BIOCHAR: REALITY AND POTENCIAL USE IN FORESTRY
Autor(a) principal: | |
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Data de Publicação: | 2018 |
Outros Autores: | , , , |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Ciência Florestal (Online) |
Texto Completo: | https://periodicos.ufsm.br/cienciaflorestal/article/view/32128 |
Resumo: | The use of carbonized plant biomass has been recovered and evaluated as an alternative of improving soil fertility. The material generated, called biochar, is the product formed by pyrolysis, which is the thermal decomposition of biomass in a closed container under limited supply of oxygen and at relatively low temperatures. The chemical and structural composition of biochar is highly heterogeneous, with the exception of pH, which is usually higher than seven. Some properties are present in all kinds of biochar, including high carbon content and degree of aromaticity, which explains its high level of recalcitrance. However, its exact chemical composition and structure depends on the combination of raw material and pyrolysis conditions. When applied to soil, biochar can increase pH, cation exchange capacity and organic carbon and nutrient availability, raises in the abundance and functioning of mycorrhizal fungi, providing refuge for micro-organisms in the biochar micropores and improving soil structure and water availability. All these features in the soil interaction make its use in the agriculture normally to have positive effects on plant growth. It is believed that the use of biochar can contribute to carbon sequestration, it is considered by many as "carbon negative" due to its ability to promote plant growth and its stability in the soil. Studies with biochar have reached worldwide proportions involving different areas, and have grown a lot in recent years. However, there are still many uncertainties about its use in agriculture, mainly because the published papers have given more focus to biochar ability to maintain and improve soil fertility and increase agricultural productivity than to clarify the possible risks involved in biochar utilization. |
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BIOCHAR: REALITY AND POTENCIAL USE IN FORESTRYBIOCARVÃO: REALIDADE E POTENCIAL DE USO NO MEIO FLORESTALplant growthpyrogenic carbonsoil fertility.crescimento vegetalcarbono pirogênicofertilidade do soloThe use of carbonized plant biomass has been recovered and evaluated as an alternative of improving soil fertility. The material generated, called biochar, is the product formed by pyrolysis, which is the thermal decomposition of biomass in a closed container under limited supply of oxygen and at relatively low temperatures. The chemical and structural composition of biochar is highly heterogeneous, with the exception of pH, which is usually higher than seven. Some properties are present in all kinds of biochar, including high carbon content and degree of aromaticity, which explains its high level of recalcitrance. However, its exact chemical composition and structure depends on the combination of raw material and pyrolysis conditions. When applied to soil, biochar can increase pH, cation exchange capacity and organic carbon and nutrient availability, raises in the abundance and functioning of mycorrhizal fungi, providing refuge for micro-organisms in the biochar micropores and improving soil structure and water availability. All these features in the soil interaction make its use in the agriculture normally to have positive effects on plant growth. It is believed that the use of biochar can contribute to carbon sequestration, it is considered by many as "carbon negative" due to its ability to promote plant growth and its stability in the soil. Studies with biochar have reached worldwide proportions involving different areas, and have grown a lot in recent years. However, there are still many uncertainties about its use in agriculture, mainly because the published papers have given more focus to biochar ability to maintain and improve soil fertility and increase agricultural productivity than to clarify the possible risks involved in biochar utilization.O uso de resíduos vegetais carbonizados vem sendo resgatado e avaliado como alternativa para melhorar a qualidade do solo. O material gerado, denominado biocarvão, é o produto formado a partir da pirólise, que é a alteração térmica da biomassa em ambiente fechado, com suprimento limitado de oxigênio e em temperaturas relativamente baixas. A composição química e estrutural do biocarvão é altamente heterogênea, mas o pH é normalmente maior que sete. Algumas propriedades estão presentes em todos os biocarvões, incluindo alto teor de carbono e grau de aromaticidade, o que explica seu alto nível de recalcitrância. Contudo, a exata composição química e estrutural é dependente da combinação da matéria-prima e das condições de pirólise. Quando aplicado ao solo, o biocarvão pode aumentar o pH, a capacidade de troca de cátions, o teor de carbono orgânico e a disponibilidade de nutrientes; alterar a abundância e funcionamento de fungos micorrízicos e prover refúgio para microrganismos nos microporos do biocarvão; e melhorar a estrutura do solo e disponibilidade de água. Todas estas características de interação com o solo fazem com que a sua utilização no meio agrícola apresente normalmente efeitos positivos para o crescimento vegetal. Acredita-se também que a utilização de biocarvão possa contribuir para o sequestro de carbono, sendo considerado por muitos como “carbono negativo”, devido a sua capacidade de promover o crescimento vegetal e pela sua estabilidade no solo. Estudos com o biocarvão já atingiram proporções de escala mundial envolvendo diversas áreas e têm crescido muito nos últimos anos. No entanto, ainda existem muitas incertezas sobre a sua utilização na agricultura, devido principalmente ao