InGaN/AlGaN双异质结绿光发光二极管

报道了用LP-MOVPE技术在蓝宝石(α-Al_2O_3)衬底上生长出以双掺Zn和Si的InGaN为有源区的绿光InGaN/AlGaN双异质结结构，并研制成功发射波长为520-540nm的绿光LED。

GSMBE GaN 膜的电子输运性质研究

用NH_3作氮源的GSMBE方法在晶向为(0001)的α-Al_2O_3衬底上生长非有意掺杂的单晶GaN外延膜，GaN膜呈N型导电，室温时的最高迁移率约为120cm~2/(V·s),相应的非有意掺杂电子浓度为9.1×10~(17)cm~(-3)。对一些GaN膜进行了变温Hall测试，通过电阻率、背景电子浓度以及Hall迁移随温度的变化研究了GaN外延膜的导电机理。结果表明，当温度较低时，以电子在施主中心之间的输运导电为主；当温度较高时，以导带中的自由电子导电为主。

GaN材料的GSMBE生长

在国内首次用NH_3作氮源的GSMBE方法在α-Al_2O_3衬底上生长出了GaN单晶外延膜。GaN生长速率可达0.5μm/h。GaN外延膜的(0002)双晶X射线衍射峰回摆曲线的半高宽最窄为8arcmin，霍尔迁移率为50cm~2/V·s。对质量好的GaN膜，室温阴极发光谱上只有一个强而锐的近带边发光峰，谱峰位于372nm处，谱峰半高宽为14nm(125meV)。

Ti和蓝宝石的界面反应

在超高真空中用电子束蒸发在抛光的(1102)取向的蓝宝石(a-Al_2O_3)衬底上蒸镀500 nm的Ti膜,在恒温炉中退火,然后用XRD(包括一般的和小角度的X射线衍射),AES和SIMS等表面分析技术详细研究了从室温至850℃,Ti与a-Al_2O_3的固相界面反应.首次系统提出了不同反应温区相应的化学反应式,讨论了采用体材料数据作热力学计算来预言Ti/a-Al_2O_3界面反应的局限性.

GaN的MOCVD生长

GaN是重要的蓝光半导体材料。以TMGa和BH_3为源在(0112)α-Al_2O_3衬底上成功的用MOCVD方法生长了GaN外延层,研究了GaN的表面形貌与结晶学、电学和光学特性。GaN(2110)面的双晶回摆曲线衍射峰的最小半高宽已达16'。并观测到GaN所发出的紫外可见光波段的阴极荧光。

基于第一性原理的金属/氧化物界面结合强度与宏观韧性的系统性研究

<正>总结介绍作者们多年来发展的基于第一性原理的系统性研究金属/氧化物界面结合强度和宏观韧性的策略方法。以应用广泛的γ-Ni/α-Al_2O_3界面为例,从第一性原

Eu~(2+)在多铝酸钠体系中的发光

应用高温固相法合成了Na的多铝酸盐，并研究了Eu2＋在体系中的发光性能．结果表明，Na1＋xMgAl11－xO17体系在整个组成范围内保持Na的β－Al2O3结构不变，而对于Na1．67－2xBaxAl10．33O17体系，在x＝0．30附近体系结构发生转变，x＜0．30，体系形成Na的外β－Al2O3结构的固溶体，x＞0．30，体系形成Ba的β－Al2O3结构的有序体；与体系组成和结构的变化相对应，Eu2＋的发射能量和发光强度产生相应的变化，在Na的β－Al2O3中Eu2＋存在高、低能两种发射中心；通过系列化研究，获得了新的组成的、具有β－Al2O3结构的荧光体Na0．67Ba0．50Mg0．67Al10．33O17：Eu2＋，在较低的掺杂浓度（0．05mol）下可以产生较强的发光.

