石油采出水灌溉试验区地下水化学成分监测

P. Stein, Germano Melo Júnior, L. C. Souza
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引用次数: 0

摘要

采出水的农业回用是水资源管理的有效手段。然而,它可能会对土壤和地下水产生影响,因此需要在整个过程中进行环境监测。从这个角度来看,本工作旨在监测巴西东北部岩溶含水层的地下水质量,利用巴西塞阿拉州Fazenda Belem油田的PW进行了灌溉实验。通过四阶段采样程序对12个监测井进行了评估:第一个监测井在灌溉实验安装前(CHA),另外三个监测井分别在试验期间(MO1)、试验结束时(MO2)和试验后(MO3)。评估中还考虑了气候影响,因为采样事件发生在不同的季节:第一次和最后一次发生在旱季结束时,第二次和第三次发生在雨季结束时。调查考虑了两组井:与实验区地下水流量有关的上游井和下游井。对于Ca2+、Mg 2+、K+、总硬度、HCO3-、F-、As、B、Li和P,监测采样中的浓度有增加的趋势,与CHA有关。然而,由于这种情况在两组井(上游和下游)中都得到了验证,其原因可能与自然因素有关。还观察到,最高浓度主要出现在MO1和MO2采样阶段,也就是说,在雨季的影响下,充水促进含水层中碳酸盐成分的溶解,从而增加其溶解浓度。地下水中分析的有机物质没有被检测到,或者检测到的浓度非常低且分散,没有任何特定来源的特征。因此,它们的起源可以归因于自然或扩散输入。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Monitoring groundwater chemical composition at an experimental area irrigated with petroleum produced water
Agricultural reuse of the produced water is an efficient means for water resource management. However it is a potentially impacting activity to soil and groundwater, and thus requires environmental monitoring throughout the process. From this perspective, the present work aims at the monitoring of groundwater quality of karstic aquifer, located in the northeast of Brazil, where an irrigation experiment was carried out using PW of the Fazenda Belem oil field, in Ceara State, Brazil. Twelve monitoring wells were evaluated through a four-stage sampling program: the first before the installation of the irrigation experiment (CHA) and the other three, respectively, during (MO1), immediately at the end (MO2) and after the experiment (MO3). The climatic effect was also considered in the evaluation, since sampling events occurred in distinct seasonal periods: the first and the last at the end of the dry season and the second and third at the end of the wet season. Investigations were performed considering two groups of wells: upstream wells and downstream wells in relation to groundwater flow in the experimental area. For Ca 2+ , Mg 2+ , K + , total hardness, HCO 3 - , F - , As, B, Li and P, there was a tendency of increasing concentrations in the Monitoring sampling, in relation to CHA. However, since this scenario was verified in both sets of wells (upstream and downstream), its causes are probably related to natural factors. It was also observed that highest concentrations occur predominantly in the MO1 and MO2 sampling stages, that is, under the influence of the wet season, when water recharges promote dissolution of carbonate constituents present in the aquifer, thus increasing its dissolved concentration. Organic substances analyzed in groundwater were not detected or were detected at very low and dispersed concentrations and without any source specific signatures. Hence, their origin can be attributed to natural or diffuse inputs.
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