fato de que os trabalhos publicados têm dado mais atenção a sua capacidade de manutenção e melhoria da fertilidade do solo e aumento da produtividade agrícola do que esclarecimentos dos possíveis riscos envolvidos na utilização do biocarvão.Universidade Federal de Santa Maria2018-06-29info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://periodicos.ufsm.br/cienciaflorestal/article/view/3212810.5902/1980509832128Ciência Florestal; Vol. 28 No. 2 (2018); 875-887Ciência Florestal; v. 28 n. 2 (2018); 875-8871980-50980103-9954reponame:Ciência Florestal (Online)instname:Universidade Federal de Santa Maria (UFSM)instacron:UFSMporhttps://periodicos.ufsm.br/cienciaflorestal/article/view/32128/pdfCopyright (c) 2018 Ciência Florestalinfo:eu-repo/semantics/openAccessTrazzi, Paulo AndréHiga, Antonio RioyeiDieckow, JefersonMangrich, Antonio SalvioHiga, Rosana Clara Vitoria2018-06-29T11:07:47Zoai:ojs.pkp.sfu.ca:article/32128Revistahttp://www.ufsm.br/cienciaflorestal/ONGhttps://old.scielo.br/oai/scielo-oai.php||cienciaflorestal@ufsm.br|| cienciaflorestal@gmail.com|| cf@smail.ufsm.br1980-50980103-9954opendoar:2018-06-29T11:07:47Ciência Florestal (Online) - Universidade Federal de Santa Maria (UFSM)false |
dc.title.none.fl_str_mv |
BIOCHAR: REALITY AND POTENCIAL USE IN FORESTRY BIOCARVÃO: REALIDADE E POTENCIAL DE USO NO MEIO FLORESTAL |
title |
BIOCHAR: REALITY AND POTENCIAL USE IN FORESTRY |
spellingShingle |
BIOCHAR: REALITY AND POTENCIAL USE IN FORESTRY Trazzi, Paulo André plant growth pyrogenic carbon soil fertility. crescimento vegetal carbono pirogênico fertilidade do solo |
title_short |
BIOCHAR: REALITY AND POTENCIAL USE IN FORESTRY |
title_full |
BIOCHAR: REALITY AND POTENCIAL USE IN FORESTRY |
title_fullStr |
BIOCHAR: REALITY AND POTENCIAL USE IN FORESTRY |
title_full_unstemmed |
BIOCHAR: REALITY AND POTENCIAL USE IN FORESTRY |
title_sort |
BIOCHAR: REALITY AND POTENCIAL USE IN FORESTRY |
author |
Trazzi, Paulo André |
author_facet |
Trazzi, Paulo André Higa, Antonio Rioyei Dieckow, Jeferson Mangrich, Antonio Salvio Higa, Rosana Clara Vitoria |
author_role |
author |
author2 |
Higa, Antonio Rioyei Dieckow, Jeferson Mangrich, Antonio Salvio Higa, Rosana Clara Vitoria |
author2_role |
author author author author |
dc.contributor.author.fl_str_mv |
Trazzi, Paulo André Higa, Antonio Rioyei Dieckow, Jeferson Mangrich, Antonio Salvio Higa, Rosana Clara Vitoria |
dc.subject.por.fl_str_mv |
plant growth pyrogenic carbon soil fertility. crescimento vegetal carbono pirogênico fertilidade do solo |
topic |
plant growth pyrogenic carbon soil fertility. crescimento vegetal carbono pirogênico fertilidade do solo |
description |
The use of carbonized plant biomass has been recovered and evaluated as an alternative of improving soil fertility. The material generated, called biochar, is the product formed by pyrolysis, which is the thermal decomposition of biomass in a closed container under limited supply of oxygen and at relatively low temperatures. The chemical and structural composition of biochar is highly heterogeneous, with the exception of pH, which is usually higher than seven. Some properties are present in all kinds of biochar, including high carbon content and degree of aromaticity, which explains its high level of recalcitrance. However, its exact chemical composition and structure depends on the combination of raw material and pyrolysis conditions. When applied to soil, biochar can increase pH, cation exchange capacity and organic carbon and nutrient availability, raises in the abundance and functioning of mycorrhizal fungi, providing refuge for micro-organisms in the biochar micropores and improving soil structure and water availability. All these features in the soil interaction make its use in the agriculture normally to have positive effects on plant growth. It is believed that the use of biochar can contribute to carbon sequestration, it is considered by many as "carbon negative" due to its ability to promote plant growth and its stability in the soil. Studies with biochar have reached worldwide proportions involving different areas, and have grown a lot in recent years. However, there are still many uncertainties about its use in agriculture, mainly because the published papers have given more focus to biochar ability to maintain and improve soil fertility and increase agricultural productivity than to clarify the possible risks involved in biochar utilization. |
publishDate |
2018 |
dc.date.none.fl_str_mv |
2018-06-29 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://periodicos.ufsm.br/cienciaflorestal/article/view/32128 10.5902/1980509832128 |
url |
https://periodicos.ufsm.br/cienciaflorestal/article/view/32128 |
identifier_str_mv |
10.5902/1980509832128 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
https://periodicos.ufsm.br/cienciaflorestal/article/view/32128/pdf |
dc.rights.driver.fl_str_mv |
Copyright (c) 2018 Ciência Florestal info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Copyright (c) 2018 Ciência Florestal |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade Federal de Santa Maria |
publisher.none.fl_str_mv |
Universidade Federal de Santa Maria |
dc.source.none.fl_str_mv |
Ciência Florestal; Vol. 28 No. 2 (2018); 875-887 Ciência Florestal; v. 28 n. 2 (2018); 875-887 1980-5098 0103-9954 reponame:Ciência Florestal (Online) instname:Universidade Federal de Santa Maria (UFSM) instacron:UFSM |
instname_str |
Universidade Federal de Santa Maria (UFSM) |
instacron_str |
UFSM |
institution |
UFSM |
reponame_str |
Ciência Florestal (Online) |
collection |
Ciência Florestal (Online) |
repository.name.fl_str_mv |
Ciência Florestal (Online) - Universidade Federal de Santa Maria (UFSM) |
repository.mail.fl_str_mv |
||cienciaflorestal@ufsm.br|| cienciaflorestal@gmail.com|| cf@smail.ufsm.br |
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1799944133354192896 |