Effects of long-term phosphorus fertilization and winter cover cropping on soil phosphorus transformations in less weathered soil
Abstract Information concerning sources and sinks of available P in soil is needed to improve soil P management and protect water quality. This study, conducted from 1989 to 1998 on a Sultan silt loam soil (Aquantic Xerochrept), determined the annual P removal rate by corn (Zea mays L.) and P transf...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Kuo, S. [verfasserIn] Huang, B. [verfasserIn] Bembenek, R. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2004 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Biology and fertility of soils - Berlin : Springer, 1985, 41(2004), 2 vom: 10. Dez., Seite 116-123 |
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| Übergeordnetes Werk: |
volume:41 ; year:2004 ; number:2 ; day:10 ; month:12 ; pages:116-123 |
| Links: |
|---|
| DOI / URN: |
10.1007/s00374-004-0807-6 |
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| Katalog-ID: |
SPR004916131 |
|---|
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| 100 | 1 | |a Kuo, S. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Effects of long-term phosphorus fertilization and winter cover cropping on soil phosphorus transformations in less weathered soil |
| 264 | 1 | |c 2004 | |
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| 520 | |a Abstract Information concerning sources and sinks of available P in soil is needed to improve soil P management and protect water quality. This study, conducted from 1989 to 1998 on a Sultan silt loam soil (Aquantic Xerochrept), determined the annual P removal rate by corn (Zea mays L.) and P transformation as affected by P rate and winter cover cropping. Treatments included two P rates (0 and 44 kg P $ ha^{−1} $) applied to corn at planting each year. All cover crops received 19.6 kg P $ ha^{−1} $ at seeding each fall. Also included was a control without any cover crop and with no P addition. Corn yield and P uptake were affected by P fertilizer additions, but not by cover crops. A fairly constant amount of P was supplied from indigenous soil P when no external P was added. When the amount of P added exceeded that removed by corn, the excess P was converted mainly to NaOH-extractable inorganic P (NaOH-$ P_{i} $). When the amount of P applied was below that removed by corn, indigenous soil NaOH-$ P_{i} $ acted as a source of available P for the plant. With no reduction of organic P ($ P_{o} $) extractable by NaOH or $ NaHCO_{3} $, the contribution from $ P_{o} $ to the available P pool appeared limited. The role of NaOH-$ P_{i} $ in P availability in the soil was substantiated by its significant correlation with labile $ NH_{4} $Cl-extractable P ($ NH_{4} $Cl-P; r2 =0.60, P <0.001) or $ NaHCO_{3} $-$ P_{i} $ (r2 =0.81, P <0.001) pools. The NaOH-$ P_{i} $ for the soil reflected the changes in soil P resulting from past fertilizer P input and P removal by the crops. | ||
| 650 | 4 | |a Phosphorus |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Transformation |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Corn |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Cover crop |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Sequential extractions |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Huang, B. |e verfasserin |4 aut | |
| 700 | 1 | |a Bembenek, R. |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Biology and fertility of soils |d Berlin : Springer, 1985 |g 41(2004), 2 vom: 10. Dez., Seite 116-123 |w (DE-627)269015426 |w (DE-600)1473419-9 |x 1432-0789 |7 nnns |
| 773 | 1 | 8 | |g volume:41 |g year:2004 |g number:2 |g day:10 |g month:12 |g pages:116-123 |
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2004 |
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10.1007/s00374-004-0807-6 doi (DE-627)SPR004916131 (SPR)s00374-004-0807-6-e DE-627 ger DE-627 rakwb eng 630 640 ASE 38.60 bkl 38.00 bkl 48.32 bkl Kuo, S. verfasserin aut Effects of long-term phosphorus fertilization and winter cover cropping on soil phosphorus transformations in less weathered soil 2004 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Information concerning sources and sinks of available P in soil is needed to improve soil P management and protect water quality. This study, conducted from 1989 to 1998 on a Sultan silt loam soil (Aquantic Xerochrept), determined the annual P removal rate by corn (Zea mays L.) and P transformation as affected by P rate and winter