Soil and tree response to P fertilization in a secondary tropical forest supported by an Oxisol
Abstract Mature tropical forests are considered to be P limited and to cycle P efficiently. Whether P limitations are significant in younger secondary tropical forests, however, remains largely unexplored. This study evaluated P limitation by observing the P fertilizer response of a naturally regene...
Ausführliche Beschreibung
Autor*in: |
Markewitz, Daniel [verfasserIn] Figueiredo, Ricardo de O. [verfasserIn] de Carvalho, Cláudio J. Reis [verfasserIn] Davidson, Eric A. [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2012 |
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Schlagwörter: |
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Übergeordnetes Werk: |
Enthalten in: Biology and fertility of soils - Berlin : Springer, 1985, 48(2012), 6 vom: 26. Jan., Seite 665-678 |
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Übergeordnetes Werk: |
volume:48 ; year:2012 ; number:6 ; day:26 ; month:01 ; pages:665-678 |
Links: |
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DOI / URN: |
10.1007/s00374-011-0659-9 |
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Katalog-ID: |
SPR004960998 |
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100 | 1 | |a Markewitz, Daniel |e verfasserin |4 aut | |
245 | 1 | 0 | |a Soil and tree response to P fertilization in a secondary tropical forest supported by an Oxisol |
264 | 1 | |c 2012 | |
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520 | |a Abstract Mature tropical forests are considered to be P limited and to cycle P efficiently. Whether P limitations are significant in younger secondary tropical forests, however, remains largely unexplored. This study evaluated P limitation by observing the P fertilizer response of a naturally regenerated 24-year-old forest and its soil. In February 1999, six 20 × 20-m plots were established in secondary forest in the Brazilian Amazon. After 1 year of pre-treatment tree measurements, 50 kg P $ ha^{−1} $ was applied in January 2000 and again in January 2001. Soil sorption of P was relatively low (∼100 μg $ g^{−1} $) in the surface 0–20 cm while sorption increased to ∼180 μg $ g^{−1} $ at 20–50 cm and approached ∼500 μg $ g^{−1} $ for the 50- to 200-cm layers. Soil P in 0–10 cm, measured as sequentially extractable fractions (resin, $ HCO_{3} $-Pi, NaOH-Pi, NaOH-Po, and 1 M HCl), increased shortly after fertilization and could account for nearly all the 50 kg P $ ha^{−1} $ added at each date. During the following 6 years, soil P in fertilized plots declined in all pools other than resin P, and by June 2006, concentrations returned to pre-fertilization levels. Despite the increase in extractable P with fertilization, increased tree growth was not detected from stand age 25 to 31 years. It appears that during secondary forest succession at this site, the forest P cycle was conservative so as to maintain available P at a sufficient concentration to meet forest P demands. | ||
650 | 4 | |a P limitation |7 (dpeaa)DE-He213 | |
650 | 4 | |a P fractionation |7 (dpeaa)DE-He213 | |
650 | 4 | |a Labile P |7 (dpeaa)DE-He213 | |
650 | 4 | |a P sorption |7 (dpeaa)DE-He213 | |
700 | 1 | |a Figueiredo, Ricardo de O. |e verfasserin |4 aut | |
700 | 1 | |a de Carvalho, Cláudio J. Reis |e verfasserin |4 aut | |
700 | 1 | |a Davidson, Eric A. |e verfasserin |4 aut | |
773 | 0 | 8 | |i Enthalten in |t Biology and fertility of soils |d Berlin : Springer, 1985 |g 48(2012), 6 vom: 26. Jan., Seite 665-678 |w (DE-627)269015426 |w (DE-600)1473419-9 |x 1432-0789 |7 nnns |
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2012 |
