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481.
重金属在牡蛎(Crassostrea virginica)中的生物积累及其影响因素的研究 总被引:11,自引:0,他引:11
牡蛎软体,贝壳和沉积物中Cd、Cr、Cu、Fe、Mn、Pb和Zn等重金属元素被同步分析研究,研究结果表明,重金属在牡蛎中的生物积累是牡自身的新陈代谢、重金属元素的地球化学性质和环境诸因素综合影响的结果,其中牡蛎斩生理作用对重金属在软体中的积累产生的影响尤为重要,而贝壳中重金属的积累对来自环境的影响更为敏感。 相似文献
482.
介绍了放射性废物微波真空干燥处理器的微波漏能现状及所采取的防护措施。监测结果表明,经过防护,有效地减弱了设备的微波漏能,达到了国家防护标准。 相似文献
483.
采用色谱技术,对二步法腈纶生产废水中所含的有机污染物,进行了系统的分析研究.结果表明,二步法腈纶废水的可生化性极差,其BOD5/CODcr的比值在0.1~0.2之间.其中所含有机污染物主要有芳香族及酚类的2,6-二(1,1-二甲基乙基)酚、硫代邻氨基苯酚、苯甲酸苄酯、邻二甲苯;腈类的丙烯腈、丁二腈、戊腈、己腈、β,β'-亚氨基二丙腈;烷烃类的壬烷异构体、十二烷及其异构体、十三烷及其异构体、十五烷及其异构体、十六烷;其它有N,N-二甲基乙酰胺、2,2'-二硫基乙醇、硫醇(丙硫醇、乙硫醇)、丙烯酸甲酯、甲基丙烯磺酸钠等. 相似文献
484.
沼泽红假单胞菌H3对酸性红B2GL染料的厌氧脱色和降解作用 总被引:7,自引:0,他引:7
从印染厂污泥中分离到一株沼泽红假单胞菌(RhodopseudomonaspalustrisH3),在光照厌氧条件下该菌生长细胞可将100mg/L酸性红B2GL染料去除到30mg/L.完整细胞脱色的最适条件为pH70,温度30℃,细胞浓度20—25mg/mL(湿重).低浓度的阳离子对脱色影响不大.在通Ar气使严格厌氧和加有还原性辅酶I的条件下无细胞提取液的脱色活性最高,比活率为154×10-2mg/(mg·h).根据降解产物的分析,推断了该菌对酸性红染料的降解代谢途径. 相似文献
485.
486.
砖瓦厂含氟废气的治理 总被引:3,自引:0,他引:3
通过实验选取了一种固氟剂添加到砖坯中后,砖块的存氟率为910%,烟道气总氟排放降低率为7678%。连续五年的生物检测试验,没有发生任何家蚕氟中毒现象。固氟剂的应用为砖厂含氟废气的治理提供了一条新的途径 相似文献
487.
在SR污水土地处理系统工艺设计中,处理场地的环境特征、限制性设计参数、作物选型及预处理方式的选择等决定了该系统运动的成败,应合理分析各必备要素以指导设计中参数的选择,达到污水处理与资源化的有机结合。 相似文献
488.
The groundwater regime in Upper Palar basin, Tamilnadu has been highly contaminated in several locations due to discharge of effluents from a large number of tanneries. At some places total dissolved solids (TDS) concentration in groundwater was found as high as 8000 mg/l. Transmissivity and storativity of the regional aquifer were estimated at a few locations. The porosity and dispersivity values were not determined in the field. These parameters were assumed based on data available for similar geological formations elsewhere. The aquifer conceptualization thus arrived at formed the basis of a numerical groundwater flow model which was constructed using the finite difference method. The flow model was calibrated for steady state and then for transient condition for the period of 1984-92. The computed heads and calibrated parameters of the flow model were used to compute groundwater velocities. The migration of contaminants for a 20 year period was computed using the hydraulic heads and effective porosity value in a pathline model using FLOWPATH software. Mass transport model was constructed using Method of Characteristics (MOC) computer code in a separate model. The seepage rate of effluent is assumed at a rate of 30% of that discharged on the surface. The mass concentration of solute in the effluent reaching the water table was assumed as 40%, the same as in the surface effluent. The mass transport model was calibrated for a 20 year period. Prediction of contaminant migration from different clusters in the basin was analyzed. The prediction results indicated elevated TDS concentration of more than 4000 mg/l from most clusters. Also the area of the contaminated zone is likely to double in 20 years from contaminated zone of 1992. 相似文献
489.
490.
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. 相似文献