LONG-TERM MONITORING OF THE ONBOARD AIRCRAFT EXPOSURE LEVEL WITH Si-DIODE BASED SPECTROMETER ) F. Spurný (1), Ts. Dachev (2)

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Paper F2.4-7 presented at 4 th COSPAR Assembly, Houston TX 1-19 Oct. 22 LONG-TERM MONITORING OF THE ONBOARD AIRCRAFT EXPOSURE LEVEL WITH Si-DIODE BASED SPECTROMETER ) F. Spurný (1), Ts. Dachev (2) (1)Nuclear Physics Institute, Czech Acad. Sci., Prague, Na Truhlařce 9/4, 188 Praha 8, Czech Republic (2) Solar Terrestrial Influence Laboratory, Bulg. Acad. Sci., Sofia, Acad. G. Bonchev St., 111 Sofia, Bulgaria ABSTRACT The radiation fields on aircraft board are complex, they contain the particles with energies up to few hundreds MeV [1]. There are different methods used to characterise this field for radiation protection purposes. We tried to test for such purposes a spectrometer based on Si-diode, largely tested at different sources and accelerator facilities. The energy deposited in the diode by a particle is analysed and permits to distinguish the contribution of different types of radiation to integral dosimetry quantities. During 21-22 years, the spectrometer was used to measure on board of commercial aircraft during five long-term exposures. It was found that the spectrum of energy deposition events onboard of aircraft is similar to that registered in CERN high-energy reference fields behind the concrete shield. We used this similarity to determine the correction factors to estimate radiation protection quantities from the results of onboard measurements. All necessary flight parameters were acquired, it permitted to calculate the effective dose and/or ambient dose equivalent on board by means of CARI- and EPCARD codes and compared them with the results of measurements treated as mentioned above. It was found that the apparent ambient dose equivalent values from measured data are in reasonable agreement with the results of calculation. Quantitative analysis of this agreement as a function of flight parameters (geomagnetic position, solar activity variations, etc.) is presented. During one of flights, an important solar event (GLE at the 15 th April 21) was registered by means of the spectrometer. In some other cases the measurements during forbush decreases were also realized. These extremes were well registered by the equipment and the data obtained are also analyzed. The contribution of events with high E dep is relatively more important during GLE, less important during forbush decreases. The semiconductor spectrometer proved we believe its possibility to characterise dosimetric characteristics of complex radiation fields on aircraft board. Further effort would improve its performance. MATERIALS AND METHODS Detector used, mobil dosimetry unit The Mobile Dosimetry Unit (MDU) can monitor simultaneously the doses and numbers of energy deposition events in a semiconductor Si-detector. It is designed as handy equipment. The amplitude of the pulses is proportional to the energy loss in the detector. Final adjustment of the energy scale is made through the kev photons of 241 Am. The amplitudes are digitised and organised in a 25-channel spectrum. The dose D [Gy] is calculated from the spectrum as: D = K.*Σ(E i *A i )/MD, where MD is the mass of the detector in [kg]; E i is the energy loss in the channel i; A i is the number of events in it; and K is a coefficient. The operational time of the instrument depends on the lifetime of the accumulators and on the rate of the memory fills up. In the case of continuous operation the lifetime is about 12 hours with the 1.5 Ah accumulators, about 14 hours with 14 Ah-batteries ) The studies were partially supported through EC Project FI5P-CT-8 and the Projects of the Grant Agency of Czech Republic Nos. 22/99/151 and 22/1/71 1

