多层In_(0.55)Al_(0.45)As/A_(0.5)Ga_(0.5)As量子点的变温光致发光研究

测量了自组织多层In_(0.55)Al_(0.45)As/Al_(0.5)Ga_(0.5)As量子点的变温光致发光谱，同时观察到来自浸润层和量子点的发光，首次直接观察了浸润层和量子点之间的载流子热转移。分析发光强度随温度的变化发现浸润发光的热淬灭包括两个过程

不同尺寸分布的自组织In_(0.55)Al_(0.45)As/Al_(0.5)Ga_(0.5)As量子点的静压光谱

在15K测量了不同尺寸分布的In_(0.55)Al_(0.45)As/Al_(0.5)Ga_(0.5)As量子点的静压我致发光，静压范围为0--1.3GPa。常压下观察到三个发光峰，分别来源于不同尺寸的量子点(横向直径分别为26、52和62nm)的发光。它产的压力系数分别为82、94和98meV/GPa,都小于In_(0.55)Al_(0.45)As体材料带边的压力系数，特别是尺寸为26nm的小量子点比In_(0.55)Al_(0.45)As体材料带边小17%，并且压力系数随量子点尺寸的变小而减小。理论计算表明有效质量的增在和Γ-X混合是量子点压力系数变小的主要原因，并得到横向直径为26和52nm的小量子点的Γ－X混合势为15和10meV。根据实验还确定In_(0.55)Al_(0.45)As/Al_(0.5)Ga_(0.5)As量子点系统X能带具有Ⅱ类结构，并且估算出价带不连续量为0.15±0.02。

Three-dimensional fluorescence characteristics of dissolved organic matter produced by Prorocentrum donghaiense Lu

Filtration and cross-flow ultrafiltration techniques were used to separate culture media of Prorocentrum donghaiense at the exponential growth, stationary and decline stages into < 0.45 mu m filtrate, 100 kDa-0.45 mu m, 10-100 kDa and 1-10 kDa retentate and < 1 kDa ultrafiltrate fractions. The fluorescence. properties of different molecular weights of dissolved organic matter (DOM) were measured by excitation-emission matrix spectra. Protein-like and humic-like fluorophores were observed in the DOM produced by P. donghaiense. The central positions of protein-like fluorophores showed a red shift with prolonged growth duration, shifting from tyrosine-like properties at the exponential growth stage to tryptophan-like properties at the stationary and decline stages. The excitation wavelengths of protein-like fluorophores exhibited some change in the exponential growth and stationary stages with increased molecular size, but showed little change in the decline stage. However, the emission wavelengths in the decline stage exhibited a blue shift. Very distinct C type and A type peaks in humic-like fluorophores were observed. With a prolonged culture time, the intensities of both of the peaks became strong and the excitation wavelengths of peak A showed a red shift, while the A:C ratios fell. More than 94% of fluorescent DOM was in the lower than 1 kDa molecular weight fraction.

