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411.
412.
综合考虑太阳因素、地形因素、地表积雪覆盖情况、云量以及非均质大气对太阳辐射的影响,基于FY2 号静止卫星构建晴空太阳总辐射计算模型,并利用山西省3 个辐射观测站2011 年逐时、逐日、逐月太阳总辐射观测资料对其估算结果进行检验。研究结果显示:逐时误差在±1 MJ·m-2之间,逐日误差在±5 MJ·m-2之间,表明模型计算的太阳辐射误差较小,稳定性较好;逐月误差结果显示,三个站模拟值都大于实测值,且误差趋势一致,均表现为冬季误差高于夏季;进一步对模拟值和实测值进行相关性分析,三站线性拟合度均在0.86~0.92 之间,且相关系数均达到显著相关水平,表明模型计算的太阳辐射准确性和精度较高,且在数值拟合上较好地反映了实际的太阳总辐射量,证实该模型应用于FY2 号气象卫星的可行性。 相似文献
413.
活性污泥絮体的分形结构分析 总被引:1,自引:1,他引:0
通过小角光散射(small-angle light scattering,SALS)实验确定出活性污泥絮体的分形区域,对絮体粒径分布进行了拟合分析,采用原子力显微镜(AFM)和激光共聚焦扫描显微镜(CLSM)对絮体在不同尺度下的形貌进行了观测.结果显示,污泥絮体是由一系列的絮团结合而成,絮体表面凹凸不平,有各种"孔洞","缝隙",絮体内部存在一系列的孔隙.较大尺度的絮体同时存在多种孔道结构,构成絮体中营养物和水流的运输通道;污泥絮体在0.5~50μm之间具有明显的分形结构,表明活性污泥絮体在较小的粒径时已经具有一定的分形特征,活性污泥的粒度分布属于Gamma分布方式,证明污泥絮体的成长过程是一种絮团-絮团的凝聚过程. 相似文献
414.
有序介孔碳载金/L-赖氨酸/纳米金修饰电极的制备及其对邻苯二酚、对苯二酚的检测响应研究 总被引:1,自引:1,他引:0
通过化学还原的方法合成有序介孔碳负载纳米金粒子,并构筑有序介孔碳载金/L-赖氨酸/纳米金复合膜修饰玻碳电极;利用扫描电镜观察介孔碳和介孔碳复合膜的微观结构,并用循环伏安法、电化学阻抗谱表征自组装电极的过程.在此基础上用差分脉冲伏安法研究对苯二酚和邻苯二酚混合物在该电极上的电催化氧化,研制了一种基于有序介孔碳载金/L-赖氨酸/纳米金复合膜修饰电极分别检测对苯二酚和邻苯二酚的传感器.在最优的实验条件下,该传感器在对苯二酚和邻苯二酚浓度为1×10-6~8×10-4mol·L-1的范围内具有良好的线性关系,检出限分别为3×10-7mol·L-1、7×10-7mol·L-1. 相似文献
415.
研究了pH 4.0的水溶液中各种金属离子对合成的δ-MnO2去除对叔辛基酚(4-t-OP)的影响.实验表明反应150 min时,δ-MnO2对4-t-OP的去除率达到100%,但当反应体系中含有金属离子时,去除效果受到抑制.抑制效果随金属离子浓度的增加而增大,并随金属离子的不同表现出较大的差异.在pH 4.0条件下,Pb2+和Mn2+的抑制效果最强,其次为过渡金属离子,再次是碱土金属离子,而碱金属离子基本上不产生抑制作用.还比较了δ-MnO2对多种金属离子的吸附能力,其对Pb2+的吸附作用最强,在其余的金属离子中,对过渡金属离子的吸附量稍大于碱土金属离子.结果表明,金属离子所产生抑制作用的源于其占据了δ-MnO2表面反应位点并与4-t-OP形成竞争,而抑制作用大小的差异主要来源于δ-MnO2与金属离子间吸附作用强弱的差别,MnO2表面结构的变化,以及溶液中自由态金属离子的分布比例及其离子半径的不同. 相似文献
416.
UV和H2 O2联合消毒灭活饮用水中大肠杆菌研究 总被引:1,自引:1,他引:0
以大肠杆菌为研究对象,对单独紫外线(UV)、H2O2及两者不同组合方式的灭活效果进行了分析.结果表明,单独H2O2对大肠杆菌基本无灭活效果,加入浓度为20 mg·L-1的H2O2接触时间为30 min时,灭活率仅为0.02个对数级;单独UV工艺可在一定程度上灭活大肠杆菌,紫外线剂量为10 mJ·cm-2时,灭活率可达到4.51个对数级.紫外线和H2O2联合消毒在一定程度上提高了消毒效果,且不同的组合方式对灭活效果有很大的影响.先UV后H2O2消毒效果优于先H2O2后UV,当紫外线剂量为5 mJ·cm-2时,加入H2O2分别反应2.5、5、10、20 min后,两者的灭活率分别较单独UV消毒增加0.09、0.35、0.38、0.68和0.01、0.07、0.14、0.53个对数级.而UV与H2O2同时消毒效果优于UV与H2O2顺序消毒,当紫外线剂量为5 mJ·cm-2时,加入H2O2反应20 min后,灭活率较UV-H2O2和H2O2-UV工艺分别增加了0.43和0.58个对数级.随着紫外线强度的增加,大肠杆菌的灭活效果不断提高. 相似文献
417.
