Liquid nitrogen flowrate alarm system for MBE

Liquid nitrogen is very important for MBE system. Most MBE systems use the liquid nitrogen to absorb the impurity molecules. If MBE cryoshroud is lack of liquid nitrogen, the pressure of the growth chamber will grow. This will affect the film quality. But too much liquid nitrogen is a waste. We have developed a liquid nitrogen flowrate alarm system to monitor the liquid nitrogen status in MBE cryoshroud. In this method, a temperature sensor is placed at the end of the cryoshroud. The temperature varies with changing of the liquid nitrogen status in cryoshroud. If the liquid nitrogen level in the cryoshroud is too low or too high, the LNFA will send out an alarm to warn the user to adjust the liquid nitrogen flowrate. In our experiments, we found this method works well, and the temperature responds sensitively. With the help of this system, people can view the liquid nitrogen status of the entire growth process. Compare with other method. it is very cheap.

基于RSA密码体制构造一类新型的CEMBS

公平性是电子商务协议的基本安全要求之一. CEMBS是一种重要的用于构造公平交换协议的密码部件.分析了现有的CEMBS构造方法中存在的问题,首次提出了一种基于RSA密码体制的简洁、高效、安全的CEMBS构造方法.在此基础上,利用这一新型的CEMBS构建了一类重要的公平交换协议.

Methane hydrate growth velocity in seepage system of Qiongdongnan Basin, South China Sea

The occurrences of diapirs, gas-filled zones and gas plumes in seawater in Qiongdongnan Basin of South China Sea indicate that there may exist seepage system gas-hydrate reservoirs. Assuming there has a methane venting zone of 1500 m in diameter, and the methane flux is 1000 kmol/a, and the temperature of methane hydrate-bearing sediments ranges from 3 degrees C to 20 degrees C, then according to the hydrate film growth theory, by numerical simulation, this paper computes the temperatures and velocities in 0 mbsf, 100 mbsf, 200 mbsf, 425 mbsf over discrete length, and gives the change charts. The results show that the cementation velocity in sediments matrix of methane hydrate is about 0.2 nm/s, and the seepage system will evolve into diffusion system over probably 35000 years. Meanwhile, the methane hydrate growth velocity in leakage system is 20 similar to 40 times faster than in diffusion system.

Hydrate dissociation conditions for gas mixtures containing carbon dioxide, hydrogen, hydrogen sulfide, nitrogen, and hydrocarbons using SAFT

A new method, a molecular thermodynamic model based on statistical mechanics, is employed to predict the hydrate dissociation conditions for binary gas mixtures with carbon dioxide, hydrogen, hydrogen sulfide, nitrogen, and hydrocarbons in the presence of aqueous solutions. The statistical associating fluid theory (SAFT) equation of state is employed to characterize the vapor and liquid phases and the statistical model of van der Waals and Platteeuw for the hydrate phase. The predictions of the proposed model were found to be in satisfactory to excellent agreement with the experimental data.

渭北泥炭资源在栽培基质中的应用研究

针对人工栽培基质中基质配比问题,采用生物试验的方法,对陕西彬县的泥炭、陕西铜川的油页岩、陕西关中土粘化层土壤,进行不同比例的配合后,再对配合基质设制不同处理,进行作物的室内栽培试验,通过生物量、生物性状(根冠比)、及产量分析来判断基质配比的优劣。研究结果表明:随着泥炭比例的增加,小青菜的产量增加,泥炭量达到一定值后,随着泥炭量的增加,小青菜的产量反而降低;泥炭与<1 mm粘土配合(PS)处理中,PS3处理(泥炭∶粘土为3∶1)小青菜地上部分产量最大;在泥炭与7~10 mm粘土配合(PB)处理中,PB2处理(泥炭∶粘土为2∶1)小青菜地上部分产量最大;对小青菜根系生物量来说,在泥炭和粘土比例较小时,小颗粒粘土处理的根量明显高于大颗粒粘土处理,在泥炭和粘土的比例较大时,大颗粒处理高于小颗粒处理。对油页岩处理而言,在泥炭量较少的配合基质中加入8%的油页岩能起到良好的增产作用;而在泥炭含量较多时,对小青菜产量的影响是负面的;石灰处理对小青菜地上部分产量影响都是负面的,但是对小青菜根系生物量的影响基本是正面的。高温处理对小青菜地上部分产量的影响基本上都是负面的,对小青菜根系的生长也基本是起负作用的。根冠比达到某一适宜值...

共价氢化物在光度分析中的应用

本论文由两部分工作组成。第一部分（铋化氢-二乙氨基二硫化甲酸银分光光度法测定铋）提出一个测定铋的新的分光光度方法，对影响方法准确度和精密度的各种因素进行实验，确定了适宜分析条件。用硼氢化钾-氯化钠-铝粉（重量比2:1:5）还原片，0.5N盐酸介质、15-25 ℃时，将铋离子转化为铋化氢，用5.0毫升0.2%的二乙氨基二硫化甲酸银氯彷溶液吸收显色。有色溶液最大吸收波长为425毫微米，摩尔吸光系数为4.6 * 10~4升。厘米~(-1)·摩尔~(-1)。铋量0-20微克符合比尔定律。经过对发光材料、铝合金和矿石中铋的测定，证明此方法有较好的实用价值。第二部分（砷、锑、铋的氢化物与二乙氨基二硫代甲酸银形成的有色物质性质的探讨）针对文献中砷化氢与AgDDC形成有色物质性质的两种不同看法，结合我们在AgDDC分光光度法测定砷、锑、铋中观察到的现象，用分光光度法对三种有色溶液的吸收光谱进行分析和讨论。实验证明，砷、锑、铋的氢化物与AgDDC形成的有色物质不可能是下列络合物：1、砷、锑、铋与二乙氨基二硫代甲酸（简称HDDC）或其它配位体形成的络合物；2、砷、锑、铋或银与HDDC形成的同核或异核的多核络合物；3、砷、锑、铋与HDCC及有机碱形成的三元络合物。同时指出，砷、锑、铋的氢化物与AgDDC之间可能发生的氧化还原反应，反应形成的有色物质属於银溶胶。由於上述三种氢化物还原AgDDC的能力不同，故所产生的银溶胶分散程度不同，而具有各自特征的颜色及吸收光谱。我们结合实验现象对砷的吸收曲线有两个吸收峰的问题进行了讨论，指出410毫微米波长处的吸收峰是砷的有色物质本身固有的，是由另一种分散程度的银溶胶产生的。

