pH为10至11时羟基磷灰石液相生成动力学

利用液相沉淀法研究了ｐＨ为１０－１１时，「Ｃａ＾２－」浓度大于０．５ｍｏｌ／Ｌ条件下基磷灰石的生成机理及其动力学。结果表明反应经历了从磷酸八钙很快转化为非晶态磷酸钙，继而转化为缺钙羟基磷酸石和羟基磷灰石的过程。     

动态表面张力与铜离子浮选的传质系数

应用单泡吸附模型处理铜离子浮选的动力学，提出了测定动态表面张力数据求算该浮选过程传质系数Ｋ_２的新方法。研究了溶液的酸度对传质系数ｋ_２的影响，所求得的最佳酸度（ｐＨ＝５．０）与实验结果完全一致。发现在ｐＨ＝２～５的范围内，ｋ２与浮选实验值ｋｅｘｐ．２存在良好的线性关系。     

钴（Ⅲ）配合物取代反应的动力学研究

用分光光度法研究了在ｐＨ为８．５７的３０％（ｖ／ｖ）乙醇溶液中，甘氨酸与二羟基二邻菲罗琳钴（Ⅲ）配合物取代反应的动力学。提出其反应机理为交换高解机理，根据静态平衡，推导其反应速度公式，并求得其反应的△Ｈ￣＋＝８２．８３ｋＪ·ｍｏｌ￣（－１），△Ｓ￣＋＝７９．４２Ｊ·ｍｏｌ￣（－１）·Ｋ￣（－１）。     

纺锤形铁黄α－FeOOH微晶合成动力学研究

本文对纺锤形α－ＦｅＯＯＨ微晶合成动力学过程进行了研究．利用复相反应经验动力学方程，考察了初始浓度、反应温度和空气流量对Ｆｅ（ＯＨ）２－ＰｅＣＯ３悬浮液氧化速率的影响，确定了α－ＦｅＯＯＨ成核－生长速率方程，证实了晶粒生长阶段存在溶解－氧化的动态平衡，根据活化能大小，推断相界面氧化反应为该复相反应的控制步骤，还对α－ＦｅＯＯＨ成核生长微观机理作了初步探讨．     

聚苯硫醚与尼龙6共混物的非等温结晶动力学

本文用差示扫描量热法(DSC)研究了聚苯硫醚(PPS)与尼龙6(N6)共混物的非等温结晶动力学,并以四种不同的数据处理方法进行了分析比较。结果表明,随着冷却速率的提高,PPS 及其共混物从熔体开始结晶的温度降低;相同冷却速率下,共混物中的 PPS 的起始结晶温度较纯 PPS 为高。Ozawa 方法及 Harnisch 和 Muschik(H-M)法均能较好地处理该体系的非等温结晶动力学数据,由这两种方法所获得的 Avrami 指数 n 值非常接近。     

钙钛矿型复合氧化物催化剂La_(0.4)Sr_(0.6)Mn_(0.6)Co_(0.4)0_3上CO氧化动力学

常压下,采用内循环无梯度反应器在160～200℃温度范围内考察了钙钛矿型复合氧化物催化剂 Lao_(0.4)Sr_(0.6)Mn_(0.6)Co_(0.4)O_3上一氧化碳氧化动力学.实验数据经多元线性加权最小二乘法拟合.其结果为一氧化碳氧化速率对 CO 和氧分压分别呈0.49级和0.48级的动力学行为.反应的表观活化能为64.0 kJ/mol.并根据动力学行为讨论了该催化剂上 CO 氧化的可能机理.     

化学沉淀过程中形成的胶粒团聚体结构的计算机模拟

以正滴淀和反滴淀两种沉淀方式制备氢氧化锆凝胶,对其凝胶团聚状态的扫描电镜观察发现,在正滴淀方式下,胶粒主要以P-C(Particle-Cluster)团聚方式团聚,在反滴淀方式下,胶粒主要以C-C(Cluster-Cluster)团聚方式团聚。运用MonteCarlo法对P-C和C-C两种团聚方式下形成的胶粒团聚结构进行了计算机模拟,结果表明,以P-C团聚方式形成的胶粒团聚体结构致密,以C-C团聚方式形成的胶粒团聚体结构较松散,在沉淀过程中加入具有空间位阻作用的粒子可使形成的胶粒团聚体结构更松散。     

Abnormal austenite-ferrite transformation behavior in pure iron

The austenite → ferrite transformation is themost important reaction route in the manufacture ofFe-based materials. Here the austenite (γ) → ferrite (α)transformation of pure iron was systematically explored byhigh-resolution dilatometry. Abnormal transformation ki-netics, multi-peak discontinuous reaction, was recognized inpure iron according to the variation of the ferrite-formationrate. The occurrence the one or the other type of γ→∝ trans-formation strongly depends on the grain size: the transfor-mation type changes from abnormal to normal (single-peakcontinuous reaction) with decreasing grain size. The inherentreason for the occurrence of abnormal transformation couldbe attributed to the repeated nucleation in front of the mov-ing γ/α interface induced by the accumulation of elastic andplastic accommodation energy.     

JWA protein binds to α-tubulin in PC12 cells

Our previous study elucidated that JWA protein was a newly identified microtubule-associated protein (MAP), which combined to and co-localized with α-tubulin. In the present study, we designed a series of experiments to explore if any interactions between JWA protein and α-tubulin existed and how JWA protein would functionally link to α-tubulin, especially in cell mitosis. Results of coimmnnoprecipitation, gene transfection and immnnoflnores-cence microscopy from PC12 and HEK293 cells provided strong evidence for a linkage between JWA protein and α-tubulin. Our data showed that JWA protein bound to α-tubulin stably no matter whether α-tubulin was polymerized or not. In addition, by using antisense oligonncleotides, cell cycle blocking agents and hypothermia disposal techniques, we also found the interaction between JWA protein and α-tubulin. The further analysis using flow cytometry and confocal microscopy showed that both proteins co-existed in PC12 cells and were independent on the cell cycle. In conclusion, JWA protein is a newly identified microtnbnle-associated protein, binds to α-tubulin, and probably plays an important role in regulation of microtnbnlar stability.     

The forecast of seasonal precipitation trend at the north Helan Mountain and Baiyinaobao regions,Inner Mongolia for the next 20 years

By using Caterpillar-SSA analysis method, through the process of embedding, singular value decomposition, grouping and diagonal averaging, the seasonal precipitation trend at north Helan Mountain and Baiyinaobo regions, Inner Mongolia for the next 20 years is forecasted. The results show an increasing precipitation trend from 1992 to 2004. In the subsequent decade the precipitation should reduce quickly, and it will reach a minimum near 2012 to 2014 in both regions. The drought caused by the decrease of the precipitation from May to July in the north Helan Mountain area during the period of 2013-2014 is probably quite similar to that around 1929. Further, the period of precipitation gradual increase follows in the researched regions.