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111.
112.
为向冷中子源装置氢系统提供17.5K的低温冷源,设计了逆布雷顿循环的液氮预冷模式和4种膨胀机预冷模式,并对这5种循环模式进行热力分析和[火用]分析,获得了各循环模式下的主要热力参数并分析比较了各自的热力性质.结果表明:带液氮预冷和前置式并联膨胀机预冷2种模式的热力性能最好,[火用]效率最高;对于膨胀机预冷循环,并联模式优于串联模式,前置式优于后置式.循环系统[火用]损失部位主要在压缩机、膨胀机和换热器,减小这3部分[火用]损失的途径有以下方面:改善循环,减小系统氦的质量流量;提高压缩机的等温效率、膨胀机的等熵效率;改善换热器的内部温度、温差、压力分布及物流分配.本研究为中国先进研究堆冷中子源氦制冷系统的设计提供了数值基础。 相似文献
113.
从冶金效果、设备性能、工艺条件等方面对LF-RH与RH-LF二次精炼法进行了全面的研究,分析了两种工艺下RH真空处理的特点,对两种工艺下管线钢中有害元素及夹杂物的控制进行了讨论.LF-RH与RH-LF工艺下生产的X70管线钢铸坯中的T[O]平均为14×10-6和19×10-6,显微夹杂物个数分别为2.48个/mm2和2.62个/mm2,达到很高的洁净度水平.LF-RH工艺铸坯中氮平均为53×10-6,RH-LF工艺条件下铸坯氮含量为平均38×10-6,为以后生产更高质量的管线钢积累了经验. 相似文献
114.
XUE Shuang ZHAO QingLiang WEI LiangLiang WANG LiNa LIU ZhiGang 《科学通报(英文版)》2007,52(18):2496-2505
The reduction of mass and trihalomethane formation potential (THMFP) of dissolved organic matter (DOM) and its fractions from secondary effluent during laboratory-scale soil-aquifer treatment (SAT) soil columns were studied. Reduction in dissolved organic carbon (DOC), absorbance of ultraviolet light at 254 nm (UV-254), biodegradable dissolved organic carbon (BDOC) and nonbiodegradable dis- solved organic carbon (NBDOC) for the bulk DOM averaged 72.35%, 53.98%, 97.49% and 35.33% across the soil columns, respectively. Using XAD-8 and XAD-4 resins, DOM was fractionated into 3 fractions: hydrophobic acid (HPO-A), transphilic acid (TPI-A) and hydrophilic fraction (HPI). HPO-A was removed by 61.06%, TPI-A by 54.86% and HPI by 74.95% as DOC as a consequence of the laboratory-scale SAT, respectively. The reduction of THMFP from HPO-A, TPI-A and HPI was 27.24%, 26.24% and 36.08%, respectively. Proton nuclear magnetic resonance (1H-NMR) spectra revealed that the HPO-A isolated from the secondary effluent contained more aromatic functional groups than the corresponding TPI-A. Fourier-transform infrared (FT-IR) spectrum analysis illustrated that TPI-A had decreased hydrocarbon and increased aromatics content in the SAT columns. Specific ultraviolet light absorbance (SUVA) and specific THMFP for each DOM fraction increased across the soil columns and HPI exhibited greater increase in both than HPO-A and TPI-A. The most problematic THM precursor was found to be HPO-A with its high quantity present in recharged water and high chlorine reactivity. 相似文献
115.
Water isotope variations in the snow pack and summer precipitation at July 1 Glacier, Qilian Mountains in northwest China 总被引:8,自引:0,他引:8
ZHOU ShiQiao NAKAWO Masayoshi SAKAI Akiko MATSUDA Yoshihiro DUAN KeQin PU JianChen 《科学通报(英文版)》2007,52(21):2963-2972
This paper presents the stable isotope data of the snow pack and summer precipitation collected at the July 1 Glacier, Qilian Mountains in northwest China and analyses their relationships with meteorologi- cal factors. On an event scale, there is no temperature effect on the δ 18O values in the summer pre- cipitation, whereas the amount effect is shown to be clear. By tracing the moisture transport history and comparing the precipitation with its isotopic composition, it is shown that this amount effect not only reflects the change in moisture trajectory, which is related to the monsoon activities, but is also associated with the cooling degree of vapor in the cloud, the evaporation of falling raindrops and the isotopic exchange between the falling drops and the atmospheric vapor. As very little precipitation occurs in winter, the snow pack profile mainly represents the precipitation in the other three seasons. There are low precipitation δ 18O ratios in summer and high ratios in spring and autumn. The Meteoric Water Line (MLW) for the summer precipitation is δ D = 7.6 δ 18O 13.3, which is similar to that at Delingha, located in the south rim of the Qilian Mountains. The MWL for the snow pack is δ D = 10.4 δ 18O 41.4, showing a large slope and intercept. The deuterium excess (d) of the snow pack is positively correlated with δ 18O, indicating that both d and δ 18O decrease from spring to summer and increase from early autumn to early spring. This then results in the high slope and intercept of the MWL. Sea- sonal fluctuations of d in the snow pack indicate the change of moisture source and trajectory. During spring and autumn, the moisture originates from continental recycling or rapid evaporation over rela- tively warm water bodies like Black, Caspian and Aral Seas when the dry westerly air masses pass over them, hence very high d values in precipitation are formed. During summer, the monsoon is responsi- ble for the low d values. This indicates that the monsoon can reach the western part of the Qilian Mountains. 相似文献
116.
PBA—PVC共混膜盐酸普鲁卡因离子选择性电极的研究 总被引:6,自引:0,他引:6
以聚丙烯酸丁酯(PBA)及聚氯乙烯(PVC)的共混物为成膜材料,四苯硼-盐酸普鲁卡因离子缔合物为电活性物,制备了盐酸普鲁卡因离子选择性电极.该电极浓度的线性范围为1.0×10 相似文献
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118.
化学方程式的自动配平是稀土数据库研究和开发中的一个重要辅助程序。已有的关于自动配平化学方程式的报道,其内容大多是数学方法的介绍和讨论,关于程序实现的论述还很少见。本文重点讨论了通过java语言实现化学方程式的配平过程,并使之更加完善,更加优化。该模块已在稀土数据库中使用。 相似文献
119.
A small solute has been obtained with column chromatography, which only exists and accumulates in the leaves of dune reed in northwest China's desert region. Its unique polyamine and aromatic features are quite different from those well-known ones accumulated under stresses. The natural quantity of the solute is strikingly proportional to the level of local high temperature, and a large section is distributed in the photosynthetic chloroplasts. Under lab conditions, we have proved that the solute plays a role in protecting or conserving chloroplasts under heat stress. So it is reasonable to suppose that the high resistance of dune reed to environmental high temperature and/or drought is at least partially due to the accumulation of this unique solute. 相似文献
120.