Effect of humic acids and iron hydroxides deposited on the surface of clay minerals on the 137Cs immobilization

Abstract The effect exerted on the relationships of 137Cs sorption by humic acids and iron hydroxides deposited on the surface of clay minerals, montmorillonite and kaolinite, differing in the exchange capacity, was studied. The presence of humic acids and Fe(OH)3 deposited on the mineral surface le...
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Autor*in:	Kobets, S. A. [verfasserIn] Fedorova, V. M. [verfasserIn] Pshinko, G. N. [verfasserIn] Kosorukov, A. A. [verfasserIn] Demchenko, V. Ya. [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2014

Schlagwörter:	cesium-137 clay minerals precipitated iron hydroxides humic acids immobilization

Übergeordnetes Werk:	Enthalten in: Radiochemistry - Moscow : MAIK Nauka / Interperiodica Publ., 2001, 56(2014), 3 vom: Mai, Seite 325-331
Übergeordnetes Werk:	volume:56 ; year:2014 ; number:3 ; month:05 ; pages:325-331

Links:	Volltext

DOI / URN:	10.1134/S1066362214030175

Katalog-ID:	SPR017016134

Internformat


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520			\|a Abstract The effect exerted on the relationships of 137Cs sorption by humic acids and iron hydroxides deposited on the surface of clay minerals, montmorillonite and kaolinite, differing in the exchange capacity, was studied. The presence of humic acids and Fe(OH)3 deposited on the mineral surface leads to an increase in the 137Cs sorption in a wide pH range (pH 4–9), suggesting the participation of functional groups of humic acids and ferrinol groups of iron(III) hydroxide in binding of the metal ions. The $ Na^{+} $, $ K^{+} $, and $ Ca^{2+} $ ions, on the contrary, with an increase in their concentration in aqueous solution decrease the immobilization of cesium radionuclides and favor their migration in the environment.
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650		4	\|a clay minerals \|7 (dpeaa)DE-He213
650		4	\|a precipitated iron hydroxides \|7 (dpeaa)DE-He213
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650		4	\|a immobilization \|7 (dpeaa)DE-He213
700	1		\|a Fedorova, V. M. \|e verfasserin \|4 aut
700	1		\|a Pshinko, G. N. \|e verfasserin \|4 aut
700	1		\|a Kosorukov, A. A. \|e verfasserin \|4 aut
700	1		\|a Demchenko, V. Ya. \|e verfasserin \|4 aut
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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
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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_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
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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_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_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
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912			\|a GBV_ILN_4338
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Indexfelder

