Extractability of aluminium and forms in solution of soils derived from granite in Portugal
Autor(a) principal: | |
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Data de Publicação: | 2018 |
Outros Autores: | |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
Texto Completo: | https://doi.org/10.19084/rca.15914 |
Resumo: | Extractable aluminium (Al) was determined in surface and subsurface horizons of eleven pedons derived from granite occurring in Portugal, under a wide range of precipitation. Five successive extractions with 1 M KCl, 0.5 M CuCl2 and 0.33 M LaCl3 were used. Monomeric (Alm) and organic (Alorg) forms of Al in the soil solution, extracted at field capacity, were also determined. Amounts of extracted Al were greatest with the 0.5 M CuCl2and lowest with the 1 M KCl. These amounts showed strong positive correlation with soil organic C contents. Soil horizons having high contents (56-80 g kg-1) of organic C showed the highest amount of extractable Al by the 0.5 M CuCl2 (12.2-30.9 cmolc kg-1). Organically bound Al extracted by the 0.5 M CuCl2 and 0.33 M LaCl3 was also highest in these soils (7.6-10.1 and 4.7-8.3 cmolc kg-1, respectively). In contrast, lowest amounts of Al extracted by the 1 M KCl, 0.5 M CuCl2 and 0.33 M LaCl3 (0.9-4.3, 4.1-17.1 and 2.2-7.2 cmolc kg-1, respectively) were observed in horizons containing low organic C content (3-22 g kg-1). Concentrations of total (AlT), monomeric (Alm) and organic (Alorg) Al in the soil solution of studied soils also increased with increasing soil organic C content, but only Alm was significantly correlated with soil organic Ccontent. Solution of soils having low organic C contents (3-6 g kg-1) showed the lowest concentrations of AlT, Alm and Alorg (0.09-1.60, 0.06-0.38 and 0.03-1.29 µg mL-1, respectively). In contrast, the concentrations of AlT (7.1-17.2 µg mL-1),Alm (0.8-0.9 µg mL-1),and Alorg (7.6-16.9 µg mL-1)were much higher in soils containing high amounts of organic C (37-73 g kg-1). In order to monitor the effects of Al in the soil and quality of sub-superficial water, changes in the concentration of monomeric forms of Al and their activities in the soil solution need further study. |
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Extractability of aluminium and forms in solution of soils derived from granite in PortugalAlumínio extraível e formas de AL na solução de solos derivados de rocha granítica em PortugalGeralExtractable aluminium (Al) was determined in surface and subsurface horizons of eleven pedons derived from granite occurring in Portugal, under a wide range of precipitation. Five successive extractions with 1 M KCl, 0.5 M CuCl2 and 0.33 M LaCl3 were used. Monomeric (Alm) and organic (Alorg) forms of Al in the soil solution, extracted at field capacity, were also determined. Amounts of extracted Al were greatest with the 0.5 M CuCl2and lowest with the 1 M KCl. These amounts showed strong positive correlation with soil organic C contents. Soil horizons having high contents (56-80 g kg-1) of organic C showed the highest amount of extractable Al by the 0.5 M CuCl2 (12.2-30.9 cmolc kg-1). Organically bound Al extracted by the 0.5 M CuCl2 and 0.33 M LaCl3 was also highest in these soils (7.6-10.1 and 4.7-8.3 cmolc kg-1, respectively). In contrast, lowest amounts of Al extracted by the 1 M KCl, 0.5 M CuCl2 and 0.33 M LaCl3 (0.9-4.3, 4.1-17.1 and 2.2-7.2 cmolc kg-1, respectively) were observed in horizons containing low organic C content (3-22 g kg-1). Concentrations of total (AlT), monomeric (Alm) and organic (Alorg) Al in the soil solution of studied soils also increased with increasing soil organic C content, but only Alm was significantly correlated with soil organic Ccontent. Solution of soils having low organic C contents (3-6 g kg-1) showed the lowest concentrations of AlT, Alm and Alorg (0.09-1.60, 0.06-0.38 and 0.03-1.29 µg mL-1, respectively). In contrast, the concentrations of AlT (7.1-17.2 µg mL-1),Alm (0.8-0.9 µg mL-1),and Alorg (7.6-16.9 µg mL-1)were much higher in soils containing high amounts of organic C (37-73 g kg-1). In order to monitor the effects of Al in the soil and quality of sub-superficial water, changes in the concentration of monomeric forms of Al and their activities in the soil solution need further study.O alumínio (Al) extraível foi determinado em onze pedones (horizontes surperficiais e subsuperficiais) desenvolvidos sobre formações graníticas, em Portugal, sob condições de precipitação média anual bastante diferenciadas. Para o efeito efectuaram-se cinco extracções sucessivas com KCl 1 M, CuCl2 0.5 M e LaCl3 0.33 M. Foram ainda determinadas as formas monoméricas (inorgânicas) e orgânicas de Al na solução do solo extraídas nas condições de capacidade de campo dos mesmos horizontes. Os teores mais elevados de Al extraídos foram obtidos por CuCl2 0.5 M e os mais baixos por KCl 1 M; em qualquer dos casos observou-se uma forte correlação positiva com o teor de C orgânico no solo. Os teores de Al extraído por KCl 1 M, LaCl3 0.33 MeCuCl2 0.5 M(5.4-7.4, 8.4-10.1, 18.0-28.9 cmolc kg-1, respectivamente)foram mais elevados em solos com elevado teor de C orgânico (63-80 g kg-1) do que em solos com baixo teor de C orgânico (3-22 g kg-1), em que se observaram teores de 0.9-4.3, 4.1-17.1 e 2.2-7.2 cmolc kg-1 para a extracção com KCl 1 M, CuCl2 0.5 Me LaCl3 0.33 M, respectivamente. As concentrações