Produtividade de Eucalyptus saligna com base nas propriedades físico-hídricas do solo e parametrização do modelo ecofisiológico 3-PG

Detalhes bibliográficos
Autor(a) principal: Cavalli, Jean Pierre
Data de Publicação: 2017
Tipo de documento: Tese
Idioma: por
Título da fonte: Manancial - Repositório Digital da UFSM
Texto Completo: http://repositorio.ufsm.br/handle/1/13332
Resumo: This study was developed in Serra do Sudeste and Encosta do Sudeste physiographic regions of Rio Grande do Sul state. The objective was to identify the physical and hydraulic soil properties related to forest yield sites in two distinct areas, including physical-structural properties and soil available water capacity (AW) of Argissolo Vermelho-Amarelo Distrófico típico, Argissolo Vermelho-Amarelo Distrófico latossólico (ARG) and Neossolo Quartzarênico Órtico típico (NEO), as well as perform parameterization of the Physiological Principles to Predicting Growth model (3-PG). In the two sites with high (ARG) and low (NEO) productive potential capacity, the growth and productivity of stands characterization was based on data from forest inventories and from destructive sampling and cube by Smalian method of 30 trees of medium quadratic mean diameter (dg). Soil properties were determined in undisturbed and disturbed soil samples, taken from 0.00-0.10, 0.10-0.20, 0.20-0.40, 0.40-0.60, 0.60-0.80, 0.80-1.00 e 1.00-1.20 m soil depths, in 12 sampling points. Eucalyptus yield was different in the ARG (from clay loam to clay texture) and NEO (sandy texture) areas, characterized by mean values of 373.9 m³ ha-1 and 272.3 m³ ha-1, for 89-months-old stands. In the ARG, AW ranged from 0.100 up to 0.304 cm3 cm-3. The highest soil bulk density (BD; 1.64 Mg m-3) was observed in the 0.00-0.10 and 0.10-0.20 m soil layers. Multiple regression analysis with BD and macroporosity (Mac) of the 0.40-0.60 m soil layer had r2 ~ 0.22 in variance estimation of mean annual volume increment (MAIV). Soil air permeability (Kar) was the main soil property related to productivity in ARG stands. In the NEO (sandy texture) areas, AW ranged from 0.025 up to 0.04 cm3 cm-3 and BD had the highest values (1.60 Mg m-3) in the 0.80-1.00 m soil layer. The BD determined from surface up to 0.60 m explained 14% of MAIV variance and 27% of the total height variance (h). Multiple regression that included BD and Kar of the surface layers explained around 23% of mean annual stem biomass increment (MAISB) variance. In the parameterization of the model 3-PG we obtained estimates characterized by r2 higher than 0.9 for the wood volume with bark (V; m3 ha-1), wood biomass (BL; Mg ha-3) and total height (h), and equal to 0.78 for the diameter at breast high (dbh; cm). The statistical efficiency described by the Nash-Sutcliffe indicator had values higher than 0.8, while the PBIAS indicator showed a tendency of underestimation of less than 12%. In the validation process of the model, performed in unused portions in the parameterization, the results were similar to those obtained in the efficiency evaluation, except for the variable dbh, which was underestimated at the lowest ages. The results showed that the soils with high water availability have their physical quality, based on productivity, determined by the properties that represent the flow of solutes and gases, while coarse soils, highly drainable, have their productive capacity inversely related to BD. The 3-PG model was efficient and accurate for the estimation of E. saligna productivity in the observed climatic conditions, with a higher sensitivity for coarse textured soils.
