二氧化碳观测卫星遥感反演研究进展

二氧化碳(CO_2)是大气中主要的温室气体,利用卫星平台观测大气干空气柱中对流层二氧化碳气体体积混合比(XCO_2)是当前温室气体监测的主流手段.首先介绍了5种具备近地面XCO_2浓度观测能力的卫星平台,并以GOSAT卫星的短波红外二级数据产品为例,重点介绍了中国2009～2016年大气XCO_2浓度的时空变化情况.结果表明,中国XCO_2浓度高值区主要出现在东南部,西部地区以及高纬度地区XCO_2浓度相对较低.8年间XCO_2平均浓度为392.28 ppm,并以2.28 ppm/a的速度持续增长.XCO_2浓度随NDVI有明显的季节变化,春季最高,夏季最低,年平均变化量达到6.2 ppm.     

带有临界增长的Kirchhoff方程极小能量变号解的存在性

为了深入研究Kirchhoff方程的性质,讨论了带有Hartree项和临界增长非线性项的Kirchhoff方程极小能量变号解的存在性。利用能量泛函在变号Nehari流形上的下确界C_λ收敛于0,得到空间E紧嵌入L~6(R~3)这一技术性结果。结果表明,利用限制变分方法和定量形变引理获得极小化序列对应的极小值点是该问题的非平凡解。研究方法在理论证明方面得到了良好的结果,对研究其他Kirchhoff方程解的存在性有一定的指导意义。     

CO2跨临界循环系统润滑油分析

为保证CO2跨临界循环系统的稳定运行，选择与之相适应的润滑油，在分析摩擦润滑特性的基础上，采用实验数据对比的方法，对POE、PAG、PAO和烷基芳香烃4类合成润滑油在CO2跨临界循环系统中的混合性、流动性、可溶性、黏度、长期稳定性及润滑性等性能进行了分析，结果表明POE类润滑油是CO2跨临界循环系统的一种相对较好的选择。     

DEGREE CONDITIONS FOR GRAPHS TO BE FRACTIONAL （a, b, n）-CRITICAL GRAPHS

Let G be a graph, and a and b be integers with a ≤ b. A graph G is called a fraetional （a, b, n）-critical graph if after any n vertices of G are deleted the remaining subgraph has a fractional [a, b]-factor. In this paper two degree conditions for graphs to be fractional （a, b, n）-eritical graphs are presented, and the degree conditions are sharp in some sense.     

宇宙临界减速因子

本文证明了如果中微子具有质量,那么膨胀宇宙的临界减速因子q_c就不是通常所说的1/2而是等于1。     

蚕沙提取果胶水解环境研究

果胶的提取率和质量与水解的环境关系密切 .本文重点在蚕沙中提取果胶从产率和颜色方面对水解的环境进行一些定性和定量的研究 ,获知各水解介质采用 0 3 %的稀硫酸液、温度 70— 80℃ ,时间 1h、pH1 5 ,提取的果胶从质量和产率上较理想     

铝合金材料LY12CZ临界空穴扩张比的适用性探讨

对光滑试样和3种不同曲率半径的切口试样，采用拉伸试验和电镜观测相结合的方法，研究了铝合金材料LY12CZ的VGC参数的适用性。证实VGC参数对材料的断裂形式较为敏感，适用于以拉伸型断裂为主的切口试样，对以剪切断裂为主的光滑拉伸试样不适用。     

合理投切降低变压器电能损耗

本文阐述了并联运行的变压器,为降低电能损耗,而根据用电负荷变化进行合理投切的临界负荷点的计算方法,并给出不同情况下的计算示例。     

Hydrostatic settling velocity of sediments

The settling of sediments is an accelerative process in which the concentration of the main sediments zone will heavily influence settling velocity, but the explicit relationship between the concentration and settling velocity has not been reported in literature. Here a theoretical function was built for the time dependent concentration and time dependent settling velocity of sediments ; then the entire settling process reflecting concentration was shown on the basis of sediments instant-settlement theory and mathematical method. Agreement of computed results and experimental data was found. Several governing parameters, including particle size,particle density,inltial suspended sediments concentration and suspension height, were discussed with a series of calculated velocity curves. The research indicated that (1) the presented concentration-velocity time relationship is rational, (2) settling process of the sediments group with variation of concentration consists of acceleration stage, uniform motion stage and deceleration stage, and (3) particle size, particle density and initial suspended sediments concentration have more influence on the settling velocity than the suspension height and water temperature.