Published 2017 | Version v1
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Hydrochemical and isotopic studies in two neighboring river basins in semiarid regions of Minas Gerais

  • 1. Centro de Desenvolvimento da Tecnologia Nuclear (CDTN/CNEN-MG), Belo Horizonte, MG (Brazil). Serviço de Meio Ambiente

Description

Groundwater is the largest reservoir of fresh water on Earth and the depletion of aquifer systems is a reality, both in semi-arid and humid regions. The hydrology of watersheds is a field of study that is concerned with the movement of waters from the rains and its physical-chemical changes. Groundwater resources in these regions are a sensitive issue, requiring careful management to avoid quality degradation. The present study focuses the groundwater system at the interface of the Pandeiros and Peruaçu river basins in the northwest region of Minas Gerais State. The methods used were the evaluations of the hydrochemistry, as well as isotopic, and physicochemical parameters, allied to geological studies to investigate surface and groundwater, their possible interactions and spatial distribution. The hydrochemical results correlated with the physicochemical measurements show water contrasts in the study area, which is geologically composed from bottom to top by gneisses and granites (Januaria Complex), limestone and siltstones (Bambuí Group), sandstones and eluvial sediments (Urucuia Group), eluvio-coluvial cover and alluvial deposits. It has been observed that waters in the context of sandstones and siliceous sediments are sodium bicarbonate waters, slightly acidic pH and low in TDS, whereas waters in pedological / geologic context of limestones are calcium bicarbonate waters exhibiting basic pH and high TDS. The deuterium (D) and oxygen-18 signatures of the groundwater are compared to the global meteoric water line (GMWL). The average values of the isotopes in the study area are slightly variable, indicating that the isotopic signatures are related to rainfall precipitation. It has been possible to suggest an evaporation line pattern starting from the position of springs, passing though streams and finally ending in the lagoon. The local evaporation line can be represented by the equation δD = 5,8 δ18O - 2,4. (author)

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Additional details

Publishing Information

Imprint Pagination
13 p.
Report number
INIS-BR--19401

Conference

Title
International Nuclear Atlantic Conference
Acronym
INAC 2017
Dates
22-27 Oct 2017
Place
Belo Horizonte, MG (Brazil)

INIS

Country of Publication
Brazil
Country of Input or Organization
Brazil
INIS RN
48103597
Subject category
S54: ENVIRONMENTAL SCIENCES;
Resource subtype / Literary indicator
Conference
Descriptors DEI
CHEMICAL ANALYSIS; GEOLOGIC SURVEYS; GROUND WATER; HYDROLOGY; ICP MASS SPECTROSCOPY; LIQUID COLUMN CHROMATOGRAPHY; RAIN WATER; RIVERS; SPATIAL DISTRIBUTION; STABLE ISOTOPES
Descriptors DEC
CHROMATOGRAPHY; DISTRIBUTION; HYDROGEN COMPOUNDS; ISOTOPES; MASS SPECTROSCOPY; OXYGEN COMPOUNDS; SEPARATION PROCESSES; SPECTROSCOPY; SURFACE WATERS; WATER