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spelling 2018-06-08T19:37:36Z2018-06-08T19:37:36Z2017-02-23http://repositorio.ufsm.br/handle/1/13332This study was developed in Serra do Sudeste and Encosta do Sudeste physiographic regions of Rio Grande do Sul state. The objective was to identify the physical and hydraulic soil properties related to forest yield sites in two distinct areas, including physical-structural properties and soil available water capacity (AW) of Argissolo Vermelho-Amarelo Distrófico típico, Argissolo Vermelho-Amarelo Distrófico latossólico (ARG) and Neossolo Quartzarênico Órtico típico (NEO), as well as perform parameterization of the Physiological Principles to Predicting Growth model (3-PG). In the two sites with high (ARG) and low (NEO) productive potential capacity, the growth and productivity of stands characterization was based on data from forest inventories and from destructive sampling and cube by Smalian method of 30 trees of medium quadratic mean diameter (dg). Soil properties were determined in undisturbed and disturbed soil samples, taken from 0.00-0.10, 0.10-0.20, 0.20-0.40, 0.40-0.60, 0.60-0.80, 0.80-1.00 e 1.00-1.20 m soil depths, in 12 sampling points. Eucalyptus yield was different in the ARG (from clay loam to clay texture) and NEO (sandy texture) areas, characterized by mean values of 373.9 m³ ha-1 and 272.3 m³ ha-1, for 89-months-old stands. In the ARG, AW ranged from 0.100 up to 0.304 cm3 cm-3. The highest soil bulk density (BD; 1.64 Mg m-3) was observed in the 0.00-0.10 and 0.10-0.20 m soil layers. Multiple regression analysis with BD and macroporosity (Mac) of the 0.40-0.60 m soil layer had r2 ~ 0.22 in variance estimation of mean annual volume increment (MAIV). Soil air permeability (Kar) was the main soil property related to productivity in ARG stands. In the NEO (sandy texture) areas, AW ranged from 0.025 up to 0.04 cm3 cm-3 and BD had the highest values (1.60 Mg m-3) in the 0.80-1.00 m soil layer. The BD determined from surface up to 0.60 m explained 14% of MAIV variance and 27% of the total height variance (h). Multiple regression that included BD and Kar of the surface layers explained around 23% of mean annual stem biomass increment (MAISB) variance. In the parameterization of the model 3-PG we obtained estimates characterized by r2 higher than 0.9 for the wood volume with bark (V; m3 ha-1), wood biomass (BL; Mg ha-3) and total height (h), and equal to 0.78 for the diameter at breast high (dbh; cm). The statistical efficiency described by the Nash-Sutcliffe indicator had values higher than 0.8, while the PBIAS indicator showed a tendency of underestimation of less than 12%. In the validation process of the model, performed in unused portions in the parameterization, the results were similar to those obtained in the efficiency evaluation, except for the variable dbh, which was underestimated at the lowest ages. The results showed that the soils with high water availability have their physical quality, based on productivity, determined by the properties that represent the flow of solutes and gases, while coarse soils, highly drainable, have their productive capacity inversely related to BD. The 3-PG model was efficient and accurate for the estimation of E. saligna productivity in the observed climatic conditions, with a higher sensitivity for coarse textured soils.O presente estudo foi realizado nas regiões fisiográficas da Serra do Sudeste e Encosta do Sudeste do estado do Rio Grande do Sul. O objetivo do estudo foi identificar as propriedades físico-hídricas dos solos relacionadas à produtividade dos sítios florestais, distintos quanto às propriedades físico-estruturais e à água disponível (AD), caracterizados pela presença de