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Registro Completo |
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
03/10/2022 |
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Data da última atualização: |
15/04/2024 |
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Tipo da produção científica: |
Documentos |
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Autoria: |
SANTOS, H. G. dos; JACOMINE, P. K. T.; ANJOS, L. H. C. dos; OLIVEIRA, V. A. de; LUMBRERAS, J. F.; COELHO, M. R.; ALMEIDA, J. A. de; ARAUJO FILHO, J. C. de. |
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Afiliação: |
HUMBERTO GONCALVES DOS SANTOS, CNPS; PAULO KLINGER TITO JACOMINE, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; LÚCIA HELENA CUNHA DOS ANJOS, UNIVERSIDADE FEDERAL RURAL DO RIO DE JANEIRO; VIRLEI ÁLVARO DE OLIVEIRA, IBGE; JOSE FRANCISCO LUMBRERAS, CNPS; MAURICIO RIZZATO COELHO, CNPS; JAIME ANTONIO DE ALMEIDA, UNIVERSIDADE DO ESTADO DE SANTA CATARINA; JOSE COELHO DE ARAUJO FILHO, CNPS. |
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Título: |
Proposta de atualização da quinta edição do Sistema Brasileiro de Classificação de Solos: ano 2022. |
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Ano de publicação: |
2022 |
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Fonte/Imprenta: |
Rio de Janeiro: Embrapa Solos, 2022. |
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Páginas: |
133 p. |
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Descrição Física: |
PDF. |
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Série: |
(Embrapa Solos. Documentos, 233). |
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ISSN: |
1517-2627 |
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Idioma: |
Português |
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Notas: |
ODS 2. |
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Conteúdo: |
Este trabalho apresenta as alterações propostas à 5ª edição do Sistema Brasileiro de Classificação de Solos (SiBCS), disponível em: https://www.embrapa.br/busca-de-publicacoes/-/publicacao/1094003/sistema-brasileiro-de-classificacao-de-solos, a exemplo da publicação Proposta de atualização da terceira edição do Sistema Brasileiro de Classificação de Solos: ano 2017, da Série Documentos 197, de 2017, disponível em: https://www.embrapa.br/busca-de-publicacoes/-/publicacao/1086196/proposta-de-atualizacao-da-terceira-edicao-do-sistema-brasileiro-de-classificacao-de-solos-ano-2017. A grafia azul refere-se às inserções, enquanto, entre as partes que foram suprimidas, aquelas consideradas mais relevantes, estão marcadas com grafia vermelha e tachadas. |
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Palavras-Chave: |
Selo ODS 2; SiBCS. |
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Thesagro: |
Classificação do Solo; Taxonomia. |
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Thesaurus Nal: |
Soil classification. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/doc/1147080/1/CNPS-DOC-233-2022.pdf
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Marc: |
LEADER 01668nam a2200301 a 4500
001 2147080
005 2024-04-15
008 2022 bl uuuu 00u1 u #d
022 $a1517-2627
100 1 $aSANTOS, H. G. dos
245 $aProposta de atualização da quinta edição do Sistema Brasileiro de Classificação de Solos$bano 2022.$h[electronic resource]
260 $aRio de Janeiro: Embrapa Solos$c2022
300 $a133 p.$cPDF.
490 $a(Embrapa Solos. Documentos, 233).
500 $aODS 2.
520 $aEste trabalho apresenta as alterações propostas à 5ª edição do Sistema Brasileiro de Classificação de Solos (SiBCS), disponível em: https://www.embrapa.br/busca-de-publicacoes/-/publicacao/1094003/sistema-brasileiro-de-classificacao-de-solos, a exemplo da publicação Proposta de atualização da terceira edição do Sistema Brasileiro de Classificação de Solos: ano 2017, da Série Documentos 197, de 2017, disponível em: https://www.embrapa.br/busca-de-publicacoes/-/publicacao/1086196/proposta-de-atualizacao-da-terceira-edicao-do-sistema-brasileiro-de-classificacao-de-solos-ano-2017. A grafia azul refere-se às inserções, enquanto, entre as partes que foram suprimidas, aquelas consideradas mais relevantes, estão marcadas com grafia vermelha e tachadas.