cover cropping. Treatments included two P rates (0 and 44 kg P $ ha^{−1} $) applied to corn at planting each year. All cover crops received 19.6 kg P $ ha^{−1} $ at seeding each fall. Also included was a control without any cover crop and with no P addition. Corn yield and P uptake were affected by P fertilizer additions, but not by cover crops. A fairly constant amount of P was supplied from indigenous soil P when no external P was added. When the amount of P added exceeded that removed by corn, the excess P was converted mainly to NaOH-extractable inorganic P (NaOH-$ P_{i} $). When the amount of P applied was below that removed by corn, indigenous soil NaOH-$ P_{i} $ acted as a source of available P for the plant. With no reduction of organic P ($ P_{o} $) extractable by NaOH or $ NaHCO_{3} $, the contribution from $ P_{o} $ to the available P pool appeared limited. The role of NaOH-$ P_{i} $ in P availability in the soil was substantiated by its significant correlation with labile $ NH_{4} $Cl-extractable P ($ NH_{4} $Cl-P; r2 =0.60, P <0.001) or $ NaHCO_{3} $-$ P_{i} $ (r2 =0.81, P <0.001) pools. The NaOH-$ P_{i} $ for the soil reflected the changes in soil P resulting from past fertilizer P input and P removal by the crops. Phosphorus (dpeaa)DE-He213 Transformation (dpeaa)DE-He213 Corn (dpeaa)DE-He213 Cover crop (dpeaa)DE-He213 Sequential extractions (dpeaa)DE-He213 Huang, B. verfasserin aut Bembenek, R. verfasserin aut Enthalten in Biology and fertility of soils Berlin : Springer, 1985 41(2004), 2 vom: 10. Dez., Seite 116-123 (DE-627)269015426 (DE-600)1473419-9 1432-0789 nnns volume:41 year:2004 number:2 day:10 month:12 pages:116-123 https://dx.doi.org/10.1007/s00374-004-0807-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-FOR SSG-OPC-ASE 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_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_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.60 ASE 38.00 ASE 48.32 ASE AR 41 2004 2 10 12 116-123 |
| spelling |
10.1007/s00374-004-0807-6 doi (DE-627)SPR004916131 (SPR)s00374-004-0807-6-e DE-627 ger DE-627 rakwb eng 630 640 ASE 38.60 bkl 38.00 bkl 48.32 bkl Kuo, S. verfasserin aut Effects of long-term phosphorus fertilization and winter cover cropping on soil phosphorus transformations in less weathered soil 2004 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Information concerning sources and sinks of available P in soil is needed to improve soil P management and protect water quality. This study, conducted from 1989 to 1998 on a Sultan silt loam soil (Aquantic Xerochrept), determined the annual P removal rate by corn (Zea mays L.) and P transformation as affected by P rate and winter cover cropping. Treatments included two P rates (0 and 44 kg P $ ha^{−1} $) applied to corn at planting each year. All cover crops received 19.6 kg P $ ha^{−1} $ at seeding each fall. Also included was a control without any cover crop and with no P addition. Corn yield and P uptake were affected by P fertilizer additions, but not by cover crops. A fairly constant amount of P was supplied from indigenous soil P when no external P was added. When the amount of P added exceeded that removed by corn, the excess P was converted mainly to NaOH-extractable inorganic P (NaOH-$ P_{i} $). When the amount of P applied was below that removed by corn, indigenous soil NaOH-$ P_{i} $ acted as a source of available P for the plant. With no reduction of organic P ($ P_{o} $) extractable by NaOH or $ NaHCO_{3} $, the contribution from $ P_{o} $ to the available P pool appeared limited. The role of NaOH-$ P_{i} $ in P availability in the soil was substantiated by its significant correlation with labile $ NH_{4} $Cl-extractable P ($ NH_{4} $Cl-P; r2 =0.60, P <0.001) or $ NaHCO_{3} $-$ P_{i} $ (r2 =0.81, P <0.001) pools. The NaOH-$ P_{i} $ for the soil reflected the changes in soil P resulting from past fertilizer P input and P removal by the crops. Phosphorus (dpeaa)DE-He213 Transformation (dpeaa)DE-He213 Corn (dpeaa)DE-He213 Cover crop (dpeaa)DE-He213 Sequential extractions (dpeaa)DE-He213 Huang, B. verfasserin aut Bembenek, R. verfasserin aut Enthalten in Biology and fertility of soils Berlin : Springer, 1985 41(2004), 2 vom: 10. Dez., Seite 116-123 (DE-627)269015426 (DE-600)1473419-9 1432-0789 nnns volume:41 year:2004 number:2 day:10 month:12 pages:116-123 https://dx.doi.org/10.1007/s00374-004-0807-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-FOR SSG-OPC-ASE 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_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_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.60 ASE 38.00 ASE 48.32 ASE AR 41 2004 2 10 12 116-123 |
