Studying the kinetics of 137Cs selective sorption by the dynamic method with the measurement of radioactivity in the sorbent solid phase
Abstract The dynamic method was proposed for studying the kinetics of 137Cs selective sorption by the measurement of the 137Cs activity directly in the sorbent solid phase. A thin layer of the sorbent in a disposable syringe membrane filter (MF) was eluted with a 137Cs solution containing $ K^{+} $...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Popov, V. E. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2011 |
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| Schlagwörter: |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2011 |
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| Übergeordnetes Werk: |
Enthalten in: Eurasian soil science - Moscow : MAIK Nauka/Interperiodica Publ., 1996, 44(2011), 5 vom: Mai, Seite 510-516 |
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| Übergeordnetes Werk: |
volume:44 ; year:2011 ; number:5 ; month:05 ; pages:510-516 |
| Links: |
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| DOI / URN: |
10.1134/S1064229311030100 |
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| Katalog-ID: |
SPR019953607 |
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| 100 | 1 | |a Popov, V. E. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Studying the kinetics of 137Cs selective sorption by the dynamic method with the measurement of radioactivity in the sorbent solid phase |
| 264 | 1 | |c 2011 | |
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| 520 | |a Abstract The dynamic method was proposed for studying the kinetics of 137Cs selective sorption by the measurement of the 137Cs activity directly in the sorbent solid phase. A thin layer of the sorbent in a disposable syringe membrane filter (MF) was eluted with a 137Cs solution containing $ K^{+} $ and $ Ca^{2+} $ ions with a gradual decrease in the solution flow rate from 6 to 0.2 $ cm^{3} $/min. The activity of the sorbed 137Cs was determined periodically by placing the same MF in the detector well of a Wizard 1480 gamma counter. It was shown that the masses of the sorbent and water in the MF had no effect on the efficiency of the 137Cs measurement. A linear relationship between the RIP(K) value and the square root of the time for the period between 4 and 30 days was revealed using this method. The relative increase in the RIP(K) with time changed by 6 times (from 0.034 to 0.208 $ days^{−0.5} $) for the soils and by 20 times (from 0.008 to 0.153 $ days^{−0.5} $) for the mineral sorbents. The RIP(K) values measured for the interaction of soddy-podzolic soils with 137Cs during 24 hours using the standard limited volume method were lower than the values determined by the proposed dynamic method for the interaction period of 30 days by 50–100%. | ||
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| 650 | 4 | |a Clinoptilolite |7 (dpeaa)DE-He213 | |
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| 650 | 4 | |a Solution Flow Rate |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Ilicheva, N. S. |4 aut | |
| 700 | 1 | |a Maslova, K. M. |4 aut | |
| 700 | 1 | |a Stepina, I. A. |4 aut | |
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10.1134/S1064229311030100 doi (DE-627)SPR019953607 (SPR)S1064229311030100-e DE-627 ger DE-627 rakwb eng Popov, V. E. verfasserin aut Studying the kinetics of 137Cs selective sorption by the dynamic method with the measurement of radioactivity in the sorbent solid phase 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract The dynamic method was proposed for studying the kinetics of 137Cs selective sorption by the measurement of the 137Cs activity directly in the sorbent solid phase. A thin layer of the sorbent in a disposable syringe membrane filter (MF) was eluted with a 137Cs solution containing $ K^{+} $ and $ Ca^{2+} $ ions with a gradual decrease in the solution flow rate from 6 to 0.2 $ cm^{3} $/min. The activity of the sorbed 137Cs was determined periodically by placing the same MF in the detector well of a Wizard 1480 gamma counter. It was shown that the masses of the sorbent and water in the MF had no effect on the efficiency of the 137Cs measurement. A linear relationship between the RIP(K) value and the square root of the time for the period between 4 and 30 days was revealed using this method. The relative increase in the RIP(K) with time changed by 6 times (from 0.034 to 0.208 $ days^{−0.5} $) for the soils and by 20 times (from 0.008 to 0.153 $ days^{−0.5} $) for the mineral sorbents. The RIP(K) values measured for the interaction of soddy-podzolic soils with 137Cs during 24 hours using the standard limited volume method were lower than the values determined by the proposed dynamic method for the interaction period of 30 days by 50–100%. EURASIAN Soil Science (dpeaa)DE-He213 Clinoptilolite (dpeaa)DE-He213 137Cs Activity (dpeaa)DE-He213 Soddy Podzolic Soil (dpeaa)DE-He213 Solution Flow Rate (dpeaa)DE-He213 Ilicheva, N. S. aut Maslova, K. M. aut Stepina, I. A. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2011), 5 vom: Mai, Seite 510-516 (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:44 year:2011 number:5 month:05 pages:510-516 https://dx.doi.org/10.1134/S1064229311030100 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 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_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_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 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 AR 44 2011 5 05 510-516 |
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10.1134/S1064229311030100 doi (DE-627)SPR019953607 (SPR)S1064229311030100-e DE-627 ger DE-627 rakwb eng Popov, V. E. verfasserin aut Studying the kinetics of 137Cs selective sorption by the dynamic method with the measurement of radioactivity in the sorbent solid phase 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract The dynamic method was proposed for studying the kinetics of 137Cs selective sorption by the measurement of the 137Cs activity directly in the sorbent solid phase. A thin layer of the sorbent in a disposable syringe membrane filter (MF) was eluted with a 137Cs solution containing $ K^{+} $ and $ Ca^{2+} $ ions with a gradual decrease in the solution flow rate from 6 to 0.2 $ cm^{3} $/min. The activity of the sorbed 137Cs was determined periodically by placing the same MF in the detector well of a Wizard 1480 gamma counter. It was shown that the masses of the sorbent and water in the MF had no effect on the efficiency of the 137Cs measurement. A linear relationship between the RIP(K) value and the square root of the time for the period between 4 and 30 days was revealed using this method. The relative increase in the RIP(K) with time changed by 6 times (from 0.034 to 0.208 $ days^{−0.5} $) for the soils and by 20 times (from 0.008 to 0.153 $ days^{−0.5} $) for the mineral sorbents. The RIP(K) values measured for the interaction of soddy-podzolic soils with 137Cs during 24 hours using the standard limited volume method were lower than the values determined by the proposed dynamic method for the interaction period of 30 days by 50–100%. EURASIAN Soil Science (dpeaa)DE-He213 Clinoptilolite (dpeaa)DE-He213 137Cs Activity (dpeaa)DE-He213 Soddy Podzolic Soil (dpeaa)DE-He213 Solution Flow Rate (dpeaa)DE-He213 Ilicheva, N. S. aut Maslova, K. M. aut Stepina, I. A. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2011), 5 vom: Mai, Seite 510-516 (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:44 year:2011 number:5 month:05 pages:510-516 https://dx.doi.org/10.1134/S1064229311030100 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 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_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_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 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 AR 44 2011 5 05 510-516 |
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10.1134/S1064229311030100 doi (DE-627)SPR019953607 (SPR)S1064229311030100-e DE-627 ger DE-627 rakwb eng Popov, V. E. verfasserin aut Studying the kinetics of 137Cs selective sorption by the dynamic method with the measurement of radioactivity in the sorbent solid phase 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract The dynamic method was proposed for studying the kinetics of 137Cs selective sorption by the measurement of the 137Cs activity directly in the sorbent solid phase. A thin layer of the sorbent in a disposable syringe membrane filter (MF) was eluted with a 137Cs solution containing $ K^{+} $ and $ Ca^{2+} $ ions with a gradual decrease in the solution flow rate from 6 to 0.2 $ cm^{3} $/min. The activity of the sorbed 137Cs was determined periodically by placing the same MF in the detector well of a Wizard 1480 gamma counter. It was shown that the masses of the sorbent and water in the MF had no effect on the efficiency of the 137Cs measurement. A linear relationship between the RIP(K) value and the square root of the time for the period between 4 and 30 days