Study of naturally occurring radioactive material (NORM) in top soil of Punjab State from the North Western part of India
Abstract The concentration levels of 238U, 232 Th, 40K and 137Cs in top soils of State of Punjab located in the North Western part of India were measured using conventional low background gamma ray spectrometric setup as well as Compton suppressed gamma ray spectrometric setup. The radioactivity lev...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Srivastava, Alok [verfasserIn] Lahiri, Susanta [verfasserIn] Maiti, Moumita [verfasserIn] Knolle, F. [verfasserIn] Hoyler, F. [verfasserIn] Scherer, U. W. [verfasserIn] Schnug, E. W. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2014 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Journal of radioanalytical and nuclear chemistry - Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968, 302(2014), 2 vom: 31. Aug., Seite 1049-1052 |
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| Übergeordnetes Werk: |
volume:302 ; year:2014 ; number:2 ; day:31 ; month:08 ; pages:1049-1052 |
| Links: |
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| DOI / URN: |
10.1007/s10967-014-3450-1 |
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| Katalog-ID: |
SPR015195821 |
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| 520 | |a Abstract The concentration levels of 238U, 232 Th, 40K and 137Cs in top soils of State of Punjab located in the North Western part of India were measured using conventional low background gamma ray spectrometric setup as well as Compton suppressed gamma ray spectrometric setup. The radioactivity level of 238U and 232Th was found to vary between 15 Bq/kg and 27 Bq/kg and between 16 Bq/kg and 57 Bq/kg respectively. The radioactivity level of 40K was found to vary between 266 Bq/kg and 799 Bq/kg. The mean radioactivity level of the NORM in general was found to be similar to what is expected as a result of their normal abundance. | ||
| 650 | 4 | |a NORM |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Top soil |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a U |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Th |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a K |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Gamma ray spectrometry |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Compton suppression system |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Lahiri, Susanta |e verfasserin |4 aut | |
| 700 | 1 | |a Maiti, Moumita |e verfasserin |4 aut | |
| 700 | 1 | |a Knolle, F. |e verfasserin |4 aut | |
| 700 | 1 | |a Hoyler, F. |e verfasserin |4 aut | |
| 700 | 1 | |a Scherer, U. W. |e verfasserin |4 aut | |
| 700 | 1 | |a Schnug, E. W. |e verfasserin |4 aut | |
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10.1007/s10967-014-3450-1 doi (DE-627)SPR015195821 (SPR)s10967-014-3450-1-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Srivastava, Alok verfasserin aut Study of naturally occurring radioactive material (NORM) in top soil of Punjab State from the North Western part of India 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The concentration levels of 238U, 232 Th, 40K and 137Cs in top soils of State of Punjab located in the North Western part of India were measured using conventional low background gamma ray spectrometric setup as well as Compton suppressed gamma ray spectrometric setup. The radioactivity level of 238U and 232Th was found to vary between 15 Bq/kg and 27 Bq/kg and between 16 Bq/kg and 57 Bq/kg respectively. The radioactivity level of 40K was found to vary between 266 Bq/kg and 799 Bq/kg. The mean radioactivity level of the NORM in general was found to be similar to what is expected as a result of their normal abundance. NORM (dpeaa)DE-He213 Top soil (dpeaa)DE-He213 U (dpeaa)DE-He213 Th (dpeaa)DE-He213 K (dpeaa)DE-He213 Gamma ray spectrometry (dpeaa)DE-He213 Compton suppression system (dpeaa)DE-He213 Lahiri, Susanta verfasserin aut Maiti, Moumita verfasserin aut Knolle, F. verfasserin aut Hoyler, F. verfasserin aut Scherer, U. W. verfasserin aut Schnug, E. W. verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 302(2014), 2 vom: 31. Aug., Seite 1049-1052 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:302 year:2014 number:2 day:31 month:08 pages:1049-1052 https://dx.doi.org/10.1007/s10967-014-3450-1 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 302 2014 2 31 08 1049-1052 |
| spelling |
10.1007/s10967-014-3450-1 doi (DE-627)SPR015195821 (SPR)s10967-014-3450-1-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Srivastava, Alok verfasserin aut Study of naturally occurring radioactive material (NORM) in top soil of Punjab State from the North Western part of India 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The concentration levels of 238U, 232 Th, 40K and 137Cs in top soils of State of Punjab located in the North Western part of India were measured using conventional low background gamma ray spectrometric setup as well as Compton suppressed gamma ray spectrometric setup. The radioactivity level of 238U and 232Th was found to vary between 15 Bq/kg and 27 Bq/kg and between 16 Bq/kg and 57 Bq/kg respectively. The radioactivity level of 40K was found to vary between 266 Bq/kg and 799 Bq/kg. The mean radioactivity level of the NORM in general was found to be similar to what is expected as a result of their normal abundance. NORM (dpeaa)DE-He213 Top soil (dpeaa)DE-He213 U (dpeaa)DE-He213 Th (dpeaa)DE-He213 K (dpeaa)DE-He213 Gamma ray spectrometry (dpeaa)DE-He213 Compton suppression system (dpeaa)DE-He213 Lahiri, Susanta verfasserin aut Maiti, Moumita verfasserin aut Knolle, F. verfasserin aut Hoyler, F. verfasserin aut Scherer, U. W. verfasserin aut Schnug, E. W. verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 302(2014), 2 vom: 31. Aug., Seite 1049-1052 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:302 year:2014 number:2 day:31 month:08 pages:1049-1052 https://dx.doi.org/10.1007/s10967-014-3450-1 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 302 2014 2 31 08 1049-1052 |
