Interceptação da chuva em diferentes formações florestais na região de Santa Maria - RS.
Autor(a) principal: | |
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Data de Publicação: | 2011 |
Tipo de documento: | Dissertação |
Idioma: | por |
Título da fonte: | Biblioteca Digital de Teses e Dissertações do UFSM |
Texto Completo: | http://repositorio.ufsm.br/handle/1/7766 |
Resumo: | ABSTRACT: In regions of natural or planted forests, rainfall interception by vegetation can be an important variable in the hydrological cycle and should not be neglected. This research analyzes the process of interception in different forest types (native and planted) in the region of Santa Maria - RS, at the head of Vacacaí Mirim. The variables Rainfall (R), stemflow (Sf), and throughfall (Tf) were monitored in the period from Dec/09 to Fev/11. Rainfall was monitored in two tipping bucket rain gauges and meteorological station installed in the subbasin on July 14th, 2010. Throughfall was monitored in three plots (areas I, II and III) with dimensions of 12 m x 50 m, 21 m x 12 m and 10 m x 20 m, respectively. The sampling points were installed 40 or 60 cm from the ground and spaced 1 m in straight line. In area I (native forest), 101 stakes were allocated to 40 instruments; where 20 collectors remained in fixed locations and 20 were rotated randomly. In the areas II (native forest) and III (eucalyptus) 60 sampling points were allocated to 20 collectors; at each new collection they were placed one sampling point ahead the former. Stemflow was based on values suggested in literature and by monitoring the flow in three selected trees within each plot, and the interception was calculated as the difference between precipitation and the sum of throughfall and stemflow. The results showed that interception is a key component of the hydrological cycle and, in general, underestimated by the hydrological models.The highest interception value was checked for native forest and the largest stemflow for eucalyptus. The stemflow was higher than the values observed by other authors, revealing that this variable cannot be ruled out in the study of interception. On the other hand, the ranges of variation of throughfall and interception were close to those reported in other studies. The results seem also to suggest that the depth parameter adopted for the calculation of interception using the leaf area index is underestimated and should be 0.4. Statistical analysis of the number of collectors used and necessary to ensure error of 5 mm of throughfall in relation to its average and 90% of confidence, showed that for vegetation such as Eucalyptus, the use of 20 rotating collectors were sufficient in 95.45% of the collections; which may be a reference to works in which there is a pattern of similarity of species. For native forest we observed that when the vegetation has a low density and the similar pattern of canopy, stem diameter and height, the use of 20 rotating collectors would be enough to ensure statistical requirements set out in 71.43% of the samples monitored. When the native vegetation is dense, with standard range of height, stem diameter and crown area, we observed the need for a higher number of collectors equipment of throughfall. The use of 40 collectors (20 fixed and 20 rotational) assured that the statistical requirements stipulated were guaranteed in 60.98% of the samples monitored. |
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2012-04-142012-04-142011-08-19SARI, Vanessa. INTERCEPTION OF RAINFALL IN DIFENTES FOREST FORMATIONS IN THE REGION OF SANTA MARIA - RS.. 2011. 211 f. Dissertação (Mestrado em Engenharia Civil) - Universidade Federal de Santa Maria, Santa Maria, 2011.http://repositorio.ufsm.br/handle/1/7766ABSTRACT: In regions of natural or planted forests, rainfall interception by vegetation can be an important variable in the hydrological cycle and should not be neglected. This research analyzes the process of interception in different forest types (native and planted) in the region of Santa Maria - RS, at the head of Vacacaí Mirim. The variables Rainfall (R), stemflow (Sf), and throughfall (Tf) were monitored in the period from Dec/09 to Fev/11. Rainfall was monitored in two tipping bucket rain gauges and meteorological station installed in the subbasin on July 14th, 2010. Throughfall was monitored in three plots (areas I, II and III) with dimensions of 12 m x 50 m, 21 m x 12 m and 10 m x 20 m, respectively. The sampling points were installed 40 or 60 cm from the ground and spaced 1 m in straight line. In area I (native forest), 101 stakes were allocated to 40 instruments; where 20 collectors remained in fixed locations and 