硼酸盐玻璃中Gd~(3+)、Dy~(3+)、Bi~(3+)对Tb~(3+)发光性质的影响

本文研究了单掺和双掺(Tb~(3+)、Tb~(3+)+Gd~(3+)、Tb~(3+)+Dy~(3+)、Tb~(3+)+Bi~(3+)约四十余种不同成份的硼酸盐玻璃。探讨了玻璃成份对Tb~(3+)发光性质的影响和Gd~(3+)、Dy~(3+)、Bj~(3+)对Tb~(3+)的胜化作用。在B_2O_2-BaO-M_mO_n(M_mO_n=Li_2O、Na_2O、K_2O、MgO、CaO、SrO、Al_2O_3、La_2O_3和Bi_2O_3)玻璃体系中,当M_mO_n分别为MgO和Al_2O_3时,Tb~(3+)的发光强度最强;M_mO-n为Bi_2O_3时,Tb~(3+)的发光强度最弱。Tb~(3+)的特征发射峰分别随着碱金属、碱土金属和三价金属的离子半径增加而红移。Gd~(3+)、Dy~(3+)、Bi~(3+)对Tb~(3+)均有敏化作用。特别是Gd~(3+),使Tb~(3+)的发光强度增加1～3.8倍,其最佳敏化浓度,因基质玻璃成份而异。

LaMn_(1-y)Fe_yO_3对CH_4和CO的催化氧化作用

用程序升温脱附试验考察了LaMn_(1-y)Fe_yO_3型催化剂中B位元素对Co、CH_4氧化活性的影响。发现催化剂的活性与TPD谱上脱氧峰的位置及面积有关,同一催化剂对CO与CH_4的氧化活性中心并不一致。以γ-Al_2O_3为载体制得的锰系ABO_3型催化剂在浸渍微量氧化物助催化剂后,能使CO在130℃完全氧化,CH_4的氧化温度为300～500℃。

Sm~(3+)在硼酸盐玻璃中的发光及Bi~(3+)对Sm~(3+)的敏化作用

早在六十年代,人们为了寻找较好的激光玻璃,曾对Sm~(3+)离子掺杂的玻璃中的光谱进行过研究。为了探寻新型的激光,发光玻璃,又进一步研究了Sm~(3+)在玻璃中的发光和敏化。我们以寻找一种高亮度,低成本的发光玻璃为目的,研究了基质玻璃组成,敏化离子及其浓度对Sm~(3+)发光性质的影响。 选择B_2O_3-BaO-M_mO_n(M_mO_n=Li_2O,Na_2O,K_2O,MgO,CaO,SrO)玻璃体系,所用原料的纯度皆为分析纯以上,用陶瓷坩埚在1250℃掺杂氧化钐(纯度均大于99％),玻璃的荧光谱和激发光谱,用MPF-4型荧光分光光度计测定。

H_2O/C复合微粒子的光学截面及红外发射率光谱的计算

在文献[1]的基础上,利用A. L. Aden和M. Kerker复合粒子Mie散射理论,计算了H_2O/C复合微粒子的散射、吸收、消光截面及发射率光谱,并与C/H_2O和Al_2O_3/C复合微粒子的结果进行比较和讨论。

含La耐硫水煤气变换催化剂的研究

CoMoK/Al_2O_3耐硫水煤气变换催化剂中加入La_2O_3后其活性与含量和处理温度有关。含有0.5—1.0％La_2O_3的催化剂和载体经600℃处理活性和耐热性最高。在500℃进行强化反应后La助化的催化剂活性下降～50％,而无La的下降～70％。以H_2S/H_2重新处理减活后的催化剂可以使活性逐渐恢复,但含La的比不含La的恢复得快。由催化剂的硫化过程和程序升温还原及吡啶吸附实验未能发现两种催化剂有明显的区别。XPS测定结果发现La助化的催化剂在反应时,其Mo可以保持较好的分散和较少形成Mo~(6+),而Mo~(6+)对反应是无活性的。

