Bacia hidrográfica do córrego granada – Aparecida de Goiânia – GO: os processos erosivos e a dinâmica espacial urbana
Autor(a) principal: | |
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Data de Publicação: | 2009 |
Tipo de documento: | Dissertação |
Idioma: | por |
Título da fonte: | Repositório Institucional da UFG |
Texto Completo: | http://repositorio.bc.ufg.br/tede/handle/tede/4193 |
Resumo: | The basin of the Granada stream, with approximately 15 km2, is placed in the central part of the Aparecida de Goiânia - GO, located in the region metropolitan of Goiânia, to the south of the Goiânia. This basin limits for the coordinates east 682,000 and 688,000, and 8.145.000 north 8.139.000m and, MC -51º, South hemisphere. Aparecida it presents a confusion growth, intensified from 1970, configuring a big horizontal urbanization, with demographic empty in the interior of the city. The ambient impacts in the city if had evidenced in the measure that the city if to expand on the deep ones of existing valleys, as in the case of the near occupations to the Granada stream. All these not calculated uses of lands in the basin, that is, without looking for to establish tools and methodologies of conservation, come back toward the ambient-urban planning, had induced negatives occurrence of the ambient impacts and partner-economic, mainly the deflagration and the acceleration of erosive processes, generally in direction to the courses of the rivers, as it is the case of the soil erosions that leave the vulnerable inhabitants the catastrophic accidents. Soon, to attain the central objective of this research, that to be understand as the urban space dynamics speeds up or to give rise to, start the erosive processes in the basin of the Granada stream, had been elaborated map of declivity, soil in-situ, occupation of lands and bending of the sources, from digital modeling of fine altimetric data with survey of field by means of topographical receiver GPS and images of satellite of diverse sensors. The study area is characterized for the ground predominance of the type Ustox soils, that had been classified how much its erodibilidade, by means of the laboratorial assay Inderbitzen, adapted in the scope of this research. With the assay it was possible to determine the loss of ground soil, for the action of the superficial draining in indeformados bodies of test. Although low the declivity of the land, the basin of Granada possess almost rectilinear, associates the deep and fragile ground, what it more than induced the to be published 30 erosions. |
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Romão, Patrícia de Araújohttp://lattes.cnpq.br/0188184635964559Romão, Patrícia de AraújoSales, Maurício MartinesGuimarães, Renato Fonteshttp://lattes.cnpq.br/9820176762513634Aguiar, Vinicius Gomes de2015-02-24T18:53:38Z2009-10-29AGUIAR, Vinicius Gomes de. Bacia hidrográfica do córrego granada – Aparecida de Goiânia – GO: os processos erosivos e a dinâmica espacial urbana. 2009. 95 f. Dissertação (Mestrado em Geotecnia, Estruturas e Construção Civil) - Universidade Federal de Goiás, Goiânia, 2009.http://repositorio.bc.ufg.br/tede/handle/tede/4193The basin of the Granada stream, with approximately 15 km2, is placed in the central part of the Aparecida de Goiânia - GO, located in the region metropolitan of Goiânia, to the south of the Goiânia. This basin limits for the coordinates east 682,000 and 688,000, and 8.145.000 north 8.139.000m and, MC -51º, South hemisphere. Aparecida it presents a confusion growth, intensified from 1970, configuring a big horizontal urbanization, with demographic empty in the interior of the city. The ambient impacts in the city if had evidenced in the measure that the city if to expand on the deep ones of existing valleys, as in the case of the near occupations to the Granada stream. All these not calculated uses of lands in the basin, that is, without looking for to establish tools and methodologies of conservation, come