PRECIPITATION IN THE Mg+2-Na+-SO3-2-SO4-2 AQUEOUS SYSTEM

Spontaneous precipitation in the aqueous system Mg₊₂-Na₊-SO₃^-2-SO₄^-2 affected by mixing solutions of MgSO₄ and Na₂SO₃, together was studied for temperature varying from 40 to 80°C and for pH from 5,5 to 9. The initial composition of a precipitating system was 0·67 and 1·17 mol of MgSO₃ and Na₂SO₄ per liter and 0·82 mol of MgSO₃ and Na₂SO₄ together with 0·83 mol of MgSO₄ per liter, respectively. Depending on the prevailing reaction conditions, solid phase consisting of MgSO₃ 6H₂O, MgSO₃ 3H₂O, Mg₂NaOH(SO₃)₂ H₂O or their mixture is formed. Each solid phase forms crystals of typical size and shape. The precipitation diagrams drawn in the temperature and pH coordinates for three different initial composition of the studied system are presented.     

盐湖老卤动态变温分离高纯结晶硫酸镁

盐湖老卤中镁资源储量丰富,现阶段的初级利用形式主要是提取结晶氯化镁。为提高过程效益,提出了兑卤及变温直接分离高纯结晶硫酸镁的方案,并分别考察MgSO₄饱和卤水、MgSO₄-NaCl共饱和卤水、MgSO₄-NaCl-MgCl₂共饱和卤水在非平衡动态降温过程中硫酸镁晶体微观形貌的变化以及降温速率对晶体形貌的影响。结果表明,MgSO₄饱和卤水非平衡动态降温过程中晶体形成的速率与降温速率有关,在-1.02℃/min的降温速率下,MgSO₄饱和卤水降温30 min后即可形成径向约1300 μm的MgSO₄·7H₂O晶体;但是,当卤水中存在NaCl时,最终的晶体形式为MgSO₄·6H₂O,且多为不规则的块状;卤水中的MgCl₂能促使晶体形成棱柱状的MgSO₄·6H₂O。在NaCl和MgCl₂的作用下,MgSO₄-NaCl-MgCl₂共饱和卤水降温15 h后可以析出完整晶型的高纯结晶硫酸镁。     

The formation of calcium sulfoaluminate hydrate compounds: Part I

The formation of ettringite (3CaO · Al₂O₃ · 3CaSO₄ · 32H₂O) and monosulfate (3CaO · Al₂O₃ · CaSO₄ · 12H₂O) from tricalcium aluminate (3CaO · Al₂O₃) and gypsum (CaSO₄ · 2H₂O) in sodium hydroxide (NaOH) solutions was investigated by isothermal calorimetry and X-ray diffraction analyses. Tricalcium aluminate/gypsum mixtures with a molar aluminate-to-sulfate ratio of 1:3 were hydrated at constant temperatures from 40 to 80°C in deionized water and 200 and 500 mM of NaOH solutions. Ettringite was the only crystalline phase ultimately formed between 40 and 80°C, regardless of whether hydration was carried out in deionized water or sodium hydroxide solutions. The rates of ettringite formation were retarded in sodium hydroxide solutions at all temperatures when compared to hydration in deionized water. The apparent activation energy for the conversion of the tricalcium aluminate/gypsum mixture to ettringite was observed to depend on the concentration of sodium hydroxide.     

Chemical dehydration coupling multi-effect evaporation to treat waste sulfuric acid in titanium dioxide production process