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10.1007/s10967-014-3450-1 doi (DE-627)SPR015195821 (SPR)s10967-014-3450-1-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Srivastava, Alok verfasserin aut Study of naturally occurring radioactive material (NORM) in top soil of Punjab State from the North Western part of India 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The concentration levels of 238U, 232 Th, 40K and 137Cs in top soils of State of Punjab located in the North Western part of India were measured using conventional low background gamma ray spectrometric setup as well as Compton suppressed gamma ray spectrometric setup. The radioactivity level of 238U and 232Th was found to vary between 15 Bq/kg and 27 Bq/kg and between 16 Bq/kg and 57 Bq/kg respectively. The radioactivity level of 40K was found to vary between 266 Bq/kg and 799 Bq/kg. The mean radioactivity level of the NORM in general was found to be similar to what is expected as a result of their normal abundance. NORM (dpeaa)DE-He213 Top soil (dpeaa)DE-He213 U (dpeaa)DE-He213 Th (dpeaa)DE-He213 K (dpeaa)DE-He213 Gamma ray spectrometry (dpeaa)DE-He213 Compton suppression system (dpeaa)DE-He213 Lahiri, Susanta verfasserin aut Maiti, Moumita verfasserin aut Knolle, F. verfasserin aut Hoyler, F. verfasserin aut Scherer, U. W. verfasserin aut Schnug, E. W. verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 302(2014), 2 vom: 31. Aug., Seite 1049-1052 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:302 year:2014 number:2 day:31 month:08 pages:1049-1052 https://dx.doi.org/10.1007/s10967-014-3450-1 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 302 2014 2 31 08 1049-1052 |
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10.1007/s10967-014-3450-1 doi (DE-627)SPR015195821 (SPR)s10967-014-3450-1-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Srivastava, Alok verfasserin aut Study of naturally occurring radioactive material (NORM) in top soil of Punjab State from the North Western part of India 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The concentration levels of 238U, 232 Th, 40K and 137Cs in top soils of State of Punjab located in the North Western part of India were measured using conventional low background gamma ray spectrometric setup as well as Compton suppressed gamma ray spectrometric setup. The radioactivity level of 238U and 232Th was found to vary between 15 Bq/kg and 27 Bq/kg and between 16 Bq/kg and 57 Bq/kg respectively. The radioactivity level of 40K was found to vary between 266 Bq/kg and 799 Bq/kg. The mean radioactivity level of the NORM in general was found to be similar to what is expected as a result of their normal abundance. NORM (dpeaa)DE-He213 Top soil (dpeaa)DE-He213 U (dpeaa)DE-He213 Th (dpeaa)DE-He213 K (dpeaa)DE-He213 Gamma ray spectrometry (dpeaa)DE-He213 Compton suppression system (dpeaa)DE-He213 Lahiri, Susanta verfasserin aut Maiti, Moumita verfasserin aut Knolle, F. verfasserin aut Hoyler, F. verfasserin aut Scherer, U. W. verfasserin aut Schnug, E. W. verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 302(2014), 2 vom: 31. Aug., Seite 1049-1052 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:302 year:2014 number:2 day:31 month:08 pages:1049-1052 https://dx.doi.org/10.1007/s10967-014-3450-1 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 302 2014 2 31 08 1049-1052 |
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10.1007/s10967-014-3450-1 doi (DE-627)SPR015195821 (SPR)s10967-014-3450-1-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Srivastava, Alok verfasserin aut Study of naturally occurring radioactive material (NORM) in top soil of Punjab State from the North Western part of India 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The concentration levels of 238U, 232 Th, 40K and 137Cs in top soils of State of Punjab located in the North Western part of India were measured using conventional low background gamma ray spectrometric setup as well as Compton suppressed gamma ray spectrometric setup. The radioactivity level of 238U and 232Th was found to vary between 15 Bq/kg and 27 Bq/kg and between 16 Bq/kg and 57 Bq/kg respectively. The radioactivity level of 40K was found to vary between 266 Bq/kg and 799 Bq/kg. The mean radioactivity level of the NORM in general was found to be similar to what is expected as a result of their normal abundance. NORM (dpeaa)DE-He213 Top soil (dpeaa)DE-He213 U (dpeaa)DE-He213 Th (dpeaa)DE-He213 K (dpeaa)DE-He213 Gamma ray spectrometry (dpeaa)DE-He213 Compton suppression system (dpeaa)DE-He213 Lahiri, Susanta verfasserin aut Maiti, Moumita verfasserin aut Knolle, F. verfasserin aut Hoyler, F. verfasserin aut Scherer, U. W. verfasserin aut Schnug, E. W. verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 302(2014), 2 vom: 31. Aug., Seite 1049-1052 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:302 year:2014 number:2 day:31 month:08 pages:1049-1052 https://dx.doi.org/10.1007/s10967-014-3450-1 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 302 2014 2 31 08 1049-1052 |
