ASSESSMENT OF HYDROGEOCHEMISTRY AND GIS-BASED EVOLUTION OF GROUNDWATER QUALITY AND SALINITY IN THE SHALLOW AQUIFER OF SÃO JOSÉ DO NORTE, SOUTHERN BRAZIL

H. Sabino, J. Menezes
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Abstract

Water salinization changes hydrogeochemistry, affects the quality and quantity of groundwater available for human consumption and its mitigation is time-consuming. A large brackish lagoon and the Atlantic Ocean surround the aquifer of the São José do Norte town (Brazil). Population and economic growth demand more groundwater for domestic and agricultural purposes, stressing the aquifer. Despise the aquifer’s social-economic status, potential impacts on the groundwater have not yet been substantially investigated. The aims of this study were to analyze the hydrogeochemistry of the São José do Norte aquifer, focusing on the search for salinization indicators, and to assess the groundwater suitability for human drinking and irrigation purpose. Ionic ratios, Piper and USSL diagrams were applied, such as new methods, as Seawater Intrusion Groundwater Quality Index (GQISWI) and the Groundwater Quality Index for human consumption (GWQIHC). The results showed that the groundwater is mostly calcium bicarbonate type and did not indicated salinization occurrence. The interior and the northern area had the highest ionic content and the lowest water quality values. Most of the samples contained at least one parameter above the maximum allowed concentration for drinking purpose according to water quality standards. High concentration of alkalinity, iron and hardness reduced the groundwater suitability for human consumption, requiring water treatment before ingestion.
巴西南部sÃo josÉ do norte浅层地下水水质和盐度的水文地球化学和gis演化评价
水的盐碱化改变了水文地球化学,影响了可供人类消费的地下水的质量和数量,缓解盐碱化需要耗费大量时间。一个巨大的咸淡咸水湖和大西洋环绕着 o jos北镇(巴西)的含水层。人口和经济增长需要更多的地下水用于家庭和农业用途,给含水层带来压力。不考虑含水层的社会经济地位,对地下水的潜在影响尚未进行实质性调查。本研究的目的是分析 o joss do Norte含水层的水文地球化学特征,重点寻找盐渍化指标,并评估地下水是否适合人类饮用和灌溉。应用离子比、Piper图和USSL图等新方法,如海水入侵地下水水质指数(GQISWI)和人类饮用地下水水质指数(GWQIHC)。结果表明:地下水以碳酸钙型为主,未见盐渍化现象;内陆和北部地区离子含量最高,水质值最低。大部分样本中至少有一项参数高于水质标准规定的最高允许饮用浓度。高浓度的碱度、铁和硬度降低了地下水对人类饮用的适宜性,需要在饮用前进行水处理。
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