多孔硅的电致发光和发光二极管

本文较详细地描述了多孔硅的电致发光(EL),以及发光的量子限制效应的机制,并且讨论了目前已经制备出的几种多孔硅发光二级管:Ps/电解液型,Schot-tky-Like,PN结等二极管。最后,讨论了多孔硅作为半导体光电材料所存在的一些问题。     

外延单晶(YNd)_3Fe_5O_(12)磁光薄膜性能分析

对钇钕铁石榴石单晶薄膜材料进行了大量的性能研究,发现了过冷度与错配度、光损耗的关系,并提出了改善其磁光性能的可行途径。同时作出了XPS能谱图,比较氧化前后能谱图的差别,对实验结果给出了明晰的解释。     

新型显示器件进展

介绍了有源（光发射）和无源（光反射）显示器件－气体－电子－荧光粉显示，冷阴极场致发射矩阵平板显示、电泳成像显示和电化学显示器件等的发展情况。     

Organic geochemistry characterisation of crude oils from Mishrif reservoir rocks in the southern Mesopotamian Basin,South Iraq: Implication for source input and paleoenvironmental conditions

Seven crude oils from Cretaceous Mishrif reservoir rocks in the southern Mesopotamian Basin, South Iraq were studied to describe oil characteristics, providing information on the source of organic matter input and the genetic link between oils and their potential source rock in the basin. This study is based on biomarker and non-biomarker analyses performed on oil samples. The analysed oils are aromatic intermediate oils as indicated by high aromatic hydrocarbon fractions with more that 50%. These oils are also characterized by high sulfur and trace metal (Ni, V) contents and relatively low API gravity values (19.0–27.2° API). The results of this study indicate that these oils were derived from a marine carbonate source rocks bearing Type II-S kerogen that were deposited under sulphate-reducing conditions. This is primary achieved from their biomarkers and bulk carbon isotope and inorganic element contents (i.e., S, Ni and V). The absence of 18a (H)-oleanane biomarker also suggests a source age older than Late Cretaceous. The biomarker characteristics of these oils are consistent with those of the Late Jurassic to Early Cretaceous source rocks in the basin. However, biomarker maturity data also indicate that the oils were generated from early maturity source rocks. This appears to result from the type of kerogen of the source rock, characterized by a high-S kerogen (Type II-S).     

Bulk geochemical characteristics and carbon isotope composition of oils from the Sayhut sub-basin in the Gulf of Aden with emphasis on organic matter input,age and maturity

The Sayhut sub-basin is undergoing hydrocarbon exploration province in the Gulf of Aden, South Yemen. In this study, geochemical analyses were performed on three oil samples from two exploration wells in the Sayhut sub-basin. The results were used to describe the source organic matter input, age and maturity and to correlate between crude oils from different pay zones.The high saturated hydrocarbon values of more than 70% indicate that the analysed oils are normal crude oils and not degraded oils. This is supported by a complete suite of their normal alkanes and acyclic isoprenoids. The hydrocarbon distributions of normal alkane and isoprenoid with bulk carbon isotope data also suggest that the analysed oils are grouped into two genetic families and were generated from marine-source rock. The family A presents by one oil sample representing Harshiyat reservoir rock and characterized by relatively high Ph/Ph ratio > 2 and δ¹³C values of their saturated and aromatic hydrocarbon fractions range from ?26.1‰ to ?24.8‰. This oil family was derived from mixed organic matter with high contribution of a terrigenous organic matter input. The family A was deposited under suboxic conditions during the Late Cretaceous age. The family B presents by two oil samples representing Ghaydah and Habshiyah reservoir rocks and characterized by relatively low Ph/Ph ratio < 2 and carbon isotope less than ?23 for their saturated and aromatic hydrocarbon fractions. These oils were generated from source rock containing high contributions of marine organic matter (e.g., algal and microbial) with minor amount of land plant source inputs that was deposited in more reducing conditions. The family B oils are consistent with those of the Paleogene Umm Er Radhuma source rock.The hydrocarbon distribution and oil composition data also indicate that the analysed oils were generated from mature source rocks with a peak oil-window maturity.     