650 $aSoil classification
650 $aClassificação do Solo
650 $aTaxonomia
653 $aSelo ODS 2
653 $aSiBCS
700 1 $aJACOMINE, P. K. T.
700 1 $aANJOS, L. H. C. dos
700 1 $aOLIVEIRA, V. A. de
700 1 $aLUMBRERAS, J. F.
700 1 $aCOELHO, M. R.
700 1 $aALMEIDA, J. A. de
700 1 $aARAUJO FILHO, J. C. de
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Registro original: |
Embrapa Solos (CNPS) |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Florestas. Para informações adicionais entre em contato com cnpf.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Florestas. |
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Data corrente: |
06/10/2008 |
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Data da última atualização: |
06/10/2008 |
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Autoria: |
HYODO, F.; TAYASU, I.; KONATÉ, S.; TONDOH, J. E.; LAVELLE, P.; WADA, E. |
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Título: |
Gradual enrichment of 15N with humification of diets in a belowground food web: relationship between 15N and diet age determined using 14C. |
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Ano de publicação: |
2008 |
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Fonte/Imprenta: |
In: INTERNATIONAL COLLOQUIUM ON SOIL ZOOLOGY, 15; INTERNATIONAL COLLOQUIUM ON APTERYGOTA, 12., 2008, Curitiba. Biodiversity, conservation and sustainabele management of soil animal: abstracts. Colombo: Embrapa Florestas. Editors: George Gardner Brown; Klaus Dieter Sautter; Renato Marques; Amarildo Pasini. 1 CD-ROM. |
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Idioma: |
Inglês |
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Conteúdo: |
Stable nitrogen (N) isotope has been widely used to disentangle food web and to infer trophic
positions of organisms based on an assumption that the stepwise enrichment occurs along
trophic levels. The enrichment of 15N in soil organisms with diet humificaition has also been
reported , but the underlying mechanism has not been fully examined. To examine the effect of
diet humification on 15N, we estimated the stable N isotope ratios and diet ages of earthworms
and termites. These organisms feed on organic matter with various degrees of humification,
ranging from undecomposed plant materials to humified organic matter (soil organic matter), in
a gallery forest and a savannah in the Ivory Coast. We defined diet age as the time elapsed
since carbon (C) in the diet of earthworms and termites was fixed from atmospheric CO2 by
photosynthesis; it was estimated by comparing the radiocarbon (14C) content of these organisms
to atmospheric 14CO2 records. Stable N isotope ratios increased along the humification
gradient of diets, and values for earthworms and termites varied from 1.8 to 9.9? and from ?
1.5 to 15.9?, respectively. Epigeic (litter-feeding) earthworms had younger diet ages (2?4 y),
whereas endogeic (soil-feeding) earthworms generally exhibited older diet ages (5?9 y). Grassfeeding
termites had young diet ages (2 y), and wood/soil-feeding termites had the oldest diet
ages (~50 y). Soil-feeding termites were similar in diet age (7?12 y) to wood feeders (8?11 y),
with the exception of one species (18?21 y) that consumes large-diameter wood. A significant
positive relationship was found between diet ages and stable N isotope ratios of the two groups
in the savannah. This relationship held in the gallery forest when termites feeding on woody
tissues were not considered. These results show that the stable N isotope ratios of organisms
can increase with diet age, unless C in the diet has been stored as organic matter, such as
woody tissue, that is able to age without being subject to humification processes. Given that
aboveground food webs are often sustained directly by material and energy flow from belowground
food webs, in addition to trophic interactions, gradual enrichment of 15N with the humification of
belowground diets should be considered when interpreting stable N isotope ratios of terrestrial
food webs. MenosStable nitrogen (N) isotope has been widely used to disentangle food web and to infer trophic
positions of organisms based on an assumption that the stepwise enrichment occurs along
trophic levels. The enrichment of 15N in soil organisms with diet humificaition has also been
reported , but the underlying mechanism has not been fully examined. To examine the effect of
diet humification on 15N, we estimated the stable N isotope ratios and diet ages of earthworms
and termites. These organisms feed on organic matter with various degrees of humification,
ranging from undecomposed plant materials to humified organic matter (soil organic matter), in
a gallery forest and a savannah in the Ivory Coast. We defined diet age as the time elapsed
since carbon (C) in the diet of earthworms and termites was fixed from atmospheric CO2 by
photosynthesis; it was estimated by comparing the radiocarbon (14C) content of these organisms
to atmospheric 14CO2 records. Stable N isotope ratios increased along the humification
gradient of diets, and values for earthworms and termites varied from 1.8 to 9.9? and from ?