Calibrations, onboard tests MDU units available were exposed in reference radiation fields. The results obtained at some photon sources are presented in Fig.1. Not only experimental but also theoretical event spectra in the semiconductor are presented there for 17 Cs and Co photons. They were calculated by means of EGS 4-transport code and one can see that the agreement of both spectra is rather satisfactory. The equipment was also exposed at some neutron sources. Rather large difference in the event spectra were observed. While for photons the maximum impulsion s height is about 1 MeV, for neutrons it reaches up to 1 MeV []. It could permit to distinguish photon and neutron induced events in other radiation fields. Tests with MDU units were performed on protons and heavy ions [2,4] and good agreement was found between the measured and predicted by the GEANT code simulations spectra. Fig. 1: Event spectra in some photon beams Fig. 4: Comparison of dose spectral distributions MDU units have been tested since the spring 2 during three calibrations runs in the CERN- EC high-energy reference field behind the concrete shield [5]. It should be stressed that in this case the spectrum was still much larger than in the case of neutron sources, reaching the highest values of the energy deposition above 2 MeV. It was found that the signal per monitor unit decreases in low E dep region with increasing intensity, due to muon background [5]. For high E dep events, it is independent of the intensity given by monitor units. It is very important for the interpretation of the data measured in reference and similar fields. As far as the values of dose calculated from the spectra are concerned, they were in very good agreement with the reference values for Co photons, the value obtained for 17 Cs photons was about 8 % lower than the reference one. In CERN reference field, the dose calculated for low E dep region were about % lower than values measured with other standard low LET measuring instruments (RSS 112 chamber, TLD s, etc.). We have observed the same behaviour also for individual electronic dosemeters based on Si-diode and taken it into account for the interpretation of these detector s readings. Main effort was given to the measurements on aircraft board and their interpretation. First, it was actually observed that the spectra registered at CERN reference field are very similar to the spectra registered on the aircraft and/or balloon (see Fig.2). To interpret the data measured on aircraft board (D(Si)), we decided to use CERN reference field results. The dose in Si measured in low E dep region was supposed to represent the contribution of low LET radiation, the dose in high E dep region that of high LET component (neutrons). Taking into account reference fields values for these components [5], D(Si) measured on board was recalculated to obtain apparent H*(1) values. Since the April 2, the spectrometer has been used during more than 5 individual and five long-term exposures, about 12 hours each, with about 4 flights in total. All necessary flight parameters were acquired from colleagues of Czech Airlines, that permitted to calculate the effective dose E on board by means of CARI and EPCARD codes and compare them with the apparent H*(1) values obtained as mentioned above. As an example for individual flights, the results obtained in the case of CSA flights from Prague to Athens and return are presented in Figs. and 4. 2

8 Flight profile PRG-ATH 19/5 12. Flight profile ATH-PRG 2/5 12 Hlow Htot altitude Hhigh CARI 9 4.5 Hlow Htot altitude Hhigh CARI 9 H(E) rates, Sv/h 4 Altitude, km H(E) rates, Sv/h. Altitude, km 2 1.5..5 1. 1.5 2. 2.5 Flight time, hours Fig. : Flight profiles Prague-Athens. 5:1 5:45 :14 :4 7:12 7:4 UTC Fig. 4: Flight profiles Athens -Prague Characteristics at quiet cosmic environment RESULTS AND DISCUSSION More detailed characteristics of long-term measurements are given in the Table 1, the record of detectors data for one of them is presented in the Figure 5. Table 1: Characteristics of long-term onboard aircraft monitoring realised in 21-22 with LIULIN semiconductor spectrometer. Period Returned flights monitored *) Total flight numbers 22/-7/5/1 PRG-NY(25), PRG-TOR(1), PRG-DUB() 18 /5-24/7/1 PRG-NY(41), PRG-TOR(12) 125 29/8-1/1/1 PRG-NY(2), PRG-TOR(1), PRG-DUB(2) 9 25/1-1/12/1 PRG-NY(2), PRG-TOR(7), PRG-AMS(1) 7 /5-28//2 PRG-NY(22), PRG-TOR(1), PRG-DUB(8), PRG- LHR(5), PRG-MAD(5) 124 *) PRG Prague, NY New York, TOR Toronto, DUB Dubai, AMS Amsterdam, LHR London, MAD Madrid Figure 5: Record of measurements for the period /5-25/7/1

