论带“五等”字号的虚封爵——晋宋之际国家官爵制度上的变化之一

晋宋之际，国家官爵制度上发生的重要变化之一就是带“五等”字号虚封爵的出现。晋末特殊军事政治形势之下，京口北府集团凭借强势军功击败高门士族，取得压倒性的军事政治优势，京口北府军功受益阶层由此形成。带“五等”字号虚封爵适时地出现则成为这个现实政治变化的典型表现之一。笔者从这种虚封爵产生的时间和目的进行详细分析，以为正是出于酬赏义熙初年京口北府集团建义之功，朝廷才创设了这种虚封爵。这种虚封爵突破既有的门阀制度优势，确立了以军功为核心的分享军事政治利益的价值导向。这使得京口北府集团凭借军功所获取的军事政治利益不仅在制度层面上得到保障，而且在价值层面上取得其正当性和合法性，也就在这个时候，京口北府军功利益阶层得以成立。酬赏军功的这一目的也直接决定了虚封爵的若干特点，对此，笔者也予以分析说明。     

离子液体[C2mim]NO3与[C2mim][MetSO4]的热力学性能研究

采用MDY-2型密度仪在常压、一定温度范围内对离子液体1-乙基-3-甲基咪唑硝酸盐(简写为[C2mim]NO3)和1-乙基-3-甲基咪唑硫酸甲酯盐(简写为[C2mim][MetSO4])的密度进行了测定.结果表明,离子液体的密度随温度升高呈线性下降的趋势.由离子液体的密度值计算得到离子液体[C2mim]NO3和[C2m...     

音幻小屋体验对学龄儿童黑暗焦虑的影响

目的：评价音幻小屋体验对学龄儿童黑暗焦虑的影响。方法：参加音幻小屋体验学龄（7-13岁）儿童78例,用焦虑自评量表（SAS）分别测定音幻小屋体验前及体验后1周,1月对黑暗刺激焦虑评分。结果：体验后1周,1月对黑暗刺激焦虑评分均高于体验前（p〈0.01）,且两者无差异（p〉0.05）。结论：学龄儿童应远离恐怖刺激,避免心理创伤。     

GPSNISNAV integrated relative navigation and attitude determination system for ultra-close spacecraft formation flying

For the improvement of accuracy and better fault-tolerant performance, a global position system (GPS)/vision navigation (VISNAV) integrated relative navigation and attitude determination approach is presented for ultra-close spacecraft formation flying. Onboard GPS and VISNAV system are adopted and a federal Kalman filter architecture is used for the total navigation system design. Simulation results indicate that the integrated system can provide a total improvement of relative navigation and attitude estimation performance in accuracy and fault-tolerance.     

[bmim]Zn_2Cl_5/NH_3溶液的比热容和过量焓

测定了离子液体[bmim]Zn_2Cl_5在T=(323.15~1 173.15)K范围内的热重曲线,结果显示[bmim]Zn_2Cl_5在T637.15 K时具有很高的热稳定性。通过DSC测试得到[bmim]Zn_2Cl_5的比热容数据,在T=(251.15~383.15)K范围内可以用一个圆锥曲线很好地拟合。实验测定了[bmim]Zn_2Cl_5(2)+NH3(1)二元体系溶液的摩尔过量焓,其中氨的摩尔分数x1=(0.60~0.95),温度值为T=288.15 K,303.15 K,318.15 K,333.15 K。采用NRTL模型对过量焓数据进行拟合,得出二元可调参数和非随机参数。过量焓数据的测量误差和最大拟合偏差分别小于4.8%和4.3%。在[bmim]Zn_2Cl_5比热容和[bmim]Zn_2Cl_5/NH3过量焓数据的基础上,计算了氨质量分数w1=(0~1)、温度范围T=(273.15~343.15)K条件下[bmim]Zn_2Cl_5/NH3溶液的焓,所得焓浓图对于研究[bmim]Zn_2Cl_5/NH3吸收式制冷系统性能至关重要。     

离子液体中纤维素的溶解及再生特性

探讨了不同来源纤维素在离子液体1-丁基-3-甲基咪唑氯代盐(［bmim］Cl)中的溶解性能,并采用红外光谱、X-射线衍射及热重分析等手段对木浆纤维素在离子液体［bmim］Cl中溶解和再生前后的结构变化进行了分析。结果表明,未经活化的纤维素可直接溶解于离子液体［bmim］Cl 而不发生其它衍生化反应,原纤维素聚合度越低,溶解越容易。再生纤维素分子量较原纤维素有所降低,结晶状态由纤维素Ⅰ转变为纤维素Ⅱ,再生后纤维素热分解温度降低,热稳定性略有下降。     