1.5 to 15.9?, respectively. Epigeic (litter-feeding) earthworms had younger diet ages (2?4 y),
whereas endogeic (soil-feeding) earthworms generally exhibited older diet ages (5?9 y). Grassfeeding
termites had young diet ages (2 y), and wood/soil-feeding termites had the oldest diet
ages (~50 y). Soil-feeding termites were similar in diet age (7?12 y) to wood feeders (8?11 y),
with the exc... Mostrar Tudo |
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Categoria do assunto: |
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Marc: |
LEADER 03163naa a2200181 a 4500
001 1315053
005 2008-10-06
008 2008 bl uuuu u00u1 u #d
100 1 $aHYODO, F.
245 $aGradual enrichment of 15N with humification of diets in a belowground food web$brelationship between 15N and diet age determined using 14C.
260 $c2008
520 $aStable nitrogen (N) isotope has been widely used to disentangle food web and to infer trophic positions of organisms based on an assumption that the stepwise enrichment occurs along trophic levels. The enrichment of 15N in soil organisms with diet humificaition has also been reported , but the underlying mechanism has not been fully examined. To examine the effect of diet humification on 15N, we estimated the stable N isotope ratios and diet ages of earthworms and termites. These organisms feed on organic matter with various degrees of humification, ranging from undecomposed plant materials to humified organic matter (soil organic matter), in a gallery forest and a savannah in the Ivory Coast. We defined diet age as the time elapsed since carbon (C) in the diet of earthworms and termites was fixed from atmospheric CO2 by photosynthesis; it was estimated by comparing the radiocarbon (14C) content of these organisms to atmospheric 14CO2 records. Stable N isotope ratios increased along the humification gradient of diets, and values for earthworms and termites varied from 1.8 to 9.9? and from ? 1.5 to 15.9?, respectively. Epigeic (litter-feeding) earthworms had younger diet ages (2?4 y), whereas endogeic (soil-feeding) earthworms generally exhibited older diet ages (5?9 y). Grassfeeding termites had young diet ages (2 y), and wood/soil-feeding termites had the oldest diet ages (~50 y). Soil-feeding termites were similar in diet age (7?12 y) to wood feeders (8?11 y), with the exception of one species (18?21 y) that consumes large-diameter wood. A significant positive relationship was found between diet ages and stable N isotope ratios of the two groups in the savannah. This relationship held in the gallery forest when termites feeding on woody tissues were not considered. These results show that the stable N isotope ratios of organisms can increase with diet age, unless C in the diet has been stored as organic matter, such as woody tissue, that is able to age without being subject to humification processes. Given that aboveground food webs are often sustained directly by material and energy flow from belowground food webs, in addition to trophic interactions, gradual enrichment of 15N with the humification of belowground diets should be considered when interpreting stable N isotope ratios of terrestrial food webs.
700 1 $aTAYASU, I.
700 1 $aKONATÉ, S.
700 1 $aTONDOH, J. E.
700 1 $aLAVELLE, P.
700 1 $aWADA, E.
773 $tIn: INTERNATIONAL COLLOQUIUM ON SOIL ZOOLOGY, 15; INTERNATIONAL COLLOQUIUM ON APTERYGOTA, 12., 2008, Curitiba. Biodiversity, conservation and sustainabele management of soil animal: abstracts. Colombo: Embrapa Florestas. Editors: George Gardner Brown; Klaus Dieter Sautter; Renato Marques; Amarildo Pasini. 1 CD-ROM.
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