In order to concentrate the diluted sulfuric acid from the titanium dioxide(TiO_2) production of sulphate process,a new concentration process was proposed by coupling chemical dehydration and multi-effect evaporation. The ferrous sulfate monohydrate(FeSO_4·H_2O), as the dehydrant, was added to the diluted sulfuric acid to form ferrous sulfate heptahydrate(FeSO_4·7H_2O) according to the H_2SO_4-FeSO_4-H_2O phase diagrams, which partially removes the water. This process was named as Chemical Dehydration Process. The residual water was further removed by two-effect evaporation and finally 70 wt% sulfuric acid was obtained. The FeSO_4·H_2O can be regenerated through drying and dehydration of FeSO_4·7H_2O. The results show that FeSO_4·H_2O is the most suitable dehydrant, the optimal reaction time of chemical dehydration process is 30 min, and low temperature is favorable for the dehydration reaction. 45.17% of the entire removed water can be removed by chemical dehydration from the diluted sulfuric acid. This chemical dehydration process is also energy efficient with 24.76% saving compared with the direct evaporation process. Furthermore, 51.21% of the FeSO_4 dissolved originally in the diluted sulfuric acid are precipitated out during the chemical dehydration, which greatly reduces the solid precipitation and effectively alleviates the scaling in the subsequent multi-effect evaporation process.     

-15℃下Na+, K+, Mg2+// Cl-, SO4-2-H2O体系相平衡

采用等温溶解平衡法,研究了Na⁺, K⁺, Mg²⁺//Cl^-, SO₄^-2-H₂O, 五元水盐体系在-15℃下NaCl·2H₂O饱和时的相平衡关系,测定了溶解度和密度,并绘制出相应的相图。研究结果表明:该五元体系平衡相图中有3个四盐共饱点,7条单变量溶解度曲线及5个两盐结晶区,5个两盐结晶区分别对应于KCl+NaCl·2H₂O、Na₂SO₄·10H₂O+ NaCl·2H₂O、MgSO₄·7H₂O+NaCl·2H₂O、MgCl₂·8H₂O+NaCl·2H₂O、KCl·MgCl₂·6H₂O+ NaCl·2H₂O;所 得-15℃相图和25℃下相图相比,相图结构大为简化:K₂SO₄·MgSO₄·4H₂O、KCl·MgSO₄·3H₂O、Na₂SO₄·3K₂SO₄、Na₂SO₄·MgSO₄·4H₂O、MgSO₄·(4～6)H₂O、K₂SO₄·MgSO₄·6H₂O结晶区均消失,Na₂SO₄结晶区转变为Na₂SO₄·10H₂O且结晶区扩大,KCl、MgSO₄·7H₂O、KCl·MgCl₂·6H₂O结晶区缩小,MgCl₂·6H₂O结晶区转变为MgCl₂·8H₂O。在此基础上研究了不同组成的盐湖卤水在降温过程中的结晶规律,为低温盐田工艺的开发提供了理论依据。     

结晶法提纯钛白副产硫酸亚铁中杂质去除规律的研究

采用冷冻结晶工艺对钛白副产硫酸亚铁进行了提纯研究,重点考察了结晶母液循环时镁、锰杂质的累积情况以及它们的去除规律,同时对可能引入体系的钠杂质影响也进行了研究。通过多次结晶可以逐渐降低七水硫酸亚铁晶体中镁、锰杂质含量,但结晶母液的循环会导致体系内镁、锰杂质逐渐累积。利用结晶液与结晶体中镁、锰含量的关系曲线推断得到：当结晶液中镁含量低于298 mg/L时,七水硫酸亚铁晶体中镁质量分数将低于0.025%;当结晶液中锰含量高于761 mg/L时,七水硫酸亚铁晶体中锰质量分数将高于0.05%。另外,结晶法提纯硫酸亚铁时应避免向体系中引入钠离子,否则会导致七水硫酸亚铁晶体中钠杂质含量超标问题。该论文研究结果可以为利用结晶法提纯钛白副产硫酸亚铁提供一定的理论和技术指导。     

黑钛液中七水硫酸亚铁结晶动力学性质

采用平衡法研究了七水硫酸亚铁在黑钛液中的溶解度,通过拟合得到了其溶解度方程,并利用FBRM在线监测溶液结晶情况,测量了其结晶介稳区.通过间歇动态法研究了七水硫酸亚铁的结晶动力学,采用矩量变化法求解了粒数衡算方程,并利用最小二乘法对动力学实验数据进行多元线性回归后得到七水硫酸亚铁成核速率和生长速率方程,结果表明:搅拌速率和降温速率对七水硫酸亚铁结晶过程影响显著,因此,针对搅拌速率和降温速率对结晶工艺的影响进行了分析,并对优化前后七水硫酸亚铁产品进行了对比,发现优化后晶体呈规则的棱形,产品粒度明显增大,小颗粒晶体显著减小.     

