Specific features of the dynamics of salts in salt-affected soils subjected to long-term seasonal freezing in the south Transbaikal region

Abstract Observations over the dynamics of the freezing-thawing processes and the migration and accumulation of salts in the soils of the Ivolginsk Depression in Buryatia showed the existence of two stages in the annual cycle of salt migration: the short-term desalinization stage alternates with the...
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Gespeichert in:

Autor*in:	Korolyuk, T. V. [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2014

Schlagwörter:	migration of salts coefficient of the seasonal accumulation of salts salinization chemistry salt regime soil degradation

Anmerkung:	© Pleiades Publishing, Ltd. 2014

Übergeordnetes Werk:	Enthalten in: Eurasian soil science - Moscow : MAIK Nauka/Interperiodica Publ., 1996, 47(2014), 5 vom: Mai, Seite 339-352
Übergeordnetes Werk:	volume:47 ; year:2014 ; number:5 ; month:05 ; pages:339-352

Links:	Volltext

DOI / URN:	10.1134/S1064229314050093

Katalog-ID:	SPR019958013

Internformat


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520			\|a Abstract Observations over the dynamics of the freezing-thawing processes and the migration and accumulation of salts in the soils of the Ivolginsk Depression in Buryatia showed the existence of two stages in the annual cycle of salt migration: the short-term desalinization stage alternates with the long-term salinization stage. The latter stage actually combines two phases: the fall and winter phase of the migration of solutions towards the freezing front and the spring phase of the ascending migration of melt water towards the drying soil surface with further concentration of the solutions owing to evapotranspiration. The desalinization stage in the summer is only typical of the upper soil horizons because of the insufficient amount of summer precipitation; moreover, this stage is not observed every year. Thus, the salt regime of the soils of the depression is greatly affected by the seasonal soil freezing; the long-term salinization in the fall, winter, and spring seasons alternates with a short period of the leaching of salts at the end of summer.
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912			\|a GBV_ILN_150
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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
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912			\|a GBV_ILN_224
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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
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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
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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
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912			\|a GBV_ILN_2044
912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2049
912			\|a GBV_ILN_2050
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author_variant	t v k tv tvk
matchkey_str	article:1556195X:2014----::pcfcetrsfhdnmcoslsnatfetdolsbetdoogemesnlre
hierarchy_sort_str	2014
publishDate	2014
allfields	10.1134/S1064229314050093 doi (DE-627)SPR019958013 (SPR)S1064229314050093-e DE-627 ger DE-627 rakwb eng Korolyuk, T. V. verfasserin aut Specific features of the dynamics of salts in salt-affected soils subjected to long-term seasonal freezing in the south Transbaikal region 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2014 Abstract Observations over the dynamics of the freezing-thawing processes and the migration and accumulation of salts in the soils of the Ivolginsk Depression in Buryatia showed the existence of two stages in the annual cycle of salt migration: the short-term desalinization stage alternates with the long-term salinization stage. The latter stage actually combines two phases: the fall and winter phase of the migration of solutions towards the freezing front and the spring phase of the ascending migration of melt water towards the drying soil surface with further concentration of the solutions owing to evapotranspiration. The desalinization stage in the summer is only typical of the upper soil horizons because of the insufficient amount of summer precipitation; moreover, this stage is not observed every year. Thus, the salt regime of the soils of the depression is greatly affected by the seasonal soil freezing; the long-term salinization in the fall, winter, and spring seasons alternates with a short period of the leaching of salts at the end of summer. migration of salts (dpeaa)DE-He213 coefficient of the seasonal accumulation of salts (dpeaa)DE-He213 salinization chemistry (dpeaa)DE-He213 salt regime (dpeaa)DE-He213 soil degradation (dpeaa)DE-He213 Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 47(2014), 5 vom: Mai, Seite 339-352 (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:47 year:2014 number:5 month:05 pages:339-352 https://dx.doi.org/10.1134/S1064229314050093 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_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 47 2014 5 05 339-352
