Estoques e mecanismos de estabiliza??o de C e N em solos da regi?o central da Amaz?nia

Detalhes bibliográficos
Autor(a) principal: Ziviani, Melania Merlo
Data de Publicação: 2020
Tipo de documento: Dissertação
Idioma: por
Título da fonte: Biblioteca Digital de Teses e Dissertações da UFRRJ
Texto Completo: https://tede.ufrrj.br/jspui/handle/jspui/6280
Resumo: Carbon (C) and nitrogen (N) preservation in Amazonian forest soils is fundamental to the maintenance of its sustainability. The soils from this region being responsible for a C sequestration potential of 126 to 141 Tg year-1. Forest maintenance depends on nutrient cycling of litter that is deposited above soil and because of that, studying this region is important to understand the dynamic and stabilization of C and N in this environment. Stabilization of C in soils is governed by the following mechanisms: recalcitrance of organic material, physical and chemical protection. There are five factors responsible for C accumulation on soils: vegetation, climate, relief, origin material and time. The objective of this work was to evaluate the influence of the relief factor on carbon and nitrogen stocks in soils from Urucu, Central Amazonia. Soil samples (disturbed and undisturbed) were collected, identified and prepared in air dried soil. The soils physical and chemical attributes were determined. With results of C and N levels their stocks were calculated until 100 cm depth. To evaluate the mechanisms responsible for C stabilization on soils a physical fractioning by organic matter density to obtain the mass of the free light fraction (FLF) and intra-aggregate light fraction (IAFL) in ten soil profiles under different drainage and vegetation conditions. Carbon Stocks vary from27,4 to 230,3 Mg ha-1 and N stocks vary from 8,5 e 42,0 Mg ha-1. Distribution of C and N levels follows as represented in most soils with the exception of Espodossolos that represented a light increase in depth. The FLF contents found in well drained soils that are under the influence of Upland Dense Tropical Rainforest, varied from 58,5 g kg-1 of soil to 291,4 g kg-1 of soil and IALF varied from 58,5 g kg-1 of soil to 291,4 g kg-1 of soil. In soil profiles found in poorly drained situation under Upland Open Tropical Rainforest influence, in river plains it was noticed that contents from 40,8 g kg-1 of soil to 57,6 g kg-1 of soil and FLF and from 6,45 g kg-1 of soil to 16,8 g kg-1 of soil of IALF. In soils found in terraces under Upland Open Tropical Rainforest influence, the quantities found in FLF were from 113,2 g kg-1 of soil to 842,4 g kg-1 of soil and from IALF from 32,8 g kg-1 of soil to 72,2 g kg-1 of soil. The obtained correlation among clay variables, C, N, N stock, C stock, FLF and IALF demonstrates the role of clay in stabilization of C and N in soils. The organic matter light fractions (FLF and IALF) are also preserved in soils with higher clay levels. These fractions are considered the first C and N input in soils and preserving them is associated with higher C and N stocks in soils. The formation of organo-minerals complexes between clay fraction and organic matter, through chemical connection cation bridge, by the presence of aluminum ion, it is an important chemical protection mechanism in Urucu soils. The relief factor influences C and N levels and stocks by providing different drainage conditions that influences not only the kind of vegetation but also the soil organic matter decomposition.
