粒度对纳米氧化锌与硫酸氢钠溶液反应动力学的影响

以纳米氧化锌与硫酸氢钠溶液的反应为模型体系,研究了反应物粒度对动力学参数的影响规律。结果表明:反应物的粒度对反应的速率常数、反应级数、表观活化能和指前因子均有较大的影响;随着反应物粒径的减小,速率常数增大,反应级数增大,表观活化能减小,指前因子减小,并且表观活化能与反应物粒径的倒数呈线性关系。     

非晶Fe77.5Si8.5B14合金晶化动力学的非等温方法研究

利用非等温差示扫描热分析法(DSC)研究了非晶Fe77.5Si8.5B14合金的晶化动力学.不同升温速率的DSC曲线表明非晶Fe77.5Si8.5B14合金的晶化过程为两步晶化.通过对不同升温速率的DSC曲线的分析,计算了两个析晶峰的晶化表观激活能E1(388.2 kJ·mol-1)和E2(339.0 kJ·mol-1),以及两个析晶峰的Avrami指数n1(1.7)和n2(3.3).根据动力学参数分析了非晶Fe77.5Si8.5B14合金的析晶机理晶化峰1的成核类型为均匀成核,晶粒生长为扩散控制的一维生长和二维生长;晶化峰2为整体析晶,晶粒生长以界面控制的二维生长和三维生长为主.最后结合表观激活能计算了两个析晶反应的频率因子ν1(4.05×1025)和ν2(1.14×1021).     

碳酸钙热分解反应动力学的不同方法研究

因比较法和主曲线法在求算热分解动力学"三因子"时基本原理和处理方法不同,为此而探讨了2种方法处理的结果是否一致.利用热重分析(TGA)技术研究了碳酸钙热分解过程,通过这2种方法分别求算了碳酸钙热分解反应动力学"三因子".比较法结果:活化能Ea为174.00kJ·mol-1,指前因子A为9.63×106s-1,机理函数微分形式和积分形式分别为f(α)=2(1-α)1/2和g(α)=1-(1-α)1/2;主曲线法结果:活化能Eα=169.81 kJ/mol,指前因子A=3.84×106s-1,机理函数微分表达式为f(α)=2(1-α)1/1.57,积分表达式为g(α)=1-(1-α)1/1.57,2种方法所得结果基本吻合,说明这2种方法判定动力学"三因子"的一致性和可靠性.     

心灵的后花园--穆旦晚年诗歌创作享虐心理探析

本文从穆旦晚年对诗及诗歌创作中的准自虐现象中探析其享虐心态的成因，以透视当代知识分子隐秘的内心和精神历程。     

铸造镍基高温合金K35的氧化动力学

用静态增重法研究了K35镍基铸造高温合金的800℃氧化动力学·结果表明,K35合金的氧化动力学遵循抛物线规律,属于完全抗氧化级·利用X射线衍射、扫描电镜和能谱分析确定K35合金氧化膜组成以Cr2O3为主,含有NiCr2O4及TiO·TiO2·由于钛氧化物的存在,在高温氧化期间,K35合金发生了内氧化·     

KOH催化环氧树脂与丙烯酸反应的动力学研究

研究了以KOH为催化剂催化环氧树脂与丙烯酸反应的动力学行为，讨论了催化剂浓度以及温度对该反应的影响。结果表示：KOH是有效的催化剂，当其用量为环氧树脂与丙烯酸质量和0.5%-0.7%jf ,在90-110℃反应，在较短时间内可达到较高的转化率；该反应为一级反应，表观活化能为61.5kJ/mol。     

铜离子金属胶束介质中PNPA水解的动力学研究

研究了25℃时，铜离子与二胺类配体DMEA和DMPA(DMEA为N，N－二甲基乙二胺，DMPA为N，N－二甲基－1,3－丙二胺)形成的配合物对PNPA(对硝基苯酚乙酸酯)催化水解的动力学，并通过了胶束催化的二元复合物动力学模型对其进行定量处理，结果表明，铜离子与不同的二胺类配体形成的配合物在CTAB胱束溶液中对PNPA的催化水解表现出不同的催化效果，而催化的机理则可能是由于与铜离子配位的水分子去质子化以后形成的亲核体对PNPA进行亲核进攻的结果。     

Kinetics of Growth and Nutrient Consumption in the Culture of Trichosanthes kirilowii Hairy Root

IntroductionThe hairy roots produced by Agrobacteriumrhizogenes infection are characterized by highgrowth rate and genetic stability. Thesegenetically transformed roots can produce similarhigher levels of secondary metabolites than intactplants[1] ,so hairy root cultures are a promisingmethod for producing valuable secondarymetabolites of many plants.Recently,two kindsof ribosome- inactivating proteins ( RIPs) [2 ] ,trichosanthin ( TCN ) [3 ] ,and TAP 2 9[4] wereidentified in Trichosanthes…     

The age of formation of the mirabilite and sand wedges in the Hexi Corridor and their paleoclimatic interpretation

The Hexi Corridor is located at the transition zone of the Asian summer monsoon and westerly airflow, and lies in an important position in terms of its ecological fragility and climatic sensitivity. During a recent field expedition to this region, we found a sedimentary mirabilite layer in a number of localities including Suwushan, Yanchi, Baitujing, Yanchi Gaotai, Huahai, Yumen, Halanuo扙r, and Dunhuang (Fig. 1), which have the potential to provide important information about environmenta…     

Triassic U-Pb age for zircon from granites in the Tonghua area and its response to the Dabie-Sulu ultrahigh-pressure collisional orogenesis

Single-grain zircon U-Pb dating was carried out to constrain the emplacement timing of granitic plutons at Chaxinzi, Xiaoweishahe and Longtou in the Tonghua area, south of Jilin Province. The results show that these plutons formed in the Triassic with ages of 203—217 Ma. Geological and geochemical characteristics indicate that the plutons are composed of quartz diorite and granite. The former was derived from partial melting of mafic lower crust, whereas the latter originated from thickened crust with garnet as the residue in the source. It appears that protoliths of these two types of granitits are different although they have the same emplacement age. Considering that these plutons are petrologically different from the coeval granites in the Xingmeng (Xing‘an-Mongolian) to Jihei (Jilin-Heilongjiang) orogenic belt in the north, it is suggested that their formation was related to the Dabie-Sulu ultrahigh-pressure collisional orogenesis since their ages are only 10—20 Ma younger than timing of the ultrahigh-pressure metamorphism, but comparable to that of the first rapid exhumation of the ultra-high-pressure metamorphic rocks and the emplacement of the post-collisional granites.