20 were rotated randomly. In the areas II (native forest) and III (eucalyptus) 60 sampling points were allocated to 20 collectors; at each new collection they were placed one sampling point ahead the former. Stemflow was based on values suggested in literature and by monitoring the flow in three selected trees within each plot, and the interception was calculated as the difference between precipitation and the sum of throughfall and stemflow. The results showed that interception is a key component of the hydrological cycle and, in general, underestimated by the hydrological models.The highest interception value was checked for native forest and the largest stemflow for eucalyptus. The stemflow was higher than the values observed by other authors, revealing that this variable cannot be ruled out in the study of interception. On the other hand, the ranges of variation of throughfall and interception were close to those reported in other studies. The results seem also to suggest that the depth parameter adopted for the calculation of interception using the leaf area index is underestimated and should be 0.4. Statistical analysis of the number of collectors used and necessary to ensure error of 5 mm of throughfall in relation to its average and 90% of confidence, showed that for vegetation such as Eucalyptus, the use of 20 rotating collectors were sufficient in 95.45% of the collections; which may be a reference to works in which there is a pattern of similarity of species. For native forest we observed that when the vegetation has a low density and the similar pattern of canopy, stem diameter and height, the use of 20 rotating collectors would be enough to ensure statistical requirements set out in 71.43% of the samples monitored. When the native vegetation is dense, with standard range of height, stem diameter and crown area, we observed the need for a higher number of collectors equipment of throughfall. The use of 40 collectors (20 fixed and 20 rotational) assured that the statistical requirements stipulated were guaranteed in 60.98% of the samples monitored.RESUMO: Nas regiões de floretas naturais ou plantadas, a interceptação da precipitação pela vegetação pode ser uma importante variável do ciclo hidrológico, não devendo ser negligenciada. Esta pesquisa analisou o processo de interceptação em diferentes formações florestais (nativa e plantada) na região de Santa Maria - RS, na cabeceira do Vacacaí Mirim. As variáveis monitoradas no período de dez/09 a fev/11 foram: precipitação inicdente (P), escoamento pelo tronco (Esct) e precipitação interna (Pi). A precipitação incidente foi monitorada em dois pluviômetros tipo cubas-basculantes e pela estação climatológica instalada na sub-bacia em 14/7/2010. A precipitação interna foi monitorada em três parcelas (área I, II e III) com dimensões de 12 m x 50 m, 21 m x 12 m e 10 m x 20 m, respectivamente. As estacas foram instaladas a 40 ou 60 cm do solo, sendo espaçadas de 1 m e em linha reta. Na área I (mata nativa), foram alocadas 101 estacas para disposição de 40 instrumentos, sendo que 20 permaneceram fixos e 20 foram rotacionados. Já nas áreas II (mata nativa) e III (eucalipto) foram alocadas 60 estacas para disposição de 20 coletores, sendo que a cada nova coleta eles eram realocados uma estaca a frente da anterior. O escoamento pelo tronco foi determinado com base em valores sugeridos em literatura e por meio de monitoramento do escoamento em três árvores escolhidas dentro de cada parcela e a interceptação foi calculada pela diferença entre P e a soma de Pi e Esct. Os resultados mostraram que a interceptação é uma componente fundamental do ciclo hidrológico e, em geral, subestimada pelos modelos hidrológicos. O maior valor de interceptação foi verificado para mata nativa e o maior Esct para eucalipto. O escoamento pelo tronco foi superior aos valores verificados por outros autores, revelando que essa variável não pode ser descartada no estudo da interceptação. Já as faixas de variação de precipitação interna e da interceptação ficaram próximas aquelas registradas em outros estudos. Os resultados parecem sugerir, ainda, que o parâmetro de lâmina adotado para o cálculo de interceptação com utilização do índice de área foliar está subestimado e deveria ser 0,4. A análise estatística do número de aparelhos utilizados e necessários para garantir 5 mm de erro de Pi em relação a sua média e 90% de confiança, mostrou que para vegetação do tipo eucalipto, o uso de 20 instrumentos rotacionáveis seriam suficientes em 95,45% das coletas realizadas. O que pode ser uma referência para trabalhos em que existe um padrão de semelhança de espécies. Já para mata nativa observou-se que, quando