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801.
Use of antibiotics in medicine, farming and aquaculture results in a continual supply of these pharmaceuticals and their breakdown products reaching the environment. A method has been developed to use for screening environmental samples to establish whether they contain antibiotics. The assay is based on a commercially available test kit and uses some modifications of the test procedure and SPE techniques to deliver a fast, semi-quantifiable result. Development of the assay and results from spiked and environmental samples are discussed. 相似文献
802.
Bottled waters are an increasingly significant product in the human diet. In this work, we present a dataset of stable isotope ratios for bottled waters sampled in Greece. A total of 25 domestic brands of bottled still waters, collected on the Greek market in 2009, were analysed for δ18O and δ2H. The measured stable isotope ratios range from − 9.9‰ to − 6.9‰ for δ18O and from − 67.50‰ to − 46.5‰ for δ2H. Comparison of bottled water isotope ratios with natural spring water isotope ratios demonstrates that on average the isotopic composition of bottled water tends to be similar to the composition of naturally available local water sources, showing that bottled water isotope ratios preserve information about the water sources from which they were derived and suggesting that in many cases bottled water should not be considered as an isotopically distinct component of the human diet. This investigation also helped to determine the natural origin of bottled water, and to indicate differences between the natural and production processes. The production process may influence the isotopic composition of waters. No such modification was observed for sampled waters in this study. The isotopic methods applied can be used for the authentication of bottled waters and for use in the regulatory monitoring of water products. 相似文献
803.
l.IntroductionWaterPervadesallofthephysicalanddynamicstructureswithintheEarthclimatesys-temthroughamyriadofhydrologicalprocesses.Thehydrologicalcycleinfluencesclimateinavarietyofways,andthereexistsrobustwaterfluxexchangebetweenoceanandatmosphere(Zhouetal.,l999).Theexchangeoffreshwaterbetweenatmosphereandoceanthroughtheair-seainterfaceisoneoftheleastelementsunderstood,butnowisconsideredasoneofthemostimportantelementsoftheclimatesystem,esPeciallyforoceancirculationchangesondecadaltomillennialt… 相似文献
804.
J. Dowgiałło 《Environmental Geology》2000,39(5):433-436
To provide additional volume of thermal water for balneotherapy and space heating the well Cieplice-1 has been deepened from
661 m to 2002.5 m. A spontaneous outflow of water with temperatures reaching 87.8 °C was obtained. Thermal logging revealed
97.7 °C at 1870 m. These results are consistent with earlier estimates based on various chemical geothermometers that indicated
water temperatures in the lower parts of the geothermal system possibly exceeding 100 °C. This was also confirmed by the
cationic composition geothermometer. The estimates based on the dependence of saturation indices on temperature did not prove
correct, suggesting 65 °C as the most probable maximum temperature of the water.
Received: 11 Sebtember 1998 · Accepted: 7 January 1999 相似文献
805.
806.
807.
Seventy-six samples of formation waters were collected from oil wells producing from the Aux Vases or Cypress Formations in the Illinois Basin. Forty core samples of the reservoir rocks were also collected from the two formations. Analyses of the samples indicated that the total dissolved solids content (TDS) of the waters ranged from 43,300 to 151,400 mg/L, far exceeding the 35,400 mg/L of TDS found in typical seawater. Cl-Br relations suggested that high salinities in the Aux Vases and Cypress formation waters resulted from the evaporation of original seawater and subsequent mixing of the evaporated seawater with concentrated halite solutions. Mixing with the halite solutions increased Na and Cl concentrations and diluted the concentration of other ions in the formation waters. The elemental concentrations were influenced further by diagenetic reactions with silicate and carbonate minerals. Diagenetic signatures revealed by fluid chemistry and rock mineralogy delineated the water-rock interactions that took place in the Aux Vases and Cypress sandstones. Dissolution of K-feldspar released K into the solution, leading to the formation of authigenic illite and mixed-layered illite/smectite. Some Mg was removed from the solution by the formation of authigenic chlorite and dolomite. Dolomitization, calcite recrystallization, and contribution from clay minerals raised Sr levels significantly in the formation waters. The trend of increasing TDS of the saline formation waters with depth can be explained with density stratification. But, it is difficult to explain the combination of the increasing TDS and increasing Ca/Na ratio with depth without invoking the controversial 'ion filtration' mechanism. 相似文献
808.
809.
秦山核电站邻近水域浮游动物的群落结构和年际变化 总被引:2,自引:0,他引:2
描述了1995~1996年度秦山核电站邻近水域浮游动物的生物量、丰度、群落结构及其与环境因子的关系,并与1989~1990年度的资料进行了对比分析。结果表明,秦山核电Ⅰ期工程运行以来,对该水域浮游动物群落结构未产生明显的影响 相似文献
810.
东沙群岛西南海域单站潮流及温盐特征分析 总被引:1,自引:0,他引:1
利用东沙群岛西南海域定点站(20°41’N,115°49’E)3个航次观测的海流、水温资料及同期的温、盐度断面资料,用谱分析方法对该站海流、水温时间序列进行分析。结果表明,该站海流和水温的时间变化都具有明显的全日周期和半日周期波动的特征,潮流为不规则全日潮,主轴顺时针方向旋转。内潮为全日内潮占优,且具有间歇特征。和总流动类似,斜压运动也主要是顺时针方向旋转的。 相似文献