Gradiente vertical de decomposição e dinâmica da água no mulch de cana-de-açúcar afetados pela quantidade de palha

Detalhes bibliográficos
Ano de defesa: 2018
Autor(a) principal: Dietrich, Guilherme lattes
Orientador(a): Giacomini, Sandro José lattes
Banca de defesa: Zwirtes, Anderson Luiz lattes, Weiler, Douglas Adams lattes
Tipo de documento: Tese
Tipo de acesso: Acesso aberto
Idioma: por
Instituição de defesa: Universidade Federal de Santa Maria
Centro de Ciências Rurais
Programa de Pós-Graduação: Programa de Pós-Graduação em Ciência do Solo
Departamento: Agronomia
País: Brasil
Palavras-chave em Português:
Palavras-chave em Inglês:
Área do conhecimento CNPq:
Link de acesso: http://repositorio.ufsm.br/handle/1/16747
Resumo: The partial removal of sugarcane straw (Saccharum spp. L.) from the soil surface after mechanized harvesting for the production of cellulosic ethanol leaves different mulch thicknesses at the soil surface. Thus, the need arises to know the amount of straw to be harvested without harming the soil conservation. The objective of the present study was to understand how the thickness of the mulch, which varies according to the amount of straw, and the nitrogen fertilization (N) affect the water dynamics and the decomposition of the mulch and the layers that compose it, as the thickness of the mulch affects the water content and the soil temperature for one year. The contribution of equivalent amounts to 0, 4, 8 and 12 DM ha-1 of straw (S), on a dry basis, with and without N, was carried out inside screened frames and left on the soil surface after harvest, in Santa Maria, RS, under subtropical climate. Furthermore, the 8S and 12S treatments were divided into top (T) and lower (L) layers and T, medium (M) and L layer of straw, respectively, and stacked in order to reconstitute the amounts of straw. The 4S treatment was considered T and L. The layers were separated by a synthetic mesh of 10 mm and sampled separately. The main analyzes carried out on straw and mulch were: moisture, carbon and nitrogen remaining (CR and NR). For the soil, the temperature and the water content were evaluated using WCR probes (CS 616 model) and T-type copper-constantan thermocouple sensors, respectively. The results showed that the mulch and N thickness did not affect the decomposition and the release of N. The moisture of the mulch increased according to the initial amount of straw, but did not reflect the degradation of the mulch (67%, on average). The different amounts of straw did not differ in the rates of decomposition because there is a compensatory effect between the layers. The lower proportion of straw in contact with the soil was compensated by higher rates of decomposition of the lower layer. Among the mulch layers, the water content and decomposition rate differed according to the position (L> M> T). The top layers presented the same humidity and decomposition rate for the three treatments. On the other hand, the lower layers decomposed more rapidly under larger quantities of straw, which also reflected in moisture (12S L> 8S M> 4S L). The remaining N showed similar behavior to C. The mulch 8S and 12S presented higher average water content and lower average soil temperature compared to the 0S and 4S mulches. Finally, this work shows that the dynamics of mulch decomposition is governed mainly by the dynamics of the water, which in turn is affected by mulch thickness, vegetative canopy cover and local weather conditions.