back toward the ambient-urban planning, had induced negatives occurrence of the ambient impacts and partner-economic, mainly the deflagration and the acceleration of erosive processes, generally in direction to the courses of the rivers, as it is the case of the soil erosions that leave the vulnerable inhabitants the catastrophic accidents. Soon, to attain the central objective of this research, that to be understand as the urban space dynamics speeds up or to give rise to, start the erosive processes in the basin of the Granada stream, had been elaborated map of declivity, soil in-situ, occupation of lands and bending of the sources, from digital modeling of fine altimetric data with survey of field by means of topographical receiver GPS and images of satellite of diverse sensors. The study area is characterized for the ground predominance of the type Ustox soils, that had been classified how much its erodibilidade, by means of the laboratorial assay Inderbitzen, adapted in the scope of this research. With the assay it was possible to determine the loss of ground soil, for the action of the superficial draining in indeformados bodies of test. Although low the declivity of the land, the basin of Granada possess almost rectilinear, associates the deep and fragile ground, what it more than induced the to be published 30 erosions.A bacia do córrego Granada, com aproximadamente 15 km2, situa-se na parte central do município de Aparecida de Goiânia – GO, localizado na Região Metropolitana de Goiânia, ao sul da capital goiana. Essa bacia limita-se pelas coordenadas leste 682.000 e 688.000, e norte 8.139.000 e 8.145.000 m, MC -51º, hemisfério Sul. Aparecida apresenta um crescimento desordenado, intensificado a partir de 1970, configurando uma urbanização horizontal, espraiada com vazios demográficos no interior da cidade. Os impactos ambientais no município se evidenciaram na medida em que a cidade se expandiu até os fundos de vales existentes, como no caso das ocupações próximas ao córrego Granada e/ou Saltador. Todos estes usos impensados das terras na bacia, ou seja, sem procurar estabelecer ferramentas e metodologias de conservação e manejo, voltadas para o planejamento ambiental-urbano, induziram a ocorrência dos impactos ambientais e sócio-econômicos negativos, principalmente a deflagração e a aceleração de processos erosivos, geralmente em direção aos cursos dos rios, como é o caso das voçorocas que deixam os moradores vulneráveis a acidentes catastróficos. Logo, para atingir o objetivo central desta pesquisa, que consiste em entender como a dinâmica espacial urbana acelera ou deflagra os processos erosivos na bacia do córrego Granada. Como principal produtos da pesquisa elaborou-se a carta de materiais inconsolidados e cartas multitemporais de ocupação das terras da bacia hidrográfica do córrego Granada. Para a elaboração desses produtos utilizou-se nessa pesquisa cartas básicas de declividades e curvatura das vertentes, a partir de modelagem digital de dados altimétricos refinados e imagens de satélite de diversos sensores. Além disso, os materiais consolidados foram classificados na carta quanto a sua erodibilidade por meio do ensaio laboratorial Inderbitzen, adaptado no âmbito dessa pesquisa. Assim foi analisada a relação entre a erodibilidade dos materiais inconsolidados e a ocupação urbana. Apesar da baixa declividade do terreno, a área de estudos possui curvaturas quase retilíneas com rampas longas, associadas a solos profundos e na maior parte erodíveis. A ocupação urbana sem a devida observação dos condicionantes naturais na área induziu a deflagração e aceleração de mais de 30 focos erosivos.Submitted by Erika Demachki (erikademachki@gmail.com) on 2015-02-24T18:53:25Z No. of bitstreams: 2 Dissertação - Vinicius Gomes de Aguiar - 2009.pdf: 12290878 bytes, checksum: 26f74c3a03bb162accbcb9ceefffb033 (MD5) license_rdf: 23148 bytes, checksum: 9da0b6dfac957114c6a7714714b86306 (MD5)Approved for entry into archive by Erika Demachki (erikademachki@gmail.com) on 2015-02-24T18:53:38Z (GMT) No. of bitstreams: 2 Dissertação - Vinicius Gomes de Aguiar - 2009.pdf: 12290878 bytes, checksum: 26f74c3a03bb162accbcb9ceefffb033 (MD5) license_rdf: 23148 bytes, checksum: 9da0b6dfac957114c6a7714714b86306 (MD5)Made available in DSpace on 2015-02-24T18:53:38Z (GMT). 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dc.title.eng.fl_str_mv |
