Promotion of the lower limit of detection of gamma emitting nuclides in radioaerosol samples after Fukushima accident

Abstract Through placement in a few hours after collecting radioaerosol samples (in Shanghai) after Fukushima nuclear power plant (NPP) accident, radionuclides with gamma-emitting rays can be found to be nuclides (132I/132Te, 129I/129Te) other than 131I, 134,137Cs because of the decrease in backgrou...
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Autor*in:	Wang, Jinglong [verfasserIn] Jiang, Yifei [verfasserIn] Huang, Dekun [verfasserIn] Wen, Tingyu [verfasserIn] Du, Jinzhou [verfasserIn] Zhang, Jing [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2011

Schlagwörter:	The lower limit of detection Gamma-ray emitting nuclides Radioaerosol Fukushima nuclear accident

Übergeordnetes Werk:	Enthalten in: Journal of radioanalytical and nuclear chemistry - Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968, 292(2011), 3 vom: 30. Dez., Seite 1297-1301
Übergeordnetes Werk:	volume:292 ; year:2011 ; number:3 ; day:30 ; month:12 ; pages:1297-1301

Links:	Volltext

DOI / URN:	10.1007/s10967-011-1594-9

Katalog-ID:	SPR015177866

Internformat


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100	1		\|a Wang, Jinglong \|e verfasserin \|4 aut
245	1	0	\|a Promotion of the lower limit of detection of gamma emitting nuclides in radioaerosol samples after Fukushima accident
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520			\|a Abstract Through placement in a few hours after collecting radioaerosol samples (in Shanghai) after Fukushima nuclear power plant (NPP) accident, radionuclides with gamma-emitting rays can be found to be nuclides (132I/132Te, 129I/129Te) other than 131I, 134,137Cs because of the decrease in background baseline after the daughter nuclides (i.e. 214Bi, 214Pb and etc.) of radon makes decay sharply. Based on aerosol sample collected by passing through 1,300 $ M^{3} $ air in 24 h, the lower limit of detection (LLD) of 132I/132Te, 129I/129Te can be decreased from 6.11 × $ 10^{−5} $, 3.46 × $ 10^{−4} $ Bq $ m^{−3} $ after half an hour sampling to 1.64 × $ 10^{−5} $, 8.19 × $ 10^{−5} $ Bq $ m^{−3} $ after sampling 48 h sampling. Similarly, LLD can be decreased from 9.63 × $ 10^{−5} $ to 1.41 × $ 10^{−5} $ Bq $ m^{−3} $ for 131I, 7.72 × $ 10^{−5} $ to 9.96 × $ 10^{−6} $ Bq $ m^{−3} $ for 134Cs and 9.67 × $ 10^{−5} $ to 1.45 × $ 10^{−5} $ Bq $ m^{−3} $ for 137Cs after the same time sampling. In the same time, the activities of daughter nuclides such as 214Pb and 212Bi from the decay of their parent nuclides 222Rn and 220Rn can sharply decrease from 2.45 × $ 10^{−2} $, 2.57 × $ 10^{−2} $ Bq $ m^{−3} $ to be ~$ 10^{−4} $ Bq $ m^{−3} $ while the activities of the concerned nuclides 132I/132Te, 129Te, 131I, 134,137Cs were almost constant. As our knowledge, it is the first time to report such case which is very helpful to monitor the leaked nuclides from NPP by aerosol sampling in both normal operation case and emergency case.
