巴西巴伊亚州lencois市地下水的水文地球化学

J. Mattos, M. Cruz, Francisco Carlos Fernandes de Paula
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引用次数: 2

摘要

本研究旨在指出巴伊亚州Lencois市的水文地球化学地下水,并根据其溶解盐的含量和类型对其进行分类。为此,选取了由沉积物、碎屑盖层和石灰岩组成的含水层地下水二十个采样点,对其电导率、温度、pH、浊度、总溶解固形物、hco3、po4、so4、Cl -、no3、Na +、K +、ca2 +、mg2 +、fe3 +、mn4 +、sr2 +和ba2 +等参数进行了分析。结果表明:连科瓦市地下水分为两个水文地球化学特征不同的带,其中最大的带受地质碎屑变质沉积岩类型(砂岩、石英岩、砾岩、碎屑盖)控制,水-岩相互作用过程允许少量的咸水、微酸性、甜、软、硫酸盐为主;另一个区域由化学变质沉积岩(石灰石)和碳酸氢盐控制,在那里它们发生硬水,微碱性,甜味和硫酸钙混合。硝酸盐、磷酸盐和硫酸盐等金属和元素的浓度一般较低,在城市地区的一些地点检测到一些偏差。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hidrogeoquímica das águas subterrâneas no município de Lençóis, Bahia, Brasil
This study aimed to point out the hydrogeochemistry groundwater in the municipality of Lencois, State of Bahia, to classify them according to the content and types of dissolved salts. To this, twenty sampling points were listed in the groundwater in aquifers formed by metasediments, detritical covers and limestones, with the purpose of analyze the following parameters: electrical conductivity, temperature, pH, turbidity, total dissolved solids, HCO 3 , PO 4 , SO 4 , Cl - , NO 3 , Na + , K + , Ca 2+ , Mg 2+ , Fe 3+ , Mn 4+ , Sr 2+ and Ba 2+ . The results showed that the groundwater in the municipality of Lencois are distributed into two zones with different hydrogeochemistry, one of the largest controlled by geological clastic metasedimentary rocks typologies (sandstones, quartzites, conglomeratics, detritical covers) where the process of water-rock interaction allows occur little quantity salt water, slightly acidic, sweet, soft and predominantly sulfated sodic. The other zone is controlled by chemical metasedimentary rocks (limestones) as well as bicarbonates, where they occur hard water, slightly alkaline, sweets and sulfated calcic and mixed. The levels of metals and elements nitrate, phosphate and sulfate presented themselves generally at low concentrations, with some deviations detected in points of the urban area.
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