H_2O对SO_2在CaO表面上吸附的影响理论研究

采用密度泛函理论研究了H_2O对SO_2在CaO(001)表面上吸附的影响。结果表明,以四种形式(-H_2O、-H、-OH和-H-OH)存在的H_2O使SO_2在CaO表面上的吸附构型发生改变。SO_2在不同形式H_2O基团邻位吸附时,-H使S原子的p轨道态密度峰明显左移且吸附能比洁净表面大90 kJ/mol,其余基团表面吸附能无明显变化;SO_2吸附于-OH和-H-OH生成HSO_3基团,吸附能相比于洁净表面较小,可能作为暂态结构;SO_2吸附于-H_2O生成SO_3基团,H_2O断键生成的H基团起主要吸附作用,CaO表面上生成类似Ca(OH)_2的局部结构且吸附能比洁净表面大45 kJ/mol。     

Thermal Behavior of Zn(Thr)SO_4·H_2O

IntroductionRecently,a considerable interest has been fo-cused on the complexes of zinc with amino acidsdue to their excellent additives in medicine foodstuff and cosmetics[1— 6] .The investigation on thethermal behavior and the thermochemistry of somezinc amino acids is important to its further applica-tion,which has been reported in references[4,5 ,7— 1 0 ].However,the studies on solid complexZn( Thr) SO4· H2 O has not been reported,whichcan provide the necessary data and the foundation…     

新疆高钠煤中钠的赋存形态及其对燃烧过程的影响

采用不同萃取液对中国新疆高钠煤进行逐级萃取实验,利用离子色谱仪和电感耦合等离子体原子发射光谱仪对萃取制得的滤液和固体煤样进行相应的元素分析,并通过逐级萃取后煤样的着火温度、燃尽温度和综合燃烧特性指数来分析高钠煤中不同存在形式钠对其燃烧特性的影响.结果表明,中国新疆高钠煤中的钠主要以水溶钠为主,有机钠和不可溶钠含量较少.影响高钠煤中水溶钠含量的主要因素有煤颗粒内部孔隙结构和颗粒粒径,且高钠煤中有机钠在各个粒径范围都保持了相对稳定的含量.煤种不同会导致煤中水溶钠与水溶氯的存在形式不同.煤中水溶钠的存在不利于高钠煤的着火温度和燃尽温度的降低与燃烧特性的提高,相反煤中的有机钠却对其具有促进作用.     

配合物[Fe(CTS)_2]·SO_4·7H_2O的热分解动力学

研究了壳聚糖对Fe2 + 的吸附行为 ,并进行了条件优化 ,得到了较为理想的合成产物。通过红外光谱和紫外光谱进行了表征 ,进而用化学分析、元素分析确定了配合物的组成 ,并利用TG DSC分析 ,采用常用的 2 2种机理函数 ,对非等温动力学数据进行了线性回归拟合处理 ,求得了配合物主要分解阶段热动力学最可机理函数和动力学参数 (E和A)。     

ZrW_(1.7)~ⅥW_(0.3)~ⅤO_7H_(0.3)(OH)_2·2H_2O的合成与表征

分别利用微乳液水热法和酸蒸气水热法合成了杂多蓝化合物 Zr W 1 .7W 0 .3O7H0 .3( OH) 2 · 2 H2 O.XRD测定结果表明 ,该化合物与 Zr Mo2 O7( OH) 2 · 2 H2 O具有相同晶体结构类型 .使用 Rietveld方法对产物进行了结构精修 ,并计算出了键参数和键价 .运用 EPR技术测定了该化合物中 W的价态 ,并利用 XPS能谱测定了 W /W 的比例 .利用价键和规则 ,指出 Zr W 1 .7W 0 .3O7H0 .3( OH) 2 · 2 H2 O中的 W— O3— H0 .1 5存在羟基化现象 ,并对杂多蓝化合物的红外吸收光谱进行了指认 .     

配合物Zn(His)SO4·H2O(s)的低温热容和热力学性质

通过精密自动绝热热量计测定了配合物Zn(His)SO4*H2O(s)在78～390K温区的摩尔热容,由热容曲线得到其起始脱水温度328.90K;用最小二乘法拟合得到摩尔热容(Cp,m)对温度(T)的多项式方程,并在此基础上计算了它的各种热力学函数.此外,研究了其在惰性气氛下的热分解过程.     