650		4	\|a The lower limit of detection \|7 (dpeaa)DE-He213
650		4	\|a Gamma-ray emitting nuclides \|7 (dpeaa)DE-He213
650		4	\|a Radioaerosol \|7 (dpeaa)DE-He213
650		4	\|a Fukushima nuclear accident \|7 (dpeaa)DE-He213
700	1		\|a Jiang, Yifei \|e verfasserin \|4 aut
700	1		\|a Huang, Dekun \|e verfasserin \|4 aut
700	1		\|a Wen, Tingyu \|e verfasserin \|4 aut
700	1		\|a Du, Jinzhou \|e verfasserin \|4 aut
700	1		\|a Zhang, Jing \|e verfasserin \|4 aut
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773	1	8	\|g volume:292 \|g year:2011 \|g number:3 \|g day:30 \|g month:12 \|g pages:1297-1301
856	4	0	\|u https://dx.doi.org/10.1007/s10967-011-1594-9 \|z lizenzpflichtig \|3 Volltext
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912			\|a GBV_ILN_24
912			\|a GBV_ILN_31
912			\|a GBV_ILN_32
912			\|a GBV_ILN_39
912			\|a GBV_ILN_40
912			\|a GBV_ILN_60
912			\|a GBV_ILN_62
912			\|a GBV_ILN_63
912			\|a GBV_ILN_69
912			\|a GBV_ILN_70
912			\|a GBV_ILN_73
912			\|a GBV_ILN_74
912			\|a GBV_ILN_90
912			\|a GBV_ILN_95
912			\|a GBV_ILN_100
912			\|a GBV_ILN_101
912			\|a GBV_ILN_105
912			\|a GBV_ILN_110
912			\|a GBV_ILN_120
912			\|a GBV_ILN_138
912			\|a GBV_ILN_150
912			\|a GBV_ILN_151
912			\|a GBV_ILN_152
912			\|a GBV_ILN_161
912			\|a GBV_ILN_170
912			\|a GBV_ILN_171
912			\|a GBV_ILN_187
912			\|a GBV_ILN_206
912			\|a GBV_ILN_213
912			\|a GBV_ILN_224
912			\|a GBV_ILN_230
912			\|a GBV_ILN_250
912			\|a GBV_ILN_281
912			\|a GBV_ILN_285
912			\|a GBV_ILN_293
912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
912			\|a GBV_ILN_636
912			\|a GBV_ILN_702
912			\|a GBV_ILN_2001
912			\|a GBV_ILN_2003
912			\|a GBV_ILN_2004
912			\|a GBV_ILN_2005
912			\|a GBV_ILN_2006
912			\|a GBV_ILN_2007
912			\|a GBV_ILN_2008
912			\|a GBV_ILN_2009
912			\|a GBV_ILN_2010
912			\|a GBV_ILN_2011
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_2015
912			\|a GBV_ILN_2020
912			\|a GBV_ILN_2021
912			\|a GBV_ILN_2025
912			\|a GBV_ILN_2026
912			\|a GBV_ILN_2027
912			\|a GBV_ILN_2031
912			\|a GBV_ILN_2034
912			\|a GBV_ILN_2037
912			\|a GBV_ILN_2038
912			\|a GBV_ILN_2039
912			\|a GBV_ILN_2044
912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2049
912			\|a GBV_ILN_2050
912			\|a GBV_ILN_2055
912			\|a GBV_ILN_2057
912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2061
912			\|a GBV_ILN_2064
912			\|a GBV_ILN_2065
912			\|a GBV_ILN_2068
912			\|a GBV_ILN_2070
912			\|a GBV_ILN_2086
912			\|a GBV_ILN_2088
912			\|a GBV_ILN_2093
912			\|a GBV_ILN_2106
912			\|a GBV_ILN_2107
912			\|a GBV_ILN_2108
912			\|a GBV_ILN_2110
912			\|a GBV_ILN_2111
912			\|a GBV_ILN_2112
912			\|a GBV_ILN_2113
912			\|a GBV_ILN_2116
912			\|a GBV_ILN_2118
912			\|a GBV_ILN_2119
912			\|a GBV_ILN_2122
912			\|a GBV_ILN_2129
912			\|a GBV_ILN_2143
912			\|a GBV_ILN_2144
912			\|a GBV_ILN_2147
912			\|a GBV_ILN_2148
912			\|a GBV_ILN_2152
912			\|a GBV_ILN_2153
912			\|a GBV_ILN_2188
912			\|a GBV_ILN_2190
912			\|a GBV_ILN_2232
912			\|a GBV_ILN_2336
912			\|a GBV_ILN_2446
912			\|a GBV_ILN_2470
912			\|a GBV_ILN_2472
912			\|a GBV_ILN_2507
912			\|a GBV_ILN_2522
912			\|a GBV_ILN_2548
912			\|a GBV_ILN_4012
912			\|a GBV_ILN_4035
912			\|a GBV_ILN_4037
912			\|a GBV_ILN_4046
912			\|a GBV_ILN_4112
912			\|a GBV_ILN_4125
912			\|a GBV_ILN_4126
912			\|a GBV_ILN_4242
912			\|a GBV_ILN_4246
912			\|a GBV_ILN_4249
912			\|a GBV_ILN_4251
912			\|a GBV_ILN_4305
912			\|a GBV_ILN_4306
912			\|a GBV_ILN_4307
912			\|a GBV_ILN_4313
912			\|a GBV_ILN_4322
912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
912			\|a GBV_ILN_4325
912			\|a GBV_ILN_4326
912			\|a GBV_ILN_4333
912			\|a GBV_ILN_4334
912			\|a GBV_ILN_4335
912			\|a GBV_ILN_4336
912			\|a GBV_ILN_4338
912			\|a GBV_ILN_4393
912			\|a GBV_ILN_4700
936	b	k	\|a 35.00 \|q ASE
951			\|a AR
952			\|d 292 \|j 2011 \|e 3 \|b 30 \|c 12 \|h 1297-1301

Indexfelder

author_variant	j w jw y j yj d h dh t w tw j d jd j z jz
matchkey_str	article:15882780:2011----::rmtooteoelmtfeetoogmamtiguldsnaiarsla