| allfields_unstemmed |
10.1007/s00374-004-0807-6 doi (DE-627)SPR004916131 (SPR)s00374-004-0807-6-e DE-627 ger DE-627 rakwb eng 630 640 ASE 38.60 bkl 38.00 bkl 48.32 bkl Kuo, S. verfasserin aut Effects of long-term phosphorus fertilization and winter cover cropping on soil phosphorus transformations in less weathered soil 2004 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Information concerning sources and sinks of available P in soil is needed to improve soil P management and protect water quality. This study, conducted from 1989 to 1998 on a Sultan silt loam soil (Aquantic Xerochrept), determined the annual P removal rate by corn (Zea mays L.) and P transformation as affected by P rate and winter cover cropping. Treatments included two P rates (0 and 44 kg P $ ha^{−1} $) applied to corn at planting each year. All cover crops received 19.6 kg P $ ha^{−1} $ at seeding each fall. Also included was a control without any cover crop and with no P addition. Corn yield and P uptake were affected by P fertilizer additions, but not by cover crops. A fairly constant amount of P was supplied from indigenous soil P when no external P was added. When the amount of P added exceeded that removed by corn, the excess P was converted mainly to NaOH-extractable inorganic P (NaOH-$ P_{i} $). When the amount of P applied was below that removed by corn, indigenous soil NaOH-$ P_{i} $ acted as a source of available P for the plant. With no reduction of organic P ($ P_{o} $) extractable by NaOH or $ NaHCO_{3} $, the contribution from $ P_{o} $ to the available P pool appeared limited. The role of NaOH-$ P_{i} $ in P availability in the soil was substantiated by its significant correlation with labile $ NH_{4} $Cl-extractable P ($ NH_{4} $Cl-P; r2 =0.60, P <0.001) or $ NaHCO_{3} $-$ P_{i} $ (r2 =0.81, P <0.001) pools. The NaOH-$ P_{i} $ for the soil reflected the changes in soil P resulting from past fertilizer P input and P removal by the crops. Phosphorus (dpeaa)DE-He213 Transformation (dpeaa)DE-He213 Corn (dpeaa)DE-He213 Cover crop (dpeaa)DE-He213 Sequential extractions (dpeaa)DE-He213 Huang, B. verfasserin aut Bembenek, R. verfasserin aut Enthalten in Biology and fertility of soils Berlin : Springer, 1985 41(2004), 2 vom: 10. Dez., Seite 116-123 (DE-627)269015426 (DE-600)1473419-9 1432-0789 nnns volume:41 year:2004 number:2 day:10 month:12 pages:116-123 https://dx.doi.org/10.1007/s00374-004-0807-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-FOR SSG-OPC-ASE 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_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_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.60 ASE 38.00 ASE 48.32 ASE AR 41 2004 2 10 12 116-123 |
| allfieldsGer |
10.1007/s00374-004-0807-6 doi (DE-627)SPR004916131 (SPR)s00374-004-0807-6-e DE-627 ger DE-627 rakwb eng 630 640 ASE 38.60 bkl 38.00 bkl 48.32 bkl Kuo, S. verfasserin aut Effects of long-term phosphorus fertilization and winter cover cropping on soil phosphorus transformations in less weathered soil 2004 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Information concerning sources and sinks of available P in soil is needed to improve soil P management and protect water quality. This study, conducted from 1989 to 1998 on a Sultan silt loam soil (Aquantic Xerochrept), determined the annual P removal rate by corn (Zea mays L.) and P transformation as affected by P rate and winter cover cropping. Treatments included two P rates (0 and 44 kg P $ ha^{−1} $) applied to corn at planting each year. All cover crops received 19.6 kg P $ ha^{−1} $ at seeding each fall. Also included was a control without any cover crop and with no P addition. Corn yield and P uptake were affected by P fertilizer additions, but not by cover crops. A fairly constant amount of P was supplied from indigenous soil P when no external P was added. When the amount of P added exceeded that removed by corn, the excess P was converted mainly to NaOH-extractable inorganic P (NaOH-$ P_{i} $). When the amount of P applied was below that removed by corn, indigenous soil NaOH-$ P_{i} $ acted as a source of available P for the plant. With no reduction of organic P ($ P_{o} $) extractable by NaOH or $ NaHCO_{3} $, the contribution from $ P_{o} $ to the available P pool appeared limited. The role of NaOH-$ P_{i} $ in P availability in the soil