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991.
采用苯萃取,HP-624 30 m×0.53 mm×3.00 μm大口径毛细管柱分离,电子捕获检测器(ECD)检测2,4-二硝基氯苯,得到了良好的分离效果、较宽的线性关系和较高的灵敏度. 相似文献
992.
993.
A Triassic sandstone aquifer polluted with a mixture of phenolic hydrocarbons has been investigated by means of high-resolution groundwater sampling. Samples taken at depth intervals of 1 m have revealed the presence of a diving pollutant plume with a sharply defined upper margin. Concentrations of pollutant phenols exceed 4 g/l in the plume core, rendering it sterile but towards the diluted upper margin evidence for bacterial sulphate reduction (BSR) has been obtained. Groundwaters have been analysed for both delta34S-SO4 and delta18O-SO4. Two reservoirs have been identified with distinct sulphate oxygen isotope ratios. Groundwater sulphate (delta18O-SO4 = 3-5/1000) outside the plume shows a simple linear mixing trend with an isotopically uniform pollutant sulphate reservoir (delta18O-SO4 = 10-12/1000) across the plume margin. The sulphur isotope ratios do not always obey a simple mixing relation, however, at one multilevel borehole, enrichment in 34SO4 at the plume margin is inversely correlated with sulphate concentration. This and the presence of 34S-depleted dissolved sulphide indicate that enrichment in 34SO4 is the result of bacterial sulphate reduction. Delta34S analysis of trace hydrogen sulphide within the plume yielded an isotope enrichment factor (epsilon) of -9.4/1000 for present-day bacterial sulphate reduction. This value agrees with a long-term estimate (-9.9/1000) obtained from a Rayleigh model of the sulphate reduction process. The model was also used to obtain an estimate of the pre-reduction sulphate concentration profile with depth. The difference between this and the present-day profiles then gave a mass balance for sulphate consumption. The organic carbon mineralisation that would account for this sulphate loss is shown to represent only 0.1/1000 of the phenol concentration in this region of the plume. Hence, the contribution of bacterial sulphate reduction to biodegradation has thus far been small. The highest total phenolic concentration (TPC) at which there is sulphur isotope evidence of bacterial sulphate reduction is 2000 mg/l. We suggest that above this concentration, the bactericidal properties of phenol render sulphate-reducing bacteria inactive. Dissolved sulphate trapped in the concentrated plume core will only be utilised by sulphate reducers when toxic phenols in the plume are diluted by dispersion during migration. 相似文献
994.
995.
固定源废气监测工作若干技术问题的探讨 总被引:5,自引:0,他引:5
从监测工况、测点位置、采样过程、结果计算等几方面出发,结合实际经验,对大气固定污染源的监测工作中存在的一些疑难问题进行探讨。 相似文献
996.
997.
对锅炉烟气处理工艺进行了改造,运行结果表明,改造后的处理效果明显提高,解决了烟尘及SO2排放浓度的超标问题,实现了达标排放。 相似文献
998.
Dale R. Van Stempvoort James Armstrong Bernhard Mayer 《Journal of contaminant hydrology》2007,92(3-4):184-207
Despite a rapid expansion over the past decade in the reliance on intrinsic bioremediation to remediate petroleum hydrocarbon plumes in groundwater, significant research gaps remain. Although it has been demonstrated that bacterial sulfate reduction can be a key electron accepting process in many petroleum plumes, little is known about the rate of this reduction process in plumes derived from crude oil and gas condensates at cold-climate sites (mean temperature <10 degrees C), and in complex hydrogeological settings such as silt/clay aquitards. In this field study, sulfate was injected into groundwater contaminated by gas condensate plumes at two petroleum sites in Alberta, Canada to enhance in-situ bioremediation. In both cases the groundwater near the water table had low temperature (6-9 degrees C). Monitoring data had provided strong evidence that bacterial sulfate reduction was a key terminal electron accepting process (TEAP) in the natural attenuation of dissolved hydrocarbons at these sites. At each site, water with approximately 2000 mg/L sulfate and a bromide tracer was injected into a low-sulfate zone within a condensate-contaminant plume. Monitoring data collected over several months yielded conservative estimates for sulfate reduction rates based on zero-order kinetics (4-6 mg/L per day) or first-order kinetics (0.003 and 0.01 day(-1)). These results favor the applicability of in-situ bioremediation techniques in this region, under natural conditions or with enhancement via sulfate injection. 相似文献
999.
通过富集不同来源堆肥过程中的腐殖质还原菌,并分析比较其异化铁还原能力差异,发现其电子转移能力从大到小依次为:蛋白类>纤维素类>木质素类.相关性分析表明,Leucobacter、Clostridium sensu stricto和Sporosarcina是极显著影响异化铁还原的腐殖质还原菌属.利用冗余分析探究关键腐殖质还原菌与堆肥过程微环境因子的响应关系,结果发现可溶性有机氮是影响这些关键腐殖质还原菌变化的主要微环境因素.在此基础上,基于堆肥微环境因子与关键腐殖质还原菌菌群结构之间的响应关系,提出一种促进异化铁还原相关的腐殖质还原菌生长的调控方法.本研究可以深入了解堆肥中影响腐殖质还原菌群落的关键因素,而且对于环境中污染物生物地球化学循环也具有重要的生态学意义. 相似文献
1000.
以双氯芬酸为目标有机药物污染物,探究其在以锰矿石为填料并接种了异化金属还原菌(Geobactermetallireducens,简称GS-15细菌)的垂直流人工湿地中的去除过程.结果表明,双氯芬酸在锰矿石人工湿地中的平均去除率最高为23.56%.采用XRD和XRF对反应前后的锰矿石进行物相和元素相对含量分析,得出锰(Mn)是参与降解双氯芬酸的关键响应元素.GS-15细菌利用锰矿石发生异化还原对双氯芬酸的氧化降解是锰矿石人工湿地对双氯芬酸的主要去除途径.此外,利用液质联用技术(LC-MS/MS)对降解产物进行鉴定,发现双氯芬酸被降解生成了5-羟基双氯芬酸、双氯芬酸-2,5-亚氨基琨和1,3-二氯苯三种降解产物,该研究成果对有机药物废水的深度处理提供新的方法和理论指导. 相似文献