固体酸催化合成富马酸二甲酯

以固体酸硫酸氢钠为酸催化剂,浓磷酸、硫脲、溴化钠为辅助剂组成混合物催化剂,用马来酸酐和甲醇为原料多相催化一步合成富马酸二甲酯.反应的最佳条件是:硫酸氢钠0.8g,浓磷酸2.0mL,硫脲1.0g,溴化钠1.0g,马来酸酐与甲醇的物质的量的比例为1∶6.回流反应3小时,产率达80.5%,该法以固体酸硫酸氢钠取代传统酸催化剂浓硫酸,具有反应时间短,产物易于分离,催化剂可回收,对环境污染小的特点.     

经激光表面晶粒细化TiAl合金的超塑扩散连接及其数学模拟

对经TiB2(体积分数ω=0．8％)颗粒细化后Ti-45Al-2Mn-2Nb合金进行了激光表面快速熔凝处理，在其表面获得了超细晶粒组织，并在T=1073～1223K,P=40-120MPa，t=0．5-1h条件下对经激光处理后的合金进行了超塑扩散连接，研究了温度、压强和时问对连接过程的影响，建立相应的理论模型对连接过程进行了模拟,研究结果表明，在晶粒度和表面粗糙度一定的条件下，温度、压强和时间对连接过程产生重要影响，而且三者之间存在一定的关系；经过激光表面处理后的合金试样在较低温度、较低压力和较短时间下(11731K/60 MPa／Ih)可达到完全冶金结合；实验结果与模拟计算结果相一致。     

微乳模板控制合成磷酸钙盐材料

可以调控和诱导矿化的CTAB／正己醇／十六烷／水和TX100／正己醇／环己烷／水的两个拟三元微乳液体系作为磷酸钙盐矿化的“模板”．利用SEM、TEM、XRD和FT—IR等手段研究了产物的微观结构和组成．结果表明：不同的微乳及微乳中不同的相可以调控产物的形状、结构和大小，而且即使在相同的微乳体系中，由于成核作用的不同也可以导致最终产物的结构的不同．     

纳米光学功能材料Gd2O3:Tb3+的反相微乳合成及发光性能

采用反相微乳液法合成Gd2O3：Tb^3 纳米粒子，对其晶体结构、发光性能和最佳发光离子浓度进行了研究，并且与草酸盐共沉淀法制得的Gd2O3：Tb^3 相比，结果表明，其粒径减小，晶体形成温度降低了近100℃．     

基于小波变换的数字遥感影像无损压缩编码系统的设计与开发

针对遥感影像的海量数据对其自身应用的影响，指出了研究图像压缩技术的必要性，从实用的角度出发，采用面向对象的技术方法，设计并实现了基于小波变换的数字遥感影像无损压缩编码系统。     

广州夏季大气中碳气溶胶浓度水平及污染特征

2002年6-7月于广州市3个采样点采集PM10和PM25样品,测定了PM10,PM25以及元素碳(EC)和有机碳(OC)的浓度.PM10和PM2.5平均浓度分别为124.77μg@m-3及78.13μg@m-3.PM10和PM2.5中的OC浓度分别为22.3μg@m-3和15.80μg@m-3,EC浓度分别为7.78和5.90μg@m-3,其中73.8%的OC和77.7%的EC存在于PM25中.在3个采样点PM10和PM25中,OC/EC比值均大于2.0,表明广州夏季大气存在二次污染.各种气象条件对OC、EC浓度及其比值的变化都有不同程度的影响,其中降水和风速是OC、EC浓度变化的主要气象因素.     

近距离红外无线数据通信技术研究

无线电通信技术得到了前所未有的发展，而红外无线数据通信相对于无线电数据通信具有低功耗、低价格、低电磁干扰、高保密性等优点，目前发展迅猛，尤其在近距离无线数据通信中得到了广泛的应用．随着编码调制技术的发展，红外无线数据通信的数据速率越来越高，成为许多移动设备、室内办公设备以及手持设备无线数据通信的一个重要途径．本介绍了红外数据通信的原理，分析了红外数据通信技术中关于收发器、控制器、通信协议等关键环节的技术现状，总结了红外数据通信技术的研究进展，并对红外无线通信技术的工程应用前景进行了展望。     

Comparison of metallogenesis and resource potential on the eastern margin of the Jiangnan Upheaval between south Anhui (Wannan) and northeast Jiangxi (Gandongbei) provinces

The southern and northern parts of the eastern margin of the Jiangnan Upheaval, located in the northeast of Jiangxi Province (Gandongbei) and the south of Anhui Province (Wannan) share many similar characteristics of basement composition and structural evolution. However, the two areas have very different metal endowments and ranges of deposit types. The aim of this paper is to compare the metallogenic conditions of the two areas in order to analyze the reasons for these differences and to estimate the preliminary resource potential of the studied areas. It is concluded that difference of the crust-mantle interactions, especially the Yanshanian magmatism in the two areas, is the main reason resulting in difference in the ore-forming processes between Wannan and Gandongbei. The resource potential of Gandongbei is significantly greater than that of Wannan.     

Approaches to prediction of impact of Qinghai-Tibet Railway construction on alpine ecosystems alongside and its recovery

With the aid of the Remote Sensing (RS) and Geographic Information System (GIS) technology, the ecosystem pattern and fragility distribution maps of the 50-km-wide zone along the Qinghai-Tibet Railway were compiled and by using the superimposition method, range, area and indexes of the impact of various engineering activities on the ecosystems alongside the railway were studied. By making reference to the ecosystem recovery process of the Qinghai-Tibet Highway, mechanisms of recovery of the alpine ecosystems alongside the Qinghai-Tibet Railway were studied and extents and rates of the recovery were predicted.The results indicate that the impact of the railway engineering on the Alpine ecosystem depends mainly on how much the original surface soil in the zone has been disturbed and how fragile of the ecosystem per se. Restoration of vegetation coverage and species abundance shows a significantly reverse relationship with disturbance of the original surface soil but an extremely positive one with the length of the restoration period and mean annual precipitation and annual mean relative humidity in the period and no obvious bearings with altitude and temperature. In sections with an annual precipitation over 200mm, as long as a certain percentage of original soil is left in situ, it takes only 30 years or so for biodiversity to get basically restored to the original level after the construction is completed but at least 45-60 years or more for vegetation coverage.     

Analysis of carbon isotopes in airborne carbonate and implications for aeolian sources

Methods were developed to determine the mass ratios of carbon isotopes in trace amounts of aerosol carbonate. A Finnigan MAT 252 mass spectrometer fitted with an on-line Kiel device was to determine the ^13C/^12C ratio in CO2 produced from the carbonate. A study using these methods was conducted to characterize the carbonate carbon isotopes in aerosol samples collected in Xi‘an on dusty and normal days during March and April 2002. Results of the study demonstrate that insights into the origin of the dust can be deduced from its isotopic composition. That is, the δ^13C ofcarbonate for dust storm samples ranged from -1.4‰ to -4.2‰, and this is consistent with sandy materials in dust source regions upwind. In contrast, for non-dusty days δ^13C ranged from -7.5% to -9.3‰, which is more similar to fine particles emitted from local surface soils. Comparisons of dust storm aerosols with surface soils from source regions and with aerosol samples collected downwind indicate that the δ^13C values did not change appreciably during longrange transport. Therefore, carbon isotopes have the potential for distinguishing among source materials, and this approach provides a powerful new tool for identifying dust provenance.