The thermal decomposition process ofjarosite residue and the solubility of various oxides presented in the decomposed residue in NH4C1-H20 system were studied. The results of heat decomposition ofjarosite residue show...The thermal decomposition process ofjarosite residue and the solubility of various oxides presented in the decomposed residue in NH4C1-H20 system were studied. The results of heat decomposition ofjarosite residue show that the insoluble ZnFe2O4 phase in the residue can be decomposed at temperatures ranging from 500 ℃ to 650 ℃ for 1 h. The OLI Systems software was used to study the thermodynamics of the solubility of various metal oxides existing in the decomposed residue in NH4CI-H20 system. The results show that the solubility ofZnO, PbO, CdO, CuO and Ag20 is high, while the solubility of Fe203 is less than 10-4 mol/L in the pH range from 4.0 to 9.0. The calculated data are in accordance with the experimental results.展开更多
The interaction of poly(ethylene oxide)(PEO)with the ionic surfactants,sodium dodecylsulfate(SDS)and cetyltrimethylammonium chloride(CTAC)respectively,in aqueous solutions containing a certain concentration of NH_4Cl,...The interaction of poly(ethylene oxide)(PEO)with the ionic surfactants,sodium dodecylsulfate(SDS)and cetyltrimethylammonium chloride(CTAC)respectively,in aqueous solutions containing a certain concentration of NH_4Cl, is studied by the viscosity measurement.It has been found that the ion-dipole interaction between PEO and ionic surfactants is changed considerably by the organic salt.For anionic suffactant of SDS,the addition of NH_4Cl into solution strengthens the interaction between PEO and the headgroup o...展开更多
Influence of NH_4 Cl on the initial atmospheric corrosion of zinc was investigated viaquartz crystal microbalance (QCM) in laboratory at 80%RH and 25℃. The resultsshow that NH_4 Cl can accelerate the initial corrosio...Influence of NH_4 Cl on the initial atmospheric corrosion of zinc was investigated viaquartz crystal microbalance (QCM) in laboratory at 80%RH and 25℃. The resultsshow that NH_4 Cl can accelerate the initial corrosion of zinc. Mass gain increase withthe exposure time, but mass gain in the later doesn't change obviously due to theformation of the insoluble simonkolleite on zinc surface in the presence of NH_4 Cl.Fourier transform infrared spectroscopy (FTIR) and X-ray diffraction (XRD) wasused to characterize the corrosion products. Zn_5Cl_2(OH)_8·H_2O,(NH_4)_2ZnCl_4 andZnO are the corrosion products on zinc. Brief discussion on the mechanisms of at-mospheric corrosion of zinc in the presence of NH_4 Cl was introduced.展开更多
【目的】研究不同温度条件下的石油烃降解产甲烷菌系中是否存在乙酸互营氧化产甲烷代谢途径。【方法】以3个不同温度条件的正十六烷烃降解产甲烷菌系Y15(15℃)、M82(35℃)和SK(55℃)作为接种物,通过乙酸喂养实验、并添加乙酸营养型产甲...【目的】研究不同温度条件下的石油烃降解产甲烷菌系中是否存在乙酸互营氧化产甲烷代谢途径。【方法】以3个不同温度条件的正十六烷烃降解产甲烷菌系Y15(15℃)、M82(35℃)和SK(55℃)作为接种物,通过乙酸喂养实验、并添加乙酸营养型产甲烷古菌的选择性抑制剂NH4Cl和CH3F,结合末端限制性片段长度多态性(terminal restriction fragment length polymorphism,T-RFLP)和克隆文库技术,分析乙酸产甲烷潜力及产甲烷古菌群落的演替趋势,推测产甲烷代谢途径的变化趋势。【结果】无论是否添加NH4Cl和CH3F,这3个菌系都可以利用乙酸生长并产生甲烷,但是添加NH4Cl和CH3F后产甲烷延滞期增加,最大比甲烷增长速率降低;只添加乙酸后,3个不同温度的菌系的古菌群落主要由乙酸营养型产甲烷古菌甲烷鬃毛菌属(Methanosaeta)组成,其丰度分别为92.8±1.4%、97.3±2.4%和82.8±9.0%;当添加选择性抑制剂NH4Cl,3个菌系中的Methanosaeta的丰度分别变为98.5±0.7%、87.4±4.8%和6.1±8.6%,中温菌系M82中氢营养型产甲烷古菌甲烷袋装菌属(Methanoculleus)的相对丰度增加到12.6±4.0%,高温菌系SK中另一类氢营养型产甲烷古菌甲烷热杆菌属(Methanothermobacter)增至84.3±1.5%;当添加选择性抑制剂CH3F,Methanosaeta丰度分别降至77.1±14.5%,86.4±6.1%和35.8±7.8%,低温菌系Y15中的甲烷八叠球菌属(Methanosarcina)增高(15.7±21%),这类产甲烷古菌具有多种产甲烷代谢途径,M82中Methanoculleus丰度上升到13.6±13.1%,SK中Methanothermobacter丰度增大到48.5±11.2%。【结论】在低温条件下,菌系Y15可能主要通过乙酸裂解完成产甲烷代谢,在中高温条件下,菌系M82和SK中可能存在乙酸互营氧化产甲烷代谢途径,并且甲烷的产生分别通过不同种群的氢营养型产甲烷古菌来完成。展开更多
基金Project(51090385) supported by the National Natural Science Foundation of China
文摘The thermal decomposition process ofjarosite residue and the solubility of various oxides presented in the decomposed residue in NH4C1-H20 system were studied. The results of heat decomposition ofjarosite residue show that the insoluble ZnFe2O4 phase in the residue can be decomposed at temperatures ranging from 500 ℃ to 650 ℃ for 1 h. The OLI Systems software was used to study the thermodynamics of the solubility of various metal oxides existing in the decomposed residue in NH4CI-H20 system. The results show that the solubility ofZnO, PbO, CdO, CuO and Ag20 is high, while the solubility of Fe203 is less than 10-4 mol/L in the pH range from 4.0 to 9.0. The calculated data are in accordance with the experimental results.