was substantiated by its significant correlation with labile $ NH_{4} $Cl-extractable P ($ NH_{4} $Cl-P; r2 =0.60, P <0.001) or $ NaHCO_{3} $-$ P_{i} $ (r2 =0.81, P <0.001) pools. The NaOH-$ P_{i} $ for the soil reflected the changes in soil P resulting from past fertilizer P input and P removal by the crops. Phosphorus (dpeaa)DE-He213 Transformation (dpeaa)DE-He213 Corn (dpeaa)DE-He213 Cover crop (dpeaa)DE-He213 Sequential extractions (dpeaa)DE-He213 Huang, B. verfasserin aut Bembenek, R. verfasserin aut Enthalten in Biology and fertility of soils Berlin : Springer, 1985 41(2004), 2 vom: 10. Dez., Seite 116-123 (DE-627)269015426 (DE-600)1473419-9 1432-0789 nnns volume:41 year:2004 number:2 day:10 month:12 pages:116-123 https://dx.doi.org/10.1007/s00374-004-0807-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-FOR SSG-OPC-ASE 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_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_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.60 ASE 38.00 ASE 48.32 ASE AR 41 2004 2 10 12 116-123 |
| allfieldsSound |
10.1007/s00374-004-0807-6 doi (DE-627)SPR004916131 (SPR)s00374-004-0807-6-e DE-627 ger DE-627 rakwb eng 630 640 ASE 38.60 bkl 38.00 bkl 48.32 bkl Kuo, S. verfasserin aut Effects of long-term phosphorus fertilization and winter cover cropping on soil phosphorus transformations in less weathered soil 2004 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Information concerning sources and sinks of available P in soil is needed to improve soil P management and protect water quality. This study, conducted from 1989 to 1998 on a Sultan silt loam soil (Aquantic Xerochrept), determined the annual P removal rate by corn (Zea mays L.) and P transformation as affected by P rate and winter cover cropping. Treatments included two P rates (0 and 44 kg P $ ha^{−1} $) applied to corn at planting each year. All cover crops received 19.6 kg P $ ha^{−1} $ at seeding each fall. Also included was a control without any cover crop and with no P addition. Corn yield and P uptake were affected by P fertilizer additions, but not by cover crops. A fairly constant amount of P was supplied from indigenous soil P when no external P was added. When the amount of P added exceeded that removed by corn, the excess P was converted mainly to NaOH-extractable inorganic P (NaOH-$ P_{i} $). When the amount of P applied was below that removed by corn, indigenous soil NaOH-$ P_{i} $ acted as a source of available P for the plant. With no reduction of organic P ($ P_{o} $) extractable by NaOH or $ NaHCO_{3} $, the contribution from $ P_{o} $ to the available P pool appeared limited. The role of NaOH-$ P_{i} $ in P availability in the soil was substantiated by its significant correlation with labile $ NH_{4} $Cl-extractable P ($ NH_{4} $Cl-P; r2 =0.60, P <0.001) or $ NaHCO_{3} $-$ P_{i} $ (r2 =0.81, P <0.001) pools. The NaOH-$ P_{i} $ for the soil reflected the changes in soil P resulting from past fertilizer P input and P removal by the crops. Phosphorus (dpeaa)DE-He213 Transformation (dpeaa)DE-He213 Corn (dpeaa)DE-He213 Cover crop (dpeaa)DE-He213 Sequential extractions (dpeaa)DE-He213 Huang, B. verfasserin aut Bembenek, R. verfasserin aut Enthalten in Biology and fertility of soils Berlin : Springer, 1985 41(2004), 2 vom: 10. Dez., Seite 116-123 (DE-627)269015426 (DE-600)1473419-9 1432-0789 nnns volume:41 year:2004 number:2 day:10 month:12 pages:116-123 https://dx.doi.org/10.1007/s00374-004-0807-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-FOR SSG-OPC-ASE 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_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_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.60 ASE 38.00 ASE 48.32 ASE AR 41 2004 2 10 12 116-123 |
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English |
| source |
Enthalten in Biology and fertility of soils 41(2004), 2 vom: 10. Dez., Seite 116-123 volume:41 year:2004 number:2 day:10 month:12 pages:116-123 |
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Enthalten in Biology and fertility of soils 41(2004), 2 vom: 10. Dez., Seite 116-123 volume:41 year:2004 number:2 day:10 month:12 pages:116-123 |
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Article |
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findex.gbv.de |
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Phosphorus Transformation Corn Cover crop Sequential extractions |
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Biology and fertility of soils |