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10.1007/s00374-011-0659-9 doi (DE-627)SPR004960998 (SPR)s00374-011-0659-9-e DE-627 ger DE-627 rakwb eng 630 640 ASE 38.60 bkl 38.00 bkl 48.32 bkl Markewitz, Daniel verfasserin aut Soil and tree response to P fertilization in a secondary tropical forest supported by an Oxisol 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Mature tropical forests are considered to be P limited and to cycle P efficiently. Whether P limitations are significant in younger secondary tropical forests, however, remains largely unexplored. This study evaluated P limitation by observing the P fertilizer response of a naturally regenerated 24-year-old forest and its soil. In February 1999, six 20 × 20-m plots were established in secondary forest in the Brazilian Amazon. After 1 year of pre-treatment tree measurements, 50 kg P $ ha^{−1} $ was applied in January 2000 and again in January 2001. Soil sorption of P was relatively low (∼100 μg $ g^{−1} $) in the surface 0–20 cm while sorption increased to ∼180 μg $ g^{−1} $ at 20–50 cm and approached ∼500 μg $ g^{−1} $ for the 50- to 200-cm layers. Soil P in 0–10 cm, measured as sequentially extractable fractions (resin, $ HCO_{3} $-Pi, NaOH-Pi, NaOH-Po, and 1 M HCl), increased shortly after fertilization and could account for nearly all the 50 kg P $ ha^{−1} $ added at each date. During the following 6 years, soil P in fertilized plots declined in all pools other than resin P, and by June 2006, concentrations returned to pre-fertilization levels. Despite the increase in extractable P with fertilization, increased tree growth was not detected from stand age 25 to 31 years. It appears that during secondary forest succession at this site, the forest P cycle was conservative so as to maintain available P at a sufficient concentration to meet forest P demands. P limitation (dpeaa)DE-He213 P fractionation (dpeaa)DE-He213 Labile P (dpeaa)DE-He213 P sorption (dpeaa)DE-He213 Figueiredo, Ricardo de O. verfasserin aut de Carvalho, Cláudio J. Reis verfasserin aut Davidson, Eric A. verfasserin aut Enthalten in Biology and fertility of soils Berlin : Springer, 1985 48(2012), 6 vom: 26. Jan., Seite 665-678 (DE-627)269015426 (DE-600)1473419-9 1432-0789 nnns volume:48 year:2012 number:6 day:26 month:01 pages:665-678 https://dx.doi.org/10.1007/s00374-011-0659-9 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 48 2012 6 26 01 665-678 |
spelling |
10.1007/s00374-011-0659-9 doi (DE-627)SPR004960998 (SPR)s00374-011-0659-9-e DE-627 ger DE-627 rakwb eng 630 640 ASE 38.60 bkl 38.00 bkl 48.32 bkl Markewitz, Daniel verfasserin aut Soil and tree response to P fertilization in a secondary tropical forest supported by an Oxisol 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Mature tropical forests are considered to be P limited and to cycle P efficiently. Whether P limitations are significant in younger secondary tropical forests, however, remains largely unexplored. This study evaluated P limitation by observing the P fertilizer response of a naturally regenerated 24-year-old forest and its soil. In February 1999, six 20 × 20-m plots were established in secondary forest in the Brazilian Amazon. After 1 year of pre-treatment tree measurements, 50 kg P $ ha^{−1} $ was applied in January 2000 and again in January 2001. Soil sorption of P was relatively low (∼100 μg $ g^{−1} $) in the surface 0–20 cm while sorption increased to ∼180 μg $ g^{−1} $ at 20–50 cm and approached ∼500 μg $ g^{−1} $ for the 50- to 200-cm layers. Soil P in 0–10 cm, measured as sequentially extractable fractions (resin, $ HCO_{3} $-Pi, NaOH-Pi, NaOH-Po, and 1 M HCl), increased shortly after fertilization and could account for nearly all the 50 kg P $ ha^{−1} $ added at each date. During the following 6 years, soil P in fertilized plots declined in all pools other than resin P, and by June 2006, concentrations returned to pre-fertilization levels. Despite the increase in extractable P with fertilization, increased tree growth was not detected from stand age 25 to 31 years. It appears that during secondary forest succession at this site, the forest P cycle was conservative so as to maintain available P at a sufficient concentration to meet forest P demands. P limitation (dpeaa)DE-He213 P fractionation (dpeaa)DE-He213 Labile P (dpeaa)DE-He213 P sorption (dpeaa)DE-He213 Figueiredo, Ricardo de O. verfasserin aut de Carvalho, Cláudio J. Reis verfasserin aut Davidson, Eric A. verfasserin aut Enthalten in Biology and fertility of soils Berlin : Springer, 1985 48(2012), 6 vom: 26. Jan., Seite 665-678 (DE-627)269015426 (DE-600)1473419-9 1432-0789 nnns volume:48 year:2012 number:6 day:26 month:01 pages:665-678 https://dx.doi.org/10.1007/s00374-011-0659-9 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 48 2012 6 26 01 665-678 |