PF6/缓冲液两相体系中固定化 β-葡萄糖醛酸苷酶催化特性研究

利用1-丁基-3-甲基咪唑六氟磷酸盐([BMIM]PF6)/缓冲液两相体系为介质,固定化β-葡萄糖醛酸苷酶催化甘草酸(GL)合成单葡萄糖醛酸甘草次酸(GAMG),以期改善酶催化效能.实验表明,当反应条件固定化酶为0.25g,两相体系中[BMIM]PF6的体积分数为35%,pH为5.0,反应温度为40℃时,酶活力最高达1 000U,远大于纯缓冲液单相体系中的最高酶活力450U.离子液体重复利用实验表明,[BMIM]PF6回收率高于85%,在含有重复回收的[BMIM]PF6介质中,固定化酶相对活力大于93%.     

江西兰科一新记录种—线柱兰

报道了产于南昌的兰科Orchidaceae线柱兰属Zeuxine线柱兰Z.strateumatica（L.）Schltr.,该种及其所在属均为江西首次发现。     

惠民南部地区油水物化性质与油气运移方向和模式

油水物化性质变化可以从古水文演化角度反应油气运移方向.本文以惠民凹陷南部地区沙河街组三段为例,利用原油密度、黏度、地层水矿化度、水型及离子组合参数变化特征,研究油气运移规律.平面上,研究区原油密度、黏度整体具有西北高、东南低的分布规律,局部具有一低四高的分布特征,反映出原油密度、黏度随运移距离的增加而增大;地层水矿化度具有以夏口断裂为中心,向南北两侧逐渐变小的分布特征,矿化度高值区的分布与夏口断层油气运移聚集有关;地层水水型和离子组合参数变化特征表明沿夏口断裂带具有两个油气聚集区,分别为双丰、江家店-瓦屋鼻状构造.通过对油气运聚关系的分析,以油气源、输导因素为基础,沿油气主要运移方向,建立了研究区近源侧向砂体输导、近源混向反Z型输导、远源混向阶梯状输导、远源混向多级反Z型输导4种油气运移模式.     

Characteristics of strontium isotopes and their implications in the Qixing Cave of Guizhou,China

The strontium isotopic compositions (87Sr/86Sr) of samples including soils, bedrock, soil waters, drip waters and their corresponding speleothems in the Qixing Cave (QXC), Guizhou Province, China, were systemically measured and analyzed. The results indicate that there are significant Sr isotopic differences among samples. The mean 87Sr/86Sr ratios in drip water for the samples 1#, 4# and 9# were 0.709568, 0.709139 and 0.708761, respectively, which possibly result from different flow paths, residence times, and other hydrogeological processes in the unsaturated zone overlying QXC. Meanwhile, levels of 40.8%, 57.6% and 72.4% of Sr in drip waters for 1#, 4# and 9#, respectively, were derived from bedrock dissolution, which was calculated by the mixture model of the two end-members (soil and bedrock). There is, however, no positive correlation between the relative proportion from bedrock dissolution (δ13C value is 1.8‰) and drip water δ13CDIC values. The mean drip water δ13CDIC value in 1# is the heaviest (–4.5‰) with the lowest contribution rate of bedrock dissolution, whereas the value in 9# is the lightest (–9.3‰) with the highest contribution rate of bedrock dissolution. The proportion from host rock dissolution in 4# is higher than that in 1# and lower than that in 9#, while its mean drip water δ13CDIC value (–8.6‰) is higher than that of 9# and lower than that for 1#. This suggests that the prior calcite precipitation (PCP) processes in the unsaturated zone overlying the cave are responsible for the δ13CDIC value differences between different drip waters, and not bedrock dissolution. Furthermore, this study also demonstrates that the 87Sr/86Sr ratios of speleothems in the 1# and 4# mainly reflect the variation in the relative proportions from the soil system (soil water) and bedrock dissolution overlying the cave. It is, therefore, feasible to use the strontium isotopic signals of speleothems as an indicator for soil chemical weathering intensity, and consequently as a monsoon proxy in the study area.