Safety assessment of Beishan pre-selection area for geological disposal of high-level radioactive waste in China
Abstract A safety assessment was conducted for Beishan region of Gansu, China, the results show that Se-79 and Cs-135 are the key nuclides released in the near field between 1000 and 4000 years after the closure of the repository. After 4000 years, Tc-99, Np-237 and U-235 are the key nuclides releas...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Li, Honghui [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2022 |
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| Schlagwörter: |
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| Anmerkung: |
© Akadémiai Kiadó, Budapest, Hungary 2022 |
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| Übergeordnetes Werk: |
Enthalten in: Journal of radioanalytical and nuclear chemistry - Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968, 331(2022), 6 vom: 20. Apr., Seite 2573-2581 |
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| Übergeordnetes Werk: |
volume:331 ; year:2022 ; number:6 ; day:20 ; month:04 ; pages:2573-2581 |
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| DOI / URN: |
10.1007/s10967-022-08300-6 |
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| 245 | 1 | 0 | |a Safety assessment of Beishan pre-selection area for geological disposal of high-level radioactive waste in China |
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| 520 | |a Abstract A safety assessment was conducted for Beishan region of Gansu, China, the results show that Se-79 and Cs-135 are the key nuclides released in the near field between 1000 and 4000 years after the closure of the repository. After 4000 years, Tc-99, Np-237 and U-235 are the key nuclides released in the near field. Within 5000 years after the closure of the repository, Se-79 is the key nuclide released from the dominant water fractures, and its peak release rate is 1 × $ 10^{5} $ mol/$ m^{3} $, peak time 4000 a. At 20,000 years after the closure of the repository, Cs-135 is the key nuclide, and its peak release rate is 5 × $ 10^{6} $ mol/$ m^{3} $, with a peak time of 100,000 a. | ||
| 650 | 4 | |a Safety assessment |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Geological disposal |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Beishan |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Database |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Dose |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Wang, Ju |4 aut | |
| 700 | 1 | |a Mao, Liang |4 aut | |
| 700 | 1 | |a Zhao, Shuaiwei |4 aut | |
| 700 | 1 | |a Jia, Meilan |4 aut | |
| 700 | 1 | |a Liu, Yuchen |4 aut | |
| 700 | 1 | |a Huang, Shulong |0 (orcid)0000-0002-3379-1094 |4 aut | |
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10.1007/s10967-022-08300-6 doi (DE-627)SPR047161817 (SPR)s10967-022-08300-6-e DE-627 ger DE-627 rakwb eng Li, Honghui verfasserin aut Safety assessment of Beishan pre-selection area for geological disposal of high-level radioactive waste in China 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó, Budapest, Hungary 2022 Abstract A safety assessment was conducted for Beishan region of Gansu, China, the results show that Se-79 and Cs-135 are the key nuclides released in the near field between 1000 and 4000 years after the closure of the repository. After 4000 years, Tc-99, Np-237 and U-235 are the key nuclides released in the near field. Within 5000 years after the closure of the repository, Se-79 is the key nuclide released from the dominant water fractures, and its peak release rate is 1 × $ 10^{5} $ mol/$ m^{3} $, peak time 4000 a. At 20,000 years after the closure of the repository, Cs-135 is the key nuclide, and its peak release rate is 5 × $ 10^{6} $ mol/$ m^{3} $, with a peak time of 100,000 a. Safety assessment (dpeaa)DE-He213 Geological disposal (dpeaa)DE-He213 Beishan (dpeaa)DE-He213 Database (dpeaa)DE-He213 Dose (dpeaa)DE-He213 Wang, Ju aut Mao, Liang aut Zhao, Shuaiwei aut Jia, Meilan aut Liu, Yuchen aut Huang, Shulong (orcid)0000-0002-3379-1094 aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 331(2022), 6 vom: 20. Apr., Seite 2573-2581 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:331 year:2022 number:6 day:20 month:04 pages:2573-2581 https://dx.doi.org/10.1007/s10967-022-08300-6 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 331 2022 6 20 04 2573-2581 |
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10.1007/s10967-022-08300-6 doi (DE-627)SPR047161817 (SPR)s10967-022-08300-6-e DE-627 ger DE-627 rakwb eng Li, Honghui verfasserin aut Safety assessment of Beishan pre-selection area for geological disposal of high-level radioactive waste in China 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó, Budapest, Hungary 2022 Abstract A safety assessment was conducted for Beishan region of Gansu, China, the results show that Se-79 and Cs-135 are the key nuclides released in the near field between 1000 and 4000 years after the closure of the repository. After 4000 years, Tc-99, Np-237 and U-235 are the key nuclides released in the near field. Within 5000 years after the closure of the repository, Se-79 is the key nuclide released from the dominant water fractures, and its peak release rate is 1 × $ 10^{5} $ mol/$ m^{3} $, peak time 4000 a. At 20,000 years after the closure of the repository, Cs-135 is the key nuclide, and its peak release rate is 5 × $ 10^{6} $ mol/$ m^{3} $, with a peak time of 100,000 a. Safety assessment (dpeaa)DE-He213 Geological disposal (dpeaa)DE-He213 Beishan (dpeaa)DE-He213 Database (dpeaa)DE-He213 Dose (dpeaa)DE-He213 Wang, Ju aut Mao, Liang aut Zhao, Shuaiwei aut Jia, Meilan aut Liu, Yuchen aut Huang, Shulong (orcid)0000-0002-3379-1094 aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 331(2022), 6 vom: 20. Apr., Seite 2573-2581 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:331 year:2022 number:6 day:20 month:04 pages:2573-2581 https://dx.doi.org/10.1007/s10967-022-08300-6 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 331 2022 6 20 04 2573-2581 |