Theoretical Studies on the Intermonomer Interaction of F~-·(H_2O)_n (n = 1, 2)

1 INTRODUCTION Hydrogen bond plays an important role in the fields of physics, biology and chemistry. It has cap- tured the interest of chemists for a long time and reports about its theory and experiment have been well represented[1～6]. Concerning its theoretical inves- tigations, most of the emphases are placed on the weak interaction energy of intramolecular hydrogen bond. But studies on its spectrum behavior are rela- tively rare. These years spectrum behavior led by hydrogen bond h…     

准东高钠煤热解过程中钠的迁移特性实验研究

针对新疆准东煤田高钠煤(简称准东高钠煤)在发电锅炉燃烧时遇到结渣黏污严重的问题,基于立式管式炉热解,利用电感耦合等离子体-原子发射光谱(ICP-AES)、X射线衍射(XRD)以及扫描电镜-能谱(SEM-EDX)等检测手段,分析了准东高钠煤在不同热解温度下碱金属钠的析出特性、赋存形态以及热解半焦的微观形貌.利用Fact sage 6.1化学热力学平衡计算软件分析了碱金属的析出形式.结果表明,准东高钠煤中的碱金属钠在热解过程中有部分析出,开始的析出温度为600 ℃,当热解温度达900 ℃时,碱金属钠的析出率为40.2%;碱金属钠在热解过程中主要以NaCl的形式析出;热解温度低于900 ℃时,没有熔融态物质生成.     

配合物Zn(Leu)SO4·O.5H2O的合成与热行为

在水-丙酮溶液中制备了zn(Leu)SO4@0.5H2O的配合物.通过热重和红外分析,研究了它的热分解机理,可分为三步完成.第一阶段配合物的脱水过程在60-180℃,形成Zn(Leu)S04,第二阶段,Zn(Leu)SO4进一步分解为Zn(Leu)SO4@9ZnSO4,随后其在728℃完全分解为ZnO.在不同线性升温5.O,10.0,15.0,20.OK@min-1条件下,用两种积分法和三种微分法研究了题目化合物失去配体过程的非等温动力学,相应过程的表观活化能E为133.78KJ@mol-1,指前因子A为1O8.19s-1,配体失去过程为三维扩散机理控制,并建立了反应过程的动力学方程.     

MaterialSO2与Fe2O3生成Fe(Ⅱ)(aq)和硫酸盐的复相反应机理

使用DRIFTS, XPS, HPLC和IC考察了常温、常压和氧气存在下SO2与Fe2O3的复相反应, 结果表明, SO2在Fe2O3表面的反应活性与Fe2O3表面含水量密切相关, 表面含水量增加有助于Fe(Ⅱ)(aq)和硫酸盐的生成.室温下(T=291 K, 相对湿度68%), 每毫克Fe2O3在30 min内可消耗53.6 μg SO2, 生成12.6 ng Fe(Ⅱ)(aq)和56.2 μg SO2-4.反应产物 SO2-4的浓度比Fe(Ⅱ)(aq)的浓度高3个数量级, 表明在生成硫酸盐的复相反应中铁对SO2氧化具有非常高的催化活性.提出了Fe(Ⅱ)(aq) 和硫酸盐的生成机理.     

O2/CO2燃烧气氛对混煤灰中矿物质间反应影响研究

对蒙煤与平七煤两种单煤及其按照不同比例组成的混煤,分别在O₂/CO₂和O₂/N₂气氛下,采用管式炉燃烧制取灰样;对灰样进行灰熔点、XRD及同步热分析（TG/DSC）测试,并进行相关热力学计算,分析了O₂/CO₂燃烧方式对混煤灰中矿物质间反应的影响。结果表明,常规灰熔点测试方法测得的两种气氛下的混煤灰熔点没有明显差别。O₂/CO₂气氛促进了煤灰/混煤灰中钙的碳酸化,且明显抑制了高温下CaCO₃的分解。气氛的改变影响了含钙矿物的转化,进而影响了混煤中钙与莫来石反应生成低温共熔物;O₂/CO₂气氛下钙更易于与莫来石发生反应生成低温共熔物,从而会增加结渣倾向。当混煤中蒙煤比例达到或大于75%时,随着蒙煤比例的逐渐增加,莫来石含量减少,O₂/CO₂气氛对钙与莫来石之间的反应影响减弱,但对含铁矿物的影响更加明显,使其更易于生成含铁玻璃体,从而也会增加结渣倾向。     

