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Registro Completo |
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Biblioteca(s): |
Embrapa Agrobiologia. |
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Data corrente: |
07/06/2000 |
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Data da última atualização: |
07/06/2000 |
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Autoria: |
VANLAUWE, B.; NWOKE, O. C.; SANGINGA, N.; MERCKX, R. |
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Título: |
Evaluation of methods for measuring microbial biomass C and N relationships between microbial biomass and soil organic matter particle size classes in West-African soils. |
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Ano de publicação: |
1999 |
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Fonte/Imprenta: |
Soil Biology and Biochemistry, Oxford, v. 31, p. 1071-1082, 1999. |
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Idioma: |
Inglês |
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Conteúdo: |
The fumigation-incubation (FI) and the fumigation-extraction (FE) ninhydrin methods for quantifying the microbial biomass pool were tested and the relationships between microbial biomass characteristics and soil organic matter fractions (separated following particle size) investigated for a range of soils representative for the West-African moist savanna zone (13 soils). Three soils from the humid forest zone were also included. Microbial C values calculated using the CO2-C production of the fumigated soils from d 10 to d 20 as control (Bio-C (II)) were better correlated with the flush of ninhydrin reactive N (NRN) during 10 d of fumigation than those calculated with the CO2-C production in the unfumigated soils from d 10 to d 20 as control (Bio-C (I)). The Bio-C (II) values also showed a more consistent range of values (22-210 mg C kg-1 soil) than the Bio-C (I) values. Using a kc factor of 0.35, which was considered to be more appropriate for our soils than a kc factor of 0.45, kc could be estimated as 22 and 16, for a 5- and 10-d fumigation, respectively. For all savanna soils, the NRN flush after 5 d of fumigation was closely related to the NRN flush after 10 d, indicating that a 5-d fumigation was sufficient provided that the k-values are adapted. Mineral N flushes during incubation and incubation after fumigation were small. Although microbial N values calculated as [NH4+ -N flush of the fumigated soils (0-10 d)] kN with KN = -0.014x(CO2-C-flush-to-NH4+ -N-flush during fumigation) + 0.39, which gave values of 14.0-100.7 mg N kg-1 soil, showed the best relationship with the NRN flush after 10 d of fumigation, microbial N values calculated as [(mineral N flush of the fumigated soils after 10 d) - (mineral N flush of the unfumigated soils after 10 d)]/0.68, which gave values of 3.4 - 46.2 mg N.kg-1 soil, including 3 values menor 2 mg N kg-1 soil and 1 negative value, yielded microbial C-to-N ratios (4.7-16.4) which were better reflecting the ratio C-flush-to-N-flush of fumigated soils (5.2-13.5). Using a kN value of 0.68, kN,NRN could be estimated as 1.5. Between 7 and 17% and between 11 and 28% of the total soil C was part of the soil litter (SL) (organic particles larger than 250 um) and the particulate organic matter (POM) (organic particles larger than 53 um), respectively. The CO2-C production of the unfumigated soils was strongly (P menor 0.01) related to the SL-C content. Inclusion of the sit and clay content in a linear regression equation increased the R value from 0.70 to 0.91. The Bio-C (II) content showed the best relationship with the C content of the soil particles between 53 and 20 um and the silt fraction. The NRN flush after 10 d showed the best relationship with the C content of the particles between 250 and 53 um and between 53 and 20 um. Maximally 48% of the variation in Bio-C (II) values was explained by the C content of the various fractions, indicating that the present methods do not exclusively measure the active microbial biomass. MenosThe fumigation-incubation (FI) and the fumigation-extraction (FE) ninhydrin methods for quantifying the microbial biomass pool were tested and the relationships between microbial biomass characteristics and soil organic matter fractions (separated following particle size) investigated for a range of soils representative for the West-African moist savanna zone (13 soils). Three soils from the humid forest zone were also included. Microbial C values calculated using the CO2-C production of the fumigated soils from d 10 to d 20 as control (Bio-C (II)) were better correlated with the flush of ninhydrin reactive N (NRN) during 10 d of fumigation than those calculated with the CO2-C production in the unfumigated soils from d 10 to d 20 as control (Bio-C (I)). The Bio-C (II) values also showed a more consistent range of values (22-210 mg C kg-1 soil) than the Bio-C (I) values. Using a kc factor of 0.35, which was considered to be more appropriate for our soils than a kc factor of 0.45, kc could be estimated as 22 and 16, for a 5- and 10-d fumigation, respectively. For all savanna soils, the NRN flush after 5 d of fumigation was closely related to the NRN flush after 10 d, indicating that a 5-d fumigation was sufficient provided that the k-values are adapted. Mineral N flushes during incubation and incubation after fumigation were small. Although microbial N values calculated as [NH4+ -N flush of the fumigated soils (0-10 d)] kN with KN = -0.014x(CO2-C-flush-to-NH4+ -N-flush during... Mostrar Tudo |
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Palavras-Chave: |
Biomassa microbiana; C; N. |
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Thesagro: |
Análise Estatística; Carbono; Fumigação; Matéria Orgânica; Mineralização; Nitrogênio; Solo. |
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Thesaurus Nal: |
carbon; fumigation; microbial biomass; mineralization; nitrogen; organic matter; soil; statistical analysis. |
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Categoria do assunto: |
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Marc: |
LEADER 04063naa a2200373 a 4500
001 1621167
005 2000-06-07
008 1999 bl --- 0-- u #d
100 1 $aVANLAUWE, B.