hierarchy_sort_str	2011
bklnumber	35.00
publishDate	2011
allfields	10.1007/s10967-011-1594-9 doi (DE-627)SPR015177866 (SPR)s10967-011-1594-9-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Wang, Jinglong verfasserin aut Promotion of the lower limit of detection of gamma emitting nuclides in radioaerosol samples after Fukushima accident 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Through placement in a few hours after collecting radioaerosol samples (in Shanghai) after Fukushima nuclear power plant (NPP) accident, radionuclides with gamma-emitting rays can be found to be nuclides (132I/132Te, 129I/129Te) other than 131I, 134,137Cs because of the decrease in background baseline after the daughter nuclides (i.e. 214Bi, 214Pb and etc.) of radon makes decay sharply. Based on aerosol sample collected by passing through 1,300 $ M^{3} $ air in 24 h, the lower limit of detection (LLD) of 132I/132Te, 129I/129Te can be decreased from 6.11 × $ 10^{−5} $, 3.46 × $ 10^{−4} $ Bq $ m^{−3} $ after half an hour sampling to 1.64 × $ 10^{−5} $, 8.19 × $ 10^{−5} $ Bq $ m^{−3} $ after sampling 48 h sampling. Similarly, LLD can be decreased from 9.63 × $ 10^{−5} $ to 1.41 × $ 10^{−5} $ Bq $ m^{−3} $ for 131I, 7.72 × $ 10^{−5} $ to 9.96 × $ 10^{−6} $ Bq $ m^{−3} $ for 134Cs and 9.67 × $ 10^{−5} $ to 1.45 × $ 10^{−5} $ Bq $ m^{−3} $ for 137Cs after the same time sampling. In the same time, the activities of daughter nuclides such as 214Pb and 212Bi from the decay of their parent nuclides 222Rn and 220Rn can sharply decrease from 2.45 × $ 10^{−2} $, 2.57 × $ 10^{−2} $ Bq $ m^{−3} $ to be ~$ 10^{−4} $ Bq $ m^{−3} $ while the activities of the concerned nuclides 132I/132Te, 129Te, 131I, 134,137Cs were almost constant. As our knowledge, it is the first time to report such case which is very helpful to monitor the leaked nuclides from NPP by aerosol sampling in both normal operation case and emergency case. The lower limit of detection (dpeaa)DE-He213 Gamma-ray emitting nuclides (dpeaa)DE-He213 Radioaerosol (dpeaa)DE-He213 Fukushima nuclear accident (dpeaa)DE-He213 Jiang, Yifei verfasserin aut Huang, Dekun verfasserin aut Wen, Tingyu verfasserin aut Du, Jinzhou verfasserin aut Zhang, Jing verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 292(2011), 3 vom: 30. Dez., Seite 1297-1301 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:292 year:2011 number:3 day:30 month:12 pages:1297-1301 https://dx.doi.org/10.1007/s10967-011-1594-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 35.00 ASE AR 292 2011 3 30 12 1297-1301
spelling	10.1007/s10967-011-1594-9 doi (DE-627)SPR015177866 (SPR)s10967-011-1594-9-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Wang, Jinglong verfasserin aut Promotion of the lower limit of detection of gamma emitting nuclides in radioaerosol samples after Fukushima accident 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Through placement in a few hours after collecting radioaerosol samples (in Shanghai) after Fukushima nuclear power plant (NPP) accident, radionuclides with gamma-emitting rays can be found to be nuclides (132I/132Te, 129I/129Te) other than 131I, 134,137Cs because of the decrease in background baseline after the daughter nuclides (i.e. 214Bi, 214Pb and etc.) of radon makes decay sharply. Based on aerosol sample collected by passing through 1,300 $ M^{3} $ air in 24 h, the lower limit of detection (LLD) of 132I/132Te, 129I/129Te can be decreased from 6.11 × $ 10^{−5} $, 3.46 × $ 10^{−4} $ Bq $ m^{−3} $ after half an hour sampling to 1.64 × $ 10^{−5} $, 8.19 × $ 10^{−5} $ Bq $ m^{−3} $ after sampling 48 h sampling. Similarly, LLD can be decreased from 9.63 × $ 10^{−5} $ to 1.41 × $ 10^{−5} $ Bq $ m^{−3} $ for 131I, 7.72 × $ 10^{−5} $ to 9.96 × $ 10^{−6} $ Bq $ m^{−3} $ for 134Cs and 9.67 × $ 10^{−5} $ to 1.45 × $ 10^{−5} $ Bq $ m^{−3} $ for 137Cs after the same time sampling. In the same time, the activities of daughter nuclides such