a vegetação apresenta baixa densidade e mesmo padrão de copa, diâmetro do caule e altura, o uso de 20 instrumentos rotacionáveis seria suficiente para garantir os requisitos estatísticos estipulados em 71,43% das coletas monitoradas. Quando a vegetação nativa é densa, com padrão variado de altura, diâmetro do caule e área da copa, percebeu-se a necessidade de um número mais elevado de equipamentos coletores de Pi. O uso de 40 instrumentos, (20 aparelhos rotacionáveis e 20 fixos), garantiu que em 60,98% das coletas monitoradas os requisitos estatísticos estipulados fossem assegurados.Conselho Nacional de Desenvolvimento Científico e Tecnológicoapplication/pdfporUniversidade Federal de Santa MariaPrograma de Pós-Graduação em Engenharia CivilUFSMBREngenharia CivilPrecipitação incidentePrecipitação internaEscoamento pelo troncoInterceptaçãoBalanço hídricoRainfallThroughfallStemflowInterceptionWater balanceCNPQ::ENGENHARIAS::ENGENHARIA CIVILInterceptação da chuva em diferentes formações florestais na região de Santa Maria - RS.Interception of rainfall in difentes forest formations in the region of Santa Maria - RS.info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesisPaiva, Eloiza Maria Cauduro Dias dehttp://lattes.cnpq.br/9290923066819802Collischonn, Walterhttp://lattes.cnpq.br/0592949496367500Tassi, Rutinéiahttp://lattes.cnpq.br/7584743367186364http://lattes.cnpq.br/8138763995619661Sari, Vanessa300100000003400300500500bfeedfad-4ea2-41e2-9393-b48336b112a4e3c52144-087d-44d5-bf7f-97bf5ff07414e8aa47ec-8384-472e-b6e9-a6fd16eedde7b3c86d3a-b872-4e93-9e9a-fca1239bf68cinfo:eu-repo/semantics/openAccessreponame:Biblioteca Digital de Teses e Dissertações do UFSMinstname:Universidade Federal de Santa Maria (UFSM)instacron:UFSMORIGINALSARI, VANESSA.pdfapplication/pdf38671913http://repositorio.ufsm.br/bitstream/1/7766/1/SARI%2c%20VANESSA.pdf18b495182fc50414d133a22286306036MD51TEXTSARI, VANESSA.pdf.txtSARI, VANESSA.pdf.txtExtracted texttext/plain534540http://repositorio.ufsm.br/bitstream/1/7766/2/SARI%2c%20VANESSA.pdf.txt1a2bb2bef8afd6ba695081fbb6e1030aMD52THUMBNAILSARI, VANESSA.pdf.jpgSARI, VANESSA.pdf.jpgIM Thumbnailimage/jpeg4548http://repositorio.ufsm.br/bitstream/1/7766/3/SARI%2c%20VANESSA.pdf.jpgc41af8efc6c31f6d66b197450a391de7MD531/77662021-10-26 16:08:02.45oai:repositorio.ufsm.br:1/7766Biblioteca Digital de Teses e Dissertaçõeshttps://repositorio.ufsm.br/ONGhttps://repositorio.ufsm.br/oai/requestatendimento.sib@ufsm.br||tedebc@gmail.comopendoar:2021-10-26T19:08:02Biblioteca Digital de Teses e Dissertações do UFSM - Universidade Federal de Santa Maria (UFSM)false |
dc.title.por.fl_str_mv |
Interceptação da chuva em diferentes formações florestais na região de Santa Maria - RS. |
dc.title.alternative.eng.fl_str_mv |
Interception of rainfall in difentes forest formations in the region of Santa Maria - RS. |
title |
Interceptação da chuva em diferentes formações florestais na região de Santa Maria - RS. |
spellingShingle |
Interceptação da chuva em diferentes formações florestais na região de Santa Maria - RS. Sari, Vanessa Precipitação incidente Precipitação interna Escoamento pelo tronco Interceptação Balanço hídrico Rainfall Throughfall Stemflow Interception Water balance CNPQ::ENGENHARIAS::ENGENHARIA CIVIL |
title_short |
Interceptação da chuva em diferentes formações florestais na região de Santa Maria - RS. |
title_full |
Interceptação da chuva em diferentes formações florestais na região de Santa Maria - RS. |
title_fullStr |
Interceptação da chuva em diferentes formações florestais na região de Santa Maria - RS. |
title_full_unstemmed |
Interceptação da chuva em diferentes formações florestais na região de Santa Maria - RS. |
title_sort |
Interceptação da chuva em diferentes formações florestais na região de Santa Maria - RS. |
author |
Sari, Vanessa |
author_facet |
Sari, Vanessa |
author_role |
author |
dc.contributor.advisor1.fl_str_mv |
Paiva, Eloiza Maria Cauduro Dias de |
dc.contributor.advisor1Lattes.fl_str_mv |
http://lattes.cnpq.br/9290923066819802 |
dc.contributor.referee1.fl_str_mv |
Collischonn, Walter |
dc.contributor.referee1Lattes.fl_str_mv |
http://lattes.cnpq.br/0592949496367500 |
dc.contributor.referee2.fl_str_mv |
Tassi, Rutinéia |
dc.contributor.referee2Lattes.fl_str_mv |
http://lattes.cnpq.br/7584743367186364 |
dc.contributor.authorLattes.fl_str_mv |
http://lattes.cnpq.br/8138763995619661 |
dc.contributor.author.fl_str_mv |
Sari, Vanessa |
contributor_str_mv |
Paiva, Eloiza Maria Cauduro Dias de Collischonn, Walter Tassi, Rutinéia |
dc.subject.por.fl_str_mv |
Precipitação incidente Precipitação interna Escoamento pelo tronco Interceptação Balanço hídrico |
topic |
