世界还在痛

三叉神经痛这种病说不清病发原因,疼起来要人命,患上这种病的人,很多坚持不到最后,有的考虑安乐死,有的甚至选择跳楼自杀。而倪家骧终止了这种局面,他靠的只是一根针,坊间把这种治疗方法称为倪氏镇痛术。     

基于氧腐蚀的热水锅炉停炉保养分析

<正>随着经济的发展和人民生活水平的提高,热水锅炉使用的数量日益增多。在日常的热水锅炉内部腐蚀防护方面,我们往往将防护工作的重点放在锅炉的运行期,忽略了锅炉停炉期内部腐蚀问题,殊不知热水锅炉停炉期内部腐蚀问题也相当严     

POWELL法在水工结构可靠度中的应用研究

一般来说,水工结构在设计基准期内,必须满足下列各项功能要求：一是在正常施工和正常使用时,能够承受可能出现的各种作用。二是在正常使用时,具有设计规定的工作性能。三是在正常维护下,具有设计规定的耐久性。四是在出现预定的偶然作用时,主体结构仍能保持必需的稳定性。以上4项总称水工结构的可靠性。因此,水工结构的可靠性可以明确定义为：在规定时间内,规定条件下,水工结构完成预定功能的能力。     

降雨历时和重现期对洪涝风险的敏感性和转移——以济南市大寺河流域起步区段大桥分区为例

为研究降雨历时和重现期对洪涝风险的敏感性和转移影响,构建了3种降雨历时和7种重现期的芝加哥降雨雨型,并建立了相应的MIKE FLOOD耦合模型,模拟了21种降雨情景下的洪涝过程;基于模拟结果,分别从洪涝空间分布、水动力特性等方面开展分析。结果表明：（1）1风险级主要位于城镇道路,5风险级主要分布于耕地、绿地和林地等径流系数较低的用地处。（2）各风险级积水总量峰值和积水总峰值均随降雨历时和降雨重现期的增加而增加,且对低重现期和短降雨历时更为敏感。（3）各洪涝等级的积水峰值面积随洪涝等级的增大逐渐增大,均随降雨历时增加而增加,增幅整体上为增长趋势。2风险级的积水峰值面积对重现期的变化敏感性最强,5风险级的积水峰值面积对重现期的变化敏感性最低。1、2风险级的积水面积峰值对短降雨历时更敏感,3、4、5风险级的积水面积峰值对长降雨历时更敏感。（4）当降雨历时相同时,随着重现期的增加,只发生无风险等级向有风险等级和从高等级向低等级转移的过程。随着降雨重现期的增大,研究区主要发生无风险到5级、5级到4级两个转移过程,且对低重现期的变化更敏感。本研究可为雨洪管理研究提供科学参考。     

麦角隐亭的发酵生产和提取

麦角菌（Ｃｌａｖｉｃｅｐｓｐｕｒｐｕｒｅａ（Ｆｒ．）Ｔｕｌ．ＡＴＣＣ２００１９）发酵生产麦角隐亭．培养时间１～２３ｄ内，产减量逐步增加，第２３ｄ菌丝体和发酵液中的减总量达１９８μｇ／ｍＬ．发酵４～６ｄ，培养基中的无机磷基本耗尽，产减量开始增加．用第４ｄ产碱期菌丝体接种，碱产量从常规接种１１２．５μｇ／ｍＬ增加到１５７．８μｇ／ｍＬ．发酵中期补加磷酸二氢钾，菌丝体生长量略有增加，但抑制麦角隐亭的合成．提取的样品经沉淀反应、薄层层析、红外谱分析，鉴定为α－麦角隐亭的酒石酸盐．     

基于效率和经济价值的期货套期保值二次决策准则

基于不同风险测度得到的期货套期保值策略不同,利用套期保值效率可以对比分析不同风险测度下的套期保值效果.然而,当考虑套保成本时,套保效率大的套保策略不一定是"最优"的.为兼顾套保效率和套保成本,引入经济价值进一步对比不同套保策略的效用,提出期货套期保值二次决策准则.首先,构建方差、VaR和CVaR等风险测度下的期货套期保...     

数模技术在陈家庄油田开发调整中的应用

利用数值模拟方法,研究了陈家庄油田的分层生产状况、水淹过程,得到了各小层含油饱和度分布图、剩余储量丰度图等。同时研究了数值模拟技术在油田水动力学开发调整中的应用,如通过历史拟合确定剩余油富集范围,优化开发调整方案,通过打加密调整井、转注高含水井、分层注水改变液流方向等。该技术的应用达到了改善油田开发效果和提高采收率的目的,取得了很好的开发效果。     

浅谈冬季施工需要注意的几个问题

本文对冬期施工前及施工过程中应注意的问题进行探讨。     

Grenvillian orogeny in the Southern Cathaysia Block: Constraints from U-Pb ages and Lu-Hf isotopes in zircon from metamorphic basement

Metamorphic basement rocks in the Cathaysia Block are composed mainly of meta-sediments with different ages. New zircon U-Pb geochronological results from the meta-sedimentary rocks exposed in the Zengcheng and Hezi areas, southern Cathaysia Block, show that they consist dominantly of early Neoproterozoic （1.0-0.9 Ga） materials with minor Paleo- to Mesoproterozoic and late Neoproterozoic （0.8-0.6 Ga） components, suggesting that the detritus mostly come from a Grenvillian orogen. The youngest detrital zircon ages place a constraint on the deposition time of these sediments in Late Neoproterozoic. Zircon Hf isotopic compositions indicate that the Grenvillian zircons were derived from the reworking of Mesoproterozoic arc magmatic rocks and Paleoproterozoic continental crust, implying an arc-continent collisional setting. Single-peak age spectra and the presence of abundant euhedral Grenvillian zircons suggest that the sedimentary provenance is not far away from the sample location. Thus, the Grenvillian orogen probably preexisted along the southern margin of the Cathaysia Block, or very close to the south. Similarity in the ages of Grenvillian orogeny and the influence of the assembly of Gondwana in South China with India and East Antarctic are discussed, with suggestion that South China was more likely linked with the India-East Antarctica continents in Early Neoproterozoic rather than between western Laurentia and eastern Australia.     

Inter-hemispheric comparison of climate change in the last millennium based on the ECHO-G simulation

The commonality and difference in the variations of temperature and precipitation between the Northern Hemisphere （NH） and Southern Hemispheres （SH） in the last millennium are investigated by analysis of the millennium simulation with the ECHO-G coupled climate model. The NH mean temperature variations are generally consistent with those of the SH counterpart on the interannual, decadal and centennial time scales. But, the transition times between the medieval warm period （MWP）, the little ice age （LIA）, and the present-day warm period （PWP） in the NH leads that in the SH; and the anomaly amplitude in the NH is significantly larger than the SH counterpart. For the precipitation variations, the NH mean precipitation varies in-phase with the SH mean precipitation on decadal and centennial scales （mainly in the mid-high latitudes） but out-of-phase on the interannual scale （mainly in the low latitudes）. During the MWP the warming has comparable amplitude in the NH and SH; however, during the PWP the NH warming is considerably stronger than the SH warming. Further, the present-day temperature rises in the NH high latitudes but decreases in the SH high latitudes, which is very different from the warming pattern during the MWP. Since during the MWP the greenhouse gases （GHG） concentration stayed at a low level, we infer that the present-day opposite temperature tendency in the high latitudes between the two hemispheres may be related to the increase of the GHG concentration.