Phosphorus in the fulvate fraction of soil organic matter

Abstract The concentration of phosphorus in preparations of fulvic acids separated from soils according to a modified IHSS method varies from 0.03 to 0.23%; it is considerably lower than the concentration of phosphorus in preparations of humic acids (0.15–1.54%). A predominant part (>90%) of phos...
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Autor*in:	Makarov, M. I. [verfasserIn] Leoshkina, N. A.

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2009

Schlagwörter:	Soil Organic Matter Humic Acid Fulvic Acid EURASIAN Soil Science Organic Phosphorus

Anmerkung:	© Pleiades Publishing, Ltd. 2009

Übergeordnetes Werk:	Enthalten in: Eurasian soil science - Moscow : MAIK Nauka/Interperiodica Publ., 1996, 42(2009), 3 vom: März, Seite 277-283
Übergeordnetes Werk:	volume:42 ; year:2009 ; number:3 ; month:03 ; pages:277-283

Links:	Volltext

DOI / URN:	10.1134/S1064229309030041

Katalog-ID:	SPR019949057

Internformat


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520			\|a Abstract The concentration of phosphorus in preparations of fulvic acids separated from soils according to a modified IHSS method varies from 0.03 to 0.23%; it is considerably lower than the concentration of phosphorus in preparations of humic acids (0.15–1.54%). A predominant part (>90%) of phosphorus-containing compounds in the fulvates is not sorbed on the polymethylmethacrylic resin Supelite DAX-8 used for the isolation of fulvic acids. These compounds are highly hydrophilic, and their sorption on the polystyrene-divinylbenzene resin XAD-4 used for the isolation of nonspecific organic compounds with a lower molecular weight and higher hydrophily does not exceed 20%. The results of the study attest to the quantitative indefiniteness of the notion of “phosphorus of fulvic acids” and cause doubt upon a hypothesis about an important role of fulvic acids in the migration of phosphorus compounds in soils and landscapes.
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matchkey_str	article:1556195X:2009----::hshrsnhflaercinfol
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publishDate	2009
allfields	10.1134/S1064229309030041 doi (DE-627)SPR019949057 (SPR)S1064229309030041-e DE-627 ger DE-627 rakwb eng Makarov, M. I. verfasserin aut Phosphorus in the fulvate fraction of soil organic matter 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2009 Abstract The concentration of phosphorus in preparations of fulvic acids separated from soils according to a modified IHSS method varies from 0.03 to 0.23%; it is considerably lower than the concentration of phosphorus in preparations of humic acids (0.15–1.54%). A predominant part (>90%) of phosphorus-containing compounds in the fulvates is not sorbed on the polymethylmethacrylic resin Supelite DAX-8 used for the isolation of fulvic acids. These compounds are highly hydrophilic, and their sorption on the polystyrene-divinylbenzene resin XAD-4 used for the isolation of nonspecific organic compounds with a lower molecular weight and higher hydrophily does not exceed 20%. The results of the study attest to the quantitative indefiniteness of the notion of “phosphorus of fulvic acids” and cause doubt upon a hypothesis about an important role of fulvic acids in the migration of phosphorus compounds in soils and landscapes. Soil Organic Matter (dpeaa)DE-He213 Humic Acid (dpeaa)DE-He213 Fulvic Acid (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Organic Phosphorus (dpeaa)DE-He213 Leoshkina, N. A. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 42(2009), 3 vom: März, Seite 277-283 (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:42 year:2009 number:3 month:03 pages:277-283 https://dx.doi.org/10.1134/S1064229309030041 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 42 2009 3 03 277-283
