紧邻浅埋暗挖地铁隧道地下密集管线及土层变形

针对地铁隧道施工影响下紧邻密集管线保护问题,依托南昌地铁实际工程,采用ABAQUS软件建立土体-密集地下管线-隧道暗挖三维有限元模型,结合现场实测数据与数值模拟结果,分析了隧道CRD (cross diaphragm)工法施工时的地层变形规律、地下管线应力特性与地下管线变形规律,并对管线周边土体有无注浆加固时的管线力学特性进行了对比。研究结果表明：(1)隧道开挖引起的管线变形以沉降为主,管土刚度差异对管线变形和应力影响显著。(2)管土刚度差异越小,管线变形趋势与土体变形趋势越接近;管土刚度差异越大,管线对地层变形的抵抗作用也越强会产生较大应力。(3)隧道左右导洞上方管段是危险区域,需重点保护。(4)密集地下管线主要表现为管线材质、管线几何特性、管线与隧道的空间位置关系不同,保护地下管线的核心在于控制地层沉降,地下管线保护关键阶段是隧道掌子面接近管线,此时应确保超前注浆效果和初期支护快速封闭,并加强对管线变形的监测。     

高层建筑外附雨篷的表面风压和气动力系数

采用风洞试验方法研究高层建筑外附雨篷的风压特征,分析风压系数、风压相关性、非高斯性和整体升力系数随风向角的变化,给出围护结构的设计风压,最后研究倾角和出挑长度对整体力系数的影响. 研究发现,高层建筑外附雨篷上表面风压系数在正迎风时最大值接近1.4,系气流受到后方高层建筑的阻挡下翻导致;上、下表面的最大整体压力系数出现正迎风情况,最大值分别为1.24和0.76;上、下表面的最大整体升力系数出现侧风面,最大值分别为1.13和1.01;上下叠加后测点风压的非高斯性比单表面增强;上表面和下表面的升力系数在0°~70°风向呈现高斯分布,在80°~180°风向呈现较强的非高斯分布;高层建筑外附雨篷上表面的极值正压大于下表面;雨篷整体升力系数按照倾角-10°、0°、10°依次递增.     

胶东-辽东-朝鲜巨型金矿集中区的分离

胶东、辽东、朝鲜北部三区在地质上表现出了极大的相似性和稳定性。它们不但在元古代地层上可以相互对比,而且还有着一个统一的硼的地球化学省,在大地构造单元上也可以相互衔接。三区可以拼合为一个整体,使辽东的丹东金矿区、朝北的平安北道金矿区和胶东的招掖金矿区正好合成一个完整的整体,构成了一个巨大的金矿集中区。这个巨型金矿集中区是在统一的古陆块上由同一成因作用形成的,后因大陆的张裂和离散被分离。文中对它的分离机制和过程进行了探讨。     

The in vivo expression of the globin genes of theβ cistron in γ-,δ-, andδβ-thalassemia heterozygotes

There is considerable evidence suggesting that the switch from to and chain production after birth is due, in part, to silencing of the genes by stage-specific factors which bind to their promoters and to the competition from the adult ( and ) genes for a common enhancer element located in the locus control region. As a consequence one can expect that the increased Hb F production in adults with hereditary persistence of fetal hemoglobin or -thalassemia is directed mainly by -globin genes in cis to the deletion(s) responsible for these conditions. Here we review data on heterozygotes with -, -, or -thalassemia, who also had an^AT mutation, in cis or in trans, which was used as a marker of gene expression. The results show that a deletion affecting adult genes favors the expression of genes in cis, while the deletion of a single gene does not affect the expression of the gene in cis but leads to a faster switch postnatally.     

Critical slope gradient for compulsory abandonment of farmland on the hilly Loess Plateau

Scientific evidence for the upper limit of farmland is proposed. Shallow gully erosion is one of erosion types distributed extensively on sloping farmland in the hilly regions of the Loess Plateau. Field observation and aerial photos interpretation, as well as laboratory experiments show that the shallow gully erosion occurring on the steeper farmland in the hilly regions of the Loess Plateau is an important factor leading to intensive erosion on slope, because of its extensive distribution and intensive runoff collection. The data on the formation, development and distribution of shallow gullies on sloping farmland indicate that critical slope gradient for shallow gully initiation ranges from 15 to 20 degrees with an average of 18.2 degrees. Therefore, it is suggested that critical slope gradient for compulsory abandonment of farmland on the hilly Loess Plateau should be kept within the critical slope gradient for shallow gully initiation to prevent shallow gully formation in order to control soil loss more effectively. But as the first step, the cultivation on the slopes with slope larger than 25 degrees where the maximum erosion occurs should be strictly forbidden.     

保守系统的混沌同步

发现保守系统相空间中的一个轨道囚禁区．用闭环控制方法将系统引入囚禁区并在其内实现了同步．     

关于运城地区发展经济林的反思

优越的农业自然条件使运城地区成为山西省重要的粮棉生产基地。但近年来经济林的迅速发展使果树栽植面积几乎占到耕地总面积的1／4。尽管平原地区广种经济林具有一定的经济效益与环境效益,但它却违背了合理利用土地的原则,若不及早采取有力措施加以控制,我国将会潜伏粮食危机,种植业的可持续发展将会受到严重影响。     

AlGaAs／GaAs HBT基区电流的研究

在ALGaAs/GaAs HBT E-M模型直流参数的研究基础上,对HBT的基区电流进行了研究,特别是针对BE结空间电荷区的复合电流和基区表面复合电流,因为在HBT的小偏置情况下,HBT的BE结空间电荷区的复合电流和基区表面复合电流在整个基区电流中占有主导地位。当BE结间外加电压为0.5-1.2V时,ALGaAs HBT的基区电流的计算机模拟值和测试值比较接近,这一研究结果有助于进一步了解HBT的直流特性和1/?噪声特性。     

Bi系高温超导带材冷压工艺优化试验

采用套管法（ＰＥＴ）制备Ｂｉ系高温超导带材,进行了冷压工艺的优化研究。试验结果表明,Ｂｉ系带材所能承受的压力有一个限值,若超过这个限值后,密度虽可提高,但晶粒破碎严重Ｊｃ值反而降低,带材优化的冷压工艺参数是８３８℃／６０ｈ＋冷压＋８３８℃／６０ｈ。第１次压力为２ＧＰａ,第２次２．５ＧＰａ;冷压压下速率为１．５×１０＾－４ｍｍ／ｓ。同时研究还表明冷压的主要作用是提高带材的致密度和晶粒取向度,最终改善     

New evidence for the Qinghai-Xizang (Tibet) Plateau as a pilot region of climatic fluctuation in China

Over 40 a observed temperature data in 172 stations in China and historical proxy data were analyzed. Evidence suggested that during 1980–1994, the warmest year appeared first in southeastern part of the Qinghai-Xizang (Tibet) Plateau (henceforth SETP) and then gradually spread northwards and eastwards to eastern China. The climatic change on century time scale in recent 600 a shows 3 relatively warm and clod stages in China. Each warm and cold stage appeared first in Tibet Plateau (henceforth TP) and then in the Qilian Mountains, then in the eastern parts of China. The warm and cold stages in TP were 10–60 a earlier than in the eastern China. The facts show that TP is a pilot region of climatic fluctuation in China on the time scale shorter than 10³a.