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spelling Pinheiro, ?rika Fl?via Machado483.564.257-00http://lattes.cnpq.br/8101589624388403Pinheiro, ?rika Fl?via MachadoPereira, Marcos GervasioCampos, David Vilas Boas de128.465.287-48https://orcid.org/0000-0002-4577-6019http://lattes.cnpq.br/3859911618682214Ziviani, Melania Merlo2023-01-26T18:33:38Z2020-02-27ZIVIANI, Melania Merlo. Estoques e mecanismos de estabiliza??o de C e N em solos da Regi?o Central da Amaz?nia. 2020. 76 f. Disserta??o (Mestrado em Agronomia, Ci?ncia do Solo) - Instituto de Agronomia, Universidade Federal Rural do Rio de Janeiro, Serop?dica, RJ, 2020.https://tede.ufrrj.br/jspui/handle/jspui/6280Carbon (C) and nitrogen (N) preservation in Amazonian forest soils is fundamental to the maintenance of its sustainability. The soils from this region being responsible for a C sequestration potential of 126 to 141 Tg year-1. Forest maintenance depends on nutrient cycling of litter that is deposited above soil and because of that, studying this region is important to understand the dynamic and stabilization of C and N in this environment. Stabilization of C in soils is governed by the following mechanisms: recalcitrance of organic material, physical and chemical protection. There are five factors responsible for C accumulation on soils: vegetation, climate, relief, origin material and time. The objective of this work was to evaluate the influence of the relief factor on carbon and nitrogen stocks in soils from Urucu, Central Amazonia. Soil samples (disturbed and undisturbed) were collected, identified and prepared in air dried soil. The soils physical and chemical attributes were determined. With results of C and N levels their stocks were calculated until 100 cm depth. To evaluate the mechanisms responsible for C stabilization on soils a physical fractioning by organic matter density to obtain the mass of the free light fraction (FLF) and intra-aggregate light fraction (IAFL) in ten soil profiles under different drainage and vegetation conditions. Carbon Stocks vary from27,4 to 230,3 Mg ha-1 and N stocks vary from 8,5 e 42,0 Mg ha-1. Distribution of C and N levels follows as represented in most soils with the exception of Espodossolos that represented a light increase in depth. The FLF contents found in well drained soils that are under the influence of Upland Dense Tropical Rainforest, varied from 58,5 g kg-1 of soil to 291,4 g kg-1 of soil and IALF varied from 58,5 g kg-1 of soil to 291,4 g kg-1 of soil. In soil profiles found in poorly drained situation under Upland Open Tropical Rainforest influence, in river plains it was noticed that contents from 40,8 g kg-1 of soil to 57,6 g kg-1 of soil and FLF and from 6,45 g kg-1 of soil to 16,8 g kg-1 of soil of IALF. In soils found in terraces under Upland Open Tropical Rainforest influence, the quantities found in FLF were from 113,2 g kg-1 of soil to 842,4 g kg-1 of soil and from IALF from 32,8 g kg-1 of soil to 72,2 g kg-1 of soil. The obtained correlation among clay variables, C, N, N stock, C stock, FLF and IALF demonstrates the role of clay in stabilization of C and N in soils. The organic matter light fractions (FLF and IALF) are also preserved in soils with higher clay levels. These fractions are considered the first C and N input in soils and preserving them is associated with higher C and N stocks in soils. The formation of organo-minerals complexes between clay fraction and organic matter, through chemical connection cation bridge, by the presence of aluminum ion, it is an important chemical protection mechanism in Urucu soils. The relief factor influences C and N levels and stocks by providing different drainage conditions that influences not only the kind of vegetation but also the soil organic matter decomposition.A preserva??o do carbono (C) e nitrog?nio (N) nos solos da Floresta Amaz?nica ? fundamental para a manuten??o de sua sustentabilidade sendo os solos dessa regi?o respons?veis por um potencial de sequestro