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spelling 2019-06-05T12:17:25Z2019-06-05T12:17:25Z2018-07-30http://repositorio.ufsm.br/handle/1/16747The partial removal of sugarcane straw (Saccharum spp. L.) from the soil surface after mechanized harvesting for the production of cellulosic ethanol leaves different mulch thicknesses at the soil surface. Thus, the need arises to know the amount of straw to be harvested without harming the soil conservation. The objective of the present study was to understand how the thickness of the mulch, which varies according to the amount of straw, and the nitrogen fertilization (N) affect the water dynamics and the decomposition of the mulch and the layers that compose it, as the thickness of the mulch affects the water content and the soil temperature for one year. The contribution of equivalent amounts to 0, 4, 8 and 12 DM ha-1 of straw (S), on a dry basis, with and without N, was carried out inside screened frames and left on the soil surface after harvest, in Santa Maria, RS, under subtropical climate. Furthermore, the 8S and 12S treatments were divided into top (T) and lower (L) layers and T, medium (M) and L layer of straw, respectively, and stacked in order to reconstitute the amounts of straw. The 4S treatment was considered T and L. The layers were separated by a synthetic mesh of 10 mm and sampled separately. The main analyzes carried out on straw and mulch were: moisture, carbon and nitrogen remaining (CR and NR). For the soil, the temperature and the water content were evaluated using WCR probes (CS 616 model) and T-type copper-constantan thermocouple sensors, respectively. The results showed that the mulch and N thickness did not affect the decomposition and the release of N. The moisture of the mulch increased according to the initial amount of straw, but did not reflect the degradation of the mulch (67%, on average). The different amounts of straw did not differ in the rates of decomposition because there is a compensatory effect between the layers. The lower proportion of straw in contact with the soil was compensated by higher rates of decomposition of the lower layer. Among the mulch layers, the water content and decomposition rate differed according to the position (L> M> T). The top layers presented the same humidity and decomposition rate for the three treatments. On the other hand, the lower layers decomposed more rapidly under larger quantities of straw, which also reflected in moisture (12S L> 8S M> 4S L). The remaining N showed similar behavior to C. The mulch 8S and 12S presented higher average water content and lower average soil temperature compared to the 0S and 4S mulches. Finally, this work shows that the dynamics of mulch decomposition is governed mainly by the dynamics of the water, which in turn is affected by mulch thickness, vegetative canopy cover and local weather conditions.A remoção parcial da palha de cana-de-açúcar (Saccharum spp. L.) da superfície do solo após a colheita mecanizada para a produção de etanol celulósico deixa diferentes espessuras de mulch na superfície do solo. Assim, surge a necessidade de conhecer a quantidade de palha a ser recolhida sem prejudicar a conservação do solo. O objetivo do presente estudo foi compreender como a espessura do mulch, que varia de acordo com a quantidade de palha, e a adubação nitrogenada (N) afetam a dinâmica da água e a decomposição do mulch e das camadas que o compõem, bem como, como a espessura do mulch afeta o conteúdo de água e a temperatura do solo durante um ano. O aporte de quantidades equivalentes a 0, 4, 8 e 12 Mg ha-1 de palha (P), em base seca, com e sem N, foi realizado no interior de quadros telados e deixados na superfície do solo após a colheita, em Santa Maria, RS, sob clima subtropical. Ainda, os tratamentos 8P e 12P foram divididos em camada superior (S) e inferior (I) e camada S, central (C) e I de palha, respectivamente, e empilhados de modo a reconstituir as quantidades de palha. O tratamento 4P foi considerado S e I. As camadas foram separadas por uma malha sintética de 10 mm e amostradas separadamente. As principais análises realizadas nas camadas da palha e no mulch foram: umidade, carbono e nitrogênio remanescentes (CR e NR). Para o solo, a temperatura e o conteúdo de água foram avaliados através de sondas WCR (modelo CS 616) e sensores termopares cobre-constantan do tipo T, respectivamente. Os resultados