spelling	10.1134/S1064229309030041 doi (DE-627)SPR019949057 (SPR)S1064229309030041-e DE-627 ger DE-627 rakwb eng Makarov, M. I. verfasserin aut Phosphorus in the fulvate fraction of soil organic matter 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2009 Abstract The concentration of phosphorus in preparations of fulvic acids separated from soils according to a modified IHSS method varies from 0.03 to 0.23%; it is considerably lower than the concentration of phosphorus in preparations of humic acids (0.15–1.54%). A predominant part (>90%) of phosphorus-containing compounds in the fulvates is not sorbed on the polymethylmethacrylic resin Supelite DAX-8 used for the isolation of fulvic acids. These compounds are highly hydrophilic, and their sorption on the polystyrene-divinylbenzene resin XAD-4 used for the isolation of nonspecific organic compounds with a lower molecular weight and higher hydrophily does not exceed 20%. The results of the study attest to the quantitative indefiniteness of the notion of “phosphorus of fulvic acids” and cause doubt upon a hypothesis about an important role of fulvic acids in the migration of phosphorus compounds in soils and landscapes. Soil Organic Matter (dpeaa)DE-He213 Humic Acid (dpeaa)DE-He213 Fulvic Acid (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Organic Phosphorus (dpeaa)DE-He213 Leoshkina, N. A. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 42(2009), 3 vom: März, Seite 277-283 (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:42 year:2009 number:3 month:03 pages:277-283 https://dx.doi.org/10.1134/S1064229309030041 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 42 2009 3 03 277-283
allfields_unstemmed	10.1134/S1064229309030041 doi (DE-627)SPR019949057 (SPR)S1064229309030041-e DE-627 ger DE-627 rakwb eng Makarov, M. I. verfasserin aut Phosphorus in the fulvate fraction of soil organic matter 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2009 Abstract The concentration of phosphorus in preparations of fulvic acids separated from soils according to a modified IHSS method varies from 0.03 to 0.23%; it is considerably lower than the concentration of phosphorus in preparations of humic acids (0.15–1.54%). A predominant part (>90%) of phosphorus-containing compounds in the fulvates is not sorbed on the polymethylmethacrylic resin Supelite DAX-8 used for the isolation of fulvic acids. These compounds are highly hydrophilic, and their sorption on the polystyrene-divinylbenzene resin XAD-4 used for the isolation of nonspecific organic compounds with a lower molecular weight and higher hydrophily does not exceed 20%. The results of the study attest to the quantitative indefiniteness of the notion of “phosphorus of fulvic acids” and cause doubt upon a hypothesis about an important role of fulvic acids in the migration of phosphorus compounds in soils and landscapes. Soil Organic Matter (dpeaa)DE-He213 Humic Acid (dpeaa)DE-He213 Fulvic Acid (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Organic Phosphorus (dpeaa)DE-He213 Leoshkina, N. A. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 42(2009), 3 vom: März, Seite 277-283 (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:42 year:2009 number:3 month:03 pages:277-283 https://dx.doi.org/10.1134/S1064229309030041 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 42 2009 3 03 277-283
allfieldsGer	10.1134/S1064229309030041 doi (DE-627)SPR019949057 (SPR)S1064229309030041-e DE-627 ger DE-627 rakwb eng Makarov, M. I. verfasserin aut Phosphorus in the fulvate fraction of soil organic matter 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2009 Abstract The concentration of phosphorus in preparations of fulvic acids separated from soils according to a modified IHSS method varies from 0.03 to 0.23%; it is considerably lower than the concentration of phosphorus in preparations of humic acids (0.15–1.54%). A predominant part (>90%) of phosphorus-containing compounds in the fulvates is not sorbed on the polymethylmethacrylic resin Supelite DAX-8 used for the isolation of fulvic acids. These compounds are highly hydrophilic, and their sorption on the polystyrene-divinylbenzene resin XAD-4 used for the isolation of nonspecific organic compounds with a lower molecular weight and higher hydrophily does not exceed 20%. The results of the study attest to the quantitative indefiniteness of the notion of “phosphorus of fulvic acids” and cause doubt upon a hypothesis about an important role of fulvic acids in the migration of phosphorus compounds in soils and landscapes. Soil Organic Matter (dpeaa)DE-He213 Humic Acid (dpeaa)DE-He213 Fulvic Acid (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Organic Phosphorus (dpeaa)DE-He213 Leoshkina, N. A. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 42(2009), 3 vom: März, Seite 277-283 (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:42 year:2009 number:3 month:03 pages:277-283 https://dx.doi.org/10.1134/S1064229309030041 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 42 2009 3 03 277-283