allfields_unstemmed |
10.1007/s00374-011-0659-9 doi (DE-627)SPR004960998 (SPR)s00374-011-0659-9-e DE-627 ger DE-627 rakwb eng 630 640 ASE 38.60 bkl 38.00 bkl 48.32 bkl Markewitz, Daniel verfasserin aut Soil and tree response to P fertilization in a secondary tropical forest supported by an Oxisol 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Mature tropical forests are considered to be P limited and to cycle P efficiently. Whether P limitations are significant in younger secondary tropical forests, however, remains largely unexplored. This study evaluated P limitation by observing the P fertilizer response of a naturally regenerated 24-year-old forest and its soil. In February 1999, six 20 × 20-m plots were established in secondary forest in the Brazilian Amazon. After 1 year of pre-treatment tree measurements, 50 kg P $ ha^{−1} $ was applied in January 2000 and again in January 2001. Soil sorption of P was relatively low (∼100 μg $ g^{−1} $) in the surface 0–20 cm while sorption increased to ∼180 μg $ g^{−1} $ at 20–50 cm and approached ∼500 μg $ g^{−1} $ for the 50- to 200-cm layers. Soil P in 0–10 cm, measured as sequentially extractable fractions (resin, $ HCO_{3} $-Pi, NaOH-Pi, NaOH-Po, and 1 M HCl), increased shortly after fertilization and could account for nearly all the 50 kg P $ ha^{−1} $ added at each date. During the following 6 years, soil P in fertilized plots declined in all pools other than resin P, and by June 2006, concentrations returned to pre-fertilization levels. Despite the increase in extractable P with fertilization, increased tree growth was not detected from stand age 25 to 31 years. It appears that during secondary forest succession at this site, the forest P cycle was conservative so as to maintain available P at a sufficient concentration to meet forest P demands. P limitation (dpeaa)DE-He213 P fractionation (dpeaa)DE-He213 Labile P (dpeaa)DE-He213 P sorption (dpeaa)DE-He213 Figueiredo, Ricardo de O. verfasserin aut de Carvalho, Cláudio J. Reis verfasserin aut Davidson, Eric A. verfasserin aut Enthalten in Biology and fertility of soils Berlin : Springer, 1985 48(2012), 6 vom: 26. Jan., Seite 665-678 (DE-627)269015426 (DE-600)1473419-9 1432-0789 nnns volume:48 year:2012 number:6 day:26 month:01 pages:665-678 https://dx.doi.org/10.1007/s00374-011-0659-9 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 48 2012 6 26 01 665-678 |
allfieldsGer |
10.1007/s00374-011-0659-9 doi (DE-627)SPR004960998 (SPR)s00374-011-0659-9-e DE-627 ger DE-627 rakwb eng 630 640 ASE 38.60 bkl 38.00 bkl 48.32 bkl Markewitz, Daniel verfasserin aut Soil and tree response to P fertilization in a secondary tropical forest supported by an Oxisol 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Mature tropical forests are considered to be P limited and to cycle P efficiently. Whether P limitations are significant in younger secondary tropical forests, however, remains largely unexplored. This study evaluated P limitation by observing the P fertilizer response of a naturally regenerated 24-year-old forest and its soil. In February 1999, six 20 × 20-m plots were established in secondary forest in the Brazilian Amazon. After 1 year of pre-treatment tree measurements, 50 kg P $ ha^{−1} $ was applied in January 2000 and again in January 2001. Soil sorption of P was relatively low (∼100 μg $ g^{−1} $) in the surface 0–20 cm while sorption increased to ∼180 μg $ g^{−1} $ at 20–50 cm and approached ∼500 μg $ g^{−1} $ for the 50- to 200-cm layers. Soil P in 0–10 cm, measured as sequentially extractable fractions (resin, $ HCO_{3} $-Pi, NaOH-Pi, NaOH-Po, and 1 M HCl), increased shortly after fertilization and could account