Argissolo Vermelho-Amarelo Distrófico típico e Argissolo Vermelho-Amarelo Distrófico latossólico (ARG) e de Neossolo Quartzarênico Órticos típicos (NEO), e ainda, realizar a parametrização do modelo Physiological Principles to Predicted Growth (3-PG). A caracterização do crescimento e produtividade dos povoamentos foi realizada por meio de inventários florestais e pela amostragem destrutiva e cubagem, pelo método de Smalian, de 30 árvores de diâmetro médio quadrático (dg). As propriedades físico-hídricas dos solos foram determinadas em amostras de solos de estrutura preservada e alterada, coletadas nas camadas de 0,00-0,10, 0,10-0,20, 0,20-0,40, 0,40-0,60, 0,60-0,80, 0,80-1,00 e 1,00-1,20 m, em 12 pontos amostrais. A produtividade foi distinta nas áreas ARG e NEO, com média de 373,9 m³ ha-1 e 272,3 m3 ha-1, aos 89 meses de idade. Nos solos ARG (classe textural franco arenosa a muito argilosa), a AD variou entre 0,100 e 0,304 m3 m-3, e os maiores valores de densidade do solo (Ds; 1,64 Mg m-3) foram observados nas camadas 0,00-0,10 e 0,10-0,20 m. Pela análise de regressão múltipla a Ds e a macroporosidade (Mac) da camada 0,40-0,60 m tiveram eficiência estatística com r2 ~ 0,22 na estimativa da variância do incremento médio anual em volume (IMAV). A permeabilidade do solo ao ar (Kar) foi a principal propriedade do solo relacionada à produtividade dos povoamentos das áreas ARG. Nas áreas NEO (classe textural areia) a AD variou entre 0,025 e 0,04 m3 m-3 e a maior Ds foi observada na camada 0,80-1,00 m (1,60 Mg m-3). A Ds determinada nas camadas acima de 0,60 m de profundidade explicou 14% da variância observada no IMAV e 27% da variância da altura total (h). Pela regressão múltipla a Ds e a Kar das camadas superficiais explicaram em torno de 23% da variância observada no incremento médio anual em biomassa de lenho (IMABL). Na parametrização do modelo 3-PG foram obtidas estimativas caracterizadas por r2 superior a 0,9 para o volume com casca (V; m3 ha-1), biomassa de lenho (BL; Mg ha-3) e altura total (h; m), e igual a 0,78 para o dap (cm). O indicador estatístico Nash-Sutcliffe teve valores superiores a 0,8, enquanto o indicador Bias percentual (PBIAS) apontou tendência de subestimativa inferior a 12%. No processo de validação do modelo, realizado em parcelas não utilizadas na parametrização, os resultados foram semelhantes aos obtidos na avaliação da eficiência, com exceção para a variável dap, que foi subestimada nas menores idades. Solos com alta disponibilidade de água podem ter sua qualidade física, com base na produtividade, determinada pelas propriedades que representam o fluxo de solutos e gases, enquanto solos de textura grossa, altamente drenáveis, têm sua capacidade produtiva inversamente relacionada a Ds. O modelo 3-PG foi eficiente e preciso para a estimativa da produtividade do E. saligna nas condições climáticas observadas, com maior sensibilidade para os solos de textura grossa.Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPESporUniversidade Federal de Santa MariaCentro de Ciências RuraisPrograma de Pós-Graduação em Engenharia FlorestalUFSMBrasilRecursos Florestais e Engenharia FlorestalAttribution-NonCommercial-NoDerivatives 4.0 Internationalhttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccessQualidade do sítioPotencial produtivoPermeabilidade do solo ao arSite qualityProductive potentialAir permeabilityCNPQ::CIENCIAS AGRARIAS::RECURSOS FLORESTAIS E ENGENHARIA FLORESTALProdutividade de Eucalyptus saligna com base nas propriedades físico-hídricas do solo e parametrização do modelo ecofisiológico 3-PGEucalyptus saligna yield based on physic-hydric soil properties and ecofisiologycal model 3-PG parameterizationinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/doctoralThesisReichert, José