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publishDate	2014
allfields	10.1134/S1066362214030175 doi (DE-627)SPR017016134 (SPR)S1066362214030175-e DE-627 ger DE-627 rakwb eng 530 620 ASE 35.15 bkl Kobets, S. A. verfasserin aut Effect of humic acids and iron hydroxides deposited on the surface of clay minerals on the 137Cs immobilization 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The effect exerted on the relationships of 137Cs sorption by humic acids and iron hydroxides deposited on the surface of clay minerals, montmorillonite and kaolinite, differing in the exchange capacity, was studied. The presence of humic acids and Fe(OH)3 deposited on the mineral surface leads to an increase in the 137Cs sorption in a wide pH range (pH 4–9), suggesting the participation of functional groups of humic acids and ferrinol groups of iron(III) hydroxide in binding of the metal ions. The $ Na^{+} $, $ K^{+} $, and $ Ca^{2+} $ ions, on the contrary, with an increase in their concentration in aqueous solution decrease the immobilization of cesium radionuclides and favor their migration in the environment. cesium-137 (dpeaa)DE-He213 clay minerals (dpeaa)DE-He213 precipitated iron hydroxides (dpeaa)DE-He213 humic acids (dpeaa)DE-He213 immobilization (dpeaa)DE-He213 Fedorova, V. M. verfasserin aut Pshinko, G. N. verfasserin aut Kosorukov, A. A. verfasserin aut Demchenko, V. Ya. verfasserin aut Enthalten in Radiochemistry Moscow : MAIK Nauka / Interperiodica Publ., 2001 56(2014), 3 vom: Mai, Seite 325-331 (DE-627)336156294 (DE-600)2060914-0 1608-3288 nnns volume:56 year:2014 number:3 month:05 pages:325-331 https://dx.doi.org/10.1134/S1066362214030175 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_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_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 35.15 ASE AR 56 2014 3 05 325-331
spelling	10.1134/S1066362214030175 doi (DE-627)SPR017016134 (SPR)S1066362214030175-e DE-627 ger DE-627 rakwb eng 530 620 ASE 35.15 bkl Kobets, S. A. verfasserin aut Effect of humic acids and iron hydroxides deposited on the surface of clay minerals on the 137Cs immobilization 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The effect exerted on the relationships of 137Cs sorption by humic acids and iron hydroxides deposited on the surface of clay minerals, montmorillonite and kaolinite, differing in the exchange capacity, was studied. The presence of humic acids and Fe(OH)3 deposited on the mineral surface leads to an increase in the 137Cs sorption in a wide pH range (pH 4–9), suggesting the participation of functional groups of humic acids and ferrinol groups of iron(III) hydroxide in binding of the metal ions. The $ Na^{+} $, $ K^{+} $, and $ Ca^{2+} $ ions, on the contrary, with an increase in their concentration in aqueous solution decrease the immobilization of cesium radionuclides and favor their migration in the environment. cesium-137 (dpeaa)DE-He213 clay minerals (dpeaa)DE-He213 precipitated iron hydroxides (dpeaa)DE-He213 humic acids (dpeaa)DE-He213 immobilization (dpeaa)DE-He213 Fedorova, V. M. verfasserin aut Pshinko, G. N. verfasserin aut Kosorukov, A. A. verfasserin aut Demchenko, V. Ya. verfasserin aut Enthalten in Radiochemistry Moscow : MAIK Nauka / Interperiodica Publ., 2001 56(2014), 3 vom: Mai, Seite 325-331 (DE-627)336156294 (DE-600)2060914-0 1608-3288 nnns volume:56 year:2014 number:3 month:05 pages:325-331 https://dx.doi.org/10.1134/S1066362214030175 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_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_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 35.15 ASE AR 56 2014 3 05 325-331
allfields_unstemmed	10.1134/S1066362214030175 doi (DE-627)SPR017016134 (SPR)S1066362214030175-e DE-627 ger DE-627 rakwb eng 530 620 ASE 35.15 bkl Kobets, S. A. verfasserin aut Effect of humic acids and iron hydroxides deposited on the surface of clay minerals on the 137Cs immobilization 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The effect exerted on the relationships of 137Cs sorption by humic acids and iron hydroxides deposited on the surface of clay minerals, montmorillonite and kaolinite, differing in the exchange capacity, was studied. The presence of humic acids and Fe(OH)3 deposited on the mineral surface leads to an increase in the 137Cs sorption in a wide pH range (pH 4–9), suggesting the participation of functional groups of humic acids and ferrinol groups of iron(III) hydroxide in binding of the metal ions. The $ Na^{+} $, $ K^{+} $, and $ Ca^{2+} $ ions, on the contrary, with an increase in their concentration in aqueous solution decrease the immobilization of cesium radionuclides and favor their migration in the environment. cesium-137 (dpeaa)DE-He213 clay minerals (dpeaa)DE-He213 precipitated iron hydroxides (dpeaa)DE-He213 humic acids (dpeaa)DE-He213 immobilization (dpeaa)DE-He213 Fedorova, V. M. verfasserin aut Pshinko, G. N. verfasserin aut Kosorukov, A. A. verfasserin aut Demchenko, V. Ya. verfasserin aut Enthalten in Radiochemistry Moscow : MAIK Nauka / Interperiodica Publ., 2001 56(2014), 3 vom: Mai, Seite 325-331 (DE-627)336156294 (DE-600)2060914-0 1608-3288 nnns volume:56 year:2014 number:3 month:05 pages:325-331 https://dx.doi.org/10.1134/S1066362214030175 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_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_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 35.15 ASE AR 56 2014 3 05 325-331