for nearly all the 50 kg P $ ha^{−1} $ added at each date. During the following 6 years, soil P in fertilized plots declined in all pools other than resin P, and by June 2006, concentrations returned to pre-fertilization levels. Despite the increase in extractable P with fertilization, increased tree growth was not detected from stand age 25 to 31 years. It appears that during secondary forest succession at this site, the forest P cycle was conservative so as to maintain available P at a sufficient concentration to meet forest P demands. P limitation (dpeaa)DE-He213 P fractionation (dpeaa)DE-He213 Labile P (dpeaa)DE-He213 P sorption (dpeaa)DE-He213 Figueiredo, Ricardo de O. verfasserin aut de Carvalho, Cláudio J. Reis verfasserin aut Davidson, Eric A. verfasserin aut Enthalten in Biology and fertility of soils Berlin : Springer, 1985 48(2012), 6 vom: 26. Jan., Seite 665-678 (DE-627)269015426 (DE-600)1473419-9 1432-0789 nnns volume:48 year:2012 number:6 day:26 month:01 pages:665-678 https://dx.doi.org/10.1007/s00374-011-0659-9 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 48 2012 6 26 01 665-678 |
allfieldsSound |
10.1007/s00374-011-0659-9 doi (DE-627)SPR004960998 (SPR)s00374-011-0659-9-e DE-627 ger DE-627 rakwb eng 630 640 ASE 38.60 bkl 38.00 bkl 48.32 bkl Markewitz, Daniel verfasserin aut Soil and tree response to P fertilization in a secondary tropical forest supported by an Oxisol 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Mature tropical forests are considered to be P limited and to cycle P efficiently. Whether P limitations are significant in younger secondary tropical forests, however, remains largely unexplored. This study evaluated P limitation by observing the P fertilizer response of a naturally regenerated 24-year-old forest and its soil. In February 1999, six 20 × 20-m plots were established in secondary forest in the Brazilian Amazon. After 1 year of pre-treatment tree measurements, 50 kg P $ ha^{−1} $ was applied in January 2000 and again in January 2001. Soil sorption of P was relatively low (∼100 μg $ g^{−1} $) in the surface 0–20 cm while sorption increased to ∼180 μg $ g^{−1} $ at 20–50 cm and approached ∼500 μg $ g^{−1} $ for the 50- to 200-cm layers. Soil P in 0–10 cm, measured as sequentially extractable fractions (resin, $ HCO_{3} $-Pi, NaOH-Pi, NaOH-Po, and 1 M HCl), increased shortly after fertilization and could account for nearly all the 50 kg P $ ha^{−1} $ added at each date. During the following 6 years, soil P in fertilized plots declined in all pools other than resin P, and by June 2006, concentrations returned to pre-fertilization levels. Despite the increase in extractable P with fertilization, increased tree growth was not detected from stand age 25 to 31 years. It appears that during secondary forest succession at this site, the forest P cycle was conservative so as to maintain available P at a sufficient concentration to meet forest P demands. P limitation (dpeaa)DE-He213 P fractionation (dpeaa)DE-He213 Labile P (dpeaa)DE-He213 P sorption (dpeaa)DE-He213 Figueiredo, Ricardo de O. verfasserin aut de Carvalho, Cláudio J. Reis verfasserin aut Davidson, Eric A. verfasserin aut Enthalten in Biology and fertility of soils Berlin : Springer, 1985 48(2012), 6 vom: 26. Jan., Seite 665-678 (DE-627)269015426 (DE-600)1473419-9 1432-0789 nnns volume:48 year:2012 number:6 day:26 month:01 pages:665-678 https://dx.doi.org/10.1007/s00374-011-0659-9 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 48 2012 6 26 01 665-678 |
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English |
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Enthalten in Biology and fertility of soils 48(2012), 6 vom: 26. Jan., Seite 665-678 volume:48 year:2012 number:6 day:26 month:01 pages:665-678 |
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Enthalten in Biology and fertility of soils 48(2012), 6 vom: 26. Jan., Seite 665-678 volume:48 year:2012 number:6 day:26 month:01 pages:665-678 |
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Biology and fertility of soils |