Precipitação incidente Precipitação interna Escoamento pelo tronco Interceptação Balanço hídrico Rainfall Throughfall Stemflow Interception Water balance CNPQ::ENGENHARIAS::ENGENHARIA CIVIL |
dc.subject.eng.fl_str_mv |
Rainfall Throughfall Stemflow Interception Water balance |
dc.subject.cnpq.fl_str_mv |
CNPQ::ENGENHARIAS::ENGENHARIA CIVIL |
description |
ABSTRACT: In regions of natural or planted forests, rainfall interception by vegetation can be an important variable in the hydrological cycle and should not be neglected. This research analyzes the process of interception in different forest types (native and planted) in the region of Santa Maria - RS, at the head of Vacacaí Mirim. The variables Rainfall (R), stemflow (Sf), and throughfall (Tf) were monitored in the period from Dec/09 to Fev/11. Rainfall was monitored in two tipping bucket rain gauges and meteorological station installed in the subbasin on July 14th, 2010. Throughfall was monitored in three plots (areas I, II and III) with dimensions of 12 m x 50 m, 21 m x 12 m and 10 m x 20 m, respectively. The sampling points were installed 40 or 60 cm from the ground and spaced 1 m in straight line. In area I (native forest), 101 stakes were allocated to 40 instruments; where 20 collectors remained in fixed locations and 20 were rotated randomly. In the areas II (native forest) and III (eucalyptus) 60 sampling points were allocated to 20 collectors; at each new collection they were placed one sampling point ahead the former. Stemflow was based on values suggested in literature and by monitoring the flow in three selected trees within each plot, and the interception was calculated as the difference between precipitation and the sum of throughfall and stemflow. The results showed that interception is a key component of the hydrological cycle and, in general, underestimated by the hydrological models.The highest interception value was checked for native forest and the largest stemflow for eucalyptus. The stemflow was higher than the values observed by other authors, revealing that this variable cannot be ruled out in the study of interception. On the other hand, the ranges of variation of throughfall and interception were close to those reported in other studies. The results seem also to suggest that the depth parameter adopted for the calculation of interception using the leaf area index is underestimated and should be 0.4. Statistical analysis of the number of collectors used and necessary to ensure error of 5 mm of throughfall in relation to its average and 90% of confidence, showed that for vegetation such as Eucalyptus, the use of 20 rotating collectors were sufficient in 95.45% of the collections; which may be a reference to works in which there is a pattern of similarity of species. For native forest we observed that when the vegetation has a low density and the similar pattern of canopy, stem diameter and height, the use of 20 rotating collectors would be enough to ensure statistical requirements set out in 71.43% of the samples monitored. When the native vegetation is dense, with standard range of height, stem diameter and crown area, we observed the need for a higher number of collectors equipment of throughfall. The use of 40 collectors (20 fixed and 20 rotational) assured that the statistical requirements stipulated were guaranteed in 60.98% of the samples monitored. |
publishDate |
2011 |
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2011-08-19 |
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2012-04-14 |
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2012-04-14 |
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publishedVersion |
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SARI, Vanessa. INTERCEPTION OF RAINFALL IN DIFENTES FOREST FORMATIONS IN THE REGION OF SANTA MARIA - RS.. 2011. 211 f. Dissertação (Mestrado em Engenharia Civil) - Universidade Federal de Santa Maria, Santa Maria, 2011. |
dc.identifier.uri.fl_str_mv |
http://repositorio.ufsm.br/handle/1/7766 |
identifier_str_mv |
SARI, Vanessa. INTERCEPTION OF RAINFALL IN DIFENTES FOREST FORMATIONS IN THE REGION OF SANTA MARIA - RS.. 2011. 211 f. Dissertação (Mestrado em Engenharia Civil) - Universidade Federal de Santa Maria, Santa Maria, 2011. |
url |
http://repositorio.ufsm.br/handle/1/7766 |
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300100000003 |
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400 300 500 500 |
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UFSM |
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Engenharia Civil |
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Universidade Federal de Santa Maria |
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