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 | Acesso ao texto completo restrito à biblioteca da Embrapa Milho e Sorgo. Para informações adicionais entre em contato com cnpms.biblioteca@embrapa.br. |
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Registro Completo |
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Biblioteca(s): |
Embrapa Caprinos e Ovinos; Embrapa Milho e Sorgo. |
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Data corrente: |
17/11/2011 |
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Data da última atualização: |
05/09/2018 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
SILVA, G. L.; LIMA, H. V.; CAMPANHA, M. M.; GILKES, R. J.; OLIVEIRA, T. S. |
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Afiliação: |
Universidade Federal do Ceará (UFC) - Fortaleza, CE.; Universidade Federal Rural do Amazonas, Belém, PA.; MONICA MATOSO CAMPANHA, CNPMS; School of Earth and Environment, The University of Western Australia, Australia; UFC, Fortaleza, CE. |
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Título: |
Soil physical quality of Luvisols under agroforestry, natural vegetation and conventional crop management systems in the Brazilian semi-arid region. |
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Ano de publicação: |
2011 |
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Fonte/Imprenta: |
Geoderma, Amsterdam, v. 167/168, p. 61-70, Nov. 2011. |
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DOI: |
10.1016/j.geoderma.2011.09.009 |
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Idioma: |
Inglês |
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Conteúdo: |
The imposition of agricultural systems changes the natural equilibrium of the soil to an extent that it becomes dependant on management practices and soil resilience. Agroforestry systems (AFs) mimic characteristics of natural ecosystems such as multistrata canopy and deep rooting and may minimize the consequences of these changes by providing soil protection and maintenance of conditions similar to those under natural vegetation. This study evaluates the physical properties of a Luvisol at a site where since 1997 alternative agroforestry systems (AFs) (agrosilvipasture?AGP and silvipasture?SILV), conventional crop management (CCM) and natural vegetation (NV) have been maintained. Undisturbed soil cores were collected in 2005 and submitted to a range of matric suction for which soil bulk density (BD), soil penetration resistance (Q) and soil water content (?) were determined. Water retention and penetration resistance were used to determine the least limiting water range (LLWR) and the slope of the soil water retention curve at its inflection point (S-value). Particle size, total organic carbon (TOC) and particle density were determined using the disturbed soil samples. Water retention and porosity followed the sequence NVNSILVNCCMNAGP. The AFs studied (AGP and SILV) improved or maintained soil physical quality when compared to NV with no significant differences between the S-values of 0.044, 0.042 and 0.050, respectively. However, the S-value of 0.035 for CCM indicates that this management was unable to maintain soil physical quality on the same levels as AFs and NV. The decrease of LLWR with BD occurred for all treatments, and the BD at a maximum effect (LLWR=0) which is called the critical BD (BDc), was, respectively, 1.69, 1.62, 1.56 and 1.56 Mg m?3 for AGP, SILV, NV and CCM. The larger values of LLWR for AFs (AGP and SILV) are similar to the value for NV, with associated superior aeration, matric suction and reduced resistance to penetration by roots. Indices such as LLWR and S-value were suitably sensitive and could be used in future research, but it is important to identify other potential indices for these situations that can show how quickly changes in soil quality may occur. MenosThe imposition of agricultural systems changes the natural equilibrium of the soil to an extent that it becomes dependant on management practices and soil resilience. Agroforestry systems (AFs) mimic characteristics of natural ecosystems such as multistrata canopy and deep rooting and may minimize the consequences of these changes by providing soil protection and maintenance of conditions similar to those under natural vegetation. This study evaluates the physical properties of a Luvisol at a site where since 1997 alternative agroforestry systems (AFs) (agrosilvipasture?AGP and silvipasture?SILV), conventional crop management (CCM) and natural vegetation (NV) have been maintained. Undisturbed soil cores were