mostraram que a espessura do mulch e o N não afetaram a decomposição e a liberação de N. A umidade do mulch aumentou conforme a quantidade inicial de palha, porém, não refletiu na degradação do mulch (67%, em média). As diferentes quantidades de palha não diferiram quanto às taxas de decomposição porque existe um efeito compensatório entre as camadas. A menor proporção de palha em contato com o solo foi compensada por maiores taxas de decomposição da camada inferior. Entre as camadas do mulch, o conteúdo de água e a taxa de decomposição diferiram de acordo com a posição (I > C > S). As camadas superiores apresentaram a mesma umidade e taxa de decomposição para os três tratamentos. Por outro lado, as camadas inferiores decompuseram mais rapidamente sob maiores quantidades de palha, o que também reflete na umidade (12P I > 8P I > 4P I). O N remanescente apresentou comportamento semelhante ao C. Os mulches 8P e 12P apresentaram maior conteúdo médio de água e menor temperatura média do solo em comparação aos mulches 0P e 4P. Por fim, este trabalho mostra que a dinâmica da decomposição do mulch é governada principalmente pela dinâmica da água, que por sua vez, é afetada pela espessura do mulch, pela cobertura do dossel vegetativo e pelas condições meteorológicas do local.Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPESporUniversidade Federal de Santa MariaCentro de Ciências RuraisPrograma de Pós-Graduação em Ciência do SoloUFSMBrasilAgronomiaAttribution-NonCommercial-NoDerivatives 4.0 Internationalhttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccessCarbonoNitrogênioEspessura do mulchColheita mecanizadaCarbonNitrogenMulch thicknessMechanized harvestCNPQ::CIENCIAS AGRARIAS::AGRONOMIAGradiente vertical de decomposição e dinâmica da água no mulch de cana-de-açúcar afetados pela quantidade de palhaVertical gradient of decomposition and dynamics of water in mulch of sugarcane affected by the quantity of strawinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/doctoralThesisGiacomini, Sandro Joséhttp://lattes.cnpq.br/1112466940331009Zwirtes, Anderson Luizhttp://lattes.cnpq.br/7105268741658406Weiler, Douglas Adamshttp://lattes.cnpq.br/2355481072308613http://lattes.cnpq.br/7394137855504607Dietrich, Guilherme500100000009600419b5a2f-20df-408a-a156-d652293f4a7385b14f98-cce4-4ce8-8c2d-85156626a8727d38eae9-903e-4cfc-acad-bb291e1a6b1e6ba36ed2-a6a6-4681-900d-84d23f85917ereponame:Biblioteca Digital de Teses e Dissertações do UFSMinstname:Universidade Federal de Santa Maria (UFSM)instacron:UFSMORIGINALTES_PPGCS_2019_DIETRICH_GUILHERME.pdfTES_PPGCS_2019_DIETRICH_GUILHERME.pdfTese de Doutoradoapplication/pdf2368560http://repositorio.ufsm.br/bitstream/1/16747/1/TES_PPGCS_2019_DIETRICH_GUILHERME.pdff7ff7a34793f36e917bfafa2d3d518a2MD51CC-LICENSElicense_rdflicense_rdfapplication/rdf+xml; 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dc.title.por.fl_str_mv Gradiente vertical de decomposição e dinâmica da água no mulch de cana-de-açúcar afetados pela quantidade de palha
dc.title.alternative.eng.fl_str_mv Vertical gradient of decomposition and dynamics of water in mulch of sugarcane affected by the quantity of straw
title Gradiente vertical de decomposição e dinâmica da água no mulch de cana-de-açúcar afetados pela quantidade de palha
spellingShingle Gradiente vertical de decomposição e dinâmica da água no mulch de cana-de-açúcar afetados pela quantidade de palha
Dietrich, Guilherme
Carbono
Nitrogênio
Espessura do mulch
Colheita mecanizada
Carbon
Nitrogen
Mulch thickness
Mechanized harvest
CNPQ::CIENCIAS AGRARIAS::AGRONOMIA
title_short Gradiente vertical de decomposição e dinâmica da água no mulch de cana-de-açúcar afetados pela quantidade de palha
title_full Gradiente vertical de decomposição e dinâmica da água no mulch de cana-de-açúcar afetados pela quantidade de palha
title_fullStr Gradiente vertical de decomposição e dinâmica da água no mulch de cana-de-açúcar afetados pela quantidade de palha
title_full_unstemmed Gradiente vertical de decomposição e dinâmica da água no mulch de cana-de-açúcar afetados pela quantidade de palha
title_sort Gradiente vertical de decomposição e dinâmica da água no mulch de cana-de-açúcar afetados pela quantidade de palha
author Dietrich, Guilherme
author_facet Dietrich, Guilherme
author_role author
dc.contributor.advisor1.fl_str_mv Giacomini, Sandro José
dc.contributor.advisor1Lattes.fl_str_mv http://lattes.cnpq.br/1112466940331009