红枫湖、百花湖水中溶解有机物分子量分布特征及环境地球化学意义

溶解有机物（dissolved organio matter， DOM）通常是指能够通过0.45μm滤膜的有机物质。0.45μm的定义是根据传统的过滤滤膜直径来划分的，不是一个绝对的定义。DOM在水环境中起着重要的作用，它是水环境中重要的配位体和吸附载体。DOM在水化学和生态环境中的重要作用，主要表现在它不仅可以和基本的金属离子和有机化合物结合，还可以与毒性金属离子和除草剂、杀虫剂结合（wershow ond Goldberg，1972）。湖泊水中DoM的浓度及物理化学性质能够影响水生态环境的结构及初级生产力。溶解有机物按元素组成来分，主要含有C、O、H、N、P、S以及灰分。按重量计算，其中C占总有机物的50％，其次是O（科O％）、H（一5％）、N（0.5～6.5％）、P（＜1.0％）、S（＜1.0％）和灰分（1.2-5.0％）（Thurman，1985）。DOM一般由多种有机化合物组成，其中腐殖物质是溶解有机质的主要组成部分，一般占有机质总量的50-80％。目前通常可人为地将腐殖物质划分为胡敏素、胡敏酸和富里酸（Aiken et oL，1 985）。其余的非腐殖类物质主要包括碳水化合物、氨基酸、叶绿素、藻类分泌物、酚酮类化合物、脂肪酸和亲水性有机酸等（Thurman，1985）a在水环境中一些金属离子和微量元素通常和DOM相结合，而这些元素的作用和在水中的迁移都受DoM的分子量分布的影响（chiou etal．，1986）。 DOM的分子量及其分布是指示水质量的一个重要参数，同时在水处理过程中对于研究DOM的去处效率有重要作用（vuorio et oL，1998）。具有不同分子量分布的DOM与金属的络合能力也不同，则它们对金属的生物有效性的作用就不同（wuetal．，2002）。分子量变化的程度可以进一步理解DOM的自然形成过程，也可以在弓！用水处理过程中优化腐殖质的去除过程。红枫湖和百花湖是贵州地区两个人工水库，通过对两湖水文条件的测量，探讨了影响DOM分子量及分布变化的环境因素，包括溶解氧的含量、水体温度、pH值、叶绿素。的含量、光照强度、藻类生长情况、生物活动等，以及溶解有机物的来源，人为污染情况等。本文采样高效体积排阻色谱法（High PerformanceSizeExclusion cbromatograP场，HPsEC）测量了红枫湖、百花湖水中的DOM的含量及分子量分布，得出了以下几点认识：1、选择HPsEC实验的最佳条件：0.03M NaCl和0.002的磷酸盐缓冲液作为流动相，pH为6.8，离子强度为0．034mol几，紫外检测波长为254nm。2、红枫湖、百花湖水中DOM主要以分子量小于3500Da的组分为主，占总溶解有机物的90％以上。根据洗脱曲线的峰面积，可以把DOM分为3个不同 分子量的组分，其中大分子量组分（MW＞2000Da）的含量占总DOM的35％一68％；中等分子量组分（Z000Da＞MW>1000Da）的含量为27％-57％；小分子量组分（MW＜1000Da）占总DOM的3％一31％。 3、红枫湖、百花湖水中Doc含量受气候条件的影响。丰水期，水体上部DOC含量较大，下部较小‘平水期和枯水期，上下水体中DOC含量一致。各组分DOc含量变化与总DOC含量变化相似。DOC含量也表现出明显的季节性变化特征。丰水期DOC含量较高，而在平水期和枯水期含量较低。红枫湖和百花湖二者之间DOC含量没有明显的差别。4、红枫湖、百花湖水中DOM平均分子量也受气候条件的影响。丰水期，随深度的增大，DoM平均分子量增大；平水期和枯水期，上下水体DOM平均分子量一致。DO入左的季节性变化与DOC相反，丰水期，DOM平均分子量偏低；而在平水期和枯水期，DOM平均分子量偏高。5、重均分子量和数均分子量虽然变化趋势相似，但是它们的变化幅度不同，所以多分散系数也会发生变化。总的来说，在水体上部多分散系数偏大，水体下部偏小。丰水期多分散系数较大，平水期和枯水期多分散系数较小。6、随着气候条件的变化，各分子量组分的DOM含量及DOC浓度也在发生变化。大分子量组分随深度而增大，而中等和小分子量组分随深度而减小。丰水期，中等和小分子量组分含量较多，而大分子量组分较少；平水期和枯水期，大分子量组分含量较多，中等和小分子量组分含量较少。

Superfluid nuclear matter in BCS theory and beyond

Medium polarization effects are studied for S-1(0) pairing in nuclear matter within BHF approach. The screening potential is calculated in the RPA limit, suitably renormalized to cure the low density mechanical instability of nuclear matter. The self-energy corrections are consistently included resulting in a strong depletion of the Fermi surface. The self-energy effects always lead to a quenching of the gap, whereas it is almost completely compensated by the anti-screening effect in nuclear matter.

Dependence of superconducting temperature on chemical bond parameters in YBa2Cu3O6+delta (delta=0-1)

The chemical bond parameters, that is ionicities and average energy gaps, for all types of chemical bonds in YBa2Cu3O6+delta have been investigated with variation of oxygen content delta (delta = 0.0, 0.35, 0.45, 0.58, 0.64, 0.73, 0.78, 0.81, 0.95, 1.00). The theory used is the complex crystal chemical bond theory, which is the development of P-V-L theory. The two plateaus near 90 K and 60 K in superconducting transition temperatures, and the disappearance of superconductivity with the change of oxygen content, were reasonably explained by chemical bond parameters. The results also showed that the Cu-O chains play a vital role in the transition from non-superconductors to superconductors, and the highest transition temperature occurred when the plane-chain reached a coupling state. (C) 1998 Elsevier Science Ltd. All rights reserved.