Mineral composition and organic geochemistry of the Lower Cretaceous Xiagou Formation source rock from the Qingxi Sag, Jiuquan Basin, Northwest China

The Lower Cretaceous Xiagou Formation contains the major source rocks for the crude oils discovered in the Qingxi Sag and the South Uplift in the Jiuquan Basin, northwestern China. The Xiagou Formation source rock was formed in a closed, anoxic, reducing, alkaline lacustrine environment with a high salinity. Its high content of brittle minerals is favorable for the fracturing of reservoirs in source rock formations in the Qingxi Sag. The Xiagou Formation contains a great number of fair to excellent source rocks, and their organic matter (OM) came chiefly from plankton/algae and high plants as well as possibly bacterial organisms. The Xiagou Formation source rocks mainly contain Type II OM and some Type III and Type I OM, with good oil-generating potential. The source rock maturity is mainly in the early-mature and mature stages, and its R_o value corresponding to oil peak is about 0.8%, which is lower than classic oil peak Ro value of 1.0%; therefore, a great deal of hydrocarbon was generated before the classic oil peak R_o = 1.0%. Mature source rock in the Xiagou Formation tends to be distributed in the older members and at a greater depth. There is a better exploration potential of tight oil in the deep Qingxi Sag.     

非稳腔激光光束质量评价的几个问题

本文讨论了研究光束质量的目的意义，认为测量光束质量的实质，是在能量守恒前提下，确定光束的传输方程。分析了虚共焦非稳腔环孔激光束的远场衍射特性，环孔衍射产生的中心亮斑比同样孔径的圆孔衍射中心亮斑细小，但强度低。环孔越窄，中心亮斑越细小，强度越低，大部分能量都分散到侧瓣上去，能量集中度下降，远场发散角增大。用能量含量百分比定义光束束宽不符合传输方程，环孔光束远场衍射的强度分布二阶矩不收敛，因此用β和Ｍ２衡量这种虚共焦非稳腔的光束质量都存在一些基本困难。顺便讨论了所谓无衍射光束和超衍射极限光束。最后也讨论了非稳腔激光光束质量评价的可能解决方法。     

高频数字锁相环的研究

论文阐述了１００ＭＨｚ数字锁相环的设计过程，用１０ＭＨｚ晶体振荡器对１００ＭＨｚ数字压控振荡器进行锁相，使１００ＭＨｚ输出信号指标得到很大改善。论文还分析了各单元电路，关键点时域波形测试，频谱测试。     

GaN材料生长研究

用常压ＭＯＣＶＤ方法我们在蓝宝石（０００１）、Ｓｉ（１１１）衬底上，成功地制备出ＧａＮ单晶薄膜材料，取得了ＧａＮ材料的初步测试结果。纯度ＧａＮ为ｎ型，载流子浓度为１０１７～１０１８ｃｍ－３，迁移率为２００～３５０ｃｍ２／Ｖ·ｓ，双晶衍射半峰宽为７′，室温ＰＬ光谱本征发光波长为３７０ｎｍ，并首次观察到掺ＺｎＧａＮ呈ｐ型电导。     

开放体系下升温速率对烃源岩产气率的影响

采用全岩开放体系程序升温热模拟实验装置,对哈2井三叠系灰黑色泥岩样品进行了不同升温速率对产气率影响的模拟实验研究,结果表明:在350~500℃期间,升温速率快时(20℃/m in)测得的产气量与升温速率慢时(5℃/m in)测得的产气量比较接近;在500℃以上,升温速率快时(20℃/m in)测得的产气量大于升温速率慢时(5℃/m in)测得的产气量。这一结果与前人所做的封闭体系下升温速率越慢产气量越高的结论正好相反,认为这主要是因为本次实验采用的是开放体系,其与封闭体系下的实验反应环境和反应过程不同,升温速率对产气率的影响可能与实验体系有一定关系。