = 400 nm 15

16 NEW TREATMENT OF ERRORS: DATA FITTING ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 16 Blue  = 470 nm) Fixed 5% relative errors Entries 29 L ± RMS[m] 54.5±2.4 Average σ fit (RMS) [m] 1.9 (0.3) Mean Prob (  2 ) (RMS) 0.46 RMS Prob (  2 ) 0.33 Entries with Prob (  2 ) < 1% 2 UV ( = 400 nm) Fixed 5% relative errors Entries 14 L ± RMS[m] 37.1±1.2 Mean σ fit (RMS) [m] 0.7 (0.1) Mean Prob (  2 ) 0.37 RMS Prob (  2 ) 0.36 Entries with Prob (  2 ) < 1% 3 Not a significant change in L (55.1 vs 54.5) Average σ fit is slightly lower than RMS of distribution (1.9 vs 2.4), but not much room for non-statistical variability Not a significant change in L (38.1 vs 37.1) Average σ fit is slightly lower that RMS of distribution (0.7 vs 1.2), but not much room for non-statistical variability  L (t-5%) < 1m

17 ΔR can be extracted from time distributions !!! tt EXTRACTION OF ABSORPTION LENGTH ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th SCATTERING CONTRIBUTION TO THE TRANSMISSION LENGTH ( L ) (“  R technique”): The effect of scattering is to increase the photon path length in ΔR on average. Perform the exponential fit using ( mean photon path ), R + ΔR instead of R. R ΔRΔR R+ΔR ΔR should be proportional to the scattering. Exponential fit with R + ΔR will be more insensitive to scattering since the greater the scattering the greater the delay and viceversa, making the L parameter closer to the real absorption length. 17

18 EXTRACTION OF ABSORPTION LENGTH ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th Parameterization of  R for MC: Extracting  R from the time distributions gives a linear dependence of R+  R on R, both for MC and data. The values of the above slopes are then related to the Rayleigh scattering (  ). MC simulations can give an idea about the scattering contribution, from the relationship between R +  R and R: R +  R = p0+p1*R (p  depends on scattering) Correlation between R and R+  R 18 Parameterization factor distributions

19 EXTRACTION OF ABSORPTION LENGTH ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 19 Transmission length ( L ) dependence on scattering parameters,  and scat (no corrected by  R): L depends on scat,eff. Almost constant if scat,eff ↑ (parameterization is needed). L- scat,eff (by 

20 EXTRACTION OF ABSORPTION LENGTH ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 20 L is strongly correlated to scat. Low values of scat, gives low values for L. (same color->same  ). L shows an anti-correlation with . High values of  give low values of L (same color -> same scat ).  SCATTERING EFFECTS ARE MOST REMARKABLE AND EVIDENT  L- scat (by  ) L-  (by scat ) Transmission length ( L ) dependence on scattering parameters,  and scat (no corrected by  R):

21 EXTRACTION OF ABSORPTION LENGTH ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 21 L → constant if scat,eff ↑ ( scat,eff > 150 m) L- scat,eff (by  L- scat,eff (by sca  Transmission length ( L ) dependence on scattering parameters,  and scat (corrected by  R):

22 EXTRACTION OF ABSORPTION LENGTH ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 22 MC transmission length ( L ) plots for dependence on  and scat (corrected by  R): When L is corrected by  R, there is not much dependence on the tested water parameters, except for extreme models. Intermediate values for scat (~50 m) and low values for  (0.14), gives the nearest value for L to abs. L- scat (by  ) L-  (by scat )

23 EXTRACTION OF ABSORPTION LENGTH ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th Parameterization constant (p1) as a function of scattering length and effective scattering length (  - scattering length): A dedicated study of the correct parameterization of  R, is actually ongoing in order to reach the best estimation in MC and then to be implemented the technique for data. Parameterization constant “p1” is correlated to scat and then to scat,eff for different  considered. For different scat, p1 has also a strong dependence to scat,eff. 23 p1- scat p1- scat,eff (by scat )

24 EXTRACTION OF ABSORPTION LENGTH ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th L with  R parameterization  MC L without  R correction  MC 24 New results of  R technique for MC simulations: Fitting L to seems to “recover” abs, with some small constant shift Some cross-overs in the p1 dependence on the input parameters seems to point out the need of more statistics (ongoing !). Results for data soon !!!  L (R-R+  R) ~ 4 – 5 m

25 CONCLUSIONS AND OUTLOOK ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th DATA FITTING: New method based on averaging the OM signals of each storey and computing the error using the Student t distribution gives reasonable χ 2 values both for blue and UV light. The “transmission length” is rather stable in time for both wavelengths and the RMS of its distribution is close to the average σ fit, therefore there is not much room for the variation of L due to changes in the medium (at least for the type of runs we use, i.e. low background periods). There are a few cases of bad fits (due mostly to one single point with very small error) and a tendency towards too high probabilities (overestimate of errors). If the errors in all the storeys are fixed by hand to 5% we get a flatter Prob( χ 2 ). In any case, the change in the computed transmission length is small (ΔL ≤ 1m). The stability in time and reproducibility of the transmission length (with different errors, for different lines, with different LEDs) gives confidence in the analysis. However, we will continue investigating possible systematic effects. 25

26 CONCLUSIONS AND OUTLOOK ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th EXTRACTION OF ABSORPTION LENGTH : Assuming that most of the effect of the scattering length in the transmission length comes from the increased path length (“ΔR”) of photons, this additional path length can be extracted from the time distribution as a function of distance. A corrected transmission length can be computed inputting R+ ΔR in the fits (instead of R). The corrected value of scat does not depend strongly on the input water parameters, except for extreme models. New runs with other values of the input abs and more statistics are underway to check the stability of the method. 26

27 27 BACKUP SLIDES

28 ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 28 STUDENTS t DISTRIBUTION: A

29 BACKUP SLIDES ANTARES collaboration meeting Clermont-Ferrand, May 17th-20th 29  2 DISTRIBUTION: A


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