was revealed using this method. The relative increase in the RIP(K) with time changed by 6 times (from 0.034 to 0.208 $ days^{−0.5} $) for the soils and by 20 times (from 0.008 to 0.153 $ days^{−0.5} $) for the mineral sorbents. The RIP(K) values measured for the interaction of soddy-podzolic soils with 137Cs during 24 hours using the standard limited volume method were lower than the values determined by the proposed dynamic method for the interaction period of 30 days by 50–100%. EURASIAN Soil Science (dpeaa)DE-He213 Clinoptilolite (dpeaa)DE-He213 137Cs Activity (dpeaa)DE-He213 Soddy Podzolic Soil (dpeaa)DE-He213 Solution Flow Rate (dpeaa)DE-He213 Ilicheva, N. S. aut Maslova, K. M. aut Stepina, I. A. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2011), 5 vom: Mai, Seite 510-516 (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:44 year:2011 number:5 month:05 pages:510-516 https://dx.doi.org/10.1134/S1064229311030100 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 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_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_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 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 AR 44 2011 5 05 510-516 |
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10.1134/S1064229311030100 doi (DE-627)SPR019953607 (SPR)S1064229311030100-e DE-627 ger DE-627 rakwb eng Popov, V. E. verfasserin aut Studying the kinetics of 137Cs selective sorption by the dynamic method with the measurement of radioactivity in the sorbent solid phase 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract The dynamic method was proposed for studying the kinetics of 137Cs selective sorption by the measurement of the 137Cs activity directly in the sorbent solid phase. A thin layer of the sorbent in a disposable syringe membrane filter (MF) was eluted with a 137Cs solution containing $ K^{+} $ and $ Ca^{2+} $ ions with a gradual decrease in the solution flow rate from 6 to 0.2 $ cm^{3} $/min. The activity of the sorbed 137Cs was determined periodically by placing the same MF in the detector well of a Wizard 1480 gamma counter. It was shown that the masses of the sorbent and water in the MF had no effect on the efficiency of the 137Cs measurement. A linear relationship between the RIP(K) value and the square root of the time for the period between 4 and 30 days was revealed using this method. The relative increase in the RIP(K) with time changed by 6 times (from 0.034 to 0.208 $ days^{−0.5} $) for the soils and by 20 times (from 0.008 to 0.153 $ days^{−0.5} $) for the mineral sorbents. The RIP(K) values measured for the interaction of soddy-podzolic soils with 137Cs during 24 hours using the standard limited volume method were lower than the values determined by the proposed dynamic method for the interaction period of 30 days by 50–100%. EURASIAN Soil Science (dpeaa)DE-He213 Clinoptilolite (dpeaa)DE-He213 137Cs Activity (dpeaa)DE-He213 Soddy Podzolic Soil (dpeaa)DE-He213 Solution Flow Rate (dpeaa)DE-He213 Ilicheva, N. S. aut Maslova, K. M. aut Stepina, I. A. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2011), 5 vom: Mai, Seite 510-516 (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:44 year:2011 number:5 month:05 pages:510-516 https://dx.doi.org/10.1134/S1064229311030100 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 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_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_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 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 AR 44 2011 5 05 510-516 |
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10.1134/S1064229311030100 doi (DE-627)SPR019953607 (SPR)S1064229311030100-e DE-627 ger DE-627 rakwb eng Popov, V. E. verfasserin aut Studying the kinetics of 137Cs selective sorption by the dynamic method with the measurement of radioactivity in the sorbent solid phase 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract The dynamic method was proposed for studying the kinetics of 137Cs selective sorption by the measurement of the 137Cs activity directly in the sorbent solid phase. A thin layer of the sorbent in a disposable syringe membrane filter (MF) was eluted with a 137Cs solution containing $ K^{+} $ and $ Ca^{2+} $ ions with a gradual decrease in the solution flow rate from 6 to 0.2 $ cm^{3} $/min. The activity of the sorbed 137Cs was determined periodically by placing the same MF in the detector well of a Wizard 1480 gamma counter. It was shown that the masses of