spelling	10.1134/S1064229314050093 doi (DE-627)SPR019958013 (SPR)S1064229314050093-e DE-627 ger DE-627 rakwb eng Korolyuk, T. V. verfasserin aut Specific features of the dynamics of salts in salt-affected soils subjected to long-term seasonal freezing in the south Transbaikal region 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2014 Abstract Observations over the dynamics of the freezing-thawing processes and the migration and accumulation of salts in the soils of the Ivolginsk Depression in Buryatia showed the existence of two stages in the annual cycle of salt migration: the short-term desalinization stage alternates with the long-term salinization stage. The latter stage actually combines two phases: the fall and winter phase of the migration of solutions towards the freezing front and the spring phase of the ascending migration of melt water towards the drying soil surface with further concentration of the solutions owing to evapotranspiration. The desalinization stage in the summer is only typical of the upper soil horizons because of the insufficient amount of summer precipitation; moreover, this stage is not observed every year. Thus, the salt regime of the soils of the depression is greatly affected by the seasonal soil freezing; the long-term salinization in the fall, winter, and spring seasons alternates with a short period of the leaching of salts at the end of summer. migration of salts (dpeaa)DE-He213 coefficient of the seasonal accumulation of salts (dpeaa)DE-He213 salinization chemistry (dpeaa)DE-He213 salt regime (dpeaa)DE-He213 soil degradation (dpeaa)DE-He213 Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 47(2014), 5 vom: Mai, Seite 339-352 (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:47 year:2014 number:5 month:05 pages:339-352 https://dx.doi.org/10.1134/S1064229314050093 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_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 47 2014 5 05 339-352
allfields_unstemmed	10.1134/S1064229314050093 doi (DE-627)SPR019958013 (SPR)S1064229314050093-e DE-627 ger DE-627 rakwb eng Korolyuk, T. V. verfasserin aut Specific features of the dynamics of salts in salt-affected soils subjected to long-term seasonal freezing in the south Transbaikal region 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2014 Abstract Observations over the dynamics of the freezing-thawing processes and the migration and accumulation of salts in the soils of the Ivolginsk Depression in Buryatia showed the existence of two stages in the annual cycle of salt migration: the short-term desalinization stage alternates with the long-term salinization stage. The latter stage actually combines two phases: the fall and winter phase of the migration of solutions towards the freezing front and the spring phase of the ascending migration of melt water towards the drying soil surface with further concentration of the solutions owing to evapotranspiration. The desalinization stage in the summer is only typical of the upper soil horizons because of the insufficient amount of summer precipitation; moreover, this stage is not observed every year. Thus, the salt regime of the soils of the depression is greatly affected by the seasonal soil freezing; the long-term salinization in the fall, winter, and spring seasons alternates with a short period of the leaching of salts at the end of summer. migration of salts (dpeaa)DE-He213 coefficient of the seasonal accumulation of salts (dpeaa)DE-He213 salinization chemistry (dpeaa)DE-He213 salt regime (dpeaa)DE-He213 soil degradation (dpeaa)DE-He213 Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 47(2014), 5 vom: Mai, Seite 339-352 (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:47 year:2014 number:5 month:05 pages:339-352 https://dx.doi.org/10.1134/S1064229314050093 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_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 47 2014 5 05 339-352
allfieldsGer	10.1134/S1064229314050093 doi (DE-627)SPR019958013 (SPR)S1064229314050093-e DE-627 ger DE-627 rakwb eng Korolyuk, T. V. verfasserin aut Specific features of the dynamics of salts in salt-affected soils subjected to long-term seasonal freezing in the south Transbaikal region 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2014 Abstract Observations over the dynamics of the freezing-thawing processes and the migration and accumulation of salts in the soils of the Ivolginsk Depression in Buryatia showed the existence of two stages in the annual cycle of salt migration: the short-term desalinization stage alternates with the long-term salinization stage. The latter stage actually combines two phases: the fall and winter phase of the migration of solutions towards the freezing front and the spring phase of the ascending migration of melt water towards the drying soil surface with further concentration of the solutions owing to evapotranspiration. The desalinization stage in the summer is only typical of the upper soil horizons because of the insufficient amount of summer precipitation; moreover, this stage is not observed every year. Thus, the salt regime of the soils of the depression is greatly affected by the seasonal soil freezing; the long-term salinization in the fall, winter, and spring seasons alternates with a short period of the leaching of salts at the end of summer. migration of salts (dpeaa)DE-He213 coefficient of the seasonal accumulation of salts (dpeaa)DE-He213 salinization chemistry (dpeaa)DE-He213 salt regime (dpeaa)DE-He213 soil degradation (dpeaa)DE-He213 Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 47(2014), 5 vom: Mai, Seite 339-352 (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:47 year:2014 number:5 month:05 pages:339-352 https://dx.doi.org/10.1134/S1064229314050093 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_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 47 2014 5 05 339-352
