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Assessment and Modeling of Groundwater Flow and Nitrate Contamination within Coastal Karst Aquifer of Puerto Rico

机译:波多黎各沿海岩溶含水层内地下水流和硝酸盐污染的评估和建模

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摘要

Karst aquifers, capable of store and transmit large amount of water, are the main source of drinking water in many regions worldwide. Their excessive permeability leads to enhanced vulnerability to contamination accordingly. In the first section of this study, a comprehensive overview of hydrological processes and concepts, assessment methods and governing equations regarding groundwater flow and contaminant transport in karst aquifers is presented. Moreover, surface water and groundwater interaction and recent groundwater remediation techniques in karst terrains are discussed. Due to the complexity of karst aquifers, different approaches are developed by researchers for investigating and predicting karst processes and groundwater behavior. Modeling techniques are among the most beneficial and powerful methods for assessing groundwater flow and contaminant transport in karst aquifers, as hydrogeological systems with complicated and unpredictable behavior. Hence, several modeling approaches, are reviewed and assessed. Moreover, associated research works conducted for northern Puerto Rico are discussed to complement ongoing hydrogeologic investigations in this island.;In the second section, groundwater Nitrate contamination, as a result of agricultural, industrial and urban development, is assessed for north-central part of Puerto Rico. Using collected field samples and historical data, a Nitrate fate and transport simulation was conducted using MODFLOW and MT3D models. The calculated results of the regional-scale simulation showed high correlation with observed values and hence, the calibrated model was used for prediction purposes. Using land cover data and by assessing agricultural development trend in the island, spatiotemporal pattern of groundwater Nitrate concentration was predicted for the next two decades. It was predicted that agricultural activities will rise dramatically after economic damages of Hurricane Maria and this will negatively impact the groundwater quality. Based on the model prediction results, recommended management plans for each municipality were presented for the use of policy makers and authorities.
机译:能够储存和传输大量水的岩溶含水层是全世界许多地区的主要饮用水来源。它们的过高的渗透性会导致相应的污染增加。在本研究的第一部分中,介绍了有关岩溶含水层中地下水流量和污染物运移的水文过程和概念,评估方法和控制方程的综合概述。此外,讨论了喀斯特地形中的地表水和地下水相互作用以及最近的地下水修复技术。由于岩溶含水层的复杂性,研究人员开发了不同的方法来调查和预测岩溶过程和地下水行为。作为具有复杂且不可预测行为的水文地质系统,建模技术是评估岩溶含水层中地下水流量和污染物迁移的最有益,最有效的方法之一。因此,审查和评估了几种建模方法。此外,还讨论了在波多黎各北部开展的相关研究工作,以补充该岛目前正在进行的水文地质调查。在第二部分中,对农业,工业和城市发展导致的地下水硝酸盐污染进行了评估,以评估该岛的中北部地区。波多黎各。利用收集的田间样本和历史数据,使用MODFLOW和MT3D模型进行了硝酸盐的归宿和迁移模拟。区域尺度模拟的计算结果显示与观测值高度相关,因此,将校准的模型用于预测目的。利用土地覆盖数据并通过评估该岛的农业发展趋势,预测了未来二十年地下水硝酸盐浓度的时空格局。据预测,飓风玛丽亚遭受经济破坏后,农业活动将急剧增加,这将对地下水质量产生负面影响。根据模型预测结果,提出了每个城市的推荐管理计划,以供决策者和当局使用。

著录项

  • 作者

    Kalhor, Koosha.;

  • 作者单位

    Northeastern University.;

  • 授予单位 Northeastern University.;
  • 学科 Hydrologic sciences.;Environmental engineering.;Civil engineering.
  • 学位 M.S.
  • 年度 2017
  • 页码 94 p.
  • 总页数 94
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-17 11:38:55

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