A morfometria da bacia hidrográfica do rio Mimoso, um sistema cárstico do Mato Grosso do Sul/ Brasil

This article aims to analyze and understand the morphometry of the relief of the Mimoso River Basin - BHRM, located in the municipality of Bonito / MS, a karst system of great importance in Mato Grosso do Sul. The study was determined the slope, horizontal dissection and vertical dissection of the B...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Rafael Brugnolli Medeiros, André Geraldo Berezuk, Charlei Aparecido da Silva
Formato: article
Lenguaje:EN
FR
PT
Publicado: Confins 2019
Materias:
G
Acceso en línea:https://doaj.org/article/e3ab617a8e9a4d7998784ac4dce50a9b
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:e3ab617a8e9a4d7998784ac4dce50a9b
record_format dspace
spelling oai:doaj.org-article:e3ab617a8e9a4d7998784ac4dce50a9b2021-12-02T10:55:52ZA morfometria da bacia hidrográfica do rio Mimoso, um sistema cárstico do Mato Grosso do Sul/ Brasil1958-921210.4000/confins.19845https://doaj.org/article/e3ab617a8e9a4d7998784ac4dce50a9b2019-05-01T00:00:00Zhttp://journals.openedition.org/confins/19845https://doaj.org/toc/1958-9212This article aims to analyze and understand the morphometry of the relief of the Mimoso River Basin - BHRM, located in the municipality of Bonito / MS, a karst system of great importance in Mato Grosso do Sul. The study was determined the slope, horizontal dissection and vertical dissection of the BHRM. The interpolation of these morphometric components revealed the potential erosive energy of the relief, based on the methodological proposals of Spiridonov (1981) and Mendes (1993). We used the Digital Terrain Model - MDT / SRTM made available by the United States Geological Survey. The methodology also consisted of conferences of the information obtained in in situ maps, from the inclinations and the length and altitude of the terrain ramps. The results pointed to a significant diversity of slope classes, horizontal and vertical dissections, evidencing the potential erosive energy of the study area that runs from the very weak to moderately average classes in the high and low BHRM courses due to the slopes and reduced altimetric amplitudes . In the middle course the middle and mildly strong classes were found due to the marked slopes of mountainous relief added to the narrow ramps elevate the erosive potential of the basin. In conclusion, the analyzes demonstrate the fragility of this karst system that suffers great pressures due to the recent expansion of the agricultural areas for the planting of soybeans and maize for export commodities.Rafael Brugnolli MedeirosAndré Geraldo BerezukCharlei Aparecido da SilvaConfinsarticleslope; horizontal dissection; vertical dissection; relief’s erosive potential energy.Geography. Anthropology. RecreationGENFRPTConfins, Vol 40 (2019)
institution DOAJ
collection DOAJ
language EN
FR
PT
topic slope; horizontal dissection; vertical dissection; relief’s erosive potential energy.
Geography. Anthropology. Recreation
G
spellingShingle slope; horizontal dissection; vertical dissection; relief’s erosive potential energy.
Geography. Anthropology. Recreation
G
Rafael Brugnolli Medeiros
André Geraldo Berezuk
Charlei Aparecido da Silva
A morfometria da bacia hidrográfica do rio Mimoso, um sistema cárstico do Mato Grosso do Sul/ Brasil
description This article aims to analyze and understand the morphometry of the relief of the Mimoso River Basin - BHRM, located in the municipality of Bonito / MS, a karst system of great importance in Mato Grosso do Sul. The study was determined the slope, horizontal dissection and vertical dissection of the BHRM. The interpolation of these morphometric components revealed the potential erosive energy of the relief, based on the methodological proposals of Spiridonov (1981) and Mendes (1993). We used the Digital Terrain Model - MDT / SRTM made available by the United States Geological Survey. The methodology also consisted of conferences of the information obtained in in situ maps, from the inclinations and the length and altitude of the terrain ramps. The results pointed to a significant diversity of slope classes, horizontal and vertical dissections, evidencing the potential erosive energy of the study area that runs from the very weak to moderately average classes in the high and low BHRM courses due to the slopes and reduced altimetric amplitudes . In the middle course the middle and mildly strong classes were found due to the marked slopes of mountainous relief added to the narrow ramps elevate the erosive potential of the basin. In conclusion, the analyzes demonstrate the fragility of this karst system that suffers great pressures due to the recent expansion of the agricultural areas for the planting of soybeans and maize for export commodities.
format article
author Rafael Brugnolli Medeiros
André Geraldo Berezuk
Charlei Aparecido da Silva
author_facet Rafael Brugnolli Medeiros
André Geraldo Berezuk
Charlei Aparecido da Silva
author_sort Rafael Brugnolli Medeiros
title A morfometria da bacia hidrográfica do rio Mimoso, um sistema cárstico do Mato Grosso do Sul/ Brasil
title_short A morfometria da bacia hidrográfica do rio Mimoso, um sistema cárstico do Mato Grosso do Sul/ Brasil
title_full A morfometria da bacia hidrográfica do rio Mimoso, um sistema cárstico do Mato Grosso do Sul/ Brasil
title_fullStr A morfometria da bacia hidrográfica do rio Mimoso, um sistema cárstico do Mato Grosso do Sul/ Brasil
title_full_unstemmed A morfometria da bacia hidrográfica do rio Mimoso, um sistema cárstico do Mato Grosso do Sul/ Brasil
title_sort morfometria da bacia hidrográfica do rio mimoso, um sistema cárstico do mato grosso do sul/ brasil
publisher Confins
publishDate 2019
url https://doaj.org/article/e3ab617a8e9a4d7998784ac4dce50a9b
work_keys_str_mv AT rafaelbrugnollimedeiros amorfometriadabaciahidrograficadoriomimosoumsistemacarsticodomatogrossodosulbrasil
AT andregeraldoberezuk amorfometriadabaciahidrograficadoriomimosoumsistemacarsticodomatogrossodosulbrasil
AT charleiaparecidodasilva amorfometriadabaciahidrograficadoriomimosoumsistemacarsticodomatogrossodosulbrasil
AT rafaelbrugnollimedeiros morfometriadabaciahidrograficadoriomimosoumsistemacarsticodomatogrossodosulbrasil
AT andregeraldoberezuk morfometriadabaciahidrograficadoriomimosoumsistemacarsticodomatogrossodosulbrasil
AT charleiaparecidodasilva morfometriadabaciahidrograficadoriomimosoumsistemacarsticodomatogrossodosulbrasil
_version_ 1718396500459913216