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10.1007/s10967-022-08300-6 doi (DE-627)SPR047161817 (SPR)s10967-022-08300-6-e DE-627 ger DE-627 rakwb eng Li, Honghui verfasserin aut Safety assessment of Beishan pre-selection area for geological disposal of high-level radioactive waste in China 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó, Budapest, Hungary 2022 Abstract A safety assessment was conducted for Beishan region of Gansu, China, the results show that Se-79 and Cs-135 are the key nuclides released in the near field between 1000 and 4000 years after the closure of the repository. After 4000 years, Tc-99, Np-237 and U-235 are the key nuclides released in the near field. Within 5000 years after the closure of the repository, Se-79 is the key nuclide released from the dominant water fractures, and its peak release rate is 1 × $ 10^{5} $ mol/$ m^{3} $, peak time 4000 a. At 20,000 years after the closure of the repository, Cs-135 is the key nuclide, and its peak release rate is 5 × $ 10^{6} $ mol/$ m^{3} $, with a peak time of 100,000 a. Safety assessment (dpeaa)DE-He213 Geological disposal (dpeaa)DE-He213 Beishan (dpeaa)DE-He213 Database (dpeaa)DE-He213 Dose (dpeaa)DE-He213 Wang, Ju aut Mao, Liang aut Zhao, Shuaiwei aut Jia, Meilan aut Liu, Yuchen aut Huang, Shulong (orcid)0000-0002-3379-1094 aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 331(2022), 6 vom: 20. Apr., Seite 2573-2581 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:331 year:2022 number:6 day:20 month:04 pages:2573-2581 https://dx.doi.org/10.1007/s10967-022-08300-6 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 331 2022 6 20 04 2573-2581 |
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10.1007/s10967-022-08300-6 doi (DE-627)SPR047161817 (SPR)s10967-022-08300-6-e DE-627 ger DE-627 rakwb eng Li, Honghui verfasserin aut Safety assessment of Beishan pre-selection area for geological disposal of high-level radioactive waste in China 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó, Budapest, Hungary 2022 Abstract A safety assessment was conducted for Beishan region of Gansu, China, the results show that Se-79 and Cs-135 are the key nuclides released in the near field between 1000 and 4000 years after the closure of the repository. After 4000 years, Tc-99, Np-237 and U-235 are the key nuclides released in the near field. Within 5000 years after the closure of the repository, Se-79 is the key nuclide released from the dominant water fractures, and its peak release rate is 1 × $ 10^{5} $ mol/$ m^{3} $, peak time 4000 a. At 20,000 years after the closure of the repository, Cs-135 is the key nuclide, and its peak release rate is 5 × $ 10^{6} $ mol/$ m^{3} $, with a peak time of 100,000 a. Safety assessment (dpeaa)DE-He213 Geological disposal (dpeaa)DE-He213 Beishan (dpeaa)DE-He213 Database (dpeaa)DE-He213 Dose (dpeaa)DE-He213 Wang, Ju aut Mao, Liang aut Zhao, Shuaiwei aut Jia, Meilan aut Liu, Yuchen aut Huang, Shulong (orcid)0000-0002-3379-1094 aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 331(2022), 6 vom: 20. Apr., Seite 2573-2581 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:331 year:2022 number:6 day:20 month:04 pages:2573-2581 https://dx.doi.org/10.1007/s10967-022-08300-6 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 331 2022 6 20 04 2573-2581 |
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10.1007/s10967-022-08300-6 doi (DE-627)SPR047161817 (SPR)s10967-022-08300-6-e DE-627 ger DE-627 rakwb eng Li, Honghui verfasserin aut Safety assessment of Beishan pre-selection area for geological disposal of high-level radioactive waste in China 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó, Budapest, Hungary 2022 Abstract A safety assessment was conducted for Beishan region of Gansu, China, the results show that Se-79 and Cs-135 are the key nuclides released in the near field between 1000 and 4000 years after the closure of the repository. After 4000 years, Tc-99, Np-237 and U-235 are the key nuclides released in the near field. Within 5000 years after the closure of the repository, Se-79 is the key nuclide released from the dominant water fractures, and its peak release rate is 1 × $ 10^{5} $ mol/$ m^{3} $, peak time 4000 a. At 20,000 years after the closure of the repository, Cs-135 is the key nuclide, and its peak release rate is 5 × $ 10^{6} $ mol/$ m^{3} $, with a peak time of 100,000 a. Safety assessment (dpeaa)DE-He213 Geological disposal (dpeaa)DE-He213 Beishan (dpeaa)DE-He213 Database (dpeaa)DE-He213 Dose (dpeaa)DE-He213 Wang, Ju aut Mao, Liang aut Zhao, Shuaiwei aut Jia, Meilan aut Liu, Yuchen aut Huang, Shulong (orcid)0000-0002-3379-1094 aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 331(2022), 6 vom: 20. Apr., Seite 2573-2581 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:331 year:2022 number:6 day:20 month:04 pages:2573-2581 https://dx.doi.org/10.1007/s10967-022-08300-6 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 331 2022 6 20 04 2573-2581 |