245 $aEvaluation of methods for measuring microbial biomass C and N relationships between microbial biomass and soil organic matter particle size classes in West-African soils.
260 $c1999
520 $aThe fumigation-incubation (FI) and the fumigation-extraction (FE) ninhydrin methods for quantifying the microbial biomass pool were tested and the relationships between microbial biomass characteristics and soil organic matter fractions (separated following particle size) investigated for a range of soils representative for the West-African moist savanna zone (13 soils). Three soils from the humid forest zone were also included. Microbial C values calculated using the CO2-C production of the fumigated soils from d 10 to d 20 as control (Bio-C (II)) were better correlated with the flush of ninhydrin reactive N (NRN) during 10 d of fumigation than those calculated with the CO2-C production in the unfumigated soils from d 10 to d 20 as control (Bio-C (I)). The Bio-C (II) values also showed a more consistent range of values (22-210 mg C kg-1 soil) than the Bio-C (I) values. Using a kc factor of 0.35, which was considered to be more appropriate for our soils than a kc factor of 0.45, kc could be estimated as 22 and 16, for a 5- and 10-d fumigation, respectively. For all savanna soils, the NRN flush after 5 d of fumigation was closely related to the NRN flush after 10 d, indicating that a 5-d fumigation was sufficient provided that the k-values are adapted. Mineral N flushes during incubation and incubation after fumigation were small. Although microbial N values calculated as [NH4+ -N flush of the fumigated soils (0-10 d)] kN with KN = -0.014x(CO2-C-flush-to-NH4+ -N-flush during fumigation) + 0.39, which gave values of 14.0-100.7 mg N kg-1 soil, showed the best relationship with the NRN flush after 10 d of fumigation, microbial N values calculated as [(mineral N flush of the fumigated soils after 10 d) - (mineral N flush of the unfumigated soils after 10 d)]/0.68, which gave values of 3.4 - 46.2 mg N.kg-1 soil, including 3 values menor 2 mg N kg-1 soil and 1 negative value, yielded microbial C-to-N ratios (4.7-16.4) which were better reflecting the ratio C-flush-to-N-flush of fumigated soils (5.2-13.5). Using a kN value of 0.68, kN,NRN could be estimated as 1.5. Between 7 and 17% and between 11 and 28% of the total soil C was part of the soil litter (SL) (organic particles larger than 250 um) and the particulate organic matter (POM) (organic particles larger than 53 um), respectively. The CO2-C production of the unfumigated soils was strongly (P menor 0.01) related to the SL-C content. Inclusion of the sit and clay content in a linear regression equation increased the R value from 0.70 to 0.91. The Bio-C (II) content showed the best relationship with the C content of the soil particles between 53 and 20 um and the silt fraction. The NRN flush after 10 d showed the best relationship with the C content of the particles between 250 and 53 um and between 53 and 20 um. Maximally 48% of the variation in Bio-C (II) values was explained by the C content of the various fractions, indicating that the present methods do not exclusively measure the active microbial biomass.
650 $acarbon
650 $afumigation
650 $amicrobial biomass
650 $amineralization
650 $anitrogen
650 $aorganic matter
650 $asoil
650 $astatistical analysis
650 $aAnálise Estatística
650 $aCarbono
650 $aFumigação
650 $aMatéria Orgânica
650 $aMineralização
650 $aNitrogênio
650 $aSolo
653 $aBiomassa microbiana
653 $aC
653 $aN
700 1 $aNWOKE, O. C.
700 1 $aSANGINGA, N.
700 1 $aMERCKX, R.
773 $tSoil Biology and Biochemistry, Oxford$gv. 31, p. 1071-1082, 1999.
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Embrapa Agrobiologia (CNPAB) |
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| 3. |  | GILLER, K. E.; ANDERSSON, J. A.; CORBEELS, M.; KIRKEGAARD, J.; MORTENSEN, D.; ERENSTEIN, O.; VANLAUWE, B. Beyond conservation agriculture. Frontiers in Plant Science, v. 6, article 870, October 2015.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
| Biblioteca(s): Embrapa Cerrados. |
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| 4. | | SANCHEZ, P. A.; AHAMED, S.; CARRÉ, F.; HARTEMINK, A. E.; HEMPEL, J.; HUISING, J.; LAGACHERIE, P.; MACBRATNEY, A. B.; MCKENZIE, N. J.; MENDONÇA-SANTOS, M. de L.; MINASNY, B.; MONTANARELLA, L.; OKOTH, P.; PALM, C. A.; SACHS, J. D.; SHEPHERD, K. D.; VAGEN, T. G.; VANLAUWE, B.; WALSH, M. G.; WINOWIECKI, L. A.; ZHANG, G. L. Digital soil map of the world. Science, v. 325, n. 5941, p. 680-681, 2009.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
| Biblioteca(s): Embrapa Solos. |
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| Registros recuperados : 4 | |
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