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| 14. |  | PEREIRA, A. V.; PEREIRA, E. B. C. Avaliação de métodos de formação de viveiro de seringueira por semeadura direta no campo, sem sementeira e repicagem. Pesquisa Agropecuária Brasileira, Brasília, DF, v. 33, n. 7, p. 1061-65, jul. 1998 Título em inglês: Evaluation of rubber nursery planting methods, by direct sowing the field, without seed bed and transplanting.| Biblioteca(s): Embrapa Unidades Centrais. |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Meio Ambiente. Para informações adicionais entre em contato com cnpma.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Meio Ambiente. |
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Data corrente: |
28/11/2017 |
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Data da última atualização: |
10/08/2022 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 1 |
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Autoria: |
BORBA, R. P.; RIBEIRINHO, V. S.; CAMARGO, O. A. de; ANDRADE, C. A. de; KIRA, C. S.; COSCIONE, A. R. |
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Afiliação: |
RICARDO PEROBELLI BORBA, IG-UNICAMP; VICTOR SANCHEZ RIBEIRINHO; OTAVIO ANTONIO DE CAMARGO, IAC; CRISTIANO ALBERTO DE ANDRADE, CNPMA; CARMEN SILVIA KIRA, Instituto Adolfo Lutz; ALINE RENEE COSCIONE, IAC. |
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Título: |
Ion leaching and soil solution acidification in a vadose zone under soil treated with sewage sludge for agriculture. |
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Ano de publicação: |
2018 |
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Fonte/Imprenta: |
Chemosphere, v. 192, p. 81-89, 2018. |
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ISSN: |
0045-6535 |
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DOI: |
https://doi.org/10.1016/j.chemosphere.2017.10.112 |
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Idioma: |
Inglês |
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Conteúdo: |
In this study, we performed monitoring of the soil solution (SS) over 10 years on a loamy/clayey-textured Dark Red Dystroferric Oxisol that received sewage sludge for agricultural purposes. The SS was obtained by lysimeters installed along the walls of a well at 1 m, 2 m, 3 m, 4 m and 5 m in depth. The major ions found in the SS were NO3-, SO42-, Cl-, Ca2+, Mg2+, Al3+, Pb2+, Cd2+ and Zn2+, and the pH level ranged from 4 to 6.5 along the profile. Throughout the first three years of monitoring, the pH to a 3-m depth became more acidic, and in the last year, this trend reached 5 m. At the 5-m depth, the pH decreased from 6.5 to 4.5 from the first to the last monitoring. The SS acidification was provoked by both nitrite oxidation and ion leaching. The leaching of H+ or the possible ion exchange/desorption of H+ due to the leached cations (Ca2+ and Mg2+) at the 4-m and 5-m depth caused the pH decrease. The ionic strength (IS) of the solution controlled the ion leaching. The sludge application increased the IS to 3 m, increasing the density of the soil charges and its ability to absorb ions. After the sludge application was completed, there was a decrease in IS of the SS as well as a decrease in ion absorption and retention abilities, which promoted leaching to greater depths. During the entire monitoring process, NO3-, Cd and Pb remained above the potability limit. |
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Palavras-Chave: |
Ion leaching; Lodo de esgoto. |
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Thesagro: |
Acidificação; Adubo de esgoto; Lodo residual; Solução do solo. |
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Thesaurus NAL: |
Ionic strength; Sewage sludge; Soil acidification; Soil solution; Vadose zone. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02380naa a2200337 a 4500
001 2080878
005 2022-08-10
008 2018 bl uuuu u00u1 u #d
022 $a0045-6535
024 7 $ahttps://doi.org/10.1016/j.chemosphere.2017.10.112$2DOI
100 1 $aBORBA, R. P.
245 $aIon leaching and soil solution acidification in a vadose zone under soil treated with sewage sludge for agriculture.$h[electronic resource]
260 $c2018
520 $aIn this study, we performed monitoring of the soil solution (SS) over 10 years on a loamy/clayey-textured Dark Red Dystroferric Oxisol that received sewage sludge for agricultural purposes. The SS was obtained by lysimeters installed along the walls of a well at 1 m, 2 m, 3 m, 4 m and 5 m in depth. The major ions found in the SS were NO3-, SO42-, Cl-, Ca2+, Mg2+, Al3+, Pb2+, Cd2+ and Zn2+, and the pH level ranged from 4 to 6.5 along the profile. Throughout the first three years of monitoring, the pH to a 3-m depth became more acidic, and in the last year, this trend reached 5 m. At the 5-m depth, the pH decreased from 6.5 to 4.5 from the first to the last monitoring. The SS acidification was provoked by both nitrite oxidation and ion leaching. The leaching of H+ or the possible ion exchange/desorption of H+ due to the leached cations (Ca2+ and Mg2+) at the 4-m and 5-m depth caused the pH decrease. The ionic strength (IS) of the solution controlled the ion leaching. The sludge application increased the IS to 3 m, increasing the density of the soil charges and its ability to absorb ions. After the sludge application was completed, there was a decrease in IS of the SS as well as a decrease in ion absorption and retention abilities, which promoted leaching to greater depths. During the entire monitoring process, NO3-, Cd and Pb remained above the potability limit.
650 $aIonic strength
650 $aSewage sludge
650 $aSoil acidification
650 $aSoil solution
650 $aVadose zone
650 $aAcidificação
650 $aAdubo de esgoto
650 $aLodo residual
650 $aSolução do solo
653 $aIon leaching
653 $aLodo de esgoto
700 1 $aRIBEIRINHO, V. S.
700 1 $aCAMARGO, O. A. de
700 1 $aANDRADE, C. A. de
700 1 $aKIRA, C. S.
700 1 $aCOSCIONE, A. R.
773 $tChemosphere$gv. 192, p. 81-89, 2018.
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