强化除磷BAF处理石化二级出水

为强化曝气生物滤池(BAF)的除磷效果,以石化二级出水为处理对象,研究了投加FeSO₄·7H₂O对BAF除磷性能的强化作用并对投量进行了优化,同时分析了FeSO₄·7H₂O投加对BAF除碳、脱氮和生物膜活性的影响。结果表明:投加少量FeSO₄·7H₂O(3~15 mg·L^-1)能有效强化BAF的除磷性能;BAF除磷的效果随FeSO₄·7H₂O投加量的增加而提高,但在投量高于9 mg·L^-1时增加趋势逐渐变缓,当FeSO₄·7H₂O的投加量为9 mg·L^-1时,TP的去除率达到57.0%以上,而同期平行运行的BAF除磷效率为7.1%。BAF中少量投加FeSO₄·7H₂O对COD的去除没有不良影响,COD的去除率比对比装置平均提高了5.4%左右,对相对分子质量较大的有机物去除明显。FeSO₄·7H₂O投加量低于12mg·L^-1时对 的去除没有不良影响,高于15 mg·L^-1时由于生物膜中微生物活性的下降 去除率有所降低。投加FeSO₄·7H₂O对TN的去除影响甚微。Fe²⁺的投加使得BAF中附着微生物的量有所降低,但在12 mg·L^-1以下时不会造成大的影响,FeSO₄·7H₂O投量在3~9 mg·L^-1时BAF中生物膜的脱氢酶活性和比好氧呼吸速率有所增加,可弥补生物量降低的影响,因此BAF的运行状况未受到影响。     

四元体系Rb+, Cs+, Mg2+ // SO42- - H2O 298.2 K相平衡研究

采用等温溶解平衡法研究了298.2 K下四元体系Rb⁺, Cs⁺, Mg²⁺ // SO₄^2- - H₂O的相平衡关系,测定了该体系的溶解度、密度以及折射率,并绘制了相应的稳定相图、水图、密度-组成图和折射率-组成图。研究表明：298.2 K下,该四元体系为复杂四元体系,有复盐Cs₂SO₄·MgSO₄·6H₂O和Rb₂SO₄·MgSO₄·6H₂O以及固溶体[(Rb, Cs）₂SO₄]生成。其稳定相图由4个四元共饱点、9条单变量曲线以及6个结晶区组成。四元共饱点中E₁、E₂、E₃为相称共饱点,E₄为不相称共饱点。6个结晶相区分别对应3种单盐Rb₂SO₄、MgSO₄·7H₂O、Cs₂SO₄,2种复盐Cs₂SO₄·MgSO₄·6H₂O、Rb₂SO₄·MgSO₄·6H₂O和1种固溶体[(Rb,Cs）₂SO₄]。其中,复盐Rb₂SO₄·MgSO₄·6H₂O结晶区最大,表明其在该体系中最易结晶析出;Cs₂SO₄结晶区最小。平衡液相的密度和折射率随着溶液中Cs₂SO₄含量变化呈规律性变化。该体系稳定相图将为硫酸镁亚型盐湖卤水中的铷、铯等资源开发利用提供理论依据。     

The homogeneous nucleation rates of H2SO4-H2O aerosol particles in air

The homogeneous nucleation rates for H₂SO₄---H₂O solution droplets at 25, 0 and −55°C are calculated and plotted as a function of H₂SO₄ concentration and H₂O concentration. The plotted contours are very useful for quick estimates of the nucleation rates of H₂SO₄---H₂O aerosols in smog chambers, polluted atmospheres and the stratosphere under different environmental conditions. The effect of the uncertainty in the saturated vapor pressure of H₂SO₄ on the nucleation rate is also discussed.     