新疆东昆仑蛇绿岩岩石学、地球化学特征及其大地构造意义

The East Kunlun area of Xinjiang (briefly EKAX) is the western part of broadly speaking East Kunlun orogenic zone. The absence of geological data (especially ophiolites) on this area has constrained our recognition to its geology since many years. Fund by National 305 Item (96-915-06-03), this paper, by choosing the two ophiolite zones (Muztag and Southwestern Margin of Aqikekule Lake ophiolite zones) exposed at EKAX as the studied objects and by the analysis of thin section, electron probe, XRF, ICP-MS, SEM and Sm-Nd isotope, totally and sys ematically dealt with the field geological, petrological, minerological, petrochemical and geochemical characteristics (including trace, rare earth element and Sm-Nd isotope) and the tectonic setting indicated by them for each ophilite zone. Especially, this paper discussed the trace and rare earth element patterns for metamorphic peridotites, their implications and related them to the other components of ophiolite in order to totally disclose ophiolite origins. Besides, this paper also studied the petrological, geochemical and paleobiological characteristics for the cherts coexsisted with the Muztag ophiolite and the tectonic setting indicated by them. Based on these, the author discussed the tectonic evolution from Proterozoic to Permian for this area. For Muztag ophiolite, their field geological, petrological, minerological, petrochemical and geochemical characteristics show that: ① outcropped along the Muztag-Jingyuhu fault with west-to-east strike, the ophiolite is composed of such three components as metamorphic peridotites, cumulates and volcanic rocks; ② metamophic peridotites consist of such types as lherzolites, serpentinized lherzolites and serpentinites, only pyroxenites is seen of cumulates and volcanic rocks include basalts, basaltic andesites and andesites; ③ mineralogical data on this ophiolite suggest it formed in supra-subduction zone (SSZ)environment, and its mantle wedge is heterogeneous; ④ whole-rock TiO_2 and Al_2O_3 of metamorphic peridotites indicate their original environment with the MORB and SSZ characteristics; ⑤ metamorphic peridotites have depleted LREE and flat REE patterns and volcanic rocks have enriched LREE patterns; ⑥ trace element characteristics of metamorphic peridotites imply that they had undergone Nb and Ta enrichment event after partial melting; ⑦ trace element characteristics of volcanic rocks and their tectonic diagrams show they are formed in the spreading and developed island arc environment with back-arc basin, such as rifted island arc, which is supported by the ε_(Nd)(t) -2.11～+3.44. In summary, the above evidence implies that Muztag ophiolite is formed in SSZ environment, where heterogeneous mantle wedge was metasomatised by the silica-enriched melt from subducted sediments and/or oceanic crust, which makes the mantle wedge enriched again, and this enriched mantle wedge later partially melted to form the volcanic rocks. For Southwestern Margin of Aqikekule Lake ophiolite, their field geological, petrological, minerological, petrochemical and geochemical characteristics show that: ① it outcropped as tectonic slices along the near west-to-east strike Kunzhong fault and is composed of metamorphic perodotties, cumulates and volcanic rocks, in which, chromites are distributed in the upper part of metamorphic peridotites as pods, or in the lower part of cumulates as near-strata; ② metamorphic peridotites include serpentinites, chromite-bearing serpentinites, thlorite-epidote schists and chromitites, of which, chromitites have nodular and orbicular structure, and cumulates include pyroxenits, serpentinites, chromite-bearing serpentinites, chromites and metamorphically mafic rocks and only basalts are seen in volcanic rocks; ③ Cr# of chromites suggest that they formed in the SSZ and Al_2O_3 and TiO_2 of metamorphic peridotites also suggest SSZ environment; ④metamorphic peridotites have V type and enriched LREE patterns, cumulates have from strongly depleted LREE, flat REE to enriched LREE patterns with universally striking positive Eu anomalies and basalts show flat REE or slight enriched LREE patterns with no Eu anomalies; ⑤ trace element and Sm-Nd isotope characteristics of metamorphic peridotites imply their strikingly heterogeneous mantle character(ε_(Nd)(t)+4.39～+26.20) and later Nb, Ta fertilization; ⑥ trace element characteristics of basalts and their tectonic diagrams show they probably formed in the rifted island arc or back-arc basin enviromnent. In summary, the above evidence shows that this ophiolite formed in the SSZ environment and melts from subudcted plate are joined during its formation. Rare earth element, whole-rock and sedimentary characteristics of cherts with the Muztag ophiolite show that they formed in the continental margin environment with developed back-arc basin, and radiolarias in the cherts indicate that the upper age of Muztag ophiolite is early carboniferous. Based on the accreted wedge models of Professor Li Jiliang for Kunlunshan Mountain and combined with study on the two typical ophiolite profiles of EKAX, the author discussed the tectonic evolution of EKAX from Proterzoic to Permian.