allfieldsGer	10.1134/S1066362214030175 doi (DE-627)SPR017016134 (SPR)S1066362214030175-e DE-627 ger DE-627 rakwb eng 530 620 ASE 35.15 bkl Kobets, S. A. verfasserin aut Effect of humic acids and iron hydroxides deposited on the surface of clay minerals on the 137Cs immobilization 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The effect exerted on the relationships of 137Cs sorption by humic acids and iron hydroxides deposited on the surface of clay minerals, montmorillonite and kaolinite, differing in the exchange capacity, was studied. The presence of humic acids and Fe(OH)3 deposited on the mineral surface leads to an increase in the 137Cs sorption in a wide pH range (pH 4–9), suggesting the participation of functional groups of humic acids and ferrinol groups of iron(III) hydroxide in binding of the metal ions. The $ Na^{+} $, $ K^{+} $, and $ Ca^{2+} $ ions, on the contrary, with an increase in their concentration in aqueous solution decrease the immobilization of cesium radionuclides and favor their migration in the environment. cesium-137 (dpeaa)DE-He213 clay minerals (dpeaa)DE-He213 precipitated iron hydroxides (dpeaa)DE-He213 humic acids (dpeaa)DE-He213 immobilization (dpeaa)DE-He213 Fedorova, V. M. verfasserin aut Pshinko, G. N. verfasserin aut Kosorukov, A. A. verfasserin aut Demchenko, V. Ya. verfasserin aut Enthalten in Radiochemistry Moscow : MAIK Nauka / Interperiodica Publ., 2001 56(2014), 3 vom: Mai, Seite 325-331 (DE-627)336156294 (DE-600)2060914-0 1608-3288 nnns volume:56 year:2014 number:3 month:05 pages:325-331 https://dx.doi.org/10.1134/S1066362214030175 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_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_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 35.15 ASE AR 56 2014 3 05 325-331
allfieldsSound	10.1134/S1066362214030175 doi (DE-627)SPR017016134 (SPR)S1066362214030175-e DE-627 ger DE-627 rakwb eng 530 620 ASE 35.15 bkl Kobets, S. A. verfasserin aut Effect of humic acids and iron hydroxides deposited on the surface of clay minerals on the 137Cs immobilization 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The effect exerted on the relationships of 137Cs sorption by humic acids and iron hydroxides deposited on the surface of clay minerals, montmorillonite and kaolinite, differing in the exchange capacity, was studied. The presence of humic acids and Fe(OH)3 deposited on the mineral surface leads to an increase in the 137Cs sorption in a wide pH range (pH 4–9), suggesting the participation of functional groups of humic acids and ferrinol groups of iron(III) hydroxide in binding of the metal ions. The $ Na^{+} $, $ K^{+} $, and $ Ca^{2+} $ ions, on the contrary, with an increase in their concentration in aqueous solution decrease the immobilization of cesium radionuclides and favor their migration in the environment. cesium-137 (dpeaa)DE-He213 clay minerals (dpeaa)DE-He213 precipitated iron hydroxides (dpeaa)DE-He213 humic acids (dpeaa)DE-He213 immobilization (dpeaa)DE-He213 Fedorova, V. M. verfasserin aut Pshinko, G. N. verfasserin aut Kosorukov, A. A. verfasserin aut Demchenko, V. Ya. verfasserin aut Enthalten in Radiochemistry Moscow : MAIK Nauka / Interperiodica Publ., 2001 56(2014), 3 vom: Mai, Seite 325-331 (DE-627)336156294 (DE-600)2060914-0 1608-3288 nnns volume:56 year:2014 number:3 month:05 pages:325-331 https://dx.doi.org/10.1134/S1066362214030175 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_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_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 35.15 ASE AR 56 2014 3 05 325-331
language	English
source	Enthalten in Radiochemistry 56(2014), 3 vom: Mai, Seite 325-331 volume:56 year:2014 number:3 month:05 pages:325-331
sourceStr	Enthalten in Radiochemistry 56(2014), 3 vom: Mai, Seite 325-331 volume:56 year:2014 number:3 month:05 pages:325-331
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	cesium-137 clay minerals precipitated iron hydroxides humic acids immobilization
dewey-raw	530
isfreeaccess_bool	false
container_title	Radiochemistry
authorswithroles_txt_mv	Kobets, S. A. @@aut@@ Fedorova, V. M. @@aut@@ Pshinko, G. N. @@aut@@ Kosorukov, A. A. @@aut@@ Demchenko, V. Ya. @@aut@@
publishDateDaySort_date	2014-05-01T00:00:00Z
hierarchy_top_id	336156294
dewey-sort	3530
id	SPR017016134