258.15 K下五元体系Li+,Na+,Mg2+//SO42-,Cl--H2O相平衡研究

中国含锂盐湖大部分位于青藏、新疆等干旱少雨、冬季寒冷且漫长的地区。为指导低温提锂工艺的开发和设计、利用冬季冷能进行目标离子的富集及明确含锂盐湖在低温下的析盐规律,采用等温溶解平衡法对258.15 K、二水氯化钠饱和条件下的交互五元体系Li⁺,Na⁺,Mg²⁺∥SO₄^2-,Cl^--H₂O相平衡关系进行研究并构建等温平衡相图。结果表明,相图中有4个共饱点、6个两盐结晶区(NaCl·2H₂O+Na₂SO₄·10H₂O、NaCl·2H₂O+MgCl₂·8H₂O、NaCl·2H₂O+MgSO₄·7H₂O、NaCl·2H₂O+Li₂SO₄·H₂...     

Diamond and graphite crystallization from C–O–H fluids under high pressure and high temperature conditions

Crystallization of diamond was studied in the CO₂–C, CO₂–H₂O–C, H₂O–C, and CH₄–H₂–C systems at 5.7 GPa and 1200–1420°C. Thermodynamic calculations show generation of CO₂, CO₂–H₂O, H₂O and CH₄–H₂ fluids in experiments with graphite and silver oxalate (Ag₂C₂O₄), oxalic acid dihydrate (H₂C₂O₄·2H₂O), water (H₂O), and anthracene (C₁₄H₁₀), respectively. Diamond nucleation and growth has been found in the CO₂–C, CO₂–H₂O–C, and H₂O–C systems at 1300–1420°C. At a temperature as low as 1200°C for 136 h there was spontaneous crystallization of diamond in the CO₂–H₂O–C system. For the CH₄–H₂–C system, at 1300–1420°C no diamond synthesis has been established, only insignificant growth on seeds was observed. Diamond octahedra form from the C–O–H fluids at all temperature ranges under investigation. Diamond formation from the fluids at 5.7 GPa and 1200–1420°C was accompanied with the active recrystallization of metastable graphite.     

玛纳斯湖卤水自然蒸发析盐规律及硼、锂富集规律研究

以ISLEC软件模拟计算了新疆玛纳斯湖晶间卤水20 ℃自然蒸发的结晶路线,以模拟计算的结果指导在室内进行了自然蒸发实验,得出了与模拟计算一致的玛纳斯湖自然蒸发结晶路线。并研究了蒸发过程中硼、锂等微量元素的富集和分布规律。玛纳斯湖水室内自然蒸发时的结晶路线:①CaSO₄·2H₂O+NaCl;②CaSO₄·2H₂O+NaCl+MgSO₄·6H₂O;③NaCl+MgSO₄·6H₂O+KCl（少量）+KCl·MgCl₂·6H₂O;④NaCl+MgSO₄·6H₂O+KCl·MgCl₂·6H₂O+MgCl₂·6H₂O。ISLEC计算得到的光卤石矿中KCl的品位为14.24%,实验得到的光卤石矿中KCl的品位为10.59%。同时,蒸发过程中硼、锂未以固相形式析出,一直富集于卤水中,至蒸发结束约富集16倍,w（B₂O₃）约为1%,Li⁺约100 mg/L。依据自然蒸发结果,给出了湖水开发利用的建议,即先经过冬季冻硝脱硫再进行盐田晒卤以获取高品质的光卤石矿。     

前驱体二水磷酸铁对磷酸铁锂电化学性能的影响

以钛白生产副产物七水硫酸亚铁为铁源,工业磷酸二氢铵为磷源,双氧水为氧化剂,采用共沉淀法合成了不同粒径和形貌的二水磷酸铁,并以此为前驱体,通过碳热还原法制备了粒径不同的LiFePO₄/C正极材料。经过对样品进行X射线衍射（XRD）、扫描电镜（SEM）以及恒电流充放电测试,研究了二水磷酸铁及LiFePO₄/C的结构、形貌以及电化学性能。结果表明,以较细的二水磷酸铁为铁源,制备得到的LiFePO₄/C颗粒较细,且具有更优异的电化学性能。0.1、0.5、1、2、5、10 C放电比容量分别为154、148、144、140、130、120 mA·h/g。     