攀西地区红格、新街岩体的岩石地球化学特征

The mafic-ultramafic layered intrusions in the Panxi, China contain large V-Ti-magnetite deposits. These layered intrusions are related with the Emeishan continental flood basalts in space and time. Two layered intrusions, Hongge and Xinjie have clear PGE mineralization at the base of the intrusions. Thus the detailed investigations of these two intrusions not only have a geological but also have an economic significance. This thesis aims to characterize the elemental and Sr-Nd isotopic features of diverse rock zones within the intrusion on the basis of systematic studies of the major, trace element and isotope ratios, therefore to constrain the petrogenesis, mantle source and evolution of the Hongge and Xinjie intrusions. Generally, both Hongge and Xinjie intrusions show the same Fe-Ti-rich and Si-M-poor characteristics. They are also enriched in rare-earth elements (REE) and large-ion lithophile elements (LILE) as well as in Sr-Nd isotope ratios (Hongge: initial Sr = 0.7056-0.7076, ε_(Nd)(t) and (Nd/Sm)_N-ε_(Nd)(t) plots, the Hongge intrusion has a similar elemental and isotopic features to the Emeishan low-Ti (LT) basalts, whereas the Xinjie intrusion was close to the Emeishan high-Ti (HT) basalt. Therefore, the Hongge intrusion may be co-genetic with the LT basalt, formed by the partial melting of the spinel-garnet transition mantle that had a slight enriched isotope character. In contrast, the Xinjie intrusion and the HT basalts are probably derived from the garnet-phases mantle with a primitive isotope character. The involvement of the components of mantle wedge into the source is considered to be the major reason of the REE and LILE enrichment and Nd isotope depletion in the Xinjie intrusion. In contrast with the systematic variations in TiO_2 content, Mg#, transition elements (Ni, Cu, Co), REE concentrations, and La/Yb, La/Sm ratios from the lower zone to upper zone, the different rock zones of the Hongge intrusion have no clear Sr-Nd isotope variations. This suggests that the Hongge intrusions were formed by the crystal fractionation from the same magma source. The rhythm may be formed by slow injection of the co-genetic magma during the crystal fractionation. The increase in K_2O and Al_2O_3 contents, REE abundance, and the degree of the REE fractionation in the base of the intrusion, together with the relatively low ε_(Nd)(t) value, may imply that the base of the Hongge intrusion was contaminated with the local crust rocks. Xinjie intrusion shows the clearly elemental and isotopic differences in diverse cumulus cycles. The observation of the systematic variations in TiO_2 content, Mg# value, transition elements (Ni, Cu, Co), REE concentrations, and La/Yb, La/Sm ratios in first cycle was not occurred in second cumulus cycle. In addition, the ε_(Nd)(t) value in second cumulus cycle is apparently higher than that of the first one. Thus the abruptly elemental and isotopic changes at the base of second cycle demonstrate that there is considerable new and depleted magma addition to the residue magma after the crystallization of the first cycle. These features are very similar to those of the well-known PGE-rich Bushveld and Stillwater layered intrusions. The PGE mineralization in Xinjie intrusion is much better than in Hongge intrusion. Therefore, the layered intrusion similar to the Xinjie in Panxi area posses the better prospects for the PGE deposits.

晋北高岭石及其热产物的矿物物理学研究

通过对晋北地区高岭石及其热产物的研究，笔者主要得到了以下几点结论：1、晋北煤矸石是一种优质的高岭石，Fe、Ti含量低，结晶度高，晶体主要呈片状形态，具有较好的开发前景，应打破仅仅局限于陶瓷工业的局面。而P-1高岭石因Fe、Ti含量高，质量差。2、在高岭石受热脱羟过程中，部分羟基一直到850℃才完全脱失。3、在高岭石-莫来石反应系列中，存在SiO_2与Al_2O_3的分凝，SiO_2与Al_2O_3反应生成莫来石是莫来石的主要形成途径，Al-Si尖晶石与SiO_2反应生成莫来石只是一个次要途径。4、在高岭石热处理产物的研究中首次测到了-70ppm附近的Al-Si尖晶石的~(29)Si MAS NMR谱峰，Al-Si尖晶石是一个不稳定相，存在的温度范围大约为850-1000℃，随着温度升高，它将转变为莫来石。5、高岭石的980℃放热峰归因于在高岭石受热相变过程中，莫来石、方英石、γ-Al_2O_3的晶出。6、在煤矸石中，Fe主要以Fe~(2+)置换Al~(3+)形式存在，其次是部分Fe~(2+)被吸附在高岭石表面；而在P-1高岭石中，Fe主要以Fe~(3+)、Fe~(2+)置换Al~(3+)及杂质氧化物的形式存在。7、以前国内一些学者提出的所谓新矿物—“偏岭石”，笔者认为很可能是高岭石受煤自然烘烤形成的变高岭石。