@article{oai:repo.qst.go.jp:00046871,
 author = {Tajika, Yukari and Yasuoka, Yumi and Hiroyuki, Nagahama and Suzuki, Toshiyuki and Homma, Yoshimi and 石川, 徹夫 and Tokonami, Shinji and Mukai, Takahiro and ミロソラフ, ヤニック and Sorimachi, Atsuyuki and Hosoda, Masahiro and et.al and 石川 徹夫 and ミロソラフ ヤニック},
 issue = {3},
 journal = {Journal of Radioanalytical and Nuclear Chemistry},
 month = {Mar},
 note = {Gas-flow ionization chambers for radioisotope (RI) monitoring systems at RI institutes throughout Japan are commonly used to measure RIs which leak from the RI institutes. Before the Japan’s 2011 Tohoku earthquake [11 March 2011, moment magnitude (M w) 9.0], ionization current data measured with a gas-flow ionization chamber at the RI institute of Fukushima Medical University were found to change. The question we must raise is whether the variation ionization current can be considered to the variation of outdoor radon concentration. The conversion factors (from ionization current to radon concentration in air) of the gas-flow ionization chamber can be obtained by measuring four levels of radon concentration (outdoor air, indoor air, high level and radon-free gas) with an AlphaGUARD monitor and the chamber itself. The two gas-flow ionization chambers consist of the air intake and terminal exhaust duct of the RI institute. It was found that the radon concentration in the exhaust air was the same as that in the air intake. This study provided evidence that variations of outdoor radon concentration could be determined using gas-flow ionization chambers for RI monitoring systems.},
 pages = {1709--1714},
 title = {Radon concentration of outdoor air: measured by an ionization chamber for radioisotope monitoring system at radioisotope institute},
 volume = {295},
 year = {2013}
}