首页> 外文OA文献 >Évolution de l'impact environnemental de lixiviats d'ordures ménagères sur les eaux superficielles et souterraines, approche hydrobiologique et hydrogéologique. Site d'étude : décharge d'Étueffont (Territoire de Belfort – France)
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Évolution de l'impact environnemental de lixiviats d'ordures ménagères sur les eaux superficielles et souterraines, approche hydrobiologique et hydrogéologique. Site d'étude : décharge d'Étueffont (Territoire de Belfort – France)

机译:生活垃圾渗滤液对地表水和地下水的环境影响的演变,水生生物和水文地质方法。研究地点:Étueffont垃圾填埋场(Territoire de Belfort-法国)

摘要

A multi approach study, using geophysics, tracing tests, water balance, geology, hydrogeology and statistics analyses on physico-chemicals data, shows (1) leachate's infiltrations between 31 and 43% accross a shaly natural interface and superior to 45% accross an artificial geomembrane interface and (2) a localized physico-chemical impact on the existing piezometer network. Collected leachates are treated by a natural lagooning system. After the suspension of waste deposits, biodegradation activity reduces and generates a decrease in leachates noxiousness, thus changing the lagoons hydrobiologic mechanisms. We note a diversification of all the microbial loop components allowing the re-use of the organic material. The new trophic pyramid organization allowed to attain a viable ecosystem for fish fauna, in the last lagoon. Treated leachates undergo a second purification by natural attenuation in the receiving stream. A bacteriological approach on leachates, lagoons and groundwater quality allowed to assess presence and survival of faecal bacteria in these various environments. This landfill doesn't represent an important source of faecal bacteria. This studied site, where landfill's leachates and septic tank sewage are mixed together, confirms the use of Escherichia coli and Entoroccocus as markers of recent faecal contaminations. The shaly aquifer resembles more in a fractured area than in an impervious zone, with a preferential circulation along cracks and fractures which doesn't assure the natural filtration and lead to a vulnerable aquifer to bacterial contaminations.
机译:使用地球物理学,示踪测试,水平衡,地质学,水文地质学和对物理化学数据进行统计分析的多方法研究显示:(1)泥质天然界面渗滤液渗透率介于31%至43%之间,人工渗滤液的渗透率高于45%土工膜界面和(2)对现有压力计网络的局部物理化学影响。收集的渗滤液通过天然泻湖系统处理。废物沉积物悬浮后,生物降解活性降低,浸出液毒性降低,从而改变了泻湖的水生生物学机制。我们注意到所有微生物环成分的多样化,允许有机材料的再利用。新的营养金字塔组织允许在最后一个泻湖中建立一个可行的鱼类生态系统。经过处理的渗滤液通过接收流中的自然衰减进行第二步提纯。对渗滤液,泻湖和地下水水质采取细菌学方法可以评估粪便细菌在这些不同环境中的存在和存活。该垃圾填埋场并不是粪便细菌的重要来源。该研究现场将垃圾填埋场的渗滤液和化粪池污水混合在一起,证实使用大肠杆菌和肠球菌作为近期粪便污染的标志。页岩含水层在裂缝区域比在不透水区域更像,沿裂缝和裂缝的优先循环,不能确保自然过滤并导致易受细菌污染的含水层。

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    Belle Emilien;

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  • 年度 2008
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