collected in 2005 and submitted to a range of matric suction for which soil bulk density (BD), soil penetration resistance (Q) and soil water content (?) were determined. Water retention and penetration resistance were used to determine the least limiting water range (LLWR) and the slope of the soil water retention curve at its inflection point (S-value). Particle size, total organic carbon (TOC) and particle density were determined using the disturbed soil samples. Water retention and porosity followed the sequence NVNSILVNCCMNAGP. The AFs studied (AGP and SILV) improved or maintained soil physical quality when compared to NV with no significant differences between the S-values of 0.044, 0.042 and 0.050, respectively. However, the S-value of 0.035 for CCM indicates that... Mostrar Tudo |
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Palavras-Chave: |
Agroecologia; Agrofloresta; Agroforestry systems; Código florestal; Higroscopicidade; Least limiting water range; Resistência à penetração; S-value; Sistemas agroflorestais. |
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Thesagro: |
Caatinga; Estrutura do solo; Manejo do solo; Retenção de água no solo; Solo. |
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Thesaurus Nal: |
Agroecology; Brazil; Hygroscopicity; Semiarid soils; Soil management; Soil penetration resistance; Soil structure. |
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Categoria do assunto: |
F Plantas e Produtos de Origem Vegetal
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 03533naa a2200433 a 4500
001 1906840
005 2018-09-05
008 2011 bl uuuu u00u1 u #d
024 7 $a10.1016/j.geoderma.2011.09.009$2DOI
100 1 $aSILVA, G. L.
245 $aSoil physical quality of Luvisols under agroforestry, natural vegetation and conventional crop management systems in the Brazilian semi-arid region.$h[electronic resource]
260 $c2011
520 $aThe imposition of agricultural systems changes the natural equilibrium of the soil to an extent that it becomes dependant on management practices and soil resilience. Agroforestry systems (AFs) mimic characteristics of natural ecosystems such as multistrata canopy and deep rooting and may minimize the consequences of these changes by providing soil protection and maintenance of conditions similar to those under natural vegetation. This study evaluates the physical properties of a Luvisol at a site where since 1997 alternative agroforestry systems (AFs) (agrosilvipasture?AGP and silvipasture?SILV), conventional crop management (CCM) and natural vegetation (NV) have been maintained. Undisturbed soil cores were collected in 2005 and submitted to a range of matric suction for which soil bulk density (BD), soil penetration resistance (Q) and soil water content (?) were determined. Water retention and penetration resistance were used to determine the least limiting water range (LLWR) and the slope of the soil water retention curve at its inflection point (S-value). Particle size, total organic carbon (TOC) and particle density were determined using the disturbed soil samples. Water retention and porosity followed the sequence NVNSILVNCCMNAGP. The AFs studied (AGP and SILV) improved or maintained soil physical quality when compared to NV with no significant differences between the S-values of 0.044, 0.042 and 0.050, respectively. However, the S-value of 0.035 for CCM indicates that this management was unable to maintain soil physical quality on the same levels as AFs and NV. The decrease of LLWR with BD occurred for all treatments, and the BD at a maximum effect (LLWR=0) which is called the critical BD (BDc), was, respectively, 1.69, 1.62, 1.56 and 1.56 Mg m?3 for AGP, SILV, NV and CCM. The larger values of LLWR for AFs (AGP and SILV) are similar to the value for NV, with associated superior aeration, matric suction and reduced resistance to penetration by roots. Indices such as LLWR and S-value were suitably sensitive and could be used in future research, but it is important to identify other potential indices for these situations that can show how quickly changes in soil quality may occur.
650 $aAgroecology
650 $aBrazil
650 $aHygroscopicity
650 $aSemiarid soils
650 $aSoil management
650 $aSoil penetration resistance
650 $aSoil structure
650 $aCaatinga
650 $aEstrutura do solo
650 $aManejo do solo
650 $aRetenção de água no solo
650 $aSolo
653 $aAgroecologia
653 $aAgrofloresta
653 $aAgroforestry systems
653 $aCódigo florestal
653 $aHigroscopicidade
653 $aLeast limiting water range
653 $aResistência à penetração
653 $aS-value
653 $aSistemas agroflorestais
700 1 $aLIMA, H. V.
700 1 $aCAMPANHA, M. M.