Electrochemical behavior of the molybdotungstate heteropoly complex with neodymium, K10H3[Nd(SiMo7W4O39)(2)]center dot xH(2)O in aqueous solution

The electrochemical behavior of the title compound (denoted Nd(SiMo7W4)(2)(13-)) in aqueous solution has been studied using cyclic voltammetry, sampled d.c. voltammetry, differential pulse voltammetry and bulk electrolysis with coulometry, The stable pH range of Nd(SiMo7W4)(2)(13-) is determined with UV-visible spectra. In the potential range between 0.70 and -0.45 V vs. SCE, the anion in pH 3.8 aqueous solution undergoes one-, one-, two- and two-electron steps of four redox processes attributed to electron addition and removal from the molybdate-oxo framework. The adsorption of the anion on the dropping mercury electrode and a self-inhibition influence of the adsorbed anions on the redox process of those anions dissolved in solution are found. The unusual dependence of the formal potentials on pH is explained with the competition of the protonation and ion-pair formation due to the high negative charge of Nd(SiMo7W4)(2)(13-) and its reduced forms. The electrocatalytic effects of the anion on the bromate are investigated.

中国北方草本植物及表土有机质碳同位素组成

Recently, more and more attention has been paid to stable isotope ratios in terrestrial depositional systems. Among them, δ~(13)C value is mainly determined by the surface vegetation, while vegetation is directly related to climate, therefore, carbon isotope ratio in soil organic matter and pedogenic carbonate has been employed as an important paleoecological indicator. In order to test the paleoecological information extracted from stable isotope ratios in terrestrial depositional systems, it is necessary to study the relationships between δ~(13)C value in standing terrestrial plants and today climate, as well as between δ~(13)C value in modern surface soil organic matter and standing vegetation. Thus, these relationships were studied in this paper by means of analysing δ~(13)C in standing plants and modem surface soil organic matter in North China. The main results and conclusions are presented as following: 1. According to their δ~(13)C values, 40 C-4 species represent about 16% of the 257 plant species sarnpled from the North China. C-4 photosynthesis mainly occurs in Poaceae, Cyperaceae and Chenopidaceae families, and percentage representation of C-4 photosynthesis is up to 56% in Poaceae family. 2. The δ~(13)C values of C-3 plant species in North China vary from -21.7‰ to -32.0‰ with an average of -27.1‰, and 93% focus on the range of -24.0‰ ～ -30.0‰; δ~(13)C values of C-4 plant species in North China are between -10.0‰ ～ -15.5‰ with an average of -12.9‰, and 90% concentrate on the range of -11.0‰ ～ -15.0‰. 3. The δ~(13)C composition of C-3 plant species collected from Beijing, a semi-moist district, mainly vary between -27.0‰ ～ -30.0‰, and the average is -28.7‰; the δ ~(13)C values of plants in the semi-arid district, east and west to the Liu Pan Moutain, focus on the range of-26.0‰ ～ -29.0‰ and -25.0‰ ～ -28.0‰, respectively, with the mean value of -27.6‰ and -26.6‰, respectively; the δ~(13)C composition in the arid district dominantly vary from -24.0‰ to -29.0‰, with the average of -26.2‰, and among them, the δ~(13)C values of C-3 plant species in deserts are often between - 22‰ ～ -24‰; the δ~(13)C values in the cold mountain district concentrate on the range of -24.0‰ to -29.0‰, with the average of -26.3‰. 4. The main range of δ~(13)C composition of C-4 plant species, derived from Beijing, a semi-moist district, are -13.0‰ ～ -15.5‰; the semi-arid district, -11.0‰ ～ -14.0‰; the arid district, -11.0‰ ～ -14.0‰. The mean values of them are -14.0‰, -12.4‰,-12.7‰, respectively. 5. From east to west in North China, δ~(13)C values of C-3 plant species increase with longitude. The correlation between δ~(13)C ratios of C-3 plant species and longitude is linear. Changing temperate and precipitation and changing atmosphere pressure are spossible explanations. 6. Almost all C-3 plant species have the trends that their δ~(13)C values gradually increase with decreasing precipitation, decreasing temperature and increasing altitude. Our results show the increases of the δ~(13)C value by 0.30 ～ 0.45‰, 0.19 ～ 0.27‰ and 1.1 ～ 1.2‰ per 100 mm, I℃ and 1000 m, respectively, for all C-3 plant species together. 7. The δ~(13)C values of all C-3 plant species together and a part of C-3 species show highly significant linear correlation with the mean annual temperature, the mean annual precipitation and the altitude, and the results suggest that they can be used as proxies of these environmental variables, while, those without highly significant correlation, may be not suitable as the proxies. 8. The extent, which of responses of δ~(13)C composition to environmental variables, is different for each C-3 plant specie. 9. The δ~(13)C variations along altitude and longitude may be non-linear for C-4 p1ant species in North China. The mean annual temperature may be not important influential factor, thus, it suggests that the δ~(13)C composition of C-4 plant species may be not suitable as the proxy of the mean annual temperature. The influences of summer temperature on δ~(13)C values are much bigger than that of annual temperature, among them, the influence of September temperature is biggest. The mean annual precipitation may be one of the dominant influential factors, and it shows a highly significant non-linear relationship with δ~(13)C values, and the result indicates that δ~(13) C composition of C-4 plant species can be employed as the proxy of the mean annual precipitation. 10. The variations of δ~(13)C ratios do not show systematic trends along longitude, latitude and altitude for modern surface soil organic in Northwest China. ll. The δ~(13)C ratios of modern surface soil organic do not exhibit systematic patterns with temperature and precipitation in Northwest China, it suggests that, unless soil organic is transferred from pure C-3 or C-4 vegetation, the δ~(13)C composition of soil organic may be not used as proxies of climatic variables. 12. The δ~(13)C values of modem surface soil organic are heavier than that of standing vegetation, and the difference ofrnean δ~(13)C between them is -2.18‰. 13. Without considering the δ~(13)C difference between vegetation and soil organic, as well as the δ~(13)C drift in various enviromnent, we may not obtain the valuable information of C-3, C-4 relative biomass in vegetation. 14. The C-4 biomass contribution in vegetation increase with decreasing latitude, increasing longitude and decreasing altitude in Northwest China. The C-4 biomass almost are zero in those regions north to 38 ° N, or west to 100°E, or above 2400 m. 15. The C-4 relative biomass in vegetation increase with growing temperature and precipitation. and, C-4 plants are rare at those regions where the mean annual temperature is less 4 ℃, or the mean annual precipitation is less 200 mm, and their biomass contribution in vegetation are almost zero. Both the mean annual temperature and the mean annual average precipitation may be the important influential factors of C-4 distribution, but the dominant factors.