Bacia hidrográfica do córrego granada – Aparecida de Goiânia – GO: os processos erosivos e a dinâmica espacial urbana |
title |
Bacia hidrográfica do córrego granada – Aparecida de Goiânia – GO: os processos erosivos e a dinâmica espacial urbana |
spellingShingle |
Bacia hidrográfica do córrego granada – Aparecida de Goiânia – GO: os processos erosivos e a dinâmica espacial urbana Aguiar, Vinicius Gomes de Aparecida de Goiânia Granada Erosão Inderbitzen Erosion ENGENHARIA CIVIL::GEOTECNICA |
title_short |
Bacia hidrográfica do córrego granada – Aparecida de Goiânia – GO: os processos erosivos e a dinâmica espacial urbana |
title_full |
Bacia hidrográfica do córrego granada – Aparecida de Goiânia – GO: os processos erosivos e a dinâmica espacial urbana |
title_fullStr |
Bacia hidrográfica do córrego granada – Aparecida de Goiânia – GO: os processos erosivos e a dinâmica espacial urbana |
title_full_unstemmed |
Bacia hidrográfica do córrego granada – Aparecida de Goiânia – GO: os processos erosivos e a dinâmica espacial urbana |
title_sort |
Bacia hidrográfica do córrego granada – Aparecida de Goiânia – GO: os processos erosivos e a dinâmica espacial urbana |
author |
Aguiar, Vinicius Gomes de |
author_facet |
Aguiar, Vinicius Gomes de |
author_role |
author |
dc.contributor.advisor1.fl_str_mv |
Romão, Patrícia de Araújo |
dc.contributor.advisor1Lattes.fl_str_mv |
http://lattes.cnpq.br/0188184635964559 |
dc.contributor.referee1.fl_str_mv |
Romão, Patrícia de Araújo |
dc.contributor.referee2.fl_str_mv |
Sales, Maurício Martines |
dc.contributor.referee3.fl_str_mv |
Guimarães, Renato Fontes |
dc.contributor.authorLattes.fl_str_mv |
http://lattes.cnpq.br/9820176762513634 |
dc.contributor.author.fl_str_mv |
Aguiar, Vinicius Gomes de |
contributor_str_mv |
Romão, Patrícia de Araújo Romão, Patrícia de Araújo Sales, Maurício Martines Guimarães, Renato Fontes |
dc.subject.por.fl_str_mv |
Aparecida de Goiânia Granada Erosão Inderbitzen |
topic |
Aparecida de Goiânia Granada Erosão Inderbitzen Erosion ENGENHARIA CIVIL::GEOTECNICA |
dc.subject.eng.fl_str_mv |
Erosion |
dc.subject.cnpq.fl_str_mv |
ENGENHARIA CIVIL::GEOTECNICA |
description |
The basin of the Granada stream, with approximately 15 km2, is placed in the central part of the Aparecida de Goiânia - GO, located in the region metropolitan of Goiânia, to the south of the Goiânia. This basin limits for the coordinates east 682,000 and 688,000, and 8.145.000 north 8.139.000m and, MC -51º, South hemisphere. Aparecida it presents a confusion growth, intensified from 1970, configuring a big horizontal urbanization, with demographic empty in the interior of the city. The ambient impacts in the city if had evidenced in the measure that the city if to expand on the deep ones of existing valleys, as in the case of the near occupations to the Granada stream. All these not calculated uses of lands in the basin, that is, without looking for to establish tools and methodologies of conservation, come back toward the ambient-urban planning, had induced negatives occurrence of the ambient impacts and partner-economic, mainly the deflagration and the acceleration of erosive processes, generally in direction to the courses of the rivers, as it is the case of the soil erosions that leave the vulnerable inhabitants the catastrophic accidents. Soon, to attain the central objective of this research, that to be understand as the urban space dynamics speeds up or to give rise to, start the erosive processes in the basin of the Granada stream, had been elaborated map of declivity, soil