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Kuo, S. @@aut@@ Huang, B. @@aut@@ Bembenek, R. @@aut@@ |
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2004-12-10T00:00:00Z |
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This study, conducted from 1989 to 1998 on a Sultan silt loam soil (Aquantic Xerochrept), determined the annual P removal rate by corn (Zea mays L.) and P transformation as affected by P rate and winter cover cropping. Treatments included two P rates (0 and 44 kg P $ ha^{−1} $) applied to corn at planting each year. All cover crops received 19.6 kg P $ ha^{−1} $ at seeding each fall. Also included was a control without any cover crop and with no P addition. Corn yield and P uptake were affected by P fertilizer additions, but not by cover crops. A fairly constant amount of P was supplied from indigenous soil P when no external P was added. When the amount of P added exceeded that removed by corn, the excess P was converted mainly to NaOH-extractable inorganic P (NaOH-$ P_{i} $). When the amount of P applied was below that removed by corn, indigenous soil NaOH-$ P_{i} $ acted as a source of available P for the plant. With no reduction of organic P ($ P_{o} $) extractable by NaOH or $ NaHCO_{3} $, the contribution from $ P_{o} $ to the available P pool appeared limited. The role of NaOH-$ P_{i} $ in P availability in the soil was substantiated by its significant correlation with labile $ NH_{4} $Cl-extractable P ($ NH_{4} $Cl-P; r2 =0.60, P <0.001) or $ NaHCO_{3} $-$ P_{i} $ (r2 =0.81, P <0.001) pools. 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|
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Kuo, S. |
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Kuo, S. ddc 630 bkl 38.60 bkl 38.00 bkl 48.32 misc Phosphorus misc Transformation misc Corn misc Cover crop misc Sequential extractions Effects of long-term phosphorus fertilization and winter cover cropping on soil phosphorus transformations in less weathered soil |
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630 640 ASE 38.60 bkl 38.00 bkl 48.32 bkl Effects of long-term phosphorus fertilization and winter cover cropping on soil phosphorus transformations in less weathered soil Phosphorus (dpeaa)DE-He213 Transformation (dpeaa)DE-He213 Corn (dpeaa)DE-He213 Cover crop (dpeaa)DE-He213 Sequential extractions (dpeaa)DE-He213 |
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ddc 630 bkl 38.60 bkl 38.00 bkl 48.32 misc Phosphorus misc Transformation misc Corn misc Cover crop misc Sequential extractions |
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ddc 630 bkl 38.60 bkl 38.00 bkl 48.32 misc Phosphorus misc Transformation misc Corn misc Cover crop misc Sequential extractions |
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ddc 630 bkl 38.60 bkl 38.00 bkl 48.32 misc Phosphorus misc Transformation misc Corn misc Cover crop misc Sequential extractions |
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Effects of long-term phosphorus fertilization and winter cover cropping on soil phosphorus transformations in less weathered soil |
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Effects of long-term phosphorus fertilization and winter cover cropping on soil phosphorus transformations in less weathered soil |
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Kuo, S. |
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Biology and fertility of soils |
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2004 |
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Kuo, S. Huang, B. Bembenek, R. |
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Kuo, S. |
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effects of long-term phosphorus fertilization and winter cover cropping on soil phosphorus transformations in less weathered soil |
| title_auth |
Effects of long-term phosphorus fertilization and winter cover cropping on soil phosphorus transformations in less weathered soil |
| abstract |