Evaluation of the Effectiveness of Representative Methods for Determining Young's Modulus and Hardness from Instrumented Indentation Data

The effectiveness of Oliver & Pharr's (O&P's) method, Cheng & Cheng's (C&C's) method, and a new method developed by our group for estimating Young's modulus and hardness based on instrumented indentation was evaluated for the case of yield stress to reduced Young's modulus ratio (sigma(y)/E-r) >= 4.55 x 10(-4) and hardening coefficient (n) <= 0.45. Dimensional theorem and finite element simulations were applied to produce reference results for this purpose. Both O&P's and C&C's methods overestimated the Young's modulus under some conditions, whereas the error can be controlled within +/- 16% if the formulation was modified with appropriate correction functions. Similar modification was not introduced to our method for determining Young's modulus, while the maximum error of results was around +/- 13%. The errors of hardness values obtained from all the three methods could be even larger and were irreducible with any correction scheme. It is therefore suggested that when hardness values of different materials are concerned, relative comparison of the data obtained from a single standard measurement technique would be more practically useful. It is noted that the ranges of error derived from the analysis could be different if different ranges of material parameters sigma(y)/E-r and n are considered.

亚微米氮化钛膜的纳米压痕和划痕测定Coatings

采用等离子电弧沉积的方法分别在GT35和40CrNiMo钢上沉积厚约为0.5mm 的氮化钛(TiN)膜。为了筛选基材，采用纳米压痕和划痕技术评价膜基界面结合和固体润滑效果。纳米压痕结果，采用等离子电弧沉积的方法，分别在GT35和40CrNiMo钢上沉积厚约为0.5$\mu $m 的氮化钛(TiN)膜。为了筛选基材，采用纳米压痕和划痕技术，评价膜基界面结合和固体润滑效果。纳米压痕结果，GT35，40CrNiMo和TiN的纳米硬度/弹性模量的典型值分别约为11.5 Gpa/330 Gpa，6.0 Gpa/210 Gpa，30 Gpa/450 Gpa。纳米划痕结果，GT35有较理想的膜基结合能力；GT35，40CrNiMo，TiN及其有机膜的摩擦系数分别约为0.25，0.45，0.15，0.10。同40CrNiMo相比，GT35是较为理想的基体材料。纳米压痕和划痕技术能提供丰富的近表面的弹塑性变形、断裂和摩擦等的信息，是评价亚微米薄膜力学性能的有效手段。