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Markewitz, Daniel @@aut@@ Figueiredo, Ricardo de O. @@aut@@ de Carvalho, Cláudio J. Reis @@aut@@ Davidson, Eric A. @@aut@@ |
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Whether P limitations are significant in younger secondary tropical forests, however, remains largely unexplored. This study evaluated P limitation by observing the P fertilizer response of a naturally regenerated 24-year-old forest and its soil. In February 1999, six 20 × 20-m plots were established in secondary forest in the Brazilian Amazon. After 1 year of pre-treatment tree measurements, 50 kg P $ ha^{−1} $ was applied in January 2000 and again in January 2001. Soil sorption of P was relatively low (∼100 μg $ g^{−1} $) in the surface 0–20 cm while sorption increased to ∼180 μg $ g^{−1} $ at 20–50 cm and approached ∼500 μg $ g^{−1} $ for the 50- to 200-cm layers. Soil P in 0–10 cm, measured as sequentially extractable fractions (resin, $ HCO_{3} $-Pi, NaOH-Pi, NaOH-Po, and 1 M HCl), increased shortly after fertilization and could account for nearly all the 50 kg P $ ha^{−1} $ added at each date. During the following 6 years, soil P in fertilized plots declined in all pools other than resin P, and by June 2006, concentrations returned to pre-fertilization levels. Despite the increase in extractable P with fertilization, increased tree growth was not detected from stand age 25 to 31 years. 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Markewitz, Daniel |
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Markewitz, Daniel ddc 630 bkl 38.60 bkl 38.00 bkl 48.32 misc P limitation misc P fractionation misc Labile P misc P sorption Soil and tree response to P fertilization in a secondary tropical forest supported by an Oxisol |
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630 640 ASE 38.60 bkl 38.00 bkl 48.32 bkl Soil and tree response to P fertilization in a secondary tropical forest supported by an Oxisol P limitation (dpeaa)DE-He213 P fractionation (dpeaa)DE-He213 Labile P (dpeaa)DE-He213 P sorption (dpeaa)DE-He213 |
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ddc 630 bkl 38.60 bkl 38.00 bkl 48.32 misc P limitation misc P fractionation misc Labile P misc P sorption |
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Soil and tree response to P fertilization in a secondary tropical forest supported by an Oxisol |
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Soil and tree response to P fertilization in a secondary tropical forest supported by an Oxisol |
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Markewitz, Daniel Figueiredo, Ricardo de O. de Carvalho, Cláudio J. Reis Davidson, Eric A. |
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Elektronische Aufsätze |
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Markewitz, Daniel |
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title_sort |
soil and tree response to p fertilization in a secondary tropical forest supported by an oxisol |
title_auth |
Soil and tree response to P fertilization in a secondary tropical forest supported by an Oxisol |
abstract |
Abstract Mature tropical forests are considered to be P limited and to cycle P efficiently. Whether P limitations are significant in younger secondary tropical forests, however, remains largely unexplored. This study evaluated P limitation by observing the P fertilizer response of a naturally regenerated 24-year-old forest and its soil. In February 1999, six 20 × 20-m plots were established in secondary forest in the Brazilian Amazon. After 1 year of pre-treatment tree measurements, 50 kg P $ ha^{−1} $ was applied in January 2000 and again in January 2001. Soil sorption of P was relatively low (∼100 μg $ g^{−1} $) in the surface 0–20 cm while sorption increased to ∼180 μg $ g^{−1} $ at 20–50 cm and approached ∼500 μg $ g^{−1} $ for the 50- to 200-cm layers. Soil P in 0–10 cm, measured as sequentially extractable fractions (resin, $ HCO_{3} $-Pi, NaOH-Pi, NaOH-Po, and 1 M HCl), increased shortly after fertilization and could account for nearly all the 50 kg P $ ha^{−1} $ added at each date. During the following 6 years, soil P in fertilized plots declined in all pools other than resin P, and by June 2006, concentrations returned to pre-fertilization levels. Despite the increase in extractable P with fertilization, increased tree growth was not detected from stand age 25 to 31 years. It appears that during secondary forest succession at this site, the forest P cycle was conservative so as to maintain available P at a sufficient concentration to meet forest P demands. |
