“高资人”化石与股骨形态变异的生物力学分析

运用生物力学方法对1980年在江苏镇江高资镇采集的2件完全石化的人类股骨进行分析,并在常规形态观测和加速器质谱14C测年的基础上对更新世人类化石及全新世现代人股骨形态的变异进行讨论.测年数据显示,"高资人"股骨可能属于全新世现代智人,但基于CT扫描数据计算出的骨干抗压抗拉强度、抗弯强度及其他形态特征都呈现某些较全新世现代人更显古老的特征.对比分析表明,人类股骨形态及测量值因其功能状况等原因具有相当大的变异,股骨形态特征不能作为判断化石系统发育地位的最关键证据.股骨生物力学参数是其功能状况的直接反映,在人类不同演化阶段因运动行为模式差异,其相对大小在不同人群存在更加明显分异,因而生物力学分析在长骨功能状况研究上具有很大应用价值.化石石化程度不是判断其年代的可靠标准.     

北京大学加速器质谱循环气体剥离系统

基于EN型串列静电加速器的北京大学加速器质谱系统(PKUAMS)将主要开展高灵敏度 ¹⁰Be 测量,为此需要对该加速器的剥离系统进行改造。介绍了PKUAMS循环气体剥离器的研制,包括真空系统物理设计、模拟实验以及控制系统设计等。     

我所经历的5个物理实验

结合亲身经历的5个物理实验,讲解了从事科学研究的独到体会。     

用于AMS的RFQ加速器能散问题研究

将 RFQ 作为加速器质谱系统(AMS)的加速器是AMS小型化的一条可能途径,减小 RFQ 加速器的输出束流能散是实现这一途径的关键.对 RFQ 加速器成形段部分对束流输出能散影响的分析表明,在减小调制系数、极间电压、同步相位,使各参数匹配的同时,适当地增大纵向聚焦力可显著降低 RFQ 输出束流能散.利用变参量 RFQ 动力学模拟程序 RFQDYN 进行模拟优化,得到输出束流能散为0.4%的 RFQ 加速器物理设计.     

正则地稳定环和模的稳定同构

设R是一个含幺结合环。如果任意两个稳定同构的有限生成投射R－模均是同构的，则称R是强Hermitian环；如果对任意正则元a,b∈R且aR bR=R,均存在y∈R使得a by可逆，则称R是正则地稳定环。本文证明了环R是强Hermitian环，当且仅当对任意自然数n有Mn(R)是正则地稳定环。还给出了正则地稳定环的一些性质和刻画。     

Peat record reflecting Holocene climatic change in the Zoigê Plateau and AMS radiocarbon dating

Through the use of reliable AMS dating of high resolution (15–30 years) peat and the establishment of monsoon climate proxies sequence, we have been able to recognize several cold, dry events in the Tibetan Plateau during the Holocene. The more obvious ones occurred around 12800, 11300, 10200, 9580, 8900, 6400, 4400, 3700, 2800 and 1500 cal. aBP. These events correlate well with both ice rafting events recorded in high latitude North Atlantic Ocean sediment cores and cooling events in the low latitude SST. Spectral analysis indicates high frequency climate variation on centennial-millennial time scale during the Holocene. This further reflects Holocene climate instability and the existence of centennial-millenium scale rhythm in mid latitude areas as well.     

试析门禁控制系统在图书馆的应用

论述了设置门禁控制系统的意义,介绍了门禁控制系统选择需注意的问题,并对目前流行的门禁系统进行了比较,分析了其在图书馆中的应用.     

AMS dating on glacial tills at the source area of the Urumqi River in the Tianshan Mountains and its implications

Using accelerating mass spectrometry (AMS) dating method, a dating has been made on the primary calcium carbonate in tills and secondary calcium carbonate coating on till gravel and the roche moutonnee formed since the Last Glaciation at the source area of the Urumqi River valley in the Tianshan Mountains, northwestern China. The results reveal that the carbonate content in the tills in this noncarbonate area is high enough to date by AMS, that the carbon in the coatings on the newly exposed roche moutons and in the modern till is modern carbon and so the¹⁴C dating results in the ancient till can represent the actual ages of the till formation, and that the warm period during the Holocene began as early as 6 500 a B. P. and lasted to 1 800 a B. P.