Pronk Michiel, Goldscheider Nico, Zopfi Jakob
Center of Hydrogeology, and Laboratory of Microbiology, Institute of Biology, University of Neuchâtel, Emile-Argand 11, 2009 Neuchâtel, Switzerland.
Environ Sci Technol. 2007 Dec 15;41(24):8400-5. doi: 10.1021/es071976f.
Continuous monitoring of particle-size distribution (PSD), total organic carbon (TOC), turbidity, discharge and physicochemical parameters, together with analyses of fecal indicator bacteria, particularly Escherichia coli, made it possible to better understand the processes governing pathogen transport in karst groundwater and to establish PSD as indicator for possible microbial contamination of drinking water from karst springs. In the study area near Yverdon-les-Bains, Switzerland, tracer tests proved connection between a sinking stream draining agricultural land and several springs, 4.8-6.3 km away. Tracing and monitoring results demonstrate that (i) suspended particles (turbidity) in the spring water either originate from remobilization of sediments inside the aquifer (autochthonous) or from the sinking stream and land surface (allochthonous); (ii) allochthonous turbidity coincides with increased E. coli and TOC levels; (iii) PSD makes it possible to distinguish the two types of turbidity; (iv) a relative increase of finer particles (0.9-10 microm) indicates allochthonous turbidity and thus possible fecal contamination. The method permits to optimize water treatment and identify periods when the spring water must be rejected. Findings from other test sites confirm the feasibility of this approach.
对粒径分布(PSD)、总有机碳(TOC)、浊度、流量和理化参数进行连续监测,同时对粪便指示菌,特别是大肠杆菌进行分析,有助于更好地理解岩溶地区地下水中病原体的传播过程,并将PSD确立为岩溶泉饮用水可能受到微生物污染的指标。在瑞士伊韦尔东莱班附近的研究区域,示踪试验证明了一条流经农田的下沉溪流与4.8 - 6.3公里外的几口泉之间存在联系。示踪和监测结果表明:(i)泉水中的悬浮颗粒(浊度)要么源自含水层内部沉积物的再悬浮(原地的),要么源自下沉溪流和地表(外来的);(ii)外来浊度与大肠杆菌和TOC水平的升高相吻合;(iii)PSD能够区分这两种浊度类型;(iv)细颗粒(0.9 - 10微米)相对增加表明存在外来浊度,进而可能存在粪便污染。该方法有助于优化水处理,并确定必须弃用泉水的时期。其他试验地点的研究结果证实了这种方法的可行性。