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141.
采用强流相对论电子束横向泵浦纯氩,获得了属于Ar的第三谱带范围内240nm中心谱区的光强随气压变化的关系.结果表明,压强为3×105Pa时是产生这一谱区的最佳气压,并证实了这一谱区是由带电的原子团簇产生的. 相似文献
142.
采用热重分析法(TGA)测量矿产品中的吸附水及烧失减量,验证了方法的准确性及精密度。对多种矿产品样品采用TGA法和常规马弗炉加热法进行测量,对比结果表明,这两种方法没有显著性差异。TGA法具有方便快捷、准确可靠等优点,是矿产品吸附水及烧失减量检验的首选。 相似文献
143.
144.
铑矿石是获取铑的重要来源,但矿石中的铑含量极低,且分布不均匀,准确测定其含量一直是分析测试中的难题。本研究建立了一种可高效富集矿石中铑元素的铅试金——石墨炉原子吸收光谱分析方法。采用金作保护剂,铅试金分离富集矿石中的铑,形成的金-铑合金用王水溶解,石墨炉原子吸收光谱法进行测定。实验结果表明:熔剂配比m(硼砂):m(纯碱):m(黄丹粉):m(淀粉)=5:5:10:1,加入15mg金做为保护剂,灰吹温度900℃,可完全富集50 μg铑。用石墨炉原子吸收光谱仪进行检测,方法的相对标准偏差RSD(n=11)为6.97%~11.23%,线性范围为0.17~50 μg?L-1,加标回收率为99.36%~100.94%,10倍于铑的其他共存贵金属对测定无干扰。方法准确、可靠、简便,可用于矿石样品中铑的日常分析。本研究对铑资源勘探开采及铑矿物的综合利用研究具有重要意义。 相似文献
145.
Milana Pavić-Čolić 《Physics letters. A》2019,383(24):2829-2835
In this paper, we consider Euler-like balance laws for mixture components that involve macroscopic velocities and temperatures for each different species. These laws are not conservation laws due to mutual interaction between species. In particular, source terms that describe the rate of change of momentum and energy of the constituents appear. These source terms are computed with the help of kinetic theory for mixtures of polyatomic gases. Moreover, if we restrict the attention to processes which occur in the neighborhood of the average velocity and temperature of the mixture, the phenomenological coefficients of extended thermodynamics can be determined from the computed source terms. 相似文献
146.
We analytically study the quantum phase diagrams of ultracold dipolar Bose gases in an optical square lattice at zero temperature by using the generalized effective-potential Landau theory (GEPLT). For a weak nearest-neighbor repulsion, our analytical results are better than the third-order strong-coupling expansion theory calculation. In contrast to a previous quantum Monte Carlo (QMC) simulation, we analytically calculate phase transition boundaries up to the third-order hopping, which are in excellent agreement with QMC simulations for second-order phase transition. 相似文献
147.
Derek Ingham Maurizio Troiano Mohamed Pourkashanian 《Proceedings of the Combustion Institute》2019,37(3):2995-3003
The tendency of ash particles to stick under high temperatures is dictated by the ash chemistry, particle physical properties, deposit surface properties and furnace operation conditions. A model has been developed in order to predict the particle sticking efficiency for fly ash deposition at high temperatures. The model incorporates the particle properties relevant to the ash chemistry, particle kinetic energy and furnace operation conditions and takes into consideration the partial sticking behaviour and the deposit layer. To test the model, the sticking behaviours of synthetic ash in a drop tube furnace are evaluated and the slagging formation from coal combustion in a down-fired furnace is modelled. Compared with the measurements, the proposed model presents reasonable prediction performance on the particle sticking behaviour and the ash deposition formation. Through a sensitivity analysis, furnace operation conditions (velocity and temperature), contact angle and particle size have been found to be the significant factors in controlling the sticking behaviours for the synthetic ash particles. The ash chemistry and furnace temperature dictate the wetting potential of the ash particles and the melting ability of the deposit surface; particle size and density not only control the particle kinetic energy, but also affect the particle temperature. The furnace velocity condition has been identified as being able to influence the selective deposition behaviour, where the maximum deposition efficiency moves to smaller particles when increasing the gas velocity. In addition, the thermophoresis effect on the arrival rate of the particles reduces with increasing the gas velocity. Further, increasing the melting degree of the deposit layer could greatly enhance the predicted deposition formation, in particular for the high furnace velocity condition. 相似文献
148.
Yong Xu 《Frontiers of Physics》2019,14(4):43402
Three-dimensional topological gapless matters with gapless degeneracies protected by a topological invariant defined over a closed manifold in momentum space have attracted considerable interest in various fields ranging from condensed matter materials to ultracold atomic gases. As a highly controllable and disorder free system, ultracold atomic gases provide a versatile platform to simulate topological gapless matters. Here, the current progress in studies of topological gapless phenomena in three-dimensional cold atom systems is summarized in the review. It is mainly focused on Weyl points, structured (type-II) Weyl points, Dirac points, nodal rings and Weyl exceptional rings in cold atoms. Since interactions in cold atoms can be controlled via Feshbach resonances, the progress in both superfluids for attractive interactions and non-interacting cold atom gases is reviewed. 相似文献
149.
天然气净化对天然气这一清洁、高效的一次能源及我国快速增长的消费需求具有重要的战略意义。离子液体因挥发性低、溶解能力强、结构和性质可调控性强等优点,在离子液体膜净化气体方面获得高度关注。本文系统地总结了离子液体膜富集分离CO2及其他气体的性能,包括常规离子液体、功能化离子液体、聚合物离子液体、离子液体混合物;讨论了离子液体结构(如阳离子取代基链长、取代基对称性、阴离子结构大小、阴离子氟化)、膜支撑材料性能(如水溶性、孔径大小)及水含量等因素对膜性能的影响;对各种方法的优缺点及使用条件进行详细的阐述;并提出今后离子液体膜在气体净化方面的发展方向。 相似文献
150.
Two hydrated hydroxy magnesium carbonate minerals brugnatellite and coalingite with a hydrotalcite‐like structure were studied by Raman spectroscopy. Intense bands are observed at 1094 cm−1 for brugnatellite and at 1093 cm−1 for coalingite attributed to the CO32−ν1 symmetric stretching mode. Additional low intensity bands are observed at 1064 cm−1. The existence of two symmetric stretching modes is accounted for in terms of different anion structural arrangements. Very low intensity bands at 1377 and 1451 cm−1 are observed for brugnatellite, and the Raman spectrum of coalingite displays two bands at 1420 and 1465 cm−1 attributed to the (CO3)2−ν3 antisymmetric stretching modes. Very low intensity bands at 792 cm−1 for brugnatellite and 797 cm−1 for coalingite are assigned to the CO32− out‐of‐plane bend (ν2). X‐ray diffraction studies by other researchers have shown that these minerals are disordered. This is reflected in the difficulty of obtaining Raman spectra of reasonable quality and explains why the Raman spectra of these minerals have not been previously or sufficiently described. A comparison is made with the Raman spectra of other hydrated magnesium carbonate minerals. Copyright © 2008 John Wiley & Sons, Ltd. 相似文献