Groundwater Vulnerability of the Basaltic Aquifer in the UFMS Campus, at Campo Grande – MS

The Federal University of Mato Grosso do Sul Campus (UFMS) is located in Campo Grande in the basin of the Bandeira stream. It has its own water well supply system from the basalts of Serra Geral aquifer. Due to the importance of this water source for the Campus and the region, two methods of aquifer...

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Main Authors: Cristine Hortência Coutinho Pontes, Giancarlo Lastoria, Antonio Conceição Paranhos Filho, Sandra Garcia Gabas, Paulo Tarso Sanches de Oliveira
Format: Article
Language:English
Published: Associação Brasileira de Águas Subterrâneas 2009-02-01
Series:Revista Águas Subterrâneas
Subjects:
Online Access:https://aguassubterraneas.abas.org/asubterraneas/article/view/14989
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spelling doaj-97055f6c86fb408494e6b8eb1f3886af2020-11-24T21:59:05ZengAssociação Brasileira de Águas SubterrâneasRevista Águas Subterrâneas0101-70042179-97842009-02-0123110.14295/ras.v23i1.1498912559Groundwater Vulnerability of the Basaltic Aquifer in the UFMS Campus, at Campo Grande – MSCristine Hortência Coutinho Pontes0Giancarlo Lastoria1Antonio Conceição Paranhos Filho2Sandra Garcia Gabas3Paulo Tarso Sanches de Oliveira4Universidade Federal de Mato Grosso do SulUniversidade Federal de Mato Grosso do SulUniversidade Federal de Mato Grosso do SulUniversidade Federal de Mato Grosso do SulUniversidade Federal de Mato Grosso do SulThe Federal University of Mato Grosso do Sul Campus (UFMS) is located in Campo Grande in the basin of the Bandeira stream. It has its own water well supply system from the basalts of Serra Geral aquifer. Due to the importance of this water source for the Campus and the region, two methods of aquifer vulnerability assessment – DRASTIC and GOD – were applied. The methods are auxiliar tools for the decision process in issues such as urban planning and economic-ecological zoning which are the base for the integrated management of the natural resources. However, the methods do not substitute the field trips and the local monitoring. On the GOD method, it was observed three great and defined areas of low, medium and high vulnerability, while on the DRASTIC method it was obtained many degrees of vulnerability – from very low, low, moderate and high vulnerability. In this study, the GOD method is the most appropriate to be used because the area of the Campus is partially urbanized and the data used in the GOD method came from the not modified sub-surface. According to the chosen method, a better management plan could be developed and applied to other areas of the state, including the other aquifers. To the continuity of this project, it is necessary to intensify the data collection, and also settle a routine of sampling. It is also important that the government disciplines the activities developed around the Campus and also inside its area in order to protect the aquifer so that the users can always use it for many purposes.https://aguassubterraneas.abas.org/asubterraneas/article/view/14989VulnerabilidadeAquífero BasálticoCampus
collection DOAJ
language English
format Article
sources DOAJ
author Cristine Hortência Coutinho Pontes
Giancarlo Lastoria
Antonio Conceição Paranhos Filho
Sandra Garcia Gabas
Paulo Tarso Sanches de Oliveira
spellingShingle Cristine Hortência Coutinho Pontes
Giancarlo Lastoria
Antonio Conceição Paranhos Filho
Sandra Garcia Gabas
Paulo Tarso Sanches de Oliveira
Groundwater Vulnerability of the Basaltic Aquifer in the UFMS Campus, at Campo Grande – MS
Revista Águas Subterrâneas
Vulnerabilidade
Aquífero Basáltico
Campus
author_facet Cristine Hortência Coutinho Pontes
Giancarlo Lastoria
Antonio Conceição Paranhos Filho
Sandra Garcia Gabas
Paulo Tarso Sanches de Oliveira
author_sort Cristine Hortência Coutinho Pontes
title Groundwater Vulnerability of the Basaltic Aquifer in the UFMS Campus, at Campo Grande – MS
title_short Groundwater Vulnerability of the Basaltic Aquifer in the UFMS Campus, at Campo Grande – MS
title_full Groundwater Vulnerability of the Basaltic Aquifer in the UFMS Campus, at Campo Grande – MS
title_fullStr Groundwater Vulnerability of the Basaltic Aquifer in the UFMS Campus, at Campo Grande – MS
title_full_unstemmed Groundwater Vulnerability of the Basaltic Aquifer in the UFMS Campus, at Campo Grande – MS
title_sort groundwater vulnerability of the basaltic aquifer in the ufms campus, at campo grande – ms
publisher Associação Brasileira de Águas Subterrâneas
series Revista Águas Subterrâneas
issn 0101-7004
2179-9784
publishDate 2009-02-01
description The Federal University of Mato Grosso do Sul Campus (UFMS) is located in Campo Grande in the basin of the Bandeira stream. It has its own water well supply system from the basalts of Serra Geral aquifer. Due to the importance of this water source for the Campus and the region, two methods of aquifer vulnerability assessment – DRASTIC and GOD – were applied. The methods are auxiliar tools for the decision process in issues such as urban planning and economic-ecological zoning which are the base for the integrated management of the natural resources. However, the methods do not substitute the field trips and the local monitoring. On the GOD method, it was observed three great and defined areas of low, medium and high vulnerability, while on the DRASTIC method it was obtained many degrees of vulnerability – from very low, low, moderate and high vulnerability. In this study, the GOD method is the most appropriate to be used because the area of the Campus is partially urbanized and the data used in the GOD method came from the not modified sub-surface. According to the chosen method, a better management plan could be developed and applied to other areas of the state, including the other aquifers. To the continuity of this project, it is necessary to intensify the data collection, and also settle a routine of sampling. It is also important that the government disciplines the activities developed around the Campus and also inside its area in order to protect the aquifer so that the users can always use it for many purposes.
topic Vulnerabilidade
Aquífero Basáltico
Campus
url https://aguassubterraneas.abas.org/asubterraneas/article/view/14989
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