奥运工程

奥运场馆“水滴”将于9月亮相;奥运村安装太阳能集热板满足赛后居民生活用水;“鸟巢”利用雨水回收每年可供水约五万立方米;08北京奥运会摔跤馆公开亮相成为学生毕业礼堂;     

统计同步算法原理及在局域网中的应用

针对局域网中计算机间的时间同步问题,分析了统计同步算法PCS的基本原理,介绍了局域网中网络延迟精确测定的方法,提出了利用一台时统设备实现局域网中PCS算法精度测试的方法,给出了频率漂移的修正公式,并在局域网中对算法性能进行了测试。测试结果表明,计算机时钟的漂移是影响算法精度的主要因素。经过频漂修正,PCS算法性能得到了很大的改善,同步周期较设计周期大大增加,算法同步精度在20min内优于1 ms。     

利用GPS OEM板对计算机进行高精度授时的研究

本文介绍了GPS OEM板的授时原理及计算机内部守时原理；分析了计数器频率的稳定性，提出了修正方案；阐述TN用GPS OEM板对计算机授时的实现过程，并做了时间比对实验。结果表明，计数器频率的漂移对授时精度有较大的影响。经频漂修正后，授时精度和守时精度都得到了很大的改善，最终授时精度优于6μs。     

自动气象站采集器显示板维修经验

根据ZQZ—CⅡ型自动气象站采集器的显示板的工作原理及维修实际经验，介绍了维修显示板的基本方法及主要芯片的性能，并对典型故障进行举例分析。     

Geochronologic Constraints on the Magmatic Underplating of the Gangdise^ Belt in the India-Eurasia Collision： Evidence of SHRIMP II Zircon U-Pb Dating

Abstract  Abundant small mafic intrusions occur associated with granitoids along the Gangdisê magmatic belt. In addition to many discrete gabbro bodies within the granitoid plutons, a gabbro‐pyroxenite zone occurs along the southern margin of the Gangdisê belt to the north of the Yarlung Zangbo suture. The mafic intrusion zone spatially corresponds to a strong aeromagnetic anomaly, which extends ～1400 km. The mafic intrusions consist of intermittently distributed small bodies and dikes of gabbro and dolerite with accumulates of pyroxenite, olivine pyroxenite, pegmatitic pyroxenite and amphibolite. Much evidence indicates that the Gangdisê gabbro‐pyroxenite assemblage is most likely a result of underplating of mantle‐derived magma. Detailed field investigation and systematic sampling of the mafic rocks was conducted at six locations along the Lhasa‐Xigazê segment of the mafic intrusive zone, and was followed by zircon SHRIMP II U‐Pb dating. In addition to the ages of two samples previously published (47.0±1 Ma and 48.9±1.1 Ma), the isotopic ages of the remaining four gabbro samples are 51.6±1.3 Ma, 52.5±3.0 Ma, 50.2±4.2 Ma and 49.9±1.1 Ma. The range of these ages (47–52.5 Ma) provide geochronologic constraints on the Eocene timing of magma underplating beneath the Gangdisê belt at ca. 50 Ma. This underplating event post‐dated the initiation of the India‐Eurasia continental collision by 15 million years and was contemporaneous with a process of magma mixing. The SHRIMP II U‐Pb isotopic analysis also found several old ages from a few zircon grains, mostly in a range of 479–526 Ma (weighted average age 503±10 Ma), thus yielding information about the pre‐existing lower crust when underplating of mafic magma took place. It is believed that magma underplating was one of the major mechanisms for crustal growth during the Indian‐Eurasia collision, possibly corresponding in time to the formation of the 14–16 km‐thick “crust‐mantle transitional zone” characterized by Vp = 6.85–6.9 km/s.     

云阳新县城高边坡变形破坏机理与数值模拟

三峡库区云阳新县城高边坡的主要破坏形式有坡面剥落、滑移式崩塌和岩块坠落.未支护的高边坡变形破坏的主要控制因素包括软、硬相间的斜坡岩体组成结构,软弱泥化夹层,含膨胀性矿物及区域性构造裂隙和卸荷裂隙.利用RFPA软件模拟了高边坡在不支护条件下变形破坏的发展趋势.