as 214Pb and 212Bi from the decay of their parent nuclides 222Rn and 220Rn can sharply decrease from 2.45 × $ 10^{−2} $, 2.57 × $ 10^{−2} $ Bq $ m^{−3} $ to be ~$ 10^{−4} $ Bq $ m^{−3} $ while the activities of the concerned nuclides 132I/132Te, 129Te, 131I, 134,137Cs were almost constant. As our knowledge, it is the first time to report such case which is very helpful to monitor the leaked nuclides from NPP by aerosol sampling in both normal operation case and emergency case. The lower limit of detection (dpeaa)DE-He213 Gamma-ray emitting nuclides (dpeaa)DE-He213 Radioaerosol (dpeaa)DE-He213 Fukushima nuclear accident (dpeaa)DE-He213 Jiang, Yifei verfasserin aut Huang, Dekun verfasserin aut Wen, Tingyu verfasserin aut Du, Jinzhou verfasserin aut Zhang, Jing verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 292(2011), 3 vom: 30. Dez., Seite 1297-1301 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:292 year:2011 number:3 day:30 month:12 pages:1297-1301 https://dx.doi.org/10.1007/s10967-011-1594-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 35.00 ASE AR 292 2011 3 30 12 1297-1301
allfields_unstemmed	10.1007/s10967-011-1594-9 doi (DE-627)SPR015177866 (SPR)s10967-011-1594-9-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Wang, Jinglong verfasserin aut Promotion of the lower limit of detection of gamma emitting nuclides in radioaerosol samples after Fukushima accident 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Through placement in a few hours after collecting radioaerosol samples (in Shanghai) after Fukushima nuclear power plant (NPP) accident, radionuclides with gamma-emitting rays can be found to be nuclides (132I/132Te, 129I/129Te) other than 131I, 134,137Cs because of the decrease in background baseline after the daughter nuclides (i.e. 214Bi, 214Pb and etc.) of radon makes decay sharply. Based on aerosol sample collected by passing through 1,300 $ M^{3} $ air in 24 h, the lower limit of detection (LLD) of 132I/132Te, 129I/129Te can be decreased from 6.11 × $ 10^{−5} $, 3.46 × $ 10^{−4} $ Bq $ m^{−3} $ after half an hour sampling to 1.64 × $ 10^{−5} $, 8.19 × $ 10^{−5} $ Bq $ m^{−3} $ after sampling 48 h sampling. Similarly, LLD can be decreased from 9.63 × $ 10^{−5} $ to 1.41 × $ 10^{−5} $ Bq $ m^{−3} $ for 131I, 7.72 × $ 10^{−5} $ to 9.96 × $ 10^{−6} $ Bq $ m^{−3} $ for 134Cs and 9.67 × $ 10^{−5} $ to 1.45 × $ 10^{−5} $ Bq $ m^{−3} $ for 137Cs after the same time sampling. In the same time, the activities of daughter nuclides such as 214Pb and 212Bi from the decay of their parent nuclides 222Rn and 220Rn can sharply decrease from 2.45 × $ 10^{−2} $, 2.57 × $ 10^{−2} $ Bq $ m^{−3} $ to be ~$ 10^{−4} $ Bq $ m^{−3} $ while the activities of the concerned nuclides 132I/132Te, 129Te, 131I, 134,137Cs were almost constant. As our knowledge, it is the first time to report such case which is very helpful to monitor the leaked nuclides from NPP by aerosol sampling in both normal operation case and emergency case. The lower limit of detection (dpeaa)DE-He213 Gamma-ray emitting nuclides (dpeaa)DE-He213 Radioaerosol (dpeaa)DE-He213 Fukushima nuclear accident (dpeaa)DE-He213 Jiang, Yifei verfasserin aut Huang, Dekun verfasserin aut Wen, Tingyu verfasserin aut Du, Jinzhou verfasserin aut Zhang, Jing verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 292(2011), 3 vom: 30. Dez., Seite 1297-1301 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:292 year:2011 number:3 day:30 month:12 pages:1297-1301 https://dx.doi.org/10.1007/s10967-011-1594-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 35.00 ASE AR 292 2011 3 30 12 1297-1301