in-situ, occupation of lands and bending of the sources, from digital modeling of fine altimetric data with survey of field by means of topographical receiver GPS and images of satellite of diverse sensors. The study area is characterized for the ground predominance of the type Ustox soils, that had been classified how much its erodibilidade, by means of the laboratorial assay Inderbitzen, adapted in the scope of this research. With the assay it was possible to determine the loss of ground soil, for the action of the superficial draining in indeformados bodies of test. Although low the declivity of the land, the basin of Granada possess almost rectilinear, associates the deep and fragile ground, what it more than induced the to be published 30 erosions. |
publishDate |
2009 |
dc.date.issued.fl_str_mv |
2009-10-29 |
dc.date.accessioned.fl_str_mv |
2015-02-24T18:53:38Z |
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 |
AGUIAR, Vinicius Gomes de. Bacia hidrográfica do córrego granada – Aparecida de Goiânia – GO: os processos erosivos e a dinâmica espacial urbana. 2009. 95 f. Dissertação (Mestrado em Geotecnia, Estruturas e Construção Civil) - Universidade Federal de Goiás, Goiânia, 2009. |
dc.identifier.uri.fl_str_mv |
http://repositorio.bc.ufg.br/tede/handle/tede/4193 |
identifier_str_mv |
AGUIAR, Vinicius Gomes de. Bacia hidrográfica do córrego granada – Aparecida de Goiânia – GO: os processos erosivos e a dinâmica espacial urbana. 2009. 95 f. Dissertação (Mestrado em Geotecnia, Estruturas e Construção Civil) - Universidade Federal de Goiás, Goiânia, 2009. |
url |
http://repositorio.bc.ufg.br/tede/handle/tede/4193 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.program.fl_str_mv |
6915322422128222104 |
dc.relation.confidence.fl_str_mv |
600 600 600 |
dc.relation.department.fl_str_mv |
724087251626315585 |
dc.relation.cnpq.fl_str_mv |
8794820169253231856 |
dc.rights.driver.fl_str_mv |
http://creativecommons.org/licenses/by-nc-nd/4.0/ info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
http://creativecommons.org/licenses/by-nc-nd/4.0/ |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade Federal de Goiás |
dc.publisher.program.fl_str_mv |
Programa de Pós-graduação em Geotecnia, Estruturas e Construção Civil (EEC) |
dc.publisher.initials.fl_str_mv |
UFG |
dc.publisher.country.fl_str_mv |
Brasil |
dc.publisher.department.fl_str_mv |
Escola de Engenharia Civil - EEC (RG) |
publisher.none.fl_str_mv |
Universidade Federal de Goiás |
dc.source.none.fl_str_mv |
reponame:Repositório Institucional da UFG instname:Universidade Federal de Goiás (UFG) instacron:UFG |
instname_str |
Universidade Federal de Goiás (UFG) |
instacron_str |
UFG |
institution |
UFG |
reponame_str |
Repositório Institucional da UFG |
collection |
Repositório Institucional da UFG |
bitstream.url.fl_str_mv |
http://repositorio.bc.ufg.br/tede/bitstreams/b4446b38-59d3-4c75-a02f-bda83b98362d/download http://repositorio.bc.ufg.br/tede/bitstreams/1e6a25ed-1fcf-4941-8a66-7daa8d2d60ff/download http://repositorio.bc.ufg.br/tede/bitstreams/6ed2edd4-1232-4d4c-9c73-9d8a56320b66/download http://repositorio.bc.ufg.br/tede/bitstreams/5fac1018-3ac6-47b0-b266-76c431eb27ba/download http://repositorio.bc.ufg.br/tede/bitstreams/7daa6837-7190-4d4b-9233-8ac58a04d6dc/download http://repositorio.bc.ufg.br/tede/bitstreams/2696835b-75d8-4962-b535-c5b62b01f605/download http://repositorio.bc.ufg.br/tede/bitstreams/0b515383-4654-4b67-aea4-0a94682f0faa/download |
bitstream.checksum.fl_str_mv |
bd3efa91386c1718a7f26a329fdcb468 4afdbb8c545fd630ea7db775da747b2f b292a83e42bd8ad62533bba1395b83ff 9da0b6dfac957114c6a7714714b86306 26f74c3a03bb162accbcb9ceefffb033 99746508574a3ad873457f92bd370481 27e98649d2ae11b8730774b78ae0bfe6 |
bitstream.checksumAlgorithm.fl_str_mv |
MD5 MD5 MD5 MD5 MD5 MD5 MD5 |
repository.name.fl_str_mv |
Repositório Institucional da UFG - Universidade Federal de Goiás (UFG) |
repository.mail.fl_str_mv |
tasesdissertacoes.bc@ufg.br |
_version_ |
1798044327987904512 |