700 1 $aGILKES, R. J.
700 1 $aOLIVEIRA, T. S.
773 $tGeoderma, Amsterdam$gv. 167/168, p. 61-70, Nov. 2011.
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Registro original: |
Embrapa Milho e Sorgo (CNPMS) |
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Registro Completo
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Biblioteca(s): |
Embrapa Florestas. |
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Data corrente: |
03/10/2008 |
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Data da última atualização: |
03/10/2008 |
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Autoria: |
HASEGAWA, M.; SUGIURA, S.; ITO, M. T.; YAMAKI, A.; HAMAGUCHI, K.; KISHIMOTO, T.; OKOCHI, I. |
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Título: |
Community structures of soil animals on Chichijima island in Ogasawara islands in relation to the survival of land snails. |
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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: |
Chichijima in Ogasawara (Bonin) Islands is located in the northwestern Pacific Ocean, about
100km south of the mainland of Japan. 95 species of land snails have been recorded from
these islands, and of which more than 90 percent are endemic to the islands (Chiba eta al.
2007). Most of the endemic species, however, have already become extinct or endangered in
Chichijima (Chiba eta al. 2007). Predation pressure by an invasive flatworm (Platyrdemus
manokwari) on the land snails was suggested as one of the cause of the decline of snails
(Ohbayashi et al. 2005, 2007, Sugiura et al. 2006). Soil fauna on Chichijima were investigated
several times (Aoki and Harada 1978 and Ishizawa and Takehara 2001), but the related studies
with decline of snails have not been conducted. The aim of this study was to investigate the
relation of soil fauna with survival of land snails from the comparison of soil fauna on snail surviving
and extinct areas of Chichijima Island.
The research was conducted in June and November of 2005. Ten sites (3 snail surviving sites
and 7 extinct sites) for soil macrofauna and six sites (3 snail surviving sites and 3 extinct sites)
for soil mesofauna were set. Sampling of soil macrofauna was conducted at six quadrates
(each 25 × 25 cm) set at 5 m intervals along a line (25 m) in each site. Litter layer and topsoil (15
cm deep) were collected at each quadrate. Soil macrofauna was immediately picked up from
the soil and litter by hands. Soil mesofauna was extracted from the soil core samples. A 100 ml
soil sample (20 cm2 × 5 cm in depth) including litter layer was taken by a cylindrical core sampler
at each of the ten points set at 5 m intervals along another line (45 m) in each site. Soil mesofauna
was extracted from the samples for three days at 35?? by Tullgren funnels.
Most of soil fauna did not show the decline. However, one undescribed but endemic carabid
species (Badister sp.), which have selective feeding habits on land snails, was not recorded on
snail extinct area. Earthworm was recorded at all study sites, and dominant in soil macrofauna.
All species of the earthworms seemed to be introduced species. The invasive flatworm P.
manokwari has been reported to feed also on the carcasses of earthworms as well as live
snails, therefore P. manokwari is expected to survive on most of the area of Chichijima Island.
Comaparison of this examination with Aoki and Harada (1978) showed that the density of
Isopods decreased. The density and species richness of ants, Collembola and oribatid mites
were not so different between snail survived and exterminated area.
In conclusion, the close relation between soil fauna and land snails has been rarely recognized
except one carabid species, but the present (current) structure of soil animals as reflected in
introduced earthworm, decline of endemic isopods and tramp species of ants indicated the
various impacts on the fauna on Chichijima island. MenosChichijima in Ogasawara (Bonin) Islands is located in the northwestern Pacific Ocean, about
100km south of the mainland of Japan. 95 species of land snails have been recorded from
these islands, and of which more than 90 percent are endemic to the islands (Chiba eta al.
2007). Most of the endemic species, however, have already become extinct or endangered in
Chichijima (Chiba eta al. 2007). Predation pressure by an invasive flatworm (Platyrdemus
manokwari) on the land snails was suggested as one of the cause of the decline of snails
(Ohbayashi et al. 2005, 2007, Sugiura et al. 2006). Soil fauna on Chichijima were investigated
several times (Aoki and Harada 1978 and Ishizawa and Takehara 2001), but the related studies
with decline of snails have not been conducted. The aim of this study was to investigate the
relation of soil fauna with survival of land snails from the comparison of soil fauna on snail surviving
and extinct areas of Chichijima Island.