allfieldsGer	10.1007/s10967-011-1594-9 doi (DE-627)SPR015177866 (SPR)s10967-011-1594-9-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Wang, Jinglong verfasserin aut Promotion of the lower limit of detection of gamma emitting nuclides in radioaerosol samples after Fukushima accident 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Through placement in a few hours after collecting radioaerosol samples (in Shanghai) after Fukushima nuclear power plant (NPP) accident, radionuclides with gamma-emitting rays can be found to be nuclides (132I/132Te, 129I/129Te) other than 131I, 134,137Cs because of the decrease in background baseline after the daughter nuclides (i.e. 214Bi, 214Pb and etc.) of radon makes decay sharply. Based on aerosol sample collected by passing through 1,300 $ M^{3} $ air in 24 h, the lower limit of detection (LLD) of 132I/132Te, 129I/129Te can be decreased from 6.11 × $ 10^{−5} $, 3.46 × $ 10^{−4} $ Bq $ m^{−3} $ after half an hour sampling to 1.64 × $ 10^{−5} $, 8.19 × $ 10^{−5} $ Bq $ m^{−3} $ after sampling 48 h sampling. Similarly, LLD can be decreased from 9.63 × $ 10^{−5} $ to 1.41 × $ 10^{−5} $ Bq $ m^{−3} $ for 131I, 7.72 × $ 10^{−5} $ to 9.96 × $ 10^{−6} $ Bq $ m^{−3} $ for 134Cs and 9.67 × $ 10^{−5} $ to 1.45 × $ 10^{−5} $ Bq $ m^{−3} $ for 137Cs after the same time sampling. In the same time, the activities of daughter nuclides such as 214Pb and 212Bi from the decay of their parent nuclides 222Rn and 220Rn can sharply decrease from 2.45 × $ 10^{−2} $, 2.57 × $ 10^{−2} $ Bq $ m^{−3} $ to be ~$ 10^{−4} $ Bq $ m^{−3} $ while the activities of the concerned nuclides 132I/132Te, 129Te, 131I, 134,137Cs were almost constant. As our knowledge, it is the first time to report such case which is very helpful to monitor the leaked nuclides from NPP by aerosol sampling in both normal operation case and emergency case. The lower limit of detection (dpeaa)DE-He213 Gamma-ray emitting nuclides (dpeaa)DE-He213 Radioaerosol (dpeaa)DE-He213 Fukushima nuclear accident (dpeaa)DE-He213 Jiang, Yifei verfasserin aut Huang, Dekun verfasserin aut Wen, Tingyu verfasserin aut Du, Jinzhou verfasserin aut Zhang, Jing verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 292(2011), 3 vom: 30. Dez., Seite 1297-1301 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:292 year:2011 number:3 day:30 month:12 pages:1297-1301 https://dx.doi.org/10.1007/s10967-011-1594-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 35.00 ASE AR 292 2011 3 30 12 1297-1301
allfieldsSound	10.1007/s10967-011-1594-9 doi (DE-627)SPR015177866 (SPR)s10967-011-1594-9-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Wang, Jinglong verfasserin aut Promotion of the lower limit of detection of gamma emitting nuclides in radioaerosol samples after Fukushima accident 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Through placement in a few hours after collecting radioaerosol samples (in Shanghai) after Fukushima nuclear power plant (NPP) accident, radionuclides with gamma-emitting rays can be found to be nuclides (132I/132Te, 129I/129Te) other than 131I, 134,137Cs because of the decrease in background baseline after the daughter nuclides (i.e. 214Bi, 214Pb and etc.) of radon makes decay sharply. Based on aerosol sample collected by passing through 1,300 $ M^{3} $ air in 24 h, the lower limit of detection (LLD) of 132I/132Te, 129I/129Te can be decreased from 6.11 × $ 10^{−5} $, 3.46 × $ 10^{−4} $ Bq $ m^{−3} $ after half an hour sampling to 1.64 × $ 10^{−5} $, 8.19 × $ 10^{−5} $ Bq $ m^{−3} $ after sampling 48 h sampling. Similarly, LLD can be decreased from 9.63 × $ 10^{−5} $ to 1.41 × $ 10^{−5} $ Bq $ m^{−3} $ for 131I, 7.72 × $ 10^{−5} $ to 9.96 × $ 10^{−6} $ Bq $ m^{−3} $ for 134Cs and 9.67 × $ 10^{−5} $ to 1.45 × $ 10^{−5} $ Bq $ m^{−3} $ for 137Cs after the same time sampling. In the same time, the activities of daughter nuclides such as 214Pb and 212Bi from the decay of their parent nuclides 222Rn and 220Rn can sharply decrease from 2.45 × $ 10^{−2} $, 2.57 × $ 10^{−2} $ Bq $ m^{−3} $ to be ~$ 10^{−4} $ Bq $ m^{−3} $ while the activities of the concerned nuclides 132I/132Te, 129Te, 131I, 134,137Cs were almost constant. As our knowledge, it is the first time to report such case which is very helpful to monitor the leaked nuclides from NPP by aerosol sampling in