allfieldsSound	10.1134/S1064229314050093 doi (DE-627)SPR019958013 (SPR)S1064229314050093-e DE-627 ger DE-627 rakwb eng Korolyuk, T. V. verfasserin aut Specific features of the dynamics of salts in salt-affected soils subjected to long-term seasonal freezing in the south Transbaikal region 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2014 Abstract Observations over the dynamics of the freezing-thawing processes and the migration and accumulation of salts in the soils of the Ivolginsk Depression in Buryatia showed the existence of two stages in the annual cycle of salt migration: the short-term desalinization stage alternates with the long-term salinization stage. The latter stage actually combines two phases: the fall and winter phase of the migration of solutions towards the freezing front and the spring phase of the ascending migration of melt water towards the drying soil surface with further concentration of the solutions owing to evapotranspiration. The desalinization stage in the summer is only typical of the upper soil horizons because of the insufficient amount of summer precipitation; moreover, this stage is not observed every year. Thus, the salt regime of the soils of the depression is greatly affected by the seasonal soil freezing; the long-term salinization in the fall, winter, and spring seasons alternates with a short period of the leaching of salts at the end of summer. migration of salts (dpeaa)DE-He213 coefficient of the seasonal accumulation of salts (dpeaa)DE-He213 salinization chemistry (dpeaa)DE-He213 salt regime (dpeaa)DE-He213 soil degradation (dpeaa)DE-He213 Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 47(2014), 5 vom: Mai, Seite 339-352 (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:47 year:2014 number:5 month:05 pages:339-352 https://dx.doi.org/10.1134/S1064229314050093 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_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 47 2014 5 05 339-352
language	English
source	Enthalten in Eurasian soil science 47(2014), 5 vom: Mai, Seite 339-352 volume:47 year:2014 number:5 month:05 pages:339-352
sourceStr	Enthalten in Eurasian soil science 47(2014), 5 vom: Mai, Seite 339-352 volume:47 year:2014 number:5 month:05 pages:339-352
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	migration of salts coefficient of the seasonal accumulation of salts salinization chemistry salt regime soil degradation
isfreeaccess_bool	false
container_title	Eurasian soil science
authorswithroles_txt_mv	Korolyuk, T. V. @@aut@@
publishDateDaySort_date	2014-05-01T00:00:00Z
hierarchy_top_id	341913227
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author	Korolyuk, T. V.
spellingShingle	Korolyuk, T. V. misc migration of salts misc coefficient of the seasonal accumulation of salts misc salinization chemistry misc salt regime misc soil degradation Specific features of the dynamics of salts in salt-affected soils subjected to long-term seasonal freezing in the south Transbaikal region
authorStr	Korolyuk, T. V.
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topic_title	Specific features of the dynamics of salts in salt-affected soils subjected to long-term seasonal freezing in the south Transbaikal region migration of salts (dpeaa)DE-He213 coefficient of the seasonal accumulation of salts (dpeaa)DE-He213 salinization chemistry (dpeaa)DE-He213 salt regime (dpeaa)DE-He213 soil degradation (dpeaa)DE-He213
topic	misc migration of salts misc coefficient of the seasonal accumulation of salts misc salinization chemistry misc salt regime misc soil degradation
topic_unstemmed	misc migration of salts misc coefficient of the seasonal accumulation of salts misc salinization chemistry misc salt regime misc soil degradation
topic_browse	misc migration of salts misc coefficient of the seasonal accumulation of salts misc salinization chemistry misc salt regime misc soil degradation
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title	Specific features of the dynamics of salts in salt-affected soils subjected to long-term seasonal freezing in the south Transbaikal region
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title_full	Specific features of the dynamics of salts in salt-affected soils subjected to long-term seasonal freezing in the south Transbaikal region
author_sort	Korolyuk, T. V.
journal	Eurasian soil science
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author_browse	Korolyuk, T. V.
