失谐力光系统中的光子-声子转换和基态冷却

研究由辐射压力引起Fabry-Perot力光腔中动力学行为.从力光系统哈密顿量出发,探讨在失谐条件下力光腔中量子现象.引入散射矩阵方案来论证光子和声子以有效并且可逆方转换.这对于光学光子和微械阵子之间量子态转变提供了一个可行方案.光声转变预着一可行量子光学器件.同我们用量子郎之万方法和主方程方法这两方法推导最声子占有数来研究械振子态冷却,并且对这两方法进行了参数比较.出在么条件下哪方法更实用.     

木质生物质常压液化及催化裂解研究

以正辛醇为溶剂，在常压下对木粉生物质进行催化液化，液化产物经γ-氧化铝负载的Ru-Co-Mo催化剂进行常压催化裂解，得到生物燃料油。对液化产物及其后的催化裂解产物分析结果表明：常压下的木粉液化率可达90.31%；经过催化裂解后的液化油产率可达69.73%；正辛醇回收率达90%；所得到的液化产物具有很好的可燃性。     

利用回音壁微腔系统克服量子点能级自然分裂

用一种全量子理论方法研究了一回音壁微腔-V型三能级量子点系统之间的耦合.量子点分别由基态、左圆极化激子态和右圆极化激子态构成,两简并回音壁腔模分别与左激子跃迁模和右激子跃迁模相耦合,其耦合率分别为gL和gR.在实空间里,我们推导了透射模与反射模的精确解,并得出其数值结果.结果显示了复合系统的耦合动力学特性;更重要的是,我们可以通过设计微腔得到合适的微腔反向散射率?,利用双模与量子点强耦合,就可以克服双激子能级精细结构的分裂(FSS).     

An experimental study of tin partition between melt and aqueous fluid in F/Cl-coexisting magma

In order to investigate the formation mechanism of tin ores associated with F-bearing granite, an ex-perimental study of tin partition between F-bearing granitic melt and coexisting HCl-bearing aqueous fluid was conducted at 850℃ and 100MPa with fo2 approaching NNO. Geochemical behavior of tin was traced by changes in starting solid materials with different alumina saturation index ASI, in F content and in starting fluids of various HCl concentrations. The results show that DSn increases with ASI of melt and peraluminous melt is favorable for tin partition into aqueous fluid in the F/Cl-coexisting sys-tem. Aqueous fluid of higher HCl concentrations is advantageous for enrichment of tin. Furthermore, chlorine contents in glass run products correlate positively with F and Cl contents in the magma. In the F/Cl-coexisting system, granitic melts with high F contents (> ~1 wt%) could extract and enrich tin in the melt which can serve as a reservoir for the formation of tin ores. However, the partition coefficient of tin would increase significantly when F contents in the melt were below 1 wt%. Therefore, the de-crease of F contents is favorable to the partition of tin into aqueous fluid with high HCl contents, thus promoting deposition of hydrothermal tin ores.     

An experimental study on the solubility of copper bichloride in water vapor

Using the solubility method, the solubility of CuCl2 in liquid-undersaturated HCl-bearing water vapor was investigated experimentally at temperatures of 330-370 ℃ and pressures of 4.2-10 MPa. The re-sults have shown that hydration could significantly enhance copper solubility and the concentrations of copper were positively correlated with PH2O. The solubility of copper in vapor phase increased with increasing PH2O at the constant temperature. CuCl2 was transported as hydrated species CuCl2(H2O)ngas in water vapor. The formation of complexes is proposed to be the result of the following reaction: CuCl2solid nH2Ogas = CuCl2 (H2O)ngas The hydration number n decreased slightly with increasing temperature. Statistical hydration numbers are 4.0, 3.6 and 3.3 at 330, 350 and 370 ℃ , respectively.