One can see there that about 5 individual flights were monitored, mostly over the North Atlantic. Figure 5 demonstrates also, how tight was flight schedule of the aircraft during the period of measurements, only three one-day interruptions can be registered in the record. Similar was the schedule also for other long-term runs, with the exception of periods during and after 11 th September event. CSA colleagues submitted us navigation data on all flights. It permitted to calculate the total exposures during them and compare calculated data with results obtained by means of procedure mentioned above. The results obtained up to now for integral values of dosimetric quantities are presented in the Table 2. Table 2: CSA aircraft (A1-) long-term exposures 21 comparison of calculated and MDU results treated using CERN calibration. Flight period during 21 year 22/-7/5 /5-24/7 29/8-1/1 25/1-1/12 CARI E, msv total 2.8.78 2. 1.88 EPCARD. neutrons 1.57 2.12 1.45 1. H * (1) others 1.8 1.4 1.5.72 msv total 2.8.52 2.5 1.72 EPCARD. neutrons 1.4 1.82 1.24.85 E-ISO others 1.77 2.9 1.7 1.17 msv total.11 4.1 2.94 2.2 Liulin-MDU neutrons 1.54 2.29 1.55 1.7 H app others 1.14 1.54 1.4.72 msv total 2.5.8 2.59 1.78 One can see that the data sets agree very well, only the values of effective dose are, when EPCARD code is used, a little, in average by 12 %, higher. Such difference is from the point of view of radiation protection largely acceptable [5]. The data from log-term measurements were also treated in the same way as for individual flights. The examples of flight records are presented in Figures and 7. Fig.: Flight profiles New York Prague Fig.7: Flight profiles Bahrajn - Prague One can see there again that the values of total apparent H*(1) are in rather good agreement with the E-values calculated by means of CARI code. Such tendency was observed in all about 4 flights treated in the same way, the average relative uncertainties of the differences between calculated and treated measured data did not exceeded 1 %. Characteristics during extremes in the cosmic environment 4

During the 1 st monitoring period, several colleagues informed us that an intense solar flare, Ground Level Event (GLE), numbered, occurred after the noon of 14 th April. The Si-spectrometer was taken away only the 7 th May to assure sufficiently high exposure of passive detectors irradiated with it. We have really observed a maximum in full record (Fig.8) situated at the 15 th April, its zoom (Fig.9) demonstrate that solar flare took place roughly hours after the taking off from Prague to New York. A good time and form-correlation s of our measurements with independent data available from Oulu (Finland) cosmic ray monitor station and/or from the GOESS system satellites was also confirmed as shown in the Figure 1. Fig.8: Record of measurements, period 22/-7/5/1 Fig.9: Zoom of the record, 14-1/4/1 1. Si Dose Rate (ugy/h) 4 2 9E+ 8E+ Event rate Dose rate HEPAD Oulu NM 5E- 4E- E- 1.5 1.4 1. 1.2 1.1 1..9.8 Event rate (cm^-2 s^-1) 1 Oulu NM counts 7E+ E+ 5E+ 2E- 1E- HEPAD@GOES-8 >85 MeV protons (cm^-2 s^-1 sr^-1) 1. 14. 15. 1. 17. Universal time Fig. 1: Correlation of spectrometer and other data Fig.11: Lomnicky stit monitor data 4 and 11/1 Another extremes occurred also during 21 year, so called forbush decreases. Particularly important there were at 12t h April and th November, as can be seen in records of Lomnický štít cosmic ray monitor data presented in the Fig.11. During them the intensity decreased rapidly by more than 1 %, it would be reminded that the geomagnetic rigidity of Lomnický štít monitor is about.9 GV. Fortunately, also during these extremes our spectrometer was flying on the board of aircraft. The aircraft with the Si-spectrometer was at the both dates mentioned flying roughly at the same time as for GLE also from Prague to New York. We treated directly measured data in the same way as for other flights and compared them with the results of calculation by means of EPCARD.1 code [7]. The results of such comparison are presented in the Table. One can see there that solar flare and forbush decrease influence the exposure level both quantitatively and qualitatively. Total exposure is 5