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Srivastava, Alok @@aut@@ Lahiri, Susanta @@aut@@ Maiti, Moumita @@aut@@ Knolle, F. @@aut@@ Hoyler, F. @@aut@@ Scherer, U. W. @@aut@@ Schnug, E. W. @@aut@@ |
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The radioactivity level of 238U and 232Th was found to vary between 15 Bq/kg and 27 Bq/kg and between 16 Bq/kg and 57 Bq/kg respectively. The radioactivity level of 40K was found to vary between 266 Bq/kg and 799 Bq/kg. 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Srivastava, Alok |
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Srivastava, Alok ddc 540 bkl 35.00 misc NORM misc Top soil misc U misc Th misc K misc Gamma ray spectrometry misc Compton suppression system Study of naturally occurring radioactive material (NORM) in top soil of Punjab State from the North Western part of India |
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540 ASE 35.00 bkl Study of naturally occurring radioactive material (NORM) in top soil of Punjab State from the North Western part of India NORM (dpeaa)DE-He213 Top soil (dpeaa)DE-He213 U (dpeaa)DE-He213 Th (dpeaa)DE-He213 K (dpeaa)DE-He213 Gamma ray spectrometry (dpeaa)DE-He213 Compton suppression system (dpeaa)DE-He213 |
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ddc 540 bkl 35.00 misc NORM misc Top soil misc U misc Th misc K misc Gamma ray spectrometry misc Compton suppression system |
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Study of naturally occurring radioactive material (NORM) in top soil of Punjab State from the North Western part of India |
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Study of naturally occurring radioactive material (NORM) in top soil of Punjab State from the North Western part of India |
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Srivastava, Alok Lahiri, Susanta Maiti, Moumita Knolle, F. Hoyler, F. Scherer, U. W. Schnug, E. W. |
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study of naturally occurring radioactive material (norm) in top soil of punjab state from the north western part of india |
| title_auth |
Study of naturally occurring radioactive material (NORM) in top soil of Punjab State from the North Western part of India |
| abstract |
Abstract The concentration levels of 238U, 232 Th, 40K and 137Cs in top soils of State of Punjab located in the North Western part of India were measured using conventional low background gamma ray spectrometric setup as well as Compton suppressed gamma ray spectrometric setup. The radioactivity level of 238U and 232Th was found to vary between 15 Bq/kg and 27 Bq/kg and between 16 Bq/kg and 57 Bq/kg respectively. The radioactivity level of 40K was found to vary between 266 Bq/kg and 799 Bq/kg. The mean radioactivity level of the NORM in general was found to be similar to what is expected as a result of their normal abundance. |
| abstractGer |
Abstract The concentration levels of 238U, 232 Th, 40K and 137Cs in top soils of State of Punjab located in the North Western part of India were measured using conventional low background gamma ray spectrometric setup as well as Compton suppressed gamma ray spectrometric setup. The radioactivity level of 238U and 232Th was found to vary between 15 Bq/kg and 27 Bq/kg and between 16 Bq/kg and 57 Bq/kg respectively. The radioactivity level of 40K was found to vary between 266 Bq/kg and 799 Bq/kg. The mean radioactivity level of the NORM in general was found to be similar to what is expected as a result of their normal abundance. |
| abstract_unstemmed |
Abstract The concentration levels of 238U, 232 Th, 40K and 137Cs in top soils of State of Punjab located in the North Western part of India were measured using conventional low background gamma ray spectrometric setup as well as Compton suppressed gamma ray spectrometric setup. The radioactivity level of 238U and 232Th was found to vary between 15 Bq/kg and 27 Bq/kg and between 16 Bq/kg and 57 Bq/kg respectively. The radioactivity level of 40K was found to vary between 266 Bq/kg and 799 Bq/kg. The mean radioactivity level of the NORM in general was found to be similar to what is expected as a result of their normal abundance. |
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| title_short |
Study of naturally occurring radioactive material (NORM) in top soil of Punjab State from the North Western part of India |
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https://dx.doi.org/10.1007/s10967-014-3450-1 |
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Lahiri, Susanta Maiti, Moumita Knolle, F. Hoyler, F. Scherer, U. W. Schnug, E. W. |
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Lahiri, Susanta Maiti, Moumita Knolle, F. Hoyler, F. Scherer, U. W. Schnug, E. W. |
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10.1007/s10967-014-3450-1 |
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2024-07-03T14:34:43.163Z |
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| score |
7.401354 |