O2/CO2气氛下O2浓度对燃煤PM2.5形成的影响

采用管式炉和荷电低压撞击器(electrical low pressure-impactor,ELPI)研究了徐州烟煤在O₂/CO₂条件下燃烧后生成的PM_2.5排放特性。结果表明,在O₂/CO₂气氛下,煤粉在不同O₂浓度燃烧所产生的PM_2.5质量浓度均呈双峰分布,峰值分别在0.1和2.0 mm左右;随着氧含量的增加,PM_2.5的质量浓度增加;S、K和Na在亚微米颗粒上明显富集,而Si和Ca未在亚微米颗粒上富集;通过对颗粒物的粒径分布、元素分析和形貌观察,认为亚微米颗粒主要是矿物质蒸发鄄凝结机制形成的,而超微米颗粒主要是煤焦与外部矿物质的破碎以及内在矿物质聚合形成的。     

Low-temperature heat capacity and standard molar enthalpy of formation of the complex Zn(Thr)SO4·H2O (s)

Low-temperature heat capacities of the complex Zn(Thr)SO₄·H₂O (s) have been precisely measured with a small sample adiabatic calorimeter over the temperature range from 78 to 373 K. The initial dehydration temperature of the complex (T_d=325.50 K) has been obtained by analysis of the heat-capacity curve. The experimental values of molar heat capacities have been fitted to a polynomial equation by least square method. The standard molar enthalpy of formation of the complex has been determined from the enthalpies of dissolution (Δ_dH_m^Θ) of [ZnSO₄·7H₂O (s) +Thr (s)] and Zn(Thr)SO₄·H₂O (s) in 100 ml of 2 mol dm⁻³ HCl solvent as: Δ_fH_{m,Zn(Thr)SO4·H2O}^Θ=−2111.7±3.4 kJ mol⁻¹. These experiments were made by using an isoperibol solution calorimeter at 298.15 K.     

流化床O2/CO2气氛下添加石灰石对燃煤PM2.5的控制

采用小型流化床研究了在O₂/CO₂气氛下添加石灰石对PM_2.5(空气动力学直径小于2.5 μm的颗粒物)的控制.实验采用荷电低压撞击器(ELPI)采集和分析燃烧后的PM_2.5.结果表明,添加石灰石是燃烧过程中影响PM_2.5生成的重要因素.添加石灰石后,生成PM_1.0的数量浓度均降低,而PM_1.0~2.5的数量浓度均略有增加;PM_2.5质量粒径分布均呈双峰分布,峰值分别出现在0.2和2.0 μm左右.随着Ca/S物质的量比的增加,PM_2.5中Si、Na、K、S和Cu的含量呈减少的趋势;随着颗粒粒径的减小,S、Cu、K和Na的含量有增大的趋势,而Si的含量有减少的趋势.     

Synthesis and crystal structure of a complex bearing interesting structural motifs: [Cu (C4H7N3) H2O (4,4′-Hbpy)]·SO4·NO3

A new complex [Cu (C₄H₇N₃) H₂O (4,4′-Hbpy)]·SO₄·NO₃ was synthesized and X-ray characterized. Elemental analysis, X-ray diffraction and infrared spectroscopy of the complex were performed. The crystal system is orthorhombic. Crystal data: Fw=498.98, spacegroup: P212121. Z=4, a=14.952(3), b=20.491(4), c=6.713 Å. V=2056.7(9) Å. λ(Mo-K)=0.71070 Å. μ=12.18 cm⁻¹, D_calc=1.66 g/cm³, F₀₀₀=1032.00, R=0.062, Rw=0.087. X-ray analysis illustrated that 4,4′-bpy is mono-protonated and that there are two kinds of anions in one molecule, which give rise to the hydrogen interaction between the molecules in the crystal. Then an extended three-dimensional network is formed along the hydrogen bonds and π–π bonds between the pyridine rings.     

