首页> 外文期刊>The Science of the Total Environment >Tracing water perturbation using NO_3~- , doc, particles size determination, and bacteria: A method development for karst aquifer water quality hazard assessment
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Tracing water perturbation using NO_3~- , doc, particles size determination, and bacteria: A method development for karst aquifer water quality hazard assessment

机译:使用NO_3〜 - ,DOC,粒子尺寸测定和细菌的追踪水扰动:喀斯特含水层水质危害评估的方法开发

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摘要

Karst systems, as well as springs, are vulnerable to water perturbation brought by infiltration. In this research, sources of water perturbations were examined. The first objective is to provide a method that can determine the origin of the water flowing in the karst outlet. The second objective is to identify the associated water quality hazards caused by the infiltration source. The method relies on these parameters: turbidity, DOC, NO_3~-, particle size, and bacteria (E. coli, enterococcus and total coliforms). As the method was applied during flood events, measurement of the water flow is also needed to have a basic knowledge on the hydrodynamic of the water resource. The proposed method is based on a high resolution monitoring of physico chemical parameters of the water flowing during flood events. Using this proposed method. (1) the origin of the water can be identified, (2) the type and nature of water perturbation can be described, and (3) the type of water perturbation that accompanies contaminants such as the one with anthropogenic source (e.g. NO_3~-) and bacterial nature can be determined. In identifying the water origin, this proposed method employed NO_3~- and DOC data normalization. Values are projected in the NO_3~-_norm = f(DOC_norm) reference frame. These are aligned to the slope. Depending on the obtained slope (α), water origin can be disclosed. If α > 1, the increase of concentration of DOC weighs more, characterizing water from surface runoff. Whereas, if α < 1, the consideration is more on the increase of NO_3 concentration, characterizing water from unsaturated zone. However if a cannot be calculated because there is no evident slope, this characterizes the water already present in the system. Water originating from the surface runoff is prone to inorganic and bacterial contamination adsorbed by the particles. Identifying the type of water perturbation needing water treatment is important in managing the water resource. Hence, the evolution through time of NO_3~- and DOC with the particle size distribution, anthropogenic nature type of contaminant (i.e. in this study NO_3~- ). and presence or absence of bacteria were examined. This method was applied in the springs of the Toulon, an important drinking water source of the city of Perigueux in France. This site was chosen considering the following factors: (1) its karst nature being vulnerable to infiltrations, having fractures and sinkholes; (2) its land use being influenced by the anthropogenic activities such as agriculture; and (3) its observed pronounced turbidity incidence. The first flood events of two hydrological cycles were assessed. Three water origins of the spring water and the respective water quality hazards were identified: (ⅰ) water from saturated zone with minerals, (ⅱ) water from unsaturated zone with nitrate, and (ⅲ) water from surface runoff with the presence of bacteria. The second and third types of water perturbation gave evidence that the Toulon springs can be contaminated. Hence, in terms of resource management, the information obtained can be used as a basis in forecasting and planning the management actions or water quality treatments needed.
机译:喀斯特系统以及Springs,易受渗透带来的水扰动。在这项研究中,检查了水扰动的来源。第一目标是提供一种方法,可以确定在岩溶出口中流动的水的起源。第二个目的是识别由渗透源引起的相关水质危害。该方法依赖于这些参数:浊度,DOC,NO_3〜 - ,粒径和细菌(大肠杆菌,肠球菌和总大肠杆菌)。随着该方法的应用在洪水事件期间,还需要测量水流的基本知识,用于水资源的流体动力学。该方法基于在洪水事件期间流动的水的物理化学参数的高分辨率监测。使用这种提出的方​​法。 (1)可以鉴定水的起源,(2)可以描述水扰动的类型和性质,并伴随着用人为源(例如NO_3〜 - )伴随污染物的水扰动类型(例如NO_3〜 - )可以确定细菌性质。在识别出水来源时,这种提出的方​​法使用NO_3〜 - 和DOC数据归一化。值在No_3〜-_norm = f(doc_norm)参考帧中投影。这些与斜坡对齐。取决于所获得的斜率(α),可以公开水来源。如果α> 1,则DOC浓度的增加重量更多,从表面径流中表征水。然而,如果α<1,则考虑更多关于NO_3浓度的增加,从不饱和区表征水。然而,如果不能计算A因为没有明显的斜率,则这表征了已经存在于系统中的水。来自表面径流的水易于被颗粒吸附的无机和细菌污染。确定需要水处理的水扰动类型对于管理水资源是重要的。因此,通过NO_3〜 - 和DOC的时间的演化与粒度分布,人为自然类型的污染物(即本研究NO_3〜 - )。检查和存在或不存在细菌。该方法应用于土城的泉水,是法国佩里格市的重要饮用水来源。选择以下因素选择本网站:(1)其喀斯特性质易受渗透,具有骨折和污水孔; (2)其土地使用受农业等人类活动的影响; (3)其观察到的明显浊度发生。评估了两个水文循环的第一次洪水事件。泉水和各自的水质危害的三个水起源是:(Ⅰ)来自饱和区的水,(Ⅱ)从不饱和区与硝酸盐的水,(Ⅲ)水从表面径流存在细菌。第二种和第三类水扰动给出了证据表明塔隆弹簧可以被污染。因此,在资源管理方面,所获得的信息可以用作预测和规划所需的管理行动或水质处理的基础。

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