allfieldsSound	10.1134/S1064229309030041 doi (DE-627)SPR019949057 (SPR)S1064229309030041-e DE-627 ger DE-627 rakwb eng Makarov, M. I. verfasserin aut Phosphorus in the fulvate fraction of soil organic matter 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2009 Abstract The concentration of phosphorus in preparations of fulvic acids separated from soils according to a modified IHSS method varies from 0.03 to 0.23%; it is considerably lower than the concentration of phosphorus in preparations of humic acids (0.15–1.54%). A predominant part (>90%) of phosphorus-containing compounds in the fulvates is not sorbed on the polymethylmethacrylic resin Supelite DAX-8 used for the isolation of fulvic acids. These compounds are highly hydrophilic, and their sorption on the polystyrene-divinylbenzene resin XAD-4 used for the isolation of nonspecific organic compounds with a lower molecular weight and higher hydrophily does not exceed 20%. The results of the study attest to the quantitative indefiniteness of the notion of “phosphorus of fulvic acids” and cause doubt upon a hypothesis about an important role of fulvic acids in the migration of phosphorus compounds in soils and landscapes. Soil Organic Matter (dpeaa)DE-He213 Humic Acid (dpeaa)DE-He213 Fulvic Acid (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Organic Phosphorus (dpeaa)DE-He213 Leoshkina, N. A. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 42(2009), 3 vom: März, Seite 277-283 (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:42 year:2009 number:3 month:03 pages:277-283 https://dx.doi.org/10.1134/S1064229309030041 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 42 2009 3 03 277-283
language	English
source	Enthalten in Eurasian soil science 42(2009), 3 vom: März, Seite 277-283 volume:42 year:2009 number:3 month:03 pages:277-283
sourceStr	Enthalten in Eurasian soil science 42(2009), 3 vom: März, Seite 277-283 volume:42 year:2009 number:3 month:03 pages:277-283
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Soil Organic Matter Humic Acid Fulvic Acid EURASIAN Soil Science Organic Phosphorus
isfreeaccess_bool	false
container_title	Eurasian soil science
authorswithroles_txt_mv	Makarov, M. I. @@aut@@ Leoshkina, N. A. @@aut@@
publishDateDaySort_date	2009-03-01T00:00:00Z
hierarchy_top_id	341913227
id	SPR019949057
language_de	englisch
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author	Makarov, M. I.
spellingShingle	Makarov, M. I. misc Soil Organic Matter misc Humic Acid misc Fulvic Acid misc EURASIAN Soil Science misc Organic Phosphorus Phosphorus in the fulvate fraction of soil organic matter
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topic_title	Phosphorus in the fulvate fraction of soil organic matter Soil Organic Matter (dpeaa)DE-He213 Humic Acid (dpeaa)DE-He213 Fulvic Acid (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Organic Phosphorus (dpeaa)DE-He213
topic	misc Soil Organic Matter misc Humic Acid misc Fulvic Acid misc EURASIAN Soil Science misc Organic Phosphorus
topic_unstemmed	misc Soil Organic Matter misc Humic Acid misc Fulvic Acid misc EURASIAN Soil Science misc Organic Phosphorus
topic_browse	misc Soil Organic Matter misc Humic Acid misc Fulvic Acid misc EURASIAN Soil Science misc Organic Phosphorus
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title	Phosphorus in the fulvate fraction of soil organic matter
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title_full	Phosphorus in the fulvate fraction of soil organic matter
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title_sort	phosphorus in the fulvate fraction of soil organic matter
title_auth	Phosphorus in the fulvate fraction of soil organic matter