de Al total (AlT), Al monomérico (Alm) e Al orgânico (Alorg) na solução do solo também apresentaram uma forte variação com o teor de C orgânico, mas só o Alm apresentou correlação significativa com esse teor. Solos com baixo teor de C orgânico mostraram as concentrações de AlT, Alm e Alorgmais baixas (0.09-1.60, 0.06-0.38 and 0.03-1.29 µg mL-1, respectivamente) na solução de solo. Por outro lado, as concentrações foram muito mais elevadas (7.1-17.7, 0.8-0.9 e 7.6-16.9 µg mL-1, respectivamente para o AlT,Alm e Alorg) em solos com elevado teor de C orgânico (3.7-7.3 g kg-1). Os efeitos do Al no solo e na qualidade das águas sub-superficiais carecem de estudos respeitantes às alterações da concentração de Al monomérico e à sua actividade na solução do mesmo.Sociedade de Ciências Agrárias de Portugal2018-12-06T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttps://doi.org/10.19084/rca.15914eng2183-041X0871-018XAuxtero, EdgardoMadeira, Manuelinfo:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2022-09-06T09:24:02Zoai:ojs.revistas.rcaap.pt:article/15914Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T15:30:40.219567Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse |
dc.title.none.fl_str_mv |
Extractability of aluminium and forms in solution of soils derived from granite in Portugal Alumínio extraível e formas de AL na solução de solos derivados de rocha granítica em Portugal |
title |
Extractability of aluminium and forms in solution of soils derived from granite in Portugal |
spellingShingle |
Extractability of aluminium and forms in solution of soils derived from granite in Portugal Auxtero, Edgardo Geral |
title_short |
Extractability of aluminium and forms in solution of soils derived from granite in Portugal |
title_full |
Extractability of aluminium and forms in solution of soils derived from granite in Portugal |
title_fullStr |
Extractability of aluminium and forms in solution of soils derived from granite in Portugal |
title_full_unstemmed |
Extractability of aluminium and forms in solution of soils derived from granite in Portugal |
title_sort |
Extractability of aluminium and forms in solution of soils derived from granite in Portugal |
author |
Auxtero, Edgardo |
author_facet |
Auxtero, Edgardo Madeira, Manuel |
author_role |
author |
author2 |
Madeira, Manuel |
author2_role |
author |
dc.contributor.author.fl_str_mv |
Auxtero, Edgardo Madeira, Manuel |
dc.subject.por.fl_str_mv |
Geral |
topic |
Geral |
description |
Extractable aluminium (Al) was determined in surface and subsurface horizons of eleven pedons derived from granite occurring in Portugal, under a wide range of precipitation. Five successive extractions with 1 M KCl, 0.5 M CuCl2 and 0.33 M LaCl3 were used. Monomeric (Alm) and organic (Alorg) forms of Al in the soil solution, extracted at field capacity, were also determined. Amounts of extracted Al were greatest with the 0.5 M CuCl2and lowest with the 1 M KCl. These amounts showed strong positive correlation with soil organic C contents. Soil horizons having high contents (56-80 g kg-1) of organic C showed the highest amount of extractable Al by the 0.5 M CuCl2 (12.2-30.9 cmolc kg-1). Organically bound Al extracted by the 0.5 M CuCl2 and 0.33 M LaCl3 was also highest in these soils (7.6-10.1 and 4.7-8.3 cmolc kg-1, respectively). In contrast, lowest amounts of Al extracted by the 1 M KCl, 0.5 M CuCl2 and 0.33 M LaCl3 (0.9-4.3, 4.1-17.1 and 2.2-7.2 cmolc kg-1, respectively) were observed in horizons containing low organic C content (3-22 g kg-1). Concentrations of total (AlT), monomeric (Alm) and organic (Alorg) Al in the soil solution of studied soils also increased with increasing soil organic C content, but only Alm was significantly correlated with soil organic Ccontent. Solution of soils having low organic C contents (3-6 g kg-1) showed the lowest concentrations of AlT, Alm and Alorg (0.09-1.60, 0.06-0.38 and 0.03-1.29 µg mL-1, respectively). In contrast, the concentrations of AlT (7.1-17.2 µg mL-1),Alm (0.8-0.9 µg mL-1),and Alorg (7.6-16.9 µg mL-1)were much higher in soils containing high amounts of organic C (37-73 g kg-1). In order to monitor the effects of Al in the soil and quality of sub-superficial water, changes in the concentration of monomeric forms of Al and their activities in the soil solution need further study. |
publishDate |
2018 |
dc.date.none.fl_str_mv |
2018-12-06T00:00:00Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://doi.org/10.19084/rca.15914 |
url |
https://doi.org/10.19084/rca.15914 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
2183-041X 0871-018X |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.publisher.none.fl_str_mv |
Sociedade de Ciências Agrárias de Portugal |
publisher.none.fl_str_mv |
Sociedade de Ciências Agrárias de Portugal |
dc.source.none.fl_str_mv |
reponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação instacron:RCAAP |
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Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
instacron_str |
RCAAP |
institution |
RCAAP |
reponame_str |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
collection |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
repository.name.fl_str_mv |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
repository.mail.fl_str_mv |
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1799130173096853504 |