-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。     

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。     

-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。     

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...     

Primary nucleation of citric acid monohydrate: influence of selected impurities

An experimental study is presented concerning solubility and primary nucleation kinetics of monohydrate citric acid from pure and selectively impure (KH₂PO₄, MgSO₄ · 7H₂O and FeSO₄ · 7H₂O) aqueous solutions. The metastable range of pure solutions is wide, ranging from 6 to 14°C, and the order of primary nucleation, equal to 2.51, is quite low. The addition of the tested impurities, which are usual fermentation aids, at concentrations lower than wt. 1%, produces negligible effects on the solubility and slightly enhances the primary nucleation rate. However, the presence of these compounds modifies the crystal habit at birth: in particular, the addition of MgSO₄ · 7H₂O and FeSO₄ · 7H₂O makes these crystals more elongated, but this effect diminishes as the crystals grow.     

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.     

四元体系NaCl+NaBO2+Na2CO3+H2O 298.15 K 相平衡研究

柴达木盐湖中具有丰富的盐湖离子,对其中的一个四元体系水盐相图开展研究,采用等温溶解平衡法开展了298.15 K时四元体系NaCl+NaBO₂+Na₂CO₃+H₂O相平衡研究,测定了体系平衡液相组成及密度和折光率,绘制了四元体系NaCl+NaBO₂+Na₂CO₃+H₂O 298.15 K的相图及相应的物化性质图。研究发现NaCl+NaBO₂+Na₂CO₃+H₂O四元体系298.15 K 时包含2个共饱点（E₁、E₂）、5条溶解度曲线（AE₁、BE₁、CE₂、DE₂、E₁E₂）、4个结晶区（NaCl、NaBO₂·4H₂O、Na₂CO₃·7H₂O、NaCl·NaBO₂·2H₂O）。其中三元体系NaCl+NaBO₂+H₂O在298.15 K下产生了复盐NaCl·NaBO₂·2H₂O,通过研究发现该四元体系NaCl+NaBO₂+Na₂CO₃+H₂O在298.15 K下也具有NaCl·NaBO₂·2H₂O复盐区。     

四元体系硼酸锂-硼酸钾-硼酸镁-水在308.15 K时固液相平衡研究

采用等温溶解平衡法研究四元体系硼酸锂-硼酸钾-硼酸镁-水在308.15 K时固液相平衡,测定了体系溶解度和平衡液相的密度、折光率和pH。研究发现：该体系308.15 K时的稳定相图中包含一个共饱点（L+Li₂B₄O₇·3H₂O+K₂B₄O₇·4H₂O+Mg₂B₆O₁₁·15H₂O）,其液相组成：w（Li₂B₄O₇）=3.112%、w（K₂B₄O₇）=16.64%、w（Mg₂B₆O₁₁）=0.101 8%;3个固相结晶区：Li₂B₄O₇·3H₂O、K₂B₄O₇·4H₂O、Mg₂B₆O₁₁·15H₂O,体系无复盐或固溶体生成。溶液中硼酸锂、硼酸钾对多水硼镁石有很强的盐析效应,液相的密度、折光率和pH随溶液中硼酸盐浓度的增加呈规律性变化。     

燃煤锅炉烟气中Na2SO4生成的化学动力学研究

准东煤燃烧过程中Na₂SO₄的形成会造成锅炉受热面沾污、尾部SCR催化剂失活等问题。烟气中Na₂SO₄形成及转化规律的研究对于预测和控制燃煤烟气中Na₂SO₄的形成有重要意义。发展了烟气中Na/Cl/S/O/H化学动力学模型,研究了烟气中Na₂SO₄的生成过程及转化机理,考察了含氧量、温度、SO₂浓度、H₂O浓度等因素对Na₂SO₄生成的影响。动力学计算结果表明,模型预测结果与实验数据吻合较好,验证了模型的准确性。烟气中的高氧气含量有利于Na₂SO₄的生成。高温加快化学反应的同时,抑制了Na₂SO₄的生成。SO₂和H₂O的影响效果受温度影响较大。反应路径分析表明,Na₂SO₄的生成路径有两个：一是依赖于SO₂直接氧化（NaCl→NaSO₃Cl→NaHSO₄→Na₂SO₄）,二是依赖于SO₂间接氧化（NaCl→NaO₂→NaSO₄→NaHSO₄→Na₂SO₄）。敏感性分析结果表明,Na₂SO₄的生成主要对系统中生成或消耗自由基的反应更为敏感。     

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.     