abstract	Abstract The concentration of phosphorus in preparations of fulvic acids separated from soils according to a modified IHSS method varies from 0.03 to 0.23%; it is considerably lower than the concentration of phosphorus in preparations of humic acids (0.15–1.54%). A predominant part (>90%) of phosphorus-containing compounds in the fulvates is not sorbed on the polymethylmethacrylic resin Supelite DAX-8 used for the isolation of fulvic acids. These compounds are highly hydrophilic, and their sorption on the polystyrene-divinylbenzene resin XAD-4 used for the isolation of nonspecific organic compounds with a lower molecular weight and higher hydrophily does not exceed 20%. The results of the study attest to the quantitative indefiniteness of the notion of “phosphorus of fulvic acids” and cause doubt upon a hypothesis about an important role of fulvic acids in the migration of phosphorus compounds in soils and landscapes. © Pleiades Publishing, Ltd. 2009
abstractGer	Abstract The concentration of phosphorus in preparations of fulvic acids separated from soils according to a modified IHSS method varies from 0.03 to 0.23%; it is considerably lower than the concentration of phosphorus in preparations of humic acids (0.15–1.54%). A predominant part (>90%) of phosphorus-containing compounds in the fulvates is not sorbed on the polymethylmethacrylic resin Supelite DAX-8 used for the isolation of fulvic acids. These compounds are highly hydrophilic, and their sorption on the polystyrene-divinylbenzene resin XAD-4 used for the isolation of nonspecific organic compounds with a lower molecular weight and higher hydrophily does not exceed 20%. The results of the study attest to the quantitative indefiniteness of the notion of “phosphorus of fulvic acids” and cause doubt upon a hypothesis about an important role of fulvic acids in the migration of phosphorus compounds in soils and landscapes. © Pleiades Publishing, Ltd. 2009
abstract_unstemmed	Abstract The concentration of phosphorus in preparations of fulvic acids separated from soils according to a modified IHSS method varies from 0.03 to 0.23%; it is considerably lower than the concentration of phosphorus in preparations of humic acids (0.15–1.54%). A predominant part (>90%) of phosphorus-containing compounds in the fulvates is not sorbed on the polymethylmethacrylic resin Supelite DAX-8 used for the isolation of fulvic acids. These compounds are highly hydrophilic, and their sorption on the polystyrene-divinylbenzene resin XAD-4 used for the isolation of nonspecific organic compounds with a lower molecular weight and higher hydrophily does not exceed 20%. The results of the study attest to the quantitative indefiniteness of the notion of “phosphorus of fulvic acids” and cause doubt upon a hypothesis about an important role of fulvic acids in the migration of phosphorus compounds in soils and landscapes. © Pleiades Publishing, Ltd. 2009
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title_short	Phosphorus in the fulvate fraction of soil organic matter
url	https://dx.doi.org/10.1134/S1064229309030041
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doi_str	10.1134/S1064229309030041
up_date	2024-07-04T03:26:06.772Z
_version_	1803617374596759552
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I.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Phosphorus in the fulvate fraction of soil organic matter</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2009</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. 2009</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The concentration of phosphorus in preparations of fulvic acids separated from soils according to a modified IHSS method varies from 0.03 to 0.23%; it is considerably lower than the concentration of phosphorus in preparations of humic acids (0.15–1.54%). A predominant part (>90%) of phosphorus-containing compounds in the fulvates is not sorbed on the polymethylmethacrylic resin Supelite DAX-8 used for the isolation of fulvic acids. These compounds are highly hydrophilic, and their sorption on the polystyrene-divinylbenzene resin XAD-4 used for the isolation of nonspecific organic compounds with a lower molecular weight and higher hydrophily does not exceed 20%. 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Phosphorus in the fulvate fraction of soil organic matter

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