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Li, Honghui @@aut@@ Wang, Ju @@aut@@ Mao, Liang @@aut@@ Zhao, Shuaiwei @@aut@@ Jia, Meilan @@aut@@ Liu, Yuchen @@aut@@ Huang, Shulong @@aut@@ |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR047161817</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230519160725.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">220602s2022 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10967-022-08300-6</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR047161817</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s10967-022-08300-6-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Li, Honghui</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Safety assessment of Beishan pre-selection area for geological disposal of high-level radioactive waste in China</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Akadémiai Kiadó, Budapest, Hungary 2022</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract A safety assessment was conducted for Beishan region of Gansu, China, the results show that Se-79 and Cs-135 are the key nuclides released in the near field between 1000 and 4000 years after the closure of the repository. After 4000 years, Tc-99, Np-237 and U-235 are the key nuclides released in the near field. Within 5000 years after the closure of the repository, Se-79 is the key nuclide released from the dominant water fractures, and its peak release rate is 1 × $ 10^{5} $ mol/$ m^{3} $, peak time 4000 a. 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Li, Honghui |
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Li, Honghui Wang, Ju Mao, Liang Zhao, Shuaiwei Jia, Meilan Liu, Yuchen Huang, Shulong |
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safety assessment of beishan pre-selection area for geological disposal of high-level radioactive waste in china |
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Safety assessment of Beishan pre-selection area for geological disposal of high-level radioactive waste in China |
| abstract |
Abstract A safety assessment was conducted for Beishan region of Gansu, China, the results show that Se-79 and Cs-135 are the key nuclides released in the near field between 1000 and 4000 years after the closure of the repository. After 4000 years, Tc-99, Np-237 and U-235 are the key nuclides released in the near field. Within 5000 years after the closure of the repository, Se-79 is the key nuclide released from the dominant water fractures, and its peak release rate is 1 × $ 10^{5} $ mol/$ m^{3} $, peak time 4000 a. At 20,000 years after the closure of the repository, Cs-135 is the key nuclide, and its peak release rate is 5 × $ 10^{6} $ mol/$ m^{3} $, with a peak time of 100,000 a. © Akadémiai Kiadó, Budapest, Hungary 2022 |
| abstractGer |
Abstract A safety assessment was conducted for Beishan region of Gansu, China, the results show that Se-79 and Cs-135 are the key nuclides released in the near field between 1000 and 4000 years after the closure of the repository. After 4000 years, Tc-99, Np-237 and U-235 are the key nuclides released in the near field. Within 5000 years after the closure of the repository, Se-79 is the key nuclide released from the dominant water fractures, and its peak release rate is 1 × $ 10^{5} $ mol/$ m^{3} $, peak time 4000 a. At 20,000 years after the closure of the repository, Cs-135 is the key nuclide, and its peak release rate is 5 × $ 10^{6} $ mol/$ m^{3} $, with a peak time of 100,000 a. © Akadémiai Kiadó, Budapest, Hungary 2022 |
| abstract_unstemmed |
Abstract A safety assessment was conducted for Beishan region of Gansu, China, the results show that Se-79 and Cs-135 are the key nuclides released in the near field between 1000 and 4000 years after the closure of the repository. After 4000 years, Tc-99, Np-237 and U-235 are the key nuclides released in the near field. Within 5000 years after the closure of the repository, Se-79 is the key nuclide released from the dominant water fractures, and its peak release rate is 1 × $ 10^{5} $ mol/$ m^{3} $, peak time 4000 a. At 20,000 years after the closure of the repository, Cs-135 is the key nuclide, and its peak release rate is 5 × $ 10^{6} $ mol/$ m^{3} $, with a peak time of 100,000 a. © Akadémiai Kiadó, Budapest, Hungary 2022 |
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6 |
| title_short |
Safety assessment of Beishan pre-selection area for geological disposal of high-level radioactive waste in China |
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https://dx.doi.org/10.1007/s10967-022-08300-6 |
| remote_bool |
true |
| author2 |
Wang, Ju Mao, Liang Zhao, Shuaiwei Jia, Meilan Liu, Yuchen Huang, Shulong |
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Wang, Ju Mao, Liang Zhao, Shuaiwei Jia, Meilan Liu, Yuchen Huang, Shulong |
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| doi_str |
10.1007/s10967-022-08300-6 |
| up_date |
2024-07-04T02:07:35.929Z |
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| score |
7.401108 |