Porous structures constructed from [SiMo12O40] and [SiW12O40] Keggin units

Three compounds, K₂(H₂O)₄H₂SiMo₁₂O₄₀ · 7H₂O (1), K₂Na₂(H₂O)₄SiW₁₂O₄₀ · 4H₂O (2), and Na₄(H₂O)₈SiMo₁₂O₄₀ · 6H₂O (3) have been synthesized and structurally characterized by single-crystal X-ray analysis, IR, and thermogravimetry. Compounds 1 and 2 both show the high symmetry trigonal space group P3₂21 and a novel 3D network structure. The Keggin anions [SiM₁₂O₄₀]⁴⁻(M = Mo, W) are linked by potassium or sodium cations to generate hexagon-shaped channels along the c-axis, in which water molecules are accommodated. Compound 3 is tetragonal, space group P4/mnc constructed from [SiMo₁₂O₄₀]⁴⁻ anions and Na ions.     

-15℃下Na+， K+， Mg2+//Cl-， NO3-， SO42——H2O体系相平衡研究

新疆卤水硝酸盐矿主要含有Na⁺、K⁺、Mg²⁺、Cl^-、NO₃^-、SO₄^2-六种离子,属于高元复杂体系,其合理利用和开发需要不同温度下的相平衡研究作为理论支撑。采用等温溶解平衡法,对Na⁺, K⁺, Mg²⁺//Cl^-, NO₃^-, SO₄^2--H₂O体系在-15℃、NaCl·2H₂O饱和条件下的相平衡进行了研究,并构建了相图。相图中有六个零变量点和八个两盐结晶区,只存在一种复盐KCl·MgCl₂·6H₂O。八个两盐结晶区,分别对应于NaCl·2H₂O+Na₂SO₄·10H₂O、NaCl·2H₂O+NaNO₃、NaCl·2H₂O+KCl、NaCl·2H₂O+KNO₃、NaCl·2H₂O+MgSO₄·7H₂O、NaCl·2H₂O+MgCl₂·8H₂O、NaCl·2H₂O+Mg(NO₃)₂·6H₂O和NaCl·2H₂O+KCl·MgCl₂·6H₂O,其中NaCl·2H₂O+Na₂SO₄·10H₂O共晶区最大,在低温时,硫酸钠的溶解度最小,降温过程中较易结晶析出。与该体系在25℃下的相图相比,复盐种类减少5种,零变量点减少19个,相关系得以极大简化。     

Study on phase equilibrium of system Na+, K+, Mg2+//Cl-, NO3-, SO42--H2O at -15℃

Xinjiang brine nitrate mine mainly contains six kinds of ions: Na⁺, K⁺, Mg²⁺, Cl^-, NO₃^-, and SO₄^2-, belonging to a high-element complex system, and its rational utilization and development require phase equilibrium studies at different temperatures as theoretical support. The phase equilibrium of the system Na⁺, K⁺, Mg²⁺//Cl^-, NO₃^-, SO₄^2--H₂O saturated with NaCl·2H₂O at -15℃ was investigated using the isothermal solution equilibrium method. According to the measured data, the phase diagrams were constructed. Only one double salt KCl·MgCl₂·6H₂O was found in the system. There are six invariant points and eight two-salt crystallization fields corresponding to NaCl·2H₂O+Na₂SO₄·10H₂O, NaCl·2H₂O+NaNO₃, NaCl·2H₂O+KCl, NaCl·2H₂O+KNO₃, NaCl·2H₂O+MgSO₄·7H₂O, NaCl·2H₂O+MgCl₂·8H₂O, NaCl·2H₂O + Mg(NO₃)₂·6H₂O and NaCl·2H₂O+KCl·MgCl₂·6H₂O. The crystallization area of NaCl·2H₂O+Na₂SO₄·10H₂O occupies the largest part because of its low solubility, and they will crystallize out easily from the mixed solution in the cooling process. Compared with the phase diagram of the system at 25℃, there are 5 types of double salts reduced, 19 zero variable points reduced, and the phase relationship is greatly simplified.     