Bacterial strain Enterobacter aerogenes TJ-D capable of utilizing 2-methylquinoline as the sole carbon and energy source was isolated from acclimated activated sludge under denitrifying conditions. The ability to degrade 2-methylquinoline by E. aerogenes TJ-D was investigated under denitrifying conditions. Under optimal conditions of temperature (35℃) and initial pH 7, 2-methylquinoline of 100 mg/L was degraded within 176 hr. The degradation of 2-methylquinoline by E. aerogenes TJ-D could be well described by the Haldane model (R2 > 0.91). During the degradation period of 2-methylquinoline (initial concentration 100 mg/L), nitrate was almost completely consumed (the removal efficiency was 98.5%), while nitrite remained at low concentration (< 0.62 mg/L) during the whole denitrification period. 1,2,3,4-Tetrahydro-2-methylquinoline, 4-ethyl-benzenamine, N-butyl-benzenamine, N-ethyl-benzenamine and 2,6-diethyl-benzenamine were metabolites produced during the degradation. The degradation pathway of 2-methylquinoline by E. aerogenes TJ-D was proposed. 2-Methylquinoline is initially hydroxylated at C-4 to form 2-methyl-4-hydroxy-quinoline, and then forms 2-methyl-4-quinolinol as a result of tautomerism. Hydrogenation of the heterocyclic ring at positions 2 and 3 produces 2,3-dihydro-2-methyl-4-quinolinol. The carbon-carbon bond at position 2 and 3 in the heterocyclic ring may cleave and form 2-ethyl-N-ethyl-benzenamine. Tautomerism may result in the formation of 2,6-diethyl-benzenamine and N-butyl-benzenamine. 4-Ethyl-benzenamine and N-ethyl-benzenamine were produced as a result of losing one ethyl group from the above molecules. 相似文献
418.
419.
The adsorption behavior of 2-mercaptobenzothiazole onto organo-bentonite was investigated.Natural bentonite from Gaozhou in Guangdong Province,China was collected.Organo-bentonite was prepared by intercalation of cetyltrimethyl ammonium bromide into the natural bentonite.The physicochemical properties of the prepared organo-bentonite were characterized by X-ray diffraction,N2 adsorption-desorption isotherm and Fourier transform infrared spectroscopy.The results showed that montmorillonite is the main component of the natural bentonite.The basal spacing of the natural bentonite is 1.47 nm,which increased to 1.98 nm on intercalation with cetyltrimethyl ammonium bromide.Moreover,both the surface area and pore volume increased with intercalation.Clear CH2 stretching(3000-2800 cm-1) and scissoring(1480-1450 cm-1) modes of the intercalated surfactants were observed for organobentonite.Compared with the pseudo first-order kinetic model,the pseudo second-order kinetic model is more suitable to describe the adsorption kinetics of 2-mercaptobenzothiazole onto organo-bentonite.The adsorption capacity of 2-mercaptobenzothiazole onto organo-bentonite increased with increasing initial concentration of 2-mercaptobenzothiazole,but decreased with increasing adsorbent dosage.The adsorption isotherm of 2-mercaptobenzothiazole onto organo-bentonite fits well with the Langmuir model.The maximum adsorption capacity of organo-bentonite for 2-mercaptobenzothiazole was 33.61 mg/g,indicating that organo-bentonite is a promising adsorbent for 2-mercaptobenzothiazole. 相似文献
420.
Effects of physical and chemical characteristics of surface sediments in the formation of shallow lake algae-induced black bloom 总被引:12,自引:0,他引:12
Qiushi Shen Cheng Liu Qilin Zhou Jingge Shang Lei Zhang ChengXin Fan 《环境科学学报(英文版)》2013,25(12):2353-2360
Surface sediments are closely related to lake black blooms. The dissolved oxygen (DO) distribution and its penetration depth in surface sediments as well as the migration and transformation of redox sensitive elements such as Fe and S at the sediment-water interface are important factors that could influence the formation of the black bloom. In this study, dredged and undredged sediment cores with different surface properties were used to simulate black blooms in the laboratory. The Micro Profiling System was employed to explore features of the DO and ∑H2S distribution at the sediment-water interface. Physical and chemical characteristics in sediments and pore waters were also analyzed. The results showed that sediment dredging effectively suppressed the black blooms. In the undredged treatment, DO penetration depth was only 50 μm. Fe^2+ concentrations, ∑H2S concentrations, and ∑H2S production rates were remarkably higher in surface sediments and pore waters compared to control and dredged treatments. Furthermore, depletion of DO and accumulation of Fe^2+ and ∑H2S in surface sediments and pore waters provided favorable redox environments and necessary material sources for the blooms. The study results proved that physical and chemical characteristics in surface sediments are important factors in the formation of the black bloom, and could provide scientific guidance for emergency treatment and long-term pre-control of black blooms. 相似文献