Abstract Information concerning sources and sinks of available P in soil is needed to improve soil P management and protect water quality. This study, conducted from 1989 to 1998 on a Sultan silt loam soil (Aquantic Xerochrept), determined the annual P removal rate by corn (Zea mays L.) and P transformation as affected by P rate and winter cover cropping. Treatments included two P rates (0 and 44 kg P $ ha^{−1} $) applied to corn at planting each year. All cover crops received 19.6 kg P $ ha^{−1} $ at seeding each fall. Also included was a control without any cover crop and with no P addition. Corn yield and P uptake were affected by P fertilizer additions, but not by cover crops. A fairly constant amount of P was supplied from indigenous soil P when no external P was added. When the amount of P added exceeded that removed by corn, the excess P was converted mainly to NaOH-extractable inorganic P (NaOH-$ P_{i} $). When the amount of P applied was below that removed by corn, indigenous soil NaOH-$ P_{i} $ acted as a source of available P for the plant. With no reduction of organic P ($ P_{o} $) extractable by NaOH or $ NaHCO_{3} $, the contribution from $ P_{o} $ to the available P pool appeared limited. The role of NaOH-$ P_{i} $ in P availability in the soil was substantiated by its significant correlation with labile $ NH_{4} $Cl-extractable P ($ NH_{4} $Cl-P; r2 =0.60, P <0.001) or $ NaHCO_{3} $-$ P_{i} $ (r2 =0.81, P <0.001) pools. The NaOH-$ P_{i} $ for the soil reflected the changes in soil P resulting from past fertilizer P input and P removal by the crops. |
| abstractGer |
Abstract Information concerning sources and sinks of available P in soil is needed to improve soil P management and protect water quality. This study, conducted from 1989 to 1998 on a Sultan silt loam soil (Aquantic Xerochrept), determined the annual P removal rate by corn (Zea mays L.) and P transformation as affected by P rate and winter cover cropping. Treatments included two P rates (0 and 44 kg P $ ha^{−1} $) applied to corn at planting each year. All cover crops received 19.6 kg P $ ha^{−1} $ at seeding each fall. Also included was a control without any cover crop and with no P addition. Corn yield and P uptake were affected by P fertilizer additions, but not by cover crops. A fairly constant amount of P was supplied from indigenous soil P when no external P was added. When the amount of P added exceeded that removed by corn, the excess P was converted mainly to NaOH-extractable inorganic P (NaOH-$ P_{i} $). When the amount of P applied was below that removed by corn, indigenous soil NaOH-$ P_{i} $ acted as a source of available P for the plant. With no reduction of organic P ($ P_{o} $) extractable by NaOH or $ NaHCO_{3} $, the contribution from $ P_{o} $ to the available P pool appeared limited. The role of NaOH-$ P_{i} $ in P availability in the soil was substantiated by its significant correlation with labile $ NH_{4} $Cl-extractable P ($ NH_{4} $Cl-P; r2 =0.60, P <0.001) or $ NaHCO_{3} $-$ P_{i} $ (r2 =0.81, P <0.001) pools. The NaOH-$ P_{i} $ for the soil reflected the changes in soil P resulting from past fertilizer P input and P removal by the crops. |
| abstract_unstemmed |
Abstract Information concerning sources and sinks of available P in soil is needed to improve soil P management and protect water quality. This study, conducted from 1989 to 1998 on a Sultan silt loam soil (Aquantic Xerochrept), determined the annual P removal rate by corn (Zea mays L.) and P transformation as affected by P rate and winter cover cropping. Treatments included two P rates (0 and 44 kg P $ ha^{−1} $) applied to corn at planting each year. All cover crops received 19.6 kg P $ ha^{−1} $ at seeding each fall. Also included was a control without any cover crop and with no P addition. Corn yield and P uptake were affected by P fertilizer additions, but not by cover crops. A fairly constant amount of P was supplied from indigenous soil P when no external P was added. When the amount of P added exceeded that removed by corn, the excess P was converted mainly to NaOH-extractable inorganic P (NaOH-$ P_{i} $). When the amount of P applied was below that removed by corn, indigenous soil NaOH-$ P_{i} $ acted as a source of available P for the plant. With no reduction of organic P ($ P_{o} $) extractable by NaOH or $ NaHCO_{3} $, the contribution from $ P_{o} $ to the available P pool appeared limited. The role of NaOH-$ P_{i} $ in P availability in the soil was substantiated by its significant correlation with labile $ NH_{4} $Cl-extractable P ($ NH_{4} $Cl-P; r2 =0.60, P <0.001) or $ NaHCO_{3} $-$ P_{i} $ (r2 =0.81, P <0.001) pools. The NaOH-$ P_{i} $ for the soil reflected the changes in soil P resulting from past fertilizer P input and P removal by the crops. |
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Effects of long-term phosphorus fertilization and winter cover cropping on soil phosphorus transformations in less weathered soil |
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| score |
7.3998156 |