language_de	englisch
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author	Kobets, S. A.
spellingShingle	Kobets, S. A. ddc 530 bkl 35.15 misc cesium-137 misc clay minerals misc precipitated iron hydroxides misc humic acids misc immobilization Effect of humic acids and iron hydroxides deposited on the surface of clay minerals on the 137Cs immobilization
authorStr	Kobets, S. A.
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topic_title	530 620 ASE 35.15 bkl Effect of humic acids and iron hydroxides deposited on the surface of clay minerals on the 137Cs immobilization cesium-137 (dpeaa)DE-He213 clay minerals (dpeaa)DE-He213 precipitated iron hydroxides (dpeaa)DE-He213 humic acids (dpeaa)DE-He213 immobilization (dpeaa)DE-He213
topic	ddc 530 bkl 35.15 misc cesium-137 misc clay minerals misc precipitated iron hydroxides misc humic acids misc immobilization
topic_unstemmed	ddc 530 bkl 35.15 misc cesium-137 misc clay minerals misc precipitated iron hydroxides misc humic acids misc immobilization
topic_browse	ddc 530 bkl 35.15 misc cesium-137 misc clay minerals misc precipitated iron hydroxides misc humic acids misc immobilization
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title	Effect of humic acids and iron hydroxides deposited on the surface of clay minerals on the 137Cs immobilization
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title_full	Effect of humic acids and iron hydroxides deposited on the surface of clay minerals on the 137Cs immobilization
author_sort	Kobets, S. A.
journal	Radiochemistry
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author_browse	Kobets, S. A. Fedorova, V. M. Pshinko, G. N. Kosorukov, A. A. Demchenko, V. Ya.
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author-letter	Kobets, S. A.
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title_sort	effect of humic acids and iron hydroxides deposited on the surface of clay minerals on the 137cs immobilization
title_auth	Effect of humic acids and iron hydroxides deposited on the surface of clay minerals on the 137Cs immobilization
abstract	Abstract The effect exerted on the relationships of 137Cs sorption by humic acids and iron hydroxides deposited on the surface of clay minerals, montmorillonite and kaolinite, differing in the exchange capacity, was studied. The presence of humic acids and Fe(OH)3 deposited on the mineral surface leads to an increase in the 137Cs sorption in a wide pH range (pH 4–9), suggesting the participation of functional groups of humic acids and ferrinol groups of iron(III) hydroxide in binding of the metal ions. The $ Na^{+} $, $ K^{+} $, and $ Ca^{2+} $ ions, on the contrary, with an increase in their concentration in aqueous solution decrease the immobilization of cesium radionuclides and favor their migration in the environment.
abstractGer	Abstract The effect exerted on the relationships of 137Cs sorption by humic acids and iron hydroxides deposited on the surface of clay minerals, montmorillonite and kaolinite, differing in the exchange capacity, was studied. The presence of humic acids and Fe(OH)3 deposited on the mineral surface leads to an increase in the 137Cs sorption in a wide pH range (pH 4–9), suggesting the participation of functional groups of humic acids and ferrinol groups of iron(III) hydroxide in binding of the metal ions. The $ Na^{+} $, $ K^{+} $, and $ Ca^{2+} $ ions, on the contrary, with an increase in their concentration in aqueous solution decrease the immobilization of cesium radionuclides and favor their migration in the environment.
abstract_unstemmed	Abstract The effect exerted on the relationships of 137Cs sorption by humic acids and iron hydroxides deposited on the surface of clay minerals, montmorillonite and kaolinite, differing in the exchange capacity, was studied. The presence of humic acids and Fe(OH)3 deposited on the mineral surface leads to an increase in the 137Cs sorption in a wide pH range (pH 4–9), suggesting the participation of functional groups of humic acids and ferrinol groups of iron(III) hydroxide in binding of the metal ions. The $ Na^{+} $, $ K^{+} $, and $ Ca^{2+} $ ions, on the contrary, with an increase in their concentration in aqueous solution decrease the immobilization of cesium radionuclides and favor their migration in the environment.
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container_issue	3
title_short	Effect of humic acids and iron hydroxides deposited on the surface of clay minerals on the 137Cs immobilization
url	https://dx.doi.org/10.1134/S1066362214030175
remote_bool	true
author2	Fedorova, V. M. Pshinko, G. N. Kosorukov, A. A. Demchenko, V. Ya
author2Str	Fedorova, V. M. Pshinko, G. N. Kosorukov, A. A. Demchenko, V. Ya
ppnlink	336156294
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doi_str	10.1134/S1066362214030175
up_date	2024-07-04T01:53:26.720Z
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