the sorbent and water in the MF had no effect on the efficiency of the 137Cs measurement. A linear relationship between the RIP(K) value and the square root of the time for the period between 4 and 30 days was revealed using this method. The relative increase in the RIP(K) with time changed by 6 times (from 0.034 to 0.208 $ days^{−0.5} $) for the soils and by 20 times (from 0.008 to 0.153 $ days^{−0.5} $) for the mineral sorbents. The RIP(K) values measured for the interaction of soddy-podzolic soils with 137Cs during 24 hours using the standard limited volume method were lower than the values determined by the proposed dynamic method for the interaction period of 30 days by 50–100%. EURASIAN Soil Science (dpeaa)DE-He213 Clinoptilolite (dpeaa)DE-He213 137Cs Activity (dpeaa)DE-He213 Soddy Podzolic Soil (dpeaa)DE-He213 Solution Flow Rate (dpeaa)DE-He213 Ilicheva, N. S. aut Maslova, K. M. aut Stepina, I. A. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2011), 5 vom: Mai, Seite 510-516 (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:44 year:2011 number:5 month:05 pages:510-516 https://dx.doi.org/10.1134/S1064229311030100 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 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_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_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 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 AR 44 2011 5 05 510-516 |
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A thin layer of the sorbent in a disposable syringe membrane filter (MF) was eluted with a 137Cs solution containing $ K^{+} $ and $ Ca^{2+} $ ions with a gradual decrease in the solution flow rate from 6 to 0.2 $ cm^{3} $/min. The activity of the sorbed 137Cs was determined periodically by placing the same MF in the detector well of a Wizard 1480 gamma counter. It was shown that the masses of the sorbent and water in the MF had no effect on the efficiency of the 137Cs measurement. A linear relationship between the RIP(K) value and the square root of the time for the period between 4 and 30 days was revealed using this method. The relative increase in the RIP(K) with time changed by 6 times (from 0.034 to 0.208 $ days^{−0.5} $) for the soils and by 20 times (from 0.008 to 0.153 $ days^{−0.5} $) for the mineral sorbents. The RIP(K) values measured for the interaction of soddy-podzolic soils with 137Cs during 24 hours using the standard limited volume method were lower than the values determined by the proposed dynamic method for the interaction period of 30 days by 50–100%.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">EURASIAN Soil Science</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Clinoptilolite</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">137Cs Activity</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Soddy Podzolic Soil</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Solution Flow Rate</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ilicheva, N. 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Popov, V. E. |
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Popov, V. E. misc EURASIAN Soil Science misc Clinoptilolite misc 137Cs Activity misc Soddy Podzolic Soil misc Solution Flow Rate Studying the kinetics of 137Cs selective sorption by the dynamic method with the measurement of radioactivity in the sorbent solid phase |
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Studying the kinetics of 137Cs selective sorption by the dynamic method with the measurement of radioactivity in the sorbent solid phase EURASIAN Soil Science (dpeaa)DE-He213 Clinoptilolite (dpeaa)DE-He213 137Cs Activity (dpeaa)DE-He213 Soddy Podzolic Soil (dpeaa)DE-He213 Solution Flow Rate (dpeaa)DE-He213 |
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misc EURASIAN Soil Science misc Clinoptilolite misc 137Cs Activity misc Soddy Podzolic Soil misc Solution Flow Rate |
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Studying the kinetics of 137Cs selective sorption by the dynamic method with the measurement of radioactivity in the sorbent solid phase |
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Studying the kinetics of 137Cs selective sorption by the dynamic method with the measurement of radioactivity in the sorbent solid phase |
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Popov, V. E. |
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10.1134/S1064229311030100 |