Chemical activation of blended cements made with lime and natural pozzolans

This paper deals with the chemical activation of lime-pozzolan cement (LPC), which consists of 80% natural pozzolan and 20% hydrated lime (by mass). Results show that the addition of 4% Na₂SO₄ can significantly improve the early strength of this cement. The presence of 4% flake calcium chloride (CaCl₂.2H₂O) is not helpful to early strength, but can increase the later strength substantially. CaSO₄.O.5H₂O and NaCl do not demonstrate an obvious effect on the strength development of the cement. Combination of activators, such as CaCl₂.2H₂O+Na₂SO₄ or Na₂SO₄+NaCl does not improve the activation effect; pastes with 2% Na₂SO₄+2% NaCl show lower strength than the pastes with 2% Na₂SO₄ alone.     

四元相变材料的制备及改性研究

为探究与制备更加适用于太阳能储能应用的四元相变材料,以Na₂HPO₄·12H₂O为主储热剂,Na₂SO₄·10H₂O,Na₂CO₃·10H₂O,Na₂S₂O₃·5H₂O与CH₃COONa·3H₂O为辅储热剂,在四种辅储热剂中任取三种与主储热剂按照设计的配比进行混合,制备四元相变储能材料,并选取纳米TiO₂,ZnO,Al₂O₃以及Na₂SiO₃和Na₂B₄O₇·10H₂O作为成核剂分别对其进行改性,通过步冷曲线、DSC、SEM、IR、XRD对样品进行数据分析。结果表明,Na₂HPO₄·12H₂O/Na₂CO₃·10H₂O/Na₂SO₄·10H₂O/Na₂S₂O₃·5H₂O为四元PCMs的最佳组合,其最佳配比(质量分数)分别为60%、10%、20%、10%(60/10/20/10)。在多种成核剂中掺加氧化锌的效果最好,当掺量10%(质量分数)时,四元PCMs的过冷度由3.0 ℃降低到0.2 ℃,相变焓由95.11 J/g升至472.39 J/g,相变温度区间从15.44~39.90 ℃改变至50.79~129.64 ℃,且无相分离。     

Photocatalytic degradation of aqueous organocholorine pesticide on the layered double hydroxide pillared by Paratungstate A ion, Mg12Al6(OH)36(W7O24)·4H2O

Layered double hydroxide pillared by Paratungstate A ion, Mg₁₂Al₆(OH)₃₆(W₇O₂₄)·4H₂O, was prepared via anion exchange reaction of the synthetic precursor, Mg₄Al₂(OH)₁₂TA·xH₂O (TA²⁻=terephthalate), and [W₇O₂₄]⁶⁻ ion. Some physico-chemical properties were measured and the preparation conditions were studied. Trace aqueous organocholorine pesticide, hexachlorocyclohexane (HCH), was totally degraded and mineralized into CO₂ and HCl by irradiating a Mg₁₂Al₆(OH)₃₆(W₇O₂₄)·4H₂O suspension in the near UV area. Disappearance of trace HCH follows Langmuir–Hinshelwood first-order kinetics. The model and mechanism for the photocatalytic degradation of HCH on the Mg₁₂Al₆(OH)₃₆(W₇O₂₄)·4H₂O were proposed, indicating that the interlayer space is the reaction field, and that photogeneration of OH√ radicals are responsible for the degradation pathway.     

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。     

四元体系LiCl-LiBO2-Li2SO4-H2O在298.15K时的相平衡

采用等温溶解平衡法开展了四元体系LiCl-LiBO₂-Li₂SO₄-H₂O在298.15 K时相平衡实验研究,测定体系溶解度和平衡溶液的折光率、密度、pH和电导率。根据实验数据,分别绘制该四元体系的干基图、水图以及相对应的物化性质-组成图。研究结果表明:在该四元体系298.15 K相图中,有2个无变度共饱点分别为相称共饱点(Li₂SO₄·H₂O + LiCl·H₂O + LiBO₂·2H₂O)和不相称共饱点(Li₂SO₄·H₂O + LiBO₂·2H₂O + LiBO₂·8H₂O)、5条溶解度曲线和4个单盐结晶相区(Li₂SO₄·H₂O、LiCl·H₂O、LiBO₂·8H₂O和LiBO₂·2H₂O),无复盐和固溶体产生,属于简单四元体系水合物Ⅱ型相图。实验研究中,发现2种偏硼酸锂水合矿物存在(LiBO₂·8H₂O和LiBO₂·2H₂O),LiCl对Li₂SO₄的盐析效应显著;四元体系平衡溶液物化性质随着溶液中氯化锂浓度的变化呈现规律性的变化。     