both normal operation case and emergency case. The lower limit of detection (dpeaa)DE-He213 Gamma-ray emitting nuclides (dpeaa)DE-He213 Radioaerosol (dpeaa)DE-He213 Fukushima nuclear accident (dpeaa)DE-He213 Jiang, Yifei verfasserin aut Huang, Dekun verfasserin aut Wen, Tingyu verfasserin aut Du, Jinzhou verfasserin aut Zhang, Jing verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 292(2011), 3 vom: 30. Dez., Seite 1297-1301 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:292 year:2011 number:3 day:30 month:12 pages:1297-1301 https://dx.doi.org/10.1007/s10967-011-1594-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 35.00 ASE AR 292 2011 3 30 12 1297-1301
language	English
source	Enthalten in Journal of radioanalytical and nuclear chemistry 292(2011), 3 vom: 30. Dez., Seite 1297-1301 volume:292 year:2011 number:3 day:30 month:12 pages:1297-1301
sourceStr	Enthalten in Journal of radioanalytical and nuclear chemistry 292(2011), 3 vom: 30. Dez., Seite 1297-1301 volume:292 year:2011 number:3 day:30 month:12 pages:1297-1301
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	The lower limit of detection Gamma-ray emitting nuclides Radioaerosol Fukushima nuclear accident
dewey-raw	540
isfreeaccess_bool	false
container_title	Journal of radioanalytical and nuclear chemistry
authorswithroles_txt_mv	Wang, Jinglong @@aut@@ Jiang, Yifei @@aut@@ Huang, Dekun @@aut@@ Wen, Tingyu @@aut@@ Du, Jinzhou @@aut@@ Zhang, Jing @@aut@@
publishDateDaySort_date	2011-12-30T00:00:00Z
hierarchy_top_id	320578011
dewey-sort	3540
id	SPR015177866
language_de	englisch
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Based on aerosol sample collected by passing through 1,300 $ M^{3} $ air in 24 h, the lower limit of detection (LLD) of 132I/132Te, 129I/129Te can be decreased from 6.11 × $ 10^{−5} $, 3.46 × $ 10^{−4} $ Bq $ m^{−3} $ after half an hour sampling to 1.64 × $ 10^{−5} $, 8.19 × $ 10^{−5} $ Bq $ m^{−3} $ after sampling 48 h sampling. Similarly, LLD can be decreased from 9.63 × $ 10^{−5} $ to 1.41 × $ 10^{−5} $ Bq $ m^{−3} $ for 131I, 7.72 × $ 10^{−5} $ to 9.96 × $ 10^{−6} $ Bq $ m^{−3} $ for 134Cs and 9.67 × $ 10^{−5} $ to 1.45 × $ 10^{−5} $ Bq $ m^{−3} $ for 137Cs after the same time sampling. In the same time, the activities of daughter nuclides such as 214Pb and 212Bi from the decay of their parent nuclides 222Rn and 220Rn can sharply decrease from 2.45 × $ 10^{−2} $, 2.57 × $ 10^{−2} $ Bq $ m^{−3} $ to be ~$ 10^{−4} $ Bq $ m^{−3} $ while the activities of the concerned nuclides 132I/132Te, 129Te, 131I, 134,137Cs were almost constant. 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author	Wang, Jinglong
spellingShingle	Wang, Jinglong ddc 540 bkl 35.00 misc The lower limit of detection misc Gamma-ray emitting nuclides misc Radioaerosol misc Fukushima nuclear accident Promotion of the lower limit of detection of gamma emitting nuclides in radioaerosol samples after Fukushima accident
authorStr	Wang, Jinglong
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topic_title	540 ASE 35.00 bkl Promotion of the lower limit of detection of gamma emitting nuclides in radioaerosol samples after Fukushima accident The lower limit of detection (dpeaa)DE-He213 Gamma-ray emitting nuclides (dpeaa)DE-He213 Radioaerosol (dpeaa)DE-He213 Fukushima nuclear accident (dpeaa)DE-He213
topic	ddc 540 bkl 35.00 misc The lower limit of detection misc Gamma-ray emitting nuclides misc Radioaerosol misc Fukushima nuclear accident
topic_unstemmed	ddc 540 bkl 35.00 misc The lower limit of detection misc Gamma-ray emitting nuclides misc Radioaerosol misc Fukushima nuclear accident
topic_browse	ddc 540 bkl 35.00 misc The lower limit of detection misc Gamma-ray emitting nuclides misc Radioaerosol misc Fukushima nuclear accident
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title	Promotion of the lower limit of detection of gamma emitting nuclides in radioaerosol samples after Fukushima accident