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studying the kinetics of 137cs selective sorption by the dynamic method with the measurement of radioactivity in the sorbent solid phase |
| title_auth |
Studying the kinetics of 137Cs selective sorption by the dynamic method with the measurement of radioactivity in the sorbent solid phase |
| abstract |
Abstract The dynamic method was proposed for studying the kinetics of 137Cs selective sorption by the measurement of the 137Cs activity directly in the sorbent solid phase. A thin layer of the sorbent in a disposable syringe membrane filter (MF) was eluted with a 137Cs solution containing $ K^{+} $ and $ Ca^{2+} $ ions with a gradual decrease in the solution flow rate from 6 to 0.2 $ cm^{3} $/min. The activity of the sorbed 137Cs was determined periodically by placing the same MF in the detector well of a Wizard 1480 gamma counter. It was shown that the masses of the sorbent and water in the MF had no effect on the efficiency of the 137Cs measurement. A linear relationship between the RIP(K) value and the square root of the time for the period between 4 and 30 days was revealed using this method. The relative increase in the RIP(K) with time changed by 6 times (from 0.034 to 0.208 $ days^{−0.5} $) for the soils and by 20 times (from 0.008 to 0.153 $ days^{−0.5} $) for the mineral sorbents. The RIP(K) values measured for the interaction of soddy-podzolic soils with 137Cs during 24 hours using the standard limited volume method were lower than the values determined by the proposed dynamic method for the interaction period of 30 days by 50–100%. © Pleiades Publishing, Ltd. 2011 |
| abstractGer |
Abstract The dynamic method was proposed for studying the kinetics of 137Cs selective sorption by the measurement of the 137Cs activity directly in the sorbent solid phase. A thin layer of the sorbent in a disposable syringe membrane filter (MF) was eluted with a 137Cs solution containing $ K^{+} $ and $ Ca^{2+} $ ions with a gradual decrease in the solution flow rate from 6 to 0.2 $ cm^{3} $/min. The activity of the sorbed 137Cs was determined periodically by placing the same MF in the detector well of a Wizard 1480 gamma counter. It was shown that the masses of the sorbent and water in the MF had no effect on the efficiency of the 137Cs measurement. A linear relationship between the RIP(K) value and the square root of the time for the period between 4 and 30 days was revealed using this method. The relative increase in the RIP(K) with time changed by 6 times (from 0.034 to 0.208 $ days^{−0.5} $) for the soils and by 20 times (from 0.008 to 0.153 $ days^{−0.5} $) for the mineral sorbents. The RIP(K) values measured for the interaction of soddy-podzolic soils with 137Cs during 24 hours using the standard limited volume method were lower than the values determined by the proposed dynamic method for the interaction period of 30 days by 50–100%. © Pleiades Publishing, Ltd. 2011 |
| abstract_unstemmed |
Abstract The dynamic method was proposed for studying the kinetics of 137Cs selective sorption by the measurement of the 137Cs activity directly in the sorbent solid phase. A thin layer of the sorbent in a disposable syringe membrane filter (MF) was eluted with a 137Cs solution containing $ K^{+} $ and $ Ca^{2+} $ ions with a gradual decrease in the solution flow rate from 6 to 0.2 $ cm^{3} $/min. The activity of the sorbed 137Cs was determined periodically by placing the same MF in the detector well of a Wizard 1480 gamma counter. It was shown that the masses of the sorbent and water in the MF had no effect on the efficiency of the 137Cs measurement. A linear relationship between the RIP(K) value and the square root of the time for the period between 4 and 30 days was revealed using this method. The relative increase in the RIP(K) with time changed by 6 times (from 0.034 to 0.208 $ days^{−0.5} $) for the soils and by 20 times (from 0.008 to 0.153 $ days^{−0.5} $) for the mineral sorbents. The RIP(K) values measured for the interaction of soddy-podzolic soils with 137Cs during 24 hours using the standard limited volume method were lower than the values determined by the proposed dynamic method for the interaction period of 30 days by 50–100%. © Pleiades Publishing, Ltd. 2011 |
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Studying the kinetics of 137Cs selective sorption by the dynamic method with the measurement of radioactivity in the sorbent solid phase |
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Ilicheva, N. S. Maslova, K. M. Stepina, I. A. |
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| score |
7.40226 |