de C de 126 a 141 Tg ano-1. A manuten??o da floresta dependente da intensa ciclagem de nutrientes da serrapilheira que ? depositada sobre o solo e por isso, estudar essa regi?o ? importante para o entendimento da din?mica e estabiliza??o do C e N nesse ambiente. A estabiliza??o do C nos solos ? governada pelos mecanismos: recalcitr?ncia do material org?nico, prote??o f?sica e qu?mica. S?o cinco os fatores respons?veis pelo ac?mulo de C nos solos: vegeta??o, clima, relevo, material de origem e tempo. O objetivo do trabalho foi avaliar a influ?ncia do fator relevo nos estoques de carbono e nitrog?nio nos solos de Urucu, Amaz?nia Central, al?m de elucidar os principais mecanismos respons?veis pela estabiliza??o do C nesses solos. Entre os meses de setembro e novembro de 2018 foram abertas trincheiras e coletadas amostras de terra de 35 perfis de solo na solos em Urucu, Amaz?nia Central. As amostras de terra (deformadas e indeformadas) foram coletadas, identificadas e preparadas em terra fina seca ao ar. Foram determinados os atributos qu?micos e f?sicos dos solos. Com os resultados dos teores de C e N foram calculados os seus estoques at? 100 cm de profundidade. Para avaliar os mecanismos respons?veis pela estabiliza??o do C nos solos foi realizado o fracionamento f?sico por densidade da mat?ria org?nica para a obten??o da massa da fra??o leve livre (FLL) e da fra??o leve intra-agregado (FLI) em dez perfis de solo em diferentes condi??es de drenagem e vegeta??o. Os estoques de carbono variaram entre 27,4 a 230,3 Mg ha-1 e os estoques de N variaram entre 8,5 e 42,0 Mg ha-1. A distribui??o dos teores de C e N segue conforme apresentada para a maioria dos solos com exce??o dos Espodossolos que apresentaram um leve incremento em profundidade. Os conte?dos de FLL encontrados em solos bem drenados que est?o sobre influ?ncia de mata fechada, variaram entre 58,5 g kg-1 de solo a 291,4 g kg-1 de solo e a FLI variou entre 7,14 g kg-1 de solo a 38,7 g kg-1 solo. Nos perfis de solo que se encontravam em situa??o de m? drenagem sob influ?ncia de mata aberta, em plan?cies fluviais, notou-se conte?dos entre 40,8 g kg-1 de solo a 57,6 g kg-1 de solo de FLL e entre 6,45 g kg-1 de solo e 16,8 g kg-1 solo de FLI. Nos solos encontrados em terra?os, sob influ?ncia de mata aberta, as quantidades encontradas de FLL estavam entre 113,2 g kg-1 solo a 842,4 g kg-1 solo e de FLI entre 32,8 g kg-1 solo a 72,2 g kg-1 solo. A correla??o obtida entre as vari?veis argila, C, N, estoque de N, estoque de C, FLL e FLI demonstra o papel da argila na estabiliza??o de C e N nos solos. As fra??es leves da mat?ria org?nica (FLL e FLI) tamb?m s?o preservadas em solos com maiores teores de argila. Essas fra??es s?o consideradas o primeiro aporte de C e N nos solos e a preserva??o das mesmas est? associada a maiores estoques de C e N nesses solos. A forma??o de complexos organo-minerais entre a fra??o argila e a mat?ria org?nica, atrav?s da liga??o qu?mica ponte cati?nica, mediada pela presen?a do ?on alum?nio, comumente observado nos solos da regi?o, ? um mecanismo de prote??o qu?mica importante nos solos de Urucu. O fator relevo influencia os teores e estoques de C e N nos solos por proporcionar diferentes condi??es de drenagem que ir?o determinar n?o somente o tipo de vegeta??o, mas tamb?m as taxas de decomposi??o da mat?ria org?nica nos solos.Submitted by Jorge Silva (jorgelmsilva@ufrrj.br) on 2023-01-26T18:33:38Z No. of bitstreams: 1 2020 - Melania Merlo Ziviani.pdf: 1383939 bytes, checksum: 54fcfcac92774ef77eac21bbdc25fcc0 (MD5)Made available in DSpace on 2023-01-26T18:33:38Z (GMT). No. of bitstreams: 1 2020 - Melania Merlo Ziviani.pdf: 1383939 bytes, checksum: 54fcfcac92774ef77eac21bbdc25fcc0 (MD5) Previous issue date: 2020-02-27CAPES - Coordena??o de Aperfei?oamento de Pessoal de N?vel SuperiorCNPq - Conselho Nacional de Desenvolvimento Cient?fico e Tecnol?gicoFAPERJ - Funda??o Carlos Chagas Filho de Amparo ? Pesquisa do Estado do Rio de Janeiroapplication/pdfhttps://tede.ufrrj.br/retrieve/71976/2020%20-%20Melania%20Merlo%20Ziviani.pdf.jpgporUniversidade Federal Rural do Rio de JaneiroPrograma de P?s-Gradua??o em Agronomia - Ci?ncia do SoloUFRRJBrasilInstituto de AgronomiaADUAN, R. E.; VILELA, M. de F.; KLINK, C. A. Ciclagem de carbono em ecossistemas terrestres: o caso do Cerrado brasileiro. Planaltina, DF: Embrapa Cerrados, p. 30, 2003. AMORIM, T. X.; SENNA, M. C. A.; CATALDI, M. Impactos do desmatamento progressivo da Amaz?nia na precipita??o do Brasil. Revista Brasileira de Climatologia, v. 24, 2019. ARA?JO, M. do S. B.; SCHAEFER, C. A.; SAMPAIO, E. V. S. 