for GLE about 44 % higher, for forbush decrease about 1 % lower. Besides, the influence is more important for high LET (neutron) radiation component. The changes observed seem to indicate that the neutron spectrum is softer during a solar flare, harder during the forbush decrease. It would correspond to the expectation. Table 2: The influence of extremes on the exposure level measured on aircraft board Flight Ratio MDU /EPCARD, H*(1) low LET high LET total PRG-JFK, 14/4 - quiet 1 1..9.98 JFK-PRG, 1/4 - quiet 2 1.1 1.1 1.1 PRG-JFK, 15/4 - with GLE 1.24 1.8 1.44 PRG-JFK, 12/4 - forbush 1.92.78.84 PRG-JFK, /11 - forbush 2.89.85.87 CONCLUSIONS 1. The semiconductor spectrometer proved according our opinion its capability to characterise dosimetric characteristics of complex radiation fields on aircraft board. Simplicity of its use and general reliability permits to perform also long-term onboard monitoring. 2. Its spectrometric properties seem to allow, together with well-chosen interpretation procedure, to obtain both qualitative and quantitative characteristics of onboard radiation fields.. These properties were able to estimate both quantitative and qualitative changes also during a solar flare and sufficiently intense forbush decreases. 4. Of course, additional effort is needed to improve its performance and to estimate still more quantitatively the validity of all approaches presented and tested. Among them: Further data on board should be accumulated, particularly in equatorial regions; Common measurements with a reference tissue-equivalent proportional counter and other instruments should be realised to compare directly masured and interpreted data. Further calibration of it in the CERN-EC reference fields is necessary. All these approaches are in further progress in our laboratories. REFERENCES 1. EURADOS, Exposure of air crew to cosmic radiation, EURADOS Report 199-1, eds.: McAulay I. et al., Luxembourg, (199), 1-77. 2. Dachev, Ts.P., Spurný, F. et al.: Calibration Results Obtained with LIULIN-4 Type Dosemeter. Paper F2.2-25 presented at rd General Assembly of COSPAR, Warsaw, Poland, July 2.. Spurný F., Dačev C.: Aircrew onboard Dosimetry with a Semiconductor Spectrometer ; paper presented at the 1 th Inter.Conf. Solid State Dosimetry, Athens, July 21, accepted for publication in the journal Radiat.Prot.Dosim. 4. Uchihori, Y., Kitamura, H., Fujitaka, K., Dachev, Ts.P., Tomov, B.T., Dimitrov, P.G., Matviichuk, Y.: Analysis of the Calibration Results Obtained with Liulin-4J Spectrometer- Dosimeter on Protons and Heavy Ions ; Radiation Measurements, 5 (22), 127-14. 5. Mitaroff A., Silari M.: The CERN-EU high-energy Reference Field (CERF) facility for dosimetry at commercial flight altitudes and in space, CERN-TIS-21--RP-PP.. Friedberg, W. Snyder, D.N. Faulkner: Radiation Exposure of Air Carrier Crew Members II ; US FAA Report DOT/FAA/AM-92-2, 1992 7. Roesler S., Heinrich W. and Schraube H., Monte Carlo Calculations of the Radiation Field at Aircraft Altitudes, Radiat. Res., in press, 22. Acknowledgements The authors are also much obliged to colleagues from Czech Airlines for the assistance in long time exposure on CSA aircraft board, they are much obliged to CERN staff for the help during calibration in reference fields. They would like also to express their thanks to colleagues from BAS laboratory (B. Tomov, Yu. Matviichuk, and Pl. Dimitrov) for their assistance during the equipment preparation and continuos technical support.