带边缘缺口碳纤维增强环氧复合材料静态与疲劳破坏特性

本文对碳纤维增强环氧复合材料0°和±45°铺层无缺口和带直边缺口层板,进行了静态拉伸和拉-拉疲劳破坏试验研究,比较和分析了不同铺层材料和有无缺口试件在静态和疲劳的特性以及损伤破坏型式。采用多种方法(声发射装置、两种位移传感器、电影摄影机、光学显微镜和扫描电镜等),检测层板的损伤。结果表明:带有垂直于载荷方向直边缺口的该类铺层碳/环氧层板受静态或疲劳拉伸时,裂缝不是沿缺口长度方向扩展,而是沿界面(纤维方向)扩展;缺口的存在基本上不影响其余无缺口部分的应力。并讨论了它的损伤破坏机理。

带边缘缺口碳纤维增强环氧复合材料拉伸破坏特性

本文对碳纤维增强环氧复合材料0°和±45°铺层带边缘缺口试件进行了拉伸破坏实验研究。结果表明:带有垂直于载荷方向边缘缺口的此种碳纤维增强复合材料受拉伸时,裂缝不是沿缺口长度方向扩展,而是沿纤维方向产生并扩展,缺口的存在基本上不影响其余无缺口部分的应力。对缺口不敏感特性与破坏模型进行了讨论。这种材料的破坏机理与各向同性材料相比具有明显的差别。

亚微米氮化钛膜的纳米压痕和划痕测定

采用等离子电弧沉积的方法，分别在GT35和40CrNiMo钢上沉积厚约为0.5μm的氮化钛(TiN)膜。为了筛选基材，采用纳米压痕和划痕技术，评价膜基界面结合和固体润滑效果。纳米压痕结果，GT35，40CrNiMo和TiN的纳米硬度/弹性模量的典型值分别约为11.5 GPa/330GPa, 6.0 GPa/210GPa, 30GPa/450GPa。纳米划痕结果，GT35有较理想的膜基结合能力；GT35，40CrNiMo，TiN及其有机膜的磨擦系数分别约为0.25，0.45，0.15, 0.10。同40CrNiMo相比，GT35是较为理想的基体材料。纳米压痕和划痕技术能提供丰富的近表面的弹塑性变形、断裂和磨擦等的信息，是评价亚微米薄膜力学性能的有效手段。

An Experimental Study on Flame Propagation in Cornstarch Dust Clouds

Following the quantitative determination of dust cloud parameters, this study investigates the flame propagation through cornstarch dust clouds in a vertical duct of 780 mm height and 160 x 160 mm square cross section, and gives particular attention to the effect of small scale turbulence and small turbulence intensity on flame characteristics. Dust suspensions in air were produced using an improved apparatus ensuring more uniform distribution and repeatable dust concentrations in the testing duct. The dispersion-induced turbulence was measured by means of a particle image velocimetry (PIV) system, and dust concentrations were estimated by direct weighing method. This quantitative assessment made it possible to correlate observed flame behaviors with the parameters of the dust cloud. Upward propagating dust flames, from both closed/open bottom end to open/closed top end of the duct, were visualized by direct light and shadow photography. From the observation of propagation regimes and the measurements of flame velocity, a critical value of the turbulence intensity can be specified below which laminar flame propagation would be established. This transition condition was determined to be 10 cm/s. Laminar flames propagated with oscillations from the closed bottom end to the open top end of the testing duct, while the turbulent flames accelerated continuously. Both laminar and turbulent flames propagated with steady velocity from the open bottom end to the closed top end of the duct. The measured propagation velocity of laminar flames appeared to be in the range of 0.45-0.56 m/s, and it was consistent with the measurements reported in the literature. In the present experimental study, the influence of dust concentration on flame propagation was also examined, and the flame propagation velocity was found weakly sensitive to the variations in dust concentration. Some information on the flame structure was revealed from the shadow records, showing the typical heterogeneous feature of the dust combustion process.

带主动冷却的超声速燃烧室传热分析

介绍了流体、固体传热耦合的一维分析方法,对带主动冷却系统的马赫数2.5超声速燃烧室进行了传热分析.该分析以实验测量的燃烧室壁面静压以及超临界煤油换热特性数据为基础,考虑了燃气的高温离解效应,燃烧特性以及碳氢燃料的高温热物理特性,对不同燃烧状态、冷却条件下的主动冷却过程进行了分析.结果表明有燃烧时壁面热流可高达1 MW/m~2以上,是无燃烧时的2～3倍.当煤油流量较小时(当量比为0.45),冷却后的壁面温度仍偏高,而且冷却壁内温度分布不均匀.随着煤油流量的增加,冷却效果明显提高,冷却壁内温度分布趋于均匀;并且煤油的出口温度也显著减小.