文摘The interaction of poly(ethylene oxide)(PEO)with the ionic surfactants,sodium dodecylsulfate(SDS)and cetyltrimethylammonium chloride(CTAC)respectively,in aqueous solutions containing a certain concentration of NH_4Cl, is studied by the viscosity measurement.It has been found that the ion-dipole interaction between PEO and ionic surfactants is changed considerably by the organic salt.For anionic suffactant of SDS,the addition of NH_4Cl into solution strengthens the interaction between PEO and the headgroup o...
文摘Influence of NH_4 Cl on the initial atmospheric corrosion of zinc was investigated viaquartz crystal microbalance (QCM) in laboratory at 80%RH and 25℃. The resultsshow that NH_4 Cl can accelerate the initial corrosion of zinc. Mass gain increase withthe exposure time, but mass gain in the later doesn't change obviously due to theformation of the insoluble simonkolleite on zinc surface in the presence of NH_4 Cl.Fourier transform infrared spectroscopy (FTIR) and X-ray diffraction (XRD) wasused to characterize the corrosion products. Zn_5Cl_2(OH)_8·H_2O,(NH_4)_2ZnCl_4 andZnO are the corrosion products on zinc. Brief discussion on the mechanisms of at-mospheric corrosion of zinc in the presence of NH_4 Cl was introduced.
文摘【目的】研究不同温度条件下的石油烃降解产甲烷菌系中是否存在乙酸互营氧化产甲烷代谢途径。【方法】以3个不同温度条件的正十六烷烃降解产甲烷菌系Y15(15℃)、M82(35℃)和SK(55℃)作为接种物,通过乙酸喂养实验、并添加乙酸营养型产甲烷古菌的选择性抑制剂NH4Cl和CH3F,结合末端限制性片段长度多态性(terminal restriction fragment length polymorphism,T-RFLP)和克隆文库技术,分析乙酸产甲烷潜力及产甲烷古菌群落的演替趋势,推测产甲烷代谢途径的变化趋势。【结果】无论是否添加NH4Cl和CH3F,这3个菌系都可以利用乙酸生长并产生甲烷,但是添加NH4Cl和CH3F后产甲烷延滞期增加,最大比甲烷增长速率降低;只添加乙酸后,3个不同温度的菌系的古菌群落主要由乙酸营养型产甲烷古菌甲烷鬃毛菌属(Methanosaeta)组成,其丰度分别为92.8±1.4%、97.3±2.4%和82.8±9.0%;当添加选择性抑制剂NH4Cl,3个菌系中的Methanosaeta的丰度分别变为98.5±0.7%、87.4±4.8%和6.1±8.6%,中温菌系M82中氢营养型产甲烷古菌甲烷袋装菌属(Methanoculleus)的相对丰度增加到12.6±4.0%,高温菌系SK中另一类氢营养型产甲烷古菌甲烷热杆菌属(Methanothermobacter)增至84.3±1.5%;当添加选择性抑制剂CH3F,Methanosaeta丰度分别降至77.1±14.5%,86.4±6.1%和35.8±7.8%,低温菌系Y15中的甲烷八叠球菌属(Methanosarcina)增高(15.7±21%),这类产甲烷古菌具有多种产甲烷代谢途径,M82中Methanoculleus丰度上升到13.6±13.1%,SK中Methanothermobacter丰度增大到48.5±11.2%。【结论】在低温条件下,菌系Y15可能主要通过乙酸裂解完成产甲烷代谢,在中高温条件下,菌系M82和SK中可能存在乙酸互营氧化产甲烷代谢途径,并且甲烷的产生分别通过不同种群的氢营养型产甲烷古菌来完成。