Miguelhttp://lattes.cnpq.br/0910765178697312Floriano, Eduardo Pagelhttp://lattes.cnpq.br/6269603006987547Marangon, Gabriel Paeshttp://lattes.cnpq.br/0522565365617852Suzuki, Luis Eduardo Akiyoshi Sancheshttp://lattes.cnpq.br/8976157511758125Lovato, Thoméhttp://lattes.cnpq.br/2837098281000604http://lattes.cnpq.br/1355762804464344Cavalli, Jean Pierre500200000003600a85444db-3c89-4606-bf03-0e1915842baa866e0665-8897-470e-bdcd-1999996f410a7acdc93b-e594-434b-9733-ddc89f88d34c0e6d98e5-8721-4115-82c2-8c745bb4825dc40a9c5f-fdc2-4aa7-be88-f24d21ade78cfe1bc639-2860-447f-be69-22a3c4d3cfcareponame:Manancial - Repositório Digital da UFSMinstname:Universidade Federal de Santa Maria (UFSM)instacron:UFSMORIGINALTES_PPGEF_2017_CAVALLI_JEAN.pdfTES_PPGEF_2017_CAVALLI_JEAN.pdfTese de Doutoradoapplication/pdf4547780http://repositorio.ufsm.br/bitstream/1/13332/1/TES_PPGEF_2017_CAVALLI_JEAN.pdf98aea17ea60eb099205728eec94f1dd3MD51LICENSElicense.txtlicense.txttext/plain; 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dc.title.por.fl_str_mv Produtividade de Eucalyptus saligna com base nas propriedades físico-hídricas do solo e parametrização do modelo ecofisiológico 3-PG
dc.title.alternative.eng.fl_str_mv Eucalyptus saligna yield based on physic-hydric soil properties and ecofisiologycal model 3-PG parameterization
title Produtividade de Eucalyptus saligna com base nas propriedades físico-hídricas do solo e parametrização do modelo ecofisiológico 3-PG
spellingShingle Produtividade de Eucalyptus saligna com base nas propriedades físico-hídricas do solo e parametrização do modelo ecofisiológico 3-PG
Cavalli, Jean Pierre
Qualidade do sítio
Potencial produtivo
Permeabilidade do solo ao ar
Site quality
Productive potential
Air permeability
CNPQ::CIENCIAS AGRARIAS::RECURSOS FLORESTAIS E ENGENHARIA FLORESTAL
title_short Produtividade de Eucalyptus saligna com base nas propriedades físico-hídricas do solo e parametrização do modelo ecofisiológico 3-PG
title_full Produtividade de Eucalyptus saligna com base nas propriedades físico-hídricas do solo e parametrização do modelo ecofisiológico 3-PG
title_fullStr Produtividade de Eucalyptus saligna com base nas propriedades físico-hídricas do solo e parametrização do modelo ecofisiológico 3-PG
title_full_unstemmed Produtividade de Eucalyptus saligna com base nas propriedades físico-hídricas do solo e parametrização do modelo ecofisiológico 3-PG
title_sort Produtividade de Eucalyptus saligna com base nas propriedades físico-hídricas do solo e parametrização do modelo ecofisiológico 3-PG
author Cavalli, Jean Pierre
author_facet Cavalli, Jean Pierre
author_role author
dc.contributor.advisor1.fl_str_mv Reichert, José Miguel
dc.contributor.advisor1Lattes.fl_str_mv http://lattes.cnpq.br/0910765178697312
dc.contributor.referee1.fl_str_mv Floriano, Eduardo Pagel
dc.contributor.referee1Lattes.fl_str_mv http://lattes.cnpq.br/6269603006987547
dc.contributor.referee2.fl_str_mv Marangon, Gabriel Paes
dc.contributor.referee2Lattes.fl_str_mv http://lattes.cnpq.br/0522565365617852
dc.contributor.referee3.fl_str_mv Suzuki, Luis Eduardo Akiyoshi Sanches
dc.contributor.referee3Lattes.fl_str_mv http://lattes.cnpq.br/8976157511758125
dc.contributor.referee4.fl_str_mv Lovato, Thomé
dc.contributor.referee4Lattes.fl_str_mv http://lattes.cnpq.br/2837098281000604
dc.contributor.authorLattes.fl_str_mv http://lattes.cnpq.br/1355762804464344
dc.contributor.author.fl_str_mv Cavalli, Jean Pierre
contributor_str_mv Reichert, José Miguel
Floriano, Eduardo Pagel
Marangon, Gabriel Paes
Suzuki, Luis Eduardo Akiyoshi Sanches
Lovato, Thomé
dc.subject.por.fl_str_mv Qualidade do sítio
Potencial produtivo
Permeabilidade do solo ao ar
topic Qualidade do sítio
Potencial produtivo