基于神经网络与遗传算法结合的硝化细菌发酵培养基优化(英文)

Two artificial intelligence techniques, artificial neural network and genetic algorithm, were applied to optimize the fermentation medium for improving the nitrite oxidization rate of nitrite oxidizing bacteria. Experiments were conducted with the composition of medium components obtained by genetic algorithm, and the experimental data were used to build a BP (back propagation) neural network model. The concentrations of six medium components were used as input vectors, and the nitrite oxidization rate was used as output vector of the model. The BP neural network model was used as the objective function of genetic algorithm to find the optimum medium composition for the maximum nitrite oxidization rate. The maximum nitrite oxidization rate was 0.952 g 2 NO-2-N·(g MLSS)-1·d-1 , obtained at the genetic algorithm optimized concentration of medium components (g·L-1 ): NaCl 0.58, MgSO 4 ·7H 2 O 0.14, FeSO 4 ·7H 2 O 0.141, KH 2 PO 4 0.8485, NaNO 2 2.52, and NaHCO 3 3.613. Validation experiments suggest that the experimental results are consistent with the best result predicted by the model. A scale-up experiment shows that the nitrite degraded completely after 34 h when cultured in the optimum medium, which is 10 h less than that cultured in the initial medium.     

安丝菌素P-3生产菌株Actinosynnema pretiosum ssp. auranticum的诱变育种及其发酵培养基优化

为了提高安丝菌素P-3（AP-3）的发酵产量,通过紫外诱变并运用紫外-分光光度法建立96孔板高通量快速筛选体系对原始菌株（Actinosynnema pretiosum ssp.auranticum）进行育种,筛选获得了一株产量较高的突变菌株B24-13。发酵7天后,其发酵液中AP-3的含量为112.5mg/L,是原始菌株的2.03倍。随后通过单因素优化与正交实验设计对突变菌株B24-13进行发酵培养基优化,得到最优发酵培养基组分：蔗糖25g/L,甘油15g/L,玉米浆25g/L,CaCO₃ 7g/L,异丁醇2g/L,缬氨酸0.5g/L,MgSO₄·7H₂O 0.5g/L,FeSO₄·7H₂O 0.01g/L。对优化结果进行验证实验,发酵7天后AP-3的产量为（127.5±6.3） mg/L。实验结果表明：通过对生产菌株的诱变育种与发酵培养基优化可有效的提高AP-3的发酵产量,也从侧面验证了该研究所建立的96孔板高通量快速筛选体系用于AP-3高产菌株的初筛是可行的。     

Revision of Charnell’s procedure towards the synthesis of large and uniform crystals of zeolites A and X

A critical replication and re-evaluation of Charnell’s procedure to the synthesis of zeolites A and X has been carried out, aiming at reliable protocols for preparation of large and uniform crystals of the respective zeolites in a scale of 50 g per batch. Triethanolamine, as an organic additive to the reacting sodium aluminosilicate hydrogel, increases the viscosity of the system, and reduces the reactivity of aluminium species towards nucleation and crystal growth through forming chelated complex compounds. The reactivity of silicate species has to be accordingly adjusted, by choosing proper source materials. Zeolite A crystals, which possess shapes of edge-truncated cubes, and sizes of 35–40 μm in edge-length, have been synthesized with a starting gel having the composition 1.7Na₂O:Al₂O₃:0.7SiO₂:165H₂O:6.1TEA in 2-l batch-size, using dissolved metallic aluminium and colloidal silica. The crystallization has been accomplished at 85 °C within 21 days. When the gel has a starting composition 2.3Na₂O:Al₂O₃:1.3SiO₂:300H₂O:10TEA (1-l batch), 70–80 μm large zeolite X crystals can be obtained at 85 °C in 35 days. Both starting gels are prepared at 0 °C, then quickly heated to the crystallization temperature.