利用空间大地测量技术研究地球动力学最新进展

空间大地测量以高精度，高时空分辨率测定地球整体（地球自转）和各圈层（特别是大气，海洋与地壳）的运动，使地球动态变化的监测，研究及应用呈现了崭新的面貌，本文介绍了近年来国际地球动力学最新发展概况，内容包括地壳运动，地球自转，重力场时间变化等。     

银河系中G型球状星团的轨道计算

选择了4个银河系中累积光谱型为G型的球状星团作为样本，采用3种不同的引力势模型，计算了它们的轨道参数并画出了轨道图，发现不同的引力势模型对轨道形态的影响并不大，但对球状星团的轨道远心距有不同程度的影响，在两个近银心距较小的样本星团的轨道图中发现了异常了异常现象，验证了混沌现象确实时存在的。     

产品生命周期模型的零售企业供应链类型界定

供应链类型的研究一直是供应链管理理论的研究热点，近几十年的研究成果逐渐形成了相应的研究角度，但是，对供应链类型的研究更多的表现在定性的描述上，尤其是针对零售企业的供应链类型，鲜有定量的界定方法。利用产品生命周期模型的相关研究成果，提出了一个从产品角度、时域的供应链界定的模型，并利用相应的数据对模型的验证与应用予与说明。     

γ-Al2O3载体孔内原位合成水滑石

以尿素为沉淀剂,利用γ-Al2O3的内孔表面铝源原位合成水滑石. 考察了晶化时间、晶化温度、初始溶液浓度、原料配比对原位合成水滑石的影响. 实验中发现晶化6 h,MgAlCO3-LDH的晶体结构已趋于完整,晶化时间大于6 h时会有NH4Al(OH)2CO3*H2O杂相生成.在实验条件范围内,生成的一次粒子大小随着晶化时间的延长逐渐增大,随着晶化温度的升高、初始溶液浓度的增大而减小.     

方程(t)=ax(t)+bx(t-τ)+cx(t+τ)关于[-τ,0]上的初始函数解的存在性

讨论了混合型方程x·(t)=ax(t)+bx(t-τ)+cx(t+τ)x(t)=φ(t)　　t≥0,t∈[-τ,0].其中φ(t)是任意给定的[-τ,0]上的连续函数,a、b、c∈R,当bc≠0时,对该混合型方程的所有解的基本形式做了详细讨论.     

论FDI对西部制度变迁的影响及对策

本文首先对我国西部地区利用FDI的现状进行了描述 ,然后运用回归分析的方法分析了FDI和制度变迁的关系 ,指出FDI是影响区域制度变迁的重要因素 ,FDI在区域分布上的不均衡严重制约着西部地区制度变迁的进程。西部地区应该加快体制改革的步伐 ,改善投资环境 ,吸引FDI ,进而通过FDI带动西部地区制度变迁的进程 ,最终形成FDI和制度变迁相互推动、相互促进的良性循环。     

Holocene lake deposits of Bosten Lake, southern Xinjiang, China

A 9.25-m-long sediment core from Bosten Lake,Xinjiang, provides detailed information about changes in the water budget and biological acticity over the last 8400 cal-endar years. The chronology is constructed from six AMS radiocarbon dates on the terrestrial plant remains. Based onanalyses of TOC, CO3, detrital compounds and biogenic SiO2,lake level fluctuations and periods of remarkably-negative water budget appeared at 8.4-8.2 cal ka, 7.38-7.25 cal ka,5.7-5.5 cal ka, 3.7-3.4 cal ka and 3.3-2.9 cal ka, respec-tively. As they are in-phase with low lake levels at Sumxl Co and Bangong Co in western Tibet Plateau and with paleo-lakes in Inner Mongolia, a climate-induced change to some-what drier and warmer conditions is inferred. A further drop in lake level after 1320 AD of about 200 yr duration may heattributed to a negative water balance prior to the main phase of the Little Ice Age. Deep and stable lake phases of 1500 yr and 1800 yr duration at 7.2-5.7 cal ka and 5.5-3.7cal ka coincide with maximum moisture during the Holocene Megathermai in China. The long term trend towards aridity since about 4.3 cal ka can dearly be recognised. The reduced water budget of Bosten Lake from 640-1200 AD may be attributed to local effects.     

Temperature variations on the Tibetan Plateau over the last two millennia

The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e.     

改变水分子簇的结构及诱发的生物效应研究

概述了水分子簇理论研究的基本状况,以及改变水分子团簇结构的4种方法,包括外加磁场、外加电场、激光辐射以及直接加热法;最后简要介绍了改变水分子团簇结构所诱发的生物效应.     

并联电压负反馈输入、输出电阻的讨论

电路中引入负反馈,使输入、输出电阻均发生变化,并且输入、输出电阻对放大电路有很大的影响.从并联电压负反馈的角度,对输入电阻和输出电阻给出了下列4种方法的定量讨论.