碱金属碳酸盐对褐煤程序升温热解过程中H2S和NH3生成的影响

以内蒙古锡盟褐煤为研究对象,通过HCl/HF洗脱煤中固有矿物质,采用机械混合法对原煤和脱矿物质煤分别负载3%的Li₂CO₃、Na₂CO₃和K₂CO₃,利用固定床程序升温热解-色谱分析法考察了煤中固有矿物质以及负载的碱金属碳酸盐对煤热解过程中H₂S和NH₃生成的影响。结果表明,煤中所固有矿物质对锡盟褐煤热解过程中H₂S和NH₃的生成和释放均有抑制作用,但对H₂S和NH₃生成的影响不同;矿物质的脱除不改变煤中有机结构及硫的存在形态,H₂S的释放温区没有发生改变,而HCN的二次反应是NH₃生成的主要来源之一,酸洗脱矿物质改变了煤中孔结构特性,从而影响不同温度段NH₃的释放。原煤及脱矿物质煤负载的碱金属碳酸盐对其热解过程中H₂S和NH₃的生成都有一定的影响,K₂CO₃除外, 负载到原煤的其他碱金属碳酸盐都抑制了H₂S的生成;Na₂CO₃除外,负载到脱矿物质煤的其他碱金属碳酸盐都促进了NH₃的生成。     

Syntheses and structural determination of nine-coordinate K3[Nd(nta)2(H2O)]·6H2O and K3[Er(nta)2(H2O)]·5H2O

The syntheses and structural determination of Nd^III and Er^III complexes with nitrilotriacetic acid (nta) were reported in this paper. Their crystal and molecular structures and compositions were determined by single-crystal X-ray structure analyses and elemental analyses, respectively. The crystal of K₃[Nd^III(nta)₂(H₂O)]·6H₂O complex belongs to monoclinic crystal system and C2/c space group. The crystal data are as follows: a=1.5490(11) nm, b=1.3028(9) nm, c=2.6237(18) nm, β=96.803(10)°, V=5.257(6) nm³, Z=8, M=763.89, D_c=1.930 g cm⁻³, μ=2.535 mm⁻¹ and F(000)=3048. The final R₁ and wR₁ are 0.0390 and 0.0703 for 4501 (I>2σ(I)) unique reflections, R₂ and wR₂ are 0.0758 and 0.0783 for all 10474 reflections, respectively. The Nd^IIIN₂O₇ part in the [Nd^III(nta)₂(H₂O)]³⁻ complex anion has a pseudo-monocapped square antiprismatic nine-coordinate structure in which the eight coordinate atoms (two N and six O) are from the two nta ligands and a water molecule coordinate to the central Nd^III ion directly. The crystal of the K₃[Er^III(nta)₂(H₂O)]·5H₂O complex also belongs to monoclinic crystal system and C2/c space group. The crystal data are as follows: a=1.5343(5) nm, b=1.2880(4) nm, c=2.6154(8) nm, b=96.033(5)°, V=5.140(3) nm³, Z=8, M=768.89, D_c=1.987 g cm⁻³, μ=3.833 mm⁻¹ and F(000)=3032. The final R₁ and wR₁ are 0.0321 and 0.0671 for 4445 (I>2σ(I)) unique reflections, R₂ and wR₂ are 0.0432 and 0.0699 for all 10207 reflections, respectively. The Er^IIIN₂O₇ part in the [Er^III(nta)₂(H₂O)]³⁻ complex anion has the same structure as Nd^IIIN₂O₇ part in which the eight coordinate atoms (two N and six O) are from the two nta ligands and a water molecule coordinate to the central Nd^III ion directly.     

贫煤O_2/CO_2气氛下燃烧时内在矿物质对SO_2和NO_x排放特性的影响

利用管式炉反应器在550-1 000℃对长治贫煤和脱矿物质煤分别在空气和O_2/CO_2气氛进行了燃烧实验。利用XRF、XRD等分析手段,对煤样的基本性能进行了分析表征,并采用热分析仪(TG-DTG)以及傅里叶红外气体分析仪(AntarisIGS)对贫煤燃烧过程中的燃烧特性和SO_2和NO_x释放规律进行了研究。结果表明,与原煤相比,脱矿物质煤的着火温度和燃烬温度有所降低;O_2/CO_2气氛下,原煤和脱矿物质煤的着火温度和燃烬温度都升高,说明当O_2浓度为20%时,空气气氛比O_2/CO_2气氛更易于着火和燃烬。此外,与长治原煤相比,脱矿物质煤在相同条件下燃烧时SO_2的释放量明显提高,而NO_x的释放量却有所降低。O_2/CO_2气氛下原煤燃烧时SO_2浓度比空气气氛下的要高,而脱矿物质煤燃烧时释放的SO_2浓度明显比空气气氛下的低;O_2/CO_2气氛下原煤和脱矿物质煤燃烧时释放的NOx浓度比空气气氛下燃烧时释放的NO_x浓度要低。