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An?lises de solo, plantas e outros materiais. 2. ed. Porto Alegre: Universidade Federal do Rio Grande do Sul, 1995. TEIXEIRA, P. C.; DONAGEMMA, G. K.; FONTANA, A.; TEIXEIRA, W. G. Manual de m?todos de an?lise de solo ? 3. ed. rev. e ampl. ? Bras?lia, DF: Embrapa, 2017. TELLES, E. de C. C.; CAMARGO, P. B. de; MARTINELLI, L. A.; TRUMBORE, S. E.; COSTA, E. S. da; SANTOS, J.; HIGUCHI, N.; OLIVEIRA JR., R. C. Influence of soil texture on carbon dynamics and storage potential in tropical forest soils of Amazonia. Global Biogeochemical Cycles, v. 17, n. 2, article ID 1040, 2003. WALKLEY, A.; BLACK, I. A. An examination of the Degtjareff method for determining soil organic matter and a proposed modification of the chromic acid titration method. Soil Science,1934.Fracionamento f?sicoFra??o leve livreFra??o leve intra-agregadoPhysical FractioningFreeFraction. 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dc.title.por.fl_str_mv Estoques e mecanismos de estabiliza??o de C e N em solos da regi?o central da Amaz?nia
dc.title.alternative.eng.fl_str_mv Stocks and stabilization mechanisms of C and N in soils of central Amazon region
title Estoques e mecanismos de estabiliza??o de C e N em solos da regi?o central da Amaz?nia
spellingShingle Estoques e mecanismos de estabiliza??o de C e N em solos da regi?o central da Amaz?nia
Ziviani, Melania Merlo
Fracionamento f?sico
Fra??o leve livre
Fra??o leve intra-agregado
Physical Fractioning
Free
Fraction. Intra-aggregate
Light Fraction
Amazonian soils
Agronomia
title_short Estoques e mecanismos de estabiliza??o de C e N em solos da regi?o central da Amaz?nia
title_full Estoques e mecanismos de estabiliza??o de C e N em solos da regi?o central da Amaz?nia
title_fullStr Estoques e mecanismos de estabiliza??o de C e N em solos da regi?o central da Amaz?nia
title_full_unstemmed Estoques e mecanismos de estabiliza??o de C e N em solos da regi?o central da Amaz?nia
title_sort Estoques e mecanismos de estabiliza??o de C e N em solos da regi?o central da Amaz?nia
author Ziviani, Melania Merlo
author_facet Ziviani, Melania Merlo
author_role author
dc.contributor.advisor1.fl_str_mv Pinheiro, ?rika Fl?via Machado
dc.contributor.advisor1ID.fl_str_mv 483.564.257-00
dc.contributor.advisor1Lattes.fl_str_mv http://lattes.cnpq.br/8101589624388403
dc.contributor.referee1.fl_str_mv Pinheiro, ?rika Fl?via Machado
dc.contributor.referee2.fl_str_mv Pereira, Marcos Gervasio
dc.contributor.referee3.fl_str_mv Campos, David Vilas Boas de
dc.contributor.authorID.fl_str_mv 128.465.287-48
https://orcid.org/0000-0002-4577-6019
dc.contributor.authorLattes.fl_str_mv http://lattes.cnpq.br/3859911618682214
dc.contributor.author.fl_str_mv Ziviani, Melania Merlo
contributor_str_mv Pinheiro, ?rika Fl?via Machado
Pinheiro, ?rika Fl?via Machado
Pereira, Marcos Gervasio
Campos, David Vilas Boas de
dc.subject.por.fl_str_mv Fracionamento f?sico
Fra??o leve livre
Fra??o leve intra-agregado
Physical Fractioning
Free
Fraction. Intra-aggregate
Light Fraction
Amazonian soils
topic Fracionamento f?sico
Fra??o leve livre
Fra??o leve intra-agregado
Physical Fractioning
Free
Fraction. Intra-aggregate
Light Fraction
Amazonian soils
Agronomia
dc.subject.cnpq.fl_str_mv Agronomia