Permeabilidade do solo ao ar
Site quality
Productive potential
Air permeability
CNPQ::CIENCIAS AGRARIAS::RECURSOS FLORESTAIS E ENGENHARIA FLORESTAL
dc.subject.eng.fl_str_mv Site quality
Productive potential
Air permeability
dc.subject.cnpq.fl_str_mv CNPQ::CIENCIAS AGRARIAS::RECURSOS FLORESTAIS E ENGENHARIA FLORESTAL
description This study was developed in Serra do Sudeste and Encosta do Sudeste physiographic regions of Rio Grande do Sul state. The objective was to identify the physical and hydraulic soil properties related to forest yield sites in two distinct areas, including physical-structural properties and soil available water capacity (AW) of Argissolo Vermelho-Amarelo Distrófico típico, Argissolo Vermelho-Amarelo Distrófico latossólico (ARG) and Neossolo Quartzarênico Órtico típico (NEO), as well as perform parameterization of the Physiological Principles to Predicting Growth model (3-PG). In the two sites with high (ARG) and low (NEO) productive potential capacity, the growth and productivity of stands characterization was based on data from forest inventories and from destructive sampling and cube by Smalian method of 30 trees of medium quadratic mean diameter (dg). Soil properties were determined in undisturbed and disturbed soil samples, taken from 0.00-0.10, 0.10-0.20, 0.20-0.40, 0.40-0.60, 0.60-0.80, 0.80-1.00 e 1.00-1.20 m soil depths, in 12 sampling points. Eucalyptus yield was different in the ARG (from clay loam to clay texture) and NEO (sandy texture) areas, characterized by mean values of 373.9 m³ ha-1 and 272.3 m³ ha-1, for 89-months-old stands. In the ARG, AW ranged from 0.100 up to 0.304 cm3 cm-3. The highest soil bulk density (BD; 1.64 Mg m-3) was observed in the 0.00-0.10 and 0.10-0.20 m soil layers. Multiple regression analysis with BD and macroporosity (Mac) of the 0.40-0.60 m soil layer had r2 ~ 0.22 in variance estimation of mean annual volume increment (MAIV). Soil air permeability (Kar) was the main soil property related to productivity in ARG stands. In the NEO (sandy texture) areas, AW ranged from 0.025 up to 0.04 cm3 cm-3 and BD had the highest values (1.60 Mg m-3) in the 0.80-1.00 m soil layer. The BD determined from surface up to 0.60 m explained 14% of MAIV variance and 27% of the total height variance (h). Multiple regression that included BD and Kar of the surface layers explained around 23% of mean annual stem biomass increment (MAISB) variance. In the parameterization of the model 3-PG we obtained estimates characterized by r2 higher than 0.9 for the wood volume with bark (V; m3 ha-1), wood biomass (BL; Mg ha-3) and total height (h), and equal to 0.78 for the diameter at breast high (dbh; cm). The statistical efficiency described by the Nash-Sutcliffe indicator had values higher than 0.8, while the PBIAS indicator showed a tendency of underestimation of less than 12%. In the validation process of the model, performed in unused portions in the parameterization, the results were similar to those obtained in the efficiency evaluation, except for the variable dbh, which was underestimated at the lowest ages. The results showed that the soils with high water availability have their physical quality, based on productivity, determined by the properties that represent the flow of solutes and gases, while coarse soils, highly drainable, have their productive capacity inversely related to BD. The 3-PG model was efficient and accurate for the estimation of E. saligna productivity in the observed climatic conditions, with a higher sensitivity for coarse textured soils.
publishDate 2017
dc.date.issued.fl_str_mv 2017-02-23
dc.date.accessioned.fl_str_mv 2018-06-08T19:37:36Z
dc.date.available.fl_str_mv 2018-06-08T19:37:36Z
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