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111.
毛细管插入液面时,液体会由于表面张力作用而上升,这就是毛细现象.大多数学者在计算毛细现象中液面上升高度时,直接假定液面为球帽型,计算液柱重力势能时,将液体近似为圆柱体,忽略球帽的重力势能.本文严格计算了液面的形状,发现当液面较窄时(小于液面上升高度),这种近似是合理的.但液面较宽时,近似计算结果与实际情况偏离较大.本文在特殊情况下验证了描述液面接触角的杨氏方程的正确性. 相似文献
112.
X80级管线钢的开发研究 总被引:2,自引:0,他引:2
根据X80级管线钢技术要求,对湘潭钢铁(集团)有限公司试制X80级管线钢进行成分设计、相变规律和再结晶规律研究,开发出了1 016×22.0 mm X80级热轧钢板.检验结果表明,各项性能指标均满足技术要求. 相似文献
113.
陈雄 《北京师范大学学报(自然科学版)》2011,47(3):235-236
证明了两参数Markov过程仅在正位矩形的有限并或可列并区域上才具有Sharp Markov性. 相似文献
114.
Pd typically exhibits relatively low catalytic activity in CO oxidation, as CO is apt to be adsorbed on Pd to poison the surface for O2 activation. In this Letter, we report that this limitation can be overcome by integrating Pd with TiO2. The TiO2 was coated on Pd nanocubes with a controllable thickness using atomic layer deposition (ALD) method. Given the different work functions of TiO2 and Pd, the electrons in TiO2 semiconductor will flow toward Pd. With the electron density increased on Pd, the adsorption of CO to Pd will be weakened while the oxygen activation can be facilitated. Meanwhile, the interface-confined sites at Pd-TiO2 may further enhance the oxygen activation. As the species adsorption and activation are strongly correlated with electron density, the performance of Pd-TiO2 in CO oxidation turns out to depend on the TiO2 thickness, which determines the number of transferred electrons, within a certain range (<1.8 nm). This work provides a new strategy for enhancing catalytic performance through tailoring charge densities in hybrid catalysts. 相似文献
115.
116.
热源塔液气比优化分析与实验研究 总被引:2,自引:0,他引:2
针对夏热冬冷地区对冬夏两季双高效供冷/供热空调设备的需求,提出了采用热源塔热泵达到夏季高效供冷而冬季高效供热效果的解决方法.对热源塔热泵的原理和工作过程及其与冷水机组和空气源热泵的异同点进行了分析,建立了叉流式热源塔装置,并在不同室外空气参数情况下,以水和溶液(乙二醇水溶液)作为介质且在不同液气比时,对热源塔换热性能进... 相似文献
117.
高铝钢连铸过程中,为了避免或减轻钢液中Al与保护渣中SiO2发生反应,设计了低SiO2、高Al2O3含量的高铝钢连铸保护渣,通过添加适量的酸性氧化物B2O3协调熔渣酸碱性,利用实验分析了B2O3含量对高铝钢保护渣熔融特性、黏度特性及渣膜传热特性的影响。结果表明,B2O3含量在4%~10%时,随着B2O3含量增加,保护渣熔化温度、黏度、黏流活化能均降低,渣膜热流密度增加;保护渣的等温转变曲线(TTT曲线)向孕育时间增加的方向移动,晶体生长速率降低;实验条件下,增加B2O3含量可抑制保护渣中CaF2的析出。 相似文献
118.
为了揭示ZnO/p-Si异质结的导电机理,基于p-n结扩散模型和Anderson扩散模型推导了ZnO/p-Si异质结在理想情况下的伏安特性,并分析了掺杂浓度、工作温度以及能带补偿的影响.结果表明:当正向偏压超过势垒高度时,界面两边多数载流子由耗尽变为堆积,形成反向势垒,对异质结的正向电流起阻碍作用;当外加正向电压等于内... 相似文献
119.
高取代度CMC取代度的紫外光谱法快速测定 总被引:1,自引:0,他引:1
研究了高取代度的羧甲基纤维素(CMC)取代度的紫外光谱测定方法.首先利用CMC与Cu(Ⅱ)反应,得到CMC-Cu(Ⅱ)溶液的紫外吸光值随稀硫酸铜溶液体积的变化曲线,发现该曲线可划分为3个区,其中Ⅰ区是CMC链上的羧基与Cu(Ⅱ)离子按照化学计量反应生成配合物的区域,且符合Lambert-Beer定律.将Ⅰ区曲线拟合得到... 相似文献
120.
ShuangXi Chen TieGang Li Zheng Tang XiaoHua Qiu ZhiFang Xiong QingYun Nan ZhaoKai Xu FengMing Chang 《科学通报(英文版)》2011,56(24):2628-2634
The deglacial δ~13C minimum events that originated from the ventilation of the deep Southern Ocean around Antarctica, have been recorded in a range of marine sediments from the southern to tropical oceans in late Pleistocene. However, the broad δ~13C minimum event was also reported as far as to the northern middle latitudes, in northwestern Pacific marginal sea areas, during the last deglaciation. In the northwestern Pacific, forcing from the northern high latitudes is strongly expressed, while the records of in- fluence from the southern high latitudes are few. The Kuroshio Source Region (KSR) forms a boundary between the northwestern Pacific and the southern, tropical Pacific. So, high-resolution planktonic foraminiferal records in core MD06-3054 from the KSR are well positioned to identify signals from the southern hemisphere in the northwestern Pacific. Planktonic foraminiferal tests from the upper 1030 cm of the core were subject to AMS14C, carbon and oxygen isotopic measurements. A negative excursion was found to occur from about 20.0-6.0 ka BP in δ~13C records of both surface (Globigerinoides ruber) and subsurface (Pulleni- atina obliquiloculata) dwellers, but the overall trends of the two curves have reversed since 26.5 ka BP. Moreover, the δ~13C rec- ord of G. ruber (the surface dweller) shows a robust link to the record of atmospheric CO2, and its changes precede the records of P. obliquiloculata (the subsurface dweller). According to the hydrologic conditions, the broad δ~13C minimum event recorded in the KSR is also a response to the increasing ventilation of the deep Southern Ocean around Antarctica during the last deglaciation. The inconsistency between the records of the surface and subsurface dwellers was possibly caused by the ways that the low δ~13C signal was transmitted. Subsurface water primarily received the low δ~13C signal from the Antarctic Intermediate Water (AAIW), whereas the surface water was probably mainly impacted by atmospheric CO2 in the KSR. The records from the KSR confirm the deduction that the broad δ~13C minimum event in the Okinawa Trough was due to the impact of tropical Pacific surface water dur- ing the last deglaciation, and suggest that signals from the southern high latitudes also can be delivered to the northern middle latitudes. 相似文献