dc.contributor.referee1.fl_str_mv Zwirtes, Anderson Luiz
dc.contributor.referee1Lattes.fl_str_mv http://lattes.cnpq.br/7105268741658406
dc.contributor.referee2.fl_str_mv Weiler, Douglas Adams
dc.contributor.referee2Lattes.fl_str_mv http://lattes.cnpq.br/2355481072308613
dc.contributor.authorLattes.fl_str_mv http://lattes.cnpq.br/7394137855504607
dc.contributor.author.fl_str_mv Dietrich, Guilherme
contributor_str_mv Giacomini, Sandro José
Zwirtes, Anderson Luiz
Weiler, Douglas Adams
dc.subject.por.fl_str_mv Carbono
Nitrogênio
Espessura do mulch
Colheita mecanizada
topic Carbono
Nitrogênio
Espessura do mulch
Colheita mecanizada
Carbon
Nitrogen
Mulch thickness
Mechanized harvest
CNPQ::CIENCIAS AGRARIAS::AGRONOMIA
dc.subject.eng.fl_str_mv Carbon
Nitrogen
Mulch thickness
Mechanized harvest
dc.subject.cnpq.fl_str_mv CNPQ::CIENCIAS AGRARIAS::AGRONOMIA
description The partial removal of sugarcane straw (Saccharum spp. L.) from the soil surface after mechanized harvesting for the production of cellulosic ethanol leaves different mulch thicknesses at the soil surface. Thus, the need arises to know the amount of straw to be harvested without harming the soil conservation. The objective of the present study was to understand how the thickness of the mulch, which varies according to the amount of straw, and the nitrogen fertilization (N) affect the water dynamics and the decomposition of the mulch and the layers that compose it, as the thickness of the mulch affects the water content and the soil temperature for one year. The contribution of equivalent amounts to 0, 4, 8 and 12 DM ha-1 of straw (S), on a dry basis, with and without N, was carried out inside screened frames and left on the soil surface after harvest, in Santa Maria, RS, under subtropical climate. Furthermore, the 8S and 12S treatments were divided into top (T) and lower (L) layers and T, medium (M) and L layer of straw, respectively, and stacked in order to reconstitute the amounts of straw. The 4S treatment was considered T and L. The layers were separated by a synthetic mesh of 10 mm and sampled separately. The main analyzes carried out on straw and mulch were: moisture, carbon and nitrogen remaining (CR and NR). For the soil, the temperature and the water content were evaluated using WCR probes (CS 616 model) and T-type copper-constantan thermocouple sensors, respectively. The results showed that the mulch and N thickness did not affect the decomposition and the release of N. The moisture of the mulch increased according to the initial amount of straw, but did not reflect the degradation of the mulch (67%, on average). The different amounts of straw did not differ in the rates of decomposition because there is a compensatory effect between the layers. The lower proportion of straw in contact with the soil was compensated by higher rates of decomposition of the lower layer. Among the mulch layers, the water content and decomposition rate differed according to the position (L> M> T). The top layers presented the same humidity and decomposition rate for the three treatments. On the other hand, the lower layers decomposed more rapidly under larger quantities of straw, which also reflected in moisture (12S L> 8S M> 4S L). The remaining N showed similar behavior to C. The mulch 8S and 12S presented higher average water content and lower average soil temperature compared to the 0S and 4S mulches. Finally, this work shows that the dynamics of mulch decomposition is governed mainly by the dynamics of the water, which in turn is affected by mulch thickness, vegetative canopy cover and local weather conditions.
publishDate 2018
dc.date.issued.fl_str_mv 2018-07-30
dc.date.accessioned.fl_str_mv 2019-06-05T12:17:25Z
dc.date.available.fl_str_mv 2019-06-05T12:17:25Z
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rights_invalid_str_mv Attribution-NonCommercial-NoDerivatives 4.0 International
http://creativecommons.org/licenses/by-nc-nd/4.0/
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dc.publisher.none.fl_str_mv Universidade Federal de Santa Maria
Centro de Ciências Rurais
dc.publisher.program.fl_str_mv Programa de Pós-Graduação em Ciência do Solo
dc.publisher.initials.fl_str_mv UFSM
dc.publisher.country.fl_str_mv Brasil
dc.publisher.department.fl_str_mv Agronomia
publisher.none.fl_str_mv Universidade Federal de Santa Maria
Centro de Ciências Rurais
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