Trihalomethanes in Drinking Water of Greater Québec Region (Canada): Occurrence, Variations and Modelling

The levels of trihalomethanes (THMs) – the main species of by-product from water chlorination – were monitored in thedistribution systems of the five major drinking water utilitiesof the greater area of Québec City in order to investigate andmodel their occurrence on a spatial and seasonal basis. Data forTHMs and other water quality and operational parametersassociated with their formation were generated through a 16 monthsampling program involving several sites representing variablewater residence times, from the plant to the system extremity.The results demonstrate that the differences in measured THMlevels between the five utilities are mainly due to the variablequality of raw waters, the type of water treatment process beingused and the type and levels of applied disinfectant. Dependingon the utility, average THM levels were from 1.3 to 2.5 timeshigher in the system extremities than in the water leaving thetreatment plant. Also, average levels of THMs measured in summerat the distribution system extremities were, depending on theutility, from 2.5 to 5 times higher than the average levelsmeasured in winter. The seasonal differences were found to besignificantly greater than those observed by others in waterutilities in the United States and Europe and are explained inlarge part by the considerable changes, over the year, in thequality and temperature of surface waters in Southern Québec. Forthe five utilities under study, multivariate regression modelswere developed in order to predict spatial and seasonalvariations of THMs. Both residual chlorine demand and temperaturewere found to be better, statistically, as predictors for THMoccurrence. The usefulness of the developed models for routineand long term water quality management, as well as for assessmentof human exposure to THMs, are also discussed.     

Breccias of the Adnet Formation: indicators of a Mid-Liassic tectonic event in the Northern Calcareous Alps (Salzburg/Austria)

Stratigraphy, lithology and depositional structures of Liassic red limestone-breccias of the Adnet Formation, including the 'Adnet Scheck', were studied at several outcrops of the Northern Calcareous Alps (NCA) south-east of Salzburg. A four-fold lithostratigraphic division is proposed for the Adnet Formation of the Osterhorn Mountains: the hemipelagic Schmiedwirt (Sinemurian) and Kehlbach (Carixian) members are separated from the pelagic Saubach Member (Toarcian) by a layer of amalgamated breccias (Scheck Member, probably Domerian to early Toarcian). Several other breccia beds occur locally from the base of the Kehlbach Member up to the lower Saubach Member. Although the sediments overlying the Scheck Member breccias are of coeval age, the ages of the underlying strata are very different. This can be explained by submarine Liassic erosion during a period of resedimentation from the middle Carixian until the early Toarcian. At least 10–15?m of partly lithified sediments were eroded by gravity flows. The entire Kehlbach Member and up to two-thirds of the Schmiedwirt Member were removed at Adnet. The breccias originated from submarine debris flows. Repeated flows over a long period and the depositional setting exclude a triggering by sea-level fluctuations. Most probably they arose from tectonically triggered slumps and slides of superficial sediments. The 'Scheck' was initiated on the steep upper slope of the drowned Triassic Adnet reef and flowed to the north-east.The Pliensbachian to early Toarcian period of tectonic activity indicated by the breccias was the most important during the Liassic in the Osterhorn Mountains and other parts of the NCA. From the large-scale regional distribution of the breccias and in accord with published data, a roughly north-east trending strike-slip fault zone is proposed, crossing the NCA south of the Osterhorn block, with a peaking activity during the Pliensbachian to early Toarcian as the cause of the tectonic movements.     

Die Membratimreaktion als Methode zur Feststellung von Verbindungsbildungen

The Science of Nature -     

14C标记的月桂酸盐在淡水勾虾（Hyalella azteca）中的生物富集、代谢及空间分布

对水的生物蓄积性监管评估通常是基于鱼类流水暴露试验得出生物浓缩因子（BCF）。这样的实验需要很多实验动物,而且费时费钱。最近,有人提出了一种替代性的有机中性化合物的测试方法,即用勾虾（Hyalella azteca）进行测试得到BCF值,该值与鱼类 BCF值有很强的相关性。本文研究了离子化合物月桂酸盐在H. azteca中的生物浓缩潜力。 采用流动和半静态的方法对勾虾H. azteca进行1-14C-月桂酸钠暴露实验。由于该化合物的生物降解速度快,需要采用半静态方法,即频繁更换介质,以确保介质浓度稳定。月桂酸盐也可被H. azteca快速代谢。在勾虾组织中测得的总放射性中有很大一部分是不能提取的,这表明矿化月桂酸盐富集在H. azteca的钙化外骨骼中。这在使用14C标记的碳酸盐的进一步研究中得到了证实。以游离脂肪酸计量,月桂酸盐的脂质标准化（5.0%）的勾虾 BCF为8.9。H. azteca的生物浓缩研究结果证实了先前在鱼类中观察到的试验项目的低生物富集潜力。然而,需要测试更多的具有不同性质的有机离子化合物,以评估鱼和勾虾的BCF数据之间是否存在一般相关性。