abstractGer |
Abstract Mature tropical forests are considered to be P limited and to cycle P efficiently. Whether P limitations are significant in younger secondary tropical forests, however, remains largely unexplored. This study evaluated P limitation by observing the P fertilizer response of a naturally regenerated 24-year-old forest and its soil. In February 1999, six 20 × 20-m plots were established in secondary forest in the Brazilian Amazon. After 1 year of pre-treatment tree measurements, 50 kg P $ ha^{−1} $ was applied in January 2000 and again in January 2001. Soil sorption of P was relatively low (∼100 μg $ g^{−1} $) in the surface 0–20 cm while sorption increased to ∼180 μg $ g^{−1} $ at 20–50 cm and approached ∼500 μg $ g^{−1} $ for the 50- to 200-cm layers. Soil P in 0–10 cm, measured as sequentially extractable fractions (resin, $ HCO_{3} $-Pi, NaOH-Pi, NaOH-Po, and 1 M HCl), increased shortly after fertilization and could account for nearly all the 50 kg P $ ha^{−1} $ added at each date. During the following 6 years, soil P in fertilized plots declined in all pools other than resin P, and by June 2006, concentrations returned to pre-fertilization levels. Despite the increase in extractable P with fertilization, increased tree growth was not detected from stand age 25 to 31 years. It appears that during secondary forest succession at this site, the forest P cycle was conservative so as to maintain available P at a sufficient concentration to meet forest P demands. |
abstract_unstemmed |
Abstract Mature tropical forests are considered to be P limited and to cycle P efficiently. Whether P limitations are significant in younger secondary tropical forests, however, remains largely unexplored. This study evaluated P limitation by observing the P fertilizer response of a naturally regenerated 24-year-old forest and its soil. In February 1999, six 20 × 20-m plots were established in secondary forest in the Brazilian Amazon. After 1 year of pre-treatment tree measurements, 50 kg P $ ha^{−1} $ was applied in January 2000 and again in January 2001. Soil sorption of P was relatively low (∼100 μg $ g^{−1} $) in the surface 0–20 cm while sorption increased to ∼180 μg $ g^{−1} $ at 20–50 cm and approached ∼500 μg $ g^{−1} $ for the 50- to 200-cm layers. Soil P in 0–10 cm, measured as sequentially extractable fractions (resin, $ HCO_{3} $-Pi, NaOH-Pi, NaOH-Po, and 1 M HCl), increased shortly after fertilization and could account for nearly all the 50 kg P $ ha^{−1} $ added at each date. During the following 6 years, soil P in fertilized plots declined in all pools other than resin P, and by June 2006, concentrations returned to pre-fertilization levels. Despite the increase in extractable P with fertilization, increased tree growth was not detected from stand age 25 to 31 years. It appears that during secondary forest succession at this site, the forest P cycle was conservative so as to maintain available P at a sufficient concentration to meet forest P demands. |
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title_short |
Soil and tree response to P fertilization in a secondary tropical forest supported by an Oxisol |
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https://dx.doi.org/10.1007/s00374-011-0659-9 |
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Figueiredo, Ricardo de O. de Carvalho, Cláudio J. Reis Davidson, Eric A. |
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|
score |
7.402936 |