Raman Investigatins of 3C-SiC Films Grown on Si (100) and Sapphire (0001) by LPCVD

The Raman measurements have been performed with the back-scattering geometry on the SiC films grown on Si(100) and sapphire (0001) by LPCVD. Typical TO and LO phonon peaks of 3C-SiC were observed for all the samples grown on Si and apphire substrates, indicating the epilayers are 3C-SiC polytype. Using a free-standing 3C-SiC film removed from Si(100) as a free-stress sample, the stresses of 3C-SiC on Si(100) and sapphire (0001) were estimated according to the shift of TO and LO phonons.

非晶氮化硅薄膜退火前后微结构的XPS研究

于2010-11-23批量导入

Thermodynamic analysis of GaSb-GaCl3 vapor phase epitaxy

A thermodynamic model for the GaSb-GaCl3 system in a closed quartz ampoule was proposed. The species in the gas phase are GaCl, GaCl3, Sb-4, Sb-2. The partial pressures of these species and total pressure in the ampoule have been calculated. The calculated results indicate that the equilibrium partial pressures of GaCl, GaCl3, Sb4, Sb2 and the total pressure in the ampoule have strong dependence on temperature, free volume inside the closed ampoule and amount of transport agent GaCl3. The total pressure will give strong influence not only on the flow pattern in the ampoule, but also on the uniformity of the epilayer.

辽东次生林土壤呼吸及主要组分分离与量化

土壤呼吸是森林生态系统碳循环的重要组成部分，对土壤呼吸的主要组分根系呼吸和土壤微生物呼吸进行分离并量化，对于了解土壤碳释放规律、估算生态系统土壤碳的年际通量以及预测气候变化条件下根系或土壤微生物对土壤碳释放格局的影响具有重要意义。本文采用挖壕法测定辽东山区蒙古栎林、杂木林和胡桃楸林的土壤表面CO2通量，并同步分析土壤水热因子及土壤有机质、N含量、根系生物量、土壤酶活性、土壤微生物生物量等。研究结果表明：（1）辽东山区次生林0-10cm土壤有机质含量为9.29-18.15%，全氮含量为0.43-0.90%，pH值为5.67-6.19；次生林生长季细根生物量平均为152.61- 447.79 g/m2，粗根生物量平均为255.42-507.42 g/m2，根系总量平均为540.93-955.22 g/m2；土壤酶活性季节变化明显，且具垂直分布特征，蒙古栎林的土壤转化酶、淀粉酶和脱氢酶活性最高，胡桃楸林最低，胡桃楸林过氧化氢酶活性相对最大；土壤微生物量碳、氮的季节变化呈明显的单峰曲线并与土壤温度相关，土壤微生物量碳氮之间具显著相关性（P<0.05）。（2）次生林土壤总呼吸、根呼吸和土壤微生物呼吸具明显的日、季变化规律，生长季根呼吸贡献相对较低，胡桃楸林根呼吸贡献率为34.0-34.8%，蒙古栎林为17.9-28.4%，杂木林为14.7-35.3%；土壤微生物呼吸贡献率为66.0-85.3%，高于根呼吸贡献率，说明辽东山区次生林土壤微生物呼吸决定土壤总呼吸的变化趋势。（3）土壤呼吸与地下5cm土壤温度呈指数函数关系，土壤总呼吸的Q10值为1.29-2.30，微生物呼吸的Q10值为1.28-2.09，根呼吸的Q10值为1.29-3.72；土壤总呼吸、微生物呼吸、根呼吸与土壤含水量均无明显相关关系；蒙古栎林根呼吸与细根生物量显著相关，杂木林根呼吸与粗根生物量及根系总生物量显著相关，胡桃楸林根呼吸与根系生物量总量显著相关（P<0.05）；微生物呼吸与淀粉酶、转化酶、脱氢酶、过氧化氢酶均无显著相关性（除胡桃楸林与过氧化氢酶显著相关）；微生物呼吸与土壤微生物量碳、氮均呈显著线性相关关系（P<0.05）。（4）蒙古栎林土壤总呼吸、根呼吸、土壤微生物呼吸年际碳释放量分别为572.78、147.78和425.59 g C m-2a-1，杂木林分别为403.12、108.92、297.51 g C m-2a-1，胡桃楸林分别为519.47、173.75、345.72 g C m-2a-1；生长季和非生长季通过根呼吸释放的碳量均小于分解土壤有机质的微生物呼吸释放的碳量，非生长季次生林土壤碳释放量为39.21-152.04 g C m-2a-1，占全年呼吸总量的10-29%，说明冬季土壤碳释放量不能忽略。