description Carbon (C) and nitrogen (N) preservation in Amazonian forest soils is fundamental to the maintenance of its sustainability. The soils from this region being responsible for a C sequestration potential of 126 to 141 Tg year-1. Forest maintenance depends on nutrient cycling of litter that is deposited above soil and because of that, studying this region is important to understand the dynamic and stabilization of C and N in this environment. Stabilization of C in soils is governed by the following mechanisms: recalcitrance of organic material, physical and chemical protection. There are five factors responsible for C accumulation on soils: vegetation, climate, relief, origin material and time. The objective of this work was to evaluate the influence of the relief factor on carbon and nitrogen stocks in soils from Urucu, Central Amazonia. Soil samples (disturbed and undisturbed) were collected, identified and prepared in air dried soil. The soils physical and chemical attributes were determined. With results of C and N levels their stocks were calculated until 100 cm depth. To evaluate the mechanisms responsible for C stabilization on soils a physical fractioning by organic matter density to obtain the mass of the free light fraction (FLF) and intra-aggregate light fraction (IAFL) in ten soil profiles under different drainage and vegetation conditions. Carbon Stocks vary from27,4 to 230,3 Mg ha-1 and N stocks vary from 8,5 e 42,0 Mg ha-1. Distribution of C and N levels follows as represented in most soils with the exception of Espodossolos that represented a light increase in depth. The FLF contents found in well drained soils that are under the influence of Upland Dense Tropical Rainforest, varied from 58,5 g kg-1 of soil to 291,4 g kg-1 of soil and IALF varied from 58,5 g kg-1 of soil to 291,4 g kg-1 of soil. In soil profiles found in poorly drained situation under Upland Open Tropical Rainforest influence, in river plains it was noticed that contents from 40,8 g kg-1 of soil to 57,6 g kg-1 of soil and FLF and from 6,45 g kg-1 of soil to 16,8 g kg-1 of soil of IALF. In soils found in terraces under Upland Open Tropical Rainforest influence, the quantities found in FLF were from 113,2 g kg-1 of soil to 842,4 g kg-1 of soil and from IALF from 32,8 g kg-1 of soil to 72,2 g kg-1 of soil. The obtained correlation among clay variables, C, N, N stock, C stock, FLF and IALF demonstrates the role of clay in stabilization of C and N in soils. The organic matter light fractions (FLF and IALF) are also preserved in soils with higher clay levels. These fractions are considered the first C and N input in soils and preserving them is associated with higher C and N stocks in soils. The formation of organo-minerals complexes between clay fraction and organic matter, through chemical connection cation bridge, by the presence of aluminum ion, it is an important chemical protection mechanism in Urucu soils. The relief factor influences C and N levels and stocks by providing different drainage conditions that influences not only the kind of vegetation but also the soil organic matter decomposition.
publishDate 2020
dc.date.issued.fl_str_mv 2020-02-27
dc.date.accessioned.fl_str_mv 2023-01-26T18:33:38Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/masterThesis
format masterThesis
status_str publishedVersion
dc.identifier.citation.fl_str_mv ZIVIANI, Melania Merlo. Estoques e mecanismos de estabiliza??o de C e N em solos da Regi?o Central da Amaz?nia. 2020. 76 f. Disserta??o (Mestrado em Agronomia, Ci?ncia do Solo) - Instituto de Agronomia, Universidade Federal Rural do Rio de Janeiro, Serop?dica, RJ, 2020.
dc.identifier.uri.fl_str_mv https://tede.ufrrj.br/jspui/handle/jspui/6280
identifier_str_mv ZIVIANI, Melania Merlo. Estoques e mecanismos de estabiliza??o de C e N em solos da Regi?o Central da Amaz?nia. 2020. 76 f. Disserta??o (Mestrado em Agronomia, Ci?ncia do Solo) - Instituto de Agronomia, Universidade Federal Rural do Rio de Janeiro, Serop?dica, RJ, 2020.
url https://tede.ufrrj.br/jspui/handle/jspui/6280
dc.language.iso.fl_str_mv por
language por
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