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author-letter	Korolyuk, T. V.
doi_str_mv	10.1134/S1064229314050093
title_sort	specific features of the dynamics of salts in salt-affected soils subjected to long-term seasonal freezing in the south transbaikal region
title_auth	Specific features of the dynamics of salts in salt-affected soils subjected to long-term seasonal freezing in the south Transbaikal region
abstract	Abstract Observations over the dynamics of the freezing-thawing processes and the migration and accumulation of salts in the soils of the Ivolginsk Depression in Buryatia showed the existence of two stages in the annual cycle of salt migration: the short-term desalinization stage alternates with the long-term salinization stage. The latter stage actually combines two phases: the fall and winter phase of the migration of solutions towards the freezing front and the spring phase of the ascending migration of melt water towards the drying soil surface with further concentration of the solutions owing to evapotranspiration. The desalinization stage in the summer is only typical of the upper soil horizons because of the insufficient amount of summer precipitation; moreover, this stage is not observed every year. Thus, the salt regime of the soils of the depression is greatly affected by the seasonal soil freezing; the long-term salinization in the fall, winter, and spring seasons alternates with a short period of the leaching of salts at the end of summer. © Pleiades Publishing, Ltd. 2014
abstractGer	Abstract Observations over the dynamics of the freezing-thawing processes and the migration and accumulation of salts in the soils of the Ivolginsk Depression in Buryatia showed the existence of two stages in the annual cycle of salt migration: the short-term desalinization stage alternates with the long-term salinization stage. The latter stage actually combines two phases: the fall and winter phase of the migration of solutions towards the freezing front and the spring phase of the ascending migration of melt water towards the drying soil surface with further concentration of the solutions owing to evapotranspiration. The desalinization stage in the summer is only typical of the upper soil horizons because of the insufficient amount of summer precipitation; moreover, this stage is not observed every year. Thus, the salt regime of the soils of the depression is greatly affected by the seasonal soil freezing; the long-term salinization in the fall, winter, and spring seasons alternates with a short period of the leaching of salts at the end of summer. © Pleiades Publishing, Ltd. 2014
abstract_unstemmed	Abstract Observations over the dynamics of the freezing-thawing processes and the migration and accumulation of salts in the soils of the Ivolginsk Depression in Buryatia showed the existence of two stages in the annual cycle of salt migration: the short-term desalinization stage alternates with the long-term salinization stage. The latter stage actually combines two phases: the fall and winter phase of the migration of solutions towards the freezing front and the spring phase of the ascending migration of melt water towards the drying soil surface with further concentration of the solutions owing to evapotranspiration. The desalinization stage in the summer is only typical of the upper soil horizons because of the insufficient amount of summer precipitation; moreover, this stage is not observed every year. Thus, the salt regime of the soils of the depression is greatly affected by the seasonal soil freezing; the long-term salinization in the fall, winter, and spring seasons alternates with a short period of the leaching of salts at the end of summer. © Pleiades Publishing, Ltd. 2014
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title_short	Specific features of the dynamics of salts in salt-affected soils subjected to long-term seasonal freezing in the south Transbaikal region
url	https://dx.doi.org/10.1134/S1064229314050093
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doi_str	10.1134/S1064229314050093
up_date	2024-07-04T03:27:52.518Z
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V.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Specific features of the dynamics of salts in salt-affected soils subjected to long-term seasonal freezing in the south Transbaikal region</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2014</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">© Pleiades Publishing, Ltd. 2014</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Observations over the dynamics of the freezing-thawing processes and the migration and accumulation of salts in the soils of the Ivolginsk Depression in Buryatia showed the existence of two stages in the annual cycle of salt migration: the short-term desalinization stage alternates with the long-term salinization stage. 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Specific features of the dynamics of salts in salt-affected soils subjected to long-term seasonal freezing in the south Transbaikal region

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