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title_full	Promotion of the lower limit of detection of gamma emitting nuclides in radioaerosol samples after Fukushima accident
author_sort	Wang, Jinglong
journal	Journal of radioanalytical and nuclear chemistry
journalStr	Journal of radioanalytical and nuclear chemistry
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author_browse	Wang, Jinglong Jiang, Yifei Huang, Dekun Wen, Tingyu Du, Jinzhou Zhang, Jing
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author-letter	Wang, Jinglong
doi_str_mv	10.1007/s10967-011-1594-9
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author2-role	verfasserin
title_sort	promotion of the lower limit of detection of gamma emitting nuclides in radioaerosol samples after fukushima accident
title_auth	Promotion of the lower limit of detection of gamma emitting nuclides in radioaerosol samples after Fukushima accident
abstract	Abstract Through placement in a few hours after collecting radioaerosol samples (in Shanghai) after Fukushima nuclear power plant (NPP) accident, radionuclides with gamma-emitting rays can be found to be nuclides (132I/132Te, 129I/129Te) other than 131I, 134,137Cs because of the decrease in background baseline after the daughter nuclides (i.e. 214Bi, 214Pb and etc.) of radon makes decay sharply. Based on aerosol sample collected by passing through 1,300 $ M^{3} $ air in 24 h, the lower limit of detection (LLD) of 132I/132Te, 129I/129Te can be decreased from 6.11 × $ 10^{−5} $, 3.46 × $ 10^{−4} $ Bq $ m^{−3} $ after half an hour sampling to 1.64 × $ 10^{−5} $, 8.19 × $ 10^{−5} $ Bq $ m^{−3} $ after sampling 48 h sampling. Similarly, LLD can be decreased from 9.63 × $ 10^{−5} $ to 1.41 × $ 10^{−5} $ Bq $ m^{−3} $ for 131I, 7.72 × $ 10^{−5} $ to 9.96 × $ 10^{−6} $ Bq $ m^{−3} $ for 134Cs and 9.67 × $ 10^{−5} $ to 1.45 × $ 10^{−5} $ Bq $ m^{−3} $ for 137Cs after the same time sampling. In the same time, the activities of daughter nuclides such as 214Pb and 212Bi from the decay of their parent nuclides 222Rn and 220Rn can sharply decrease from 2.45 × $ 10^{−2} $, 2.57 × $ 10^{−2} $ Bq $ m^{−3} $ to be ~$ 10^{−4} $ Bq $ m^{−3} $ while the activities of the concerned nuclides 132I/132Te, 129Te, 131I, 134,137Cs were almost constant. As our knowledge, it is the first time to report such case which is very helpful to monitor the leaked nuclides from NPP by aerosol sampling in both normal operation case and emergency case.
abstractGer	Abstract Through placement in a few hours after collecting radioaerosol samples (in Shanghai) after Fukushima nuclear power plant (NPP) accident, radionuclides with gamma-emitting rays can be found to be nuclides (132I/132Te, 129I/129Te) other than 131I, 134,137Cs because of the decrease in background baseline after the daughter nuclides (i.e. 214Bi, 214Pb and etc.) of radon makes decay sharply. Based on aerosol sample collected by passing through 1,300 $ M^{3} $ air in 24 h, the lower limit of detection (LLD) of 132I/132Te, 129I/129Te can be decreased from 6.11 × $ 10^{−5} $, 3.46 × $ 10^{−4} $ Bq $ m^{−3} $ after half an hour sampling to 1.64 × $ 10^{−5} $, 8.19 × $ 10^{−5} $ Bq $ m^{−3} $ after sampling 48 h sampling. Similarly, LLD can be decreased from 9.63 × $ 10^{−5} $ to 1.41 × $ 10^{−5} $ Bq $ m^{−3} $ for 131I, 7.72 × $ 10^{−5} $ to 9.96 × $ 10^{−6} $ Bq $ m^{−3} $ for 134Cs and 9.67 × $ 10^{−5} $ to 1.45 × $ 10^{−5} $ Bq $ m^{−3} $ for 137Cs after the same time sampling. In the same time, the activities of daughter nuclides such as 214Pb and 212Bi from the decay of their parent nuclides 222Rn and 220Rn can sharply decrease from 2.45 × $ 10^{−2} $, 2.57 × $ 10^{−2} $ Bq $ m^{−3} $ to be ~$ 10^{−4} $ Bq $ m^{−3} $ while the activities of the concerned nuclides 132I/132Te, 129Te, 131I, 134,137Cs were almost constant. As our knowledge, it is the first time to report such case which is very helpful to monitor the leaked nuclides from NPP by aerosol sampling in both normal operation case and emergency case.