The research was conducted in June and November of 2005. Ten sites (3 snail surviving sites
and 7 extinct sites) for soil macrofauna and six sites (3 snail surviving sites and 3 extinct sites)
for soil mesofauna were set. Sampling of soil macrofauna was conducted at six quadrates
(each 25 × 25 cm) set at 5 m intervals along a line (25 m) in each site. Litter layer and topsoil (15
cm deep) were collected at each quadrate. Soil macrofauna was immediately picked up from
the soil and litter by hands. Soil mesofauna was extracted fro... Mostrar Tudo |
|
Categoria do assunto: |
-- |
|
Marc: |
LEADER 03773naa a2200193 a 4500
001 1315027
005 2008-10-03
008 2008 bl uuuu u00u1 u #d
100 1 $aHASEGAWA, M.
245 $aCommunity structures of soil animals on Chichijima island in Ogasawara islands in relation to the survival of land snails.
260 $c2008
520 $aChichijima in Ogasawara (Bonin) Islands is located in the northwestern Pacific Ocean, about 100km south of the mainland of Japan. 95 species of land snails have been recorded from these islands, and of which more than 90 percent are endemic to the islands (Chiba eta al. 2007). Most of the endemic species, however, have already become extinct or endangered in Chichijima (Chiba eta al. 2007). Predation pressure by an invasive flatworm (Platyrdemus manokwari) on the land snails was suggested as one of the cause of the decline of snails (Ohbayashi et al. 2005, 2007, Sugiura et al. 2006). Soil fauna on Chichijima were investigated several times (Aoki and Harada 1978 and Ishizawa and Takehara 2001), but the related studies with decline of snails have not been conducted. The aim of this study was to investigate the relation of soil fauna with survival of land snails from the comparison of soil fauna on snail surviving and extinct areas of Chichijima Island. The research was conducted in June and November of 2005. Ten sites (3 snail surviving sites and 7 extinct sites) for soil macrofauna and six sites (3 snail surviving sites and 3 extinct sites) for soil mesofauna were set. Sampling of soil macrofauna was conducted at six quadrates (each 25 × 25 cm) set at 5 m intervals along a line (25 m) in each site. Litter layer and topsoil (15 cm deep) were collected at each quadrate. Soil macrofauna was immediately picked up from the soil and litter by hands. Soil mesofauna was extracted from the soil core samples. A 100 ml soil sample (20 cm2 × 5 cm in depth) including litter layer was taken by a cylindrical core sampler at each of the ten points set at 5 m intervals along another line (45 m) in each site. Soil mesofauna was extracted from the samples for three days at 35?? by Tullgren funnels. Most of soil fauna did not show the decline. However, one undescribed but endemic carabid species (Badister sp.), which have selective feeding habits on land snails, was not recorded on snail extinct area. Earthworm was recorded at all study sites, and dominant in soil macrofauna. All species of the earthworms seemed to be introduced species. The invasive flatworm P. manokwari has been reported to feed also on the carcasses of earthworms as well as live snails, therefore P. manokwari is expected to survive on most of the area of Chichijima Island. Comaparison of this examination with Aoki and Harada (1978) showed that the density of Isopods decreased. The density and species richness of ants, Collembola and oribatid mites were not so different between snail survived and exterminated area. In conclusion, the close relation between soil fauna and land snails has been rarely recognized except one carabid species, but the present (current) structure of soil animals as reflected in introduced earthworm, decline of endemic isopods and tramp species of ants indicated the various impacts on the fauna on Chichijima island.
700 1 $aSUGIURA, S.
700 1 $aITO, M. T.
700 1 $aYAMAKI, A.
700 1 $aHAMAGUCHI, K.
700 1 $aKISHIMOTO, T.
700 1 $aOKOCHI, I.
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.
Download
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