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This document is copyright 1996 Ambrose Au, and it's a free document.

这份文件版权属於 Ambrose Au 1999，而且是免费的文件。

The specific heat,the enthalpy and the density of liquid Au-Cu and Ti-Al alloys behave anomalously,and the Neuman-Kopp rule does not apply to these two bianary systems.

对Au-Cu和Ti-Al合金的比热和密度进行了系统的模拟，发现比热和密度偏离理想行为，Neuman-Kopp定律不适用。

The results showed that Au doping did not affect the texture properties of La0.8Sr0.2MnO3, but Au actually enhanced the surficial oxygen mobility of catalysts, and increased catalytic oxidation activity at a low temperature.

结果表明，Au掺杂并不改变La0.8Sr0.2MnO3催化剂的织构性质，但明显增强了催化剂表面氧的活动性，提高了其低温催化氧化活性。

An investigation of Au/Ti/Ni and Au/Ti/Pt ohmic contacts to n-type 4H-SiC and the behavior of metal films on SiC with thermal anneals is reported.

研究了热退火条件下Au/Ti/Ni-4H-SiC欧姆接触形成机制。

Based on the detailed study of seismic tomography image in South China, and according to the geotectonic environment and shape and heat of asthenosphere upwelling, we divided the structure of lithosphereasthenosphere at the Mesozoic upper mantle of Eastern China into three types.(1)Continental platform area (North China platform and Yangtze platform): asthenosphere upwelled along paleorift; over the plume head, the granitic rocks of crust and mantle mixed and correspondingly, Au, Cu, Mo, PbZn, etc. mineralizationconcentrated regions were formed; and at the steep contact belt of asthenosphere and the thick area of lithosphere, mediatebasic complex was formed.(2)Central area of fold zone: asthenosphere was "recumbent" at suitable depth, with adequate heat and in a great extent; by heat conduction, the interior of partial crust remelted, and the crustsource granitic rocks, and correspondingly, W, Sn and rare elements mineralizationconcentrated regions were formed.

在深入研究华南地震层析成像的基础上，按照大地构造环境和软流圈上涌形状和热度，将中国东部中生代上地幔中岩石圈软流圈构造划分为3类：(1)陆台区，软流圈沿古裂陷上涌，其柱头上方形成幔壳混熔花岗质岩及相应Au、Cu、Mo、PbZn等矿集区，并于软流圈与岩石圈厚区之陡接触带形成中基性杂岩及相应Fe矿集区；(2)褶皱带中心区，软流圈在适当深度、热量充足、较大范围内&平卧&，因热传导而致使地壳内物质部分重熔，形成壳源型花岗质岩及相应的W、Sn、稀有元素矿集区；(3)褶皱带边缘区(大兴安岭南部及华南南缘)，在软流圈上涌柱上方形成幔源或幔壳混熔的花岗质岩，相应为Cu、Au、PbZn、Mo、Ag矿集区。

The mixing of the mother magmas and the crustal matters released Cu, Au-bearing epithermal. These ore metal-bearing epithermal ultimately formed ore deposits in the Tongling region.

我们认为，俯冲作用导致板片洋壳部分释放的超临界流体，受其影响地幔楔熔融形成富集S等挥发份和Cu、Au等成矿元素的母岩浆，为铜陵地区提供了成矿物质来源，其与地壳物质的混合释放出含Cu，Au的热液，最终形成铜陵地区目前矿床分布格局

Among the present methods for protein detection using aptamers, some of them are with high sensitivity, some with high sensitivity but require expensive instrument. This study takes use of aptamer modified by Au naloparticle to construct a new method for protein detection. This methos can fastly detect proteins with high sensitivity compairing to other methods, and requires no expensive instruments. It has wide application prospect and large market value.

当前利用Aptamer的蛋白质检测方法，有的灵敏度不是很高，有的虽有较高灵敏度，但需要昂贵的仪器，本研究利用金纳米颗粒(Au nanoparticle，Au NP)修饰的Aptamer来建立一个蛋白质检测的新方法，与其他方法相比，本方法有较高灵敏度、不需昂贵仪器，简单快捷，具有广泛的应用前景和巨大的市场价值。

It is also found that Au content varies substantially in different crystal striations, therefore it is proposed that Au came into the crystal structure of the arsenopyrites when they formed.

此外，金含量在不同的生长环带中有显著变化，表明Au是在毒砂形成过程中进入其晶格的。

One monolayer of CSB deposited on Au/Ge(111)-√3 at 220 K followed by cooling to 100 K leads to the formation of a well ordered (2×1) structure as observed by LEED. The TPD spectra for CSB thermal desorption from Au/Ge(111)-√3 exhibit showed two well-resolved peaks at Tp = 243 and 274 K corresponding to multilayer and monolayer desorption, respectively.

我们也尝试利用LEED观察二苯乙烯吸附在(√3×√3)R30°表面的规则排列，并且成功看到(2×1)的LEED绕射图谱，另外我们也架设一组氦氖雷射来测定表面上吸附物的光学反射率变化，在金属覆盖的锗(111)单晶表面上，确定Au覆盖量不同会造成反射的变化。

Using a three-strand hybridization system, we were able to conjugate oligonucleotides modified Fe2O3 and Au nanoparticles.

经由杂交所形成的复合物(Au/Fe2O3)，在加热至70℃的温度下，会破坏氢键，使复合物(Au/Fe2O3)分开，而回溶於水溶液中。

Do you know, i need you to come back

你知道吗，我需要你回来

Yang yinshu、Wang xiangsheng、Li decang,The first discovery of haemaphysalis conicinna.

1〕 杨银书，王祥生，李德昌。安徽省首次发现嗜群血蜱。