abstract_unstemmed	Abstract Through placement in a few hours after collecting radioaerosol samples (in Shanghai) after Fukushima nuclear power plant (NPP) accident, radionuclides with gamma-emitting rays can be found to be nuclides (132I/132Te, 129I/129Te) other than 131I, 134,137Cs because of the decrease in background baseline after the daughter nuclides (i.e. 214Bi, 214Pb and etc.) of radon makes decay sharply. Based on aerosol sample collected by passing through 1,300 $ M^{3} $ air in 24 h, the lower limit of detection (LLD) of 132I/132Te, 129I/129Te can be decreased from 6.11 × $ 10^{−5} $, 3.46 × $ 10^{−4} $ Bq $ m^{−3} $ after half an hour sampling to 1.64 × $ 10^{−5} $, 8.19 × $ 10^{−5} $ Bq $ m^{−3} $ after sampling 48 h sampling. Similarly, LLD can be decreased from 9.63 × $ 10^{−5} $ to 1.41 × $ 10^{−5} $ Bq $ m^{−3} $ for 131I, 7.72 × $ 10^{−5} $ to 9.96 × $ 10^{−6} $ Bq $ m^{−3} $ for 134Cs and 9.67 × $ 10^{−5} $ to 1.45 × $ 10^{−5} $ Bq $ m^{−3} $ for 137Cs after the same time sampling. In the same time, the activities of daughter nuclides such as 214Pb and 212Bi from the decay of their parent nuclides 222Rn and 220Rn can sharply decrease from 2.45 × $ 10^{−2} $, 2.57 × $ 10^{−2} $ Bq $ m^{−3} $ to be ~$ 10^{−4} $ Bq $ m^{−3} $ while the activities of the concerned nuclides 132I/132Te, 129Te, 131I, 134,137Cs were almost constant. As our knowledge, it is the first time to report such case which is very helpful to monitor the leaked nuclides from NPP by aerosol sampling in both normal operation case and emergency case.
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container_issue	3
title_short	Promotion of the lower limit of detection of gamma emitting nuclides in radioaerosol samples after Fukushima accident
url	https://dx.doi.org/10.1007/s10967-011-1594-9
remote_bool	true
author2	Jiang, Yifei Huang, Dekun Wen, Tingyu Du, Jinzhou Zhang, Jing
author2Str	Jiang, Yifei Huang, Dekun Wen, Tingyu Du, Jinzhou Zhang, Jing
ppnlink	320578011
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doi_str	10.1007/s10967-011-1594-9
up_date	2024-07-03T14:26:48.503Z
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Based on aerosol sample collected by passing through 1,300 $ M^{3} $ air in 24 h, the lower limit of detection (LLD) of 132I/132Te, 129I/129Te can be decreased from 6.11 × $ 10^{−5} $, 3.46 × $ 10^{−4} $ Bq $ m^{−3} $ after half an hour sampling to 1.64 × $ 10^{−5} $, 8.19 × $ 10^{−5} $ Bq $ m^{−3} $ after sampling 48 h sampling. Similarly, LLD can be decreased from 9.63 × $ 10^{−5} $ to 1.41 × $ 10^{−5} $ Bq $ m^{−3} $ for 131I, 7.72 × $ 10^{−5} $ to 9.96 × $ 10^{−6} $ Bq $ m^{−3} $ for 134Cs and 9.67 × $ 10^{−5} $ to 1.45 × $ 10^{−5} $ Bq $ m^{−3} $ for 137Cs after the same time sampling. In the same time, the activities of daughter nuclides such as 214Pb and 212Bi from the decay of their parent nuclides 222Rn and 220Rn can sharply decrease from 2.45 × $ 10^{−2} $, 2.57 × $ 10^{−2} $ Bq $ m^{−3} $ to be ~$ 10^{−4} $ Bq $ m^{−3} $ while the activities of the concerned nuclides 132I/132Te, 129Te, 131I, 134,137Cs were almost constant. 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Promotion of the lower limit of detection of gamma emitting nuclides in radioaerosol samples after Fukushima accident

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