四元体系（Li+， Mg2+//Cl-， borate-H2O）308.15 K相平衡与相图研究

采用等温溶解平衡法,开展四元体系Li⁺, Mg²⁺//Cl^-, borate–H₂O固液相平衡与相图研究,测定平衡溶液的液相组成、密度、折射率和pH。该四元体系相图中存在的盐类矿物为：LiCl·H₂O、Li₂B₄O₇·3H₂O、 MgCl₂·6H₂O、Mg₂B₆O₁₁·15H₂O和锂光卤石LiCl·MgCl₂·7H₂O,其中锂光卤石LiCl·MgCl₂·7H₂O是异成分复盐,溶液中MgCl₂存在下章氏硼镁石（MgB₄O₇·9H₂O）不稳定,转化为多水硼镁石（Mg₂B₆O₁₁·15H₂O）。多水硼镁石结晶区最大,表明镁硼酸盐易于结晶析出,而锂光卤石结晶区最小。采用Pitzer热力学模型对该四元体系的溶解度进行理论预测,计算相图与实验相图吻合较好。该四元体系的稳定相平衡与相图研究,可为含锂硼盐湖老卤中锂、镁、硼产品开发及其综合利用提供理论依据。     

Effect of alkalies on portland cement hydration II. Alkalies present in form of sulphates

Alkalies present in cement in the form of Na₂SO₄ and/or K₂SO₄ do not alter the progress of C₃S and C₃A hydration. The setting time becomes accelerated especially with K₂SO₄ due to the formation of syngenite CaSO₄·K₂SO₄·H₂O. The compressive strength is lowered significantly.     

AgBr/Zn3(OH)2V2O7·2H2O可见光催化降解亚甲基蓝溶液

采用水热和沉淀两步合成法制备AgBr/Zn₃(OH)₂V₂O₇·2H₂O催化剂,研究其在可见光下降解亚甲基蓝溶液的性能,并考察催化剂用量、亚甲基蓝溶液初始浓度、pH值以及盐浓度对光催化性能的影响,评价AgBr/Zn₃(OH)₂V₂O₇·2H₂O催化剂的重复使用性能。结果表明,在前驱液pH为10、120 ℃水热10 h、Ag与Br物质的量比为0.20条件下制备的复合催化剂在可见光下反应120 min后,1.0 g·L^-1的催化剂对10 mg·L^-1的亚甲基蓝溶液脱色率达到85.2%。NaCl对亚甲基蓝的降解起抑制作用,Na₂SO₄对亚甲基蓝的降解起促进作用。催化剂重复使用4次后,光照120 min后的亚甲基蓝溶液脱色率可达66.4%。催化剂对不同初始浓度亚甲基蓝溶液的光催化降解符合一级动力学模型。     

313.15 K四元体系Na+// S O 4 2 - ， C O 3 2 - ， N O 3 - -H2O固液相平衡研究

采用等温溶解法研究313.15 K下四元体系Na⁺// \mathrm{S} {\mathrm{O}}_4^{2-} , \mathrm{C} {\mathrm{O}}_3^{2-} , \mathrm{N} {\mathrm{O}}_3^{-} -H₂O的固液相平衡关系。测定了平衡溶液的溶解度数据及物理性质数据,包括密度、黏度、折射率。根据实验数据,绘制了相应的干盐相图、水图及物理性质-组成图。实验结果表明：313.15 K下,此四元体系相图包括两个共饱和点,六条单变曲线以及五个单盐结晶区域(分别为NaNO₃,Na₂SO₄,Na₂CO₃·H₂O, Bur(Na₂CO₃·2Na₂SO₄),Da(NaNO₃·Na₂SO₄·H₂O)),其中Bur的结晶区域最大,最容易从混合溶液中结晶析出。实验中的物理性质(黏度、密度、折射率)随J(Na₂SO₄)的变化呈现相似性规律。该体系中存在复盐碱芒硝Bur(Na₂CO₃·2Na₂SO₄)、钠硝矾Da(NaNO₃·Na₂SO₄·H₂O),结晶水合物(Na₂CO₃·H₂O),没有固溶体存在,故该体系是一个复杂的共饱和型。实验所获数据和结论对煤化工过程产生的高盐废水结晶析盐工艺开发及实现资源梯级综合利用具有重要意义。     

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.