航道护岸工程中基槽边坡稳定研究

航道护岸工程中经常发生基槽边坡滑坡失稳事故，从而造成经济和安全问题。因此，就滑坡发生机理进行研究对保障航道护岸工程顺利建设有重大意义。从极限平衡原理出发，分别运用Fellenius法和Bishop法验算了苏北某航道护岸工程开挖边坡的设计稳定性，并分析比较两种方法的差异，得出了在多层土的计算中有时会出现Fellenius法比Bishop法的安全系数略大的结论。结合工程实际中可能出现的渗流和超载等因素，计算得到边坡安全系数的变化规律和极限平衡状态时的临界负荷，从而提出了相应的预防渗流、控制超载等措施，可以为航道护岸建设提供参考。     

基于全寿命周期的大型建设项目集成风险管理研究

改造了大型建设项目全寿命周期的四阶段划分法,探讨了基于全寿命周期的集成风险管理子系统及系统模型的集成设计思路,提出了基于全寿命周期的大型建设项目集成风险管理模型(LC IRM),并对LC IRM模型的应用载体E-PM C作了探讨。     

杆式破片不同攻角垂直侵彻硬铝靶板数值模拟

采用LS-DYNA显示分析,研究了杆式破片在不同攻角垂直侵彻硬铝靶板的响应,得出了不同着靶角度下破片侵彻能力,分析了临界速度、剩余速度、破口直径以及靶板塑性区域等参数,并总结了这些参数的变化规律。     

铁道车辆结构强度可靠性和安全性技术展望

铁路运输正向高速、重载发展,结构强度可靠性与安全性技术是其中关键课题之一。在探讨现状基础上,预测了发展趋势。阐明了名义应力法较难合理应用于有限元分析结果和现场应变计检测结果;作者等人的试验工作揭示了材料循环应力 应变(CSS)响应存在分散性现象,这是现有理论与方法尚未涉及的领域。建议考虑随机CSS关系,建立局部应变强度可靠性理论体系、开展寿命周期理论研究,提升综合效能、创建车辆强度可靠性与安全性标准等3个值得研究的课题。     

柴油机不可逆循环性能分析及优化

建立了不可逆diesel循环的热力学模型，对diesel循环进行了有限时间热力学分析。推导出在内可逆、内外均不可逆时diesel循环在给定热力学模型下输出功率与热效率之间的关系式，并证明了内可逆diesel循环有一最大输出功率，而此时循环热效率即为著名的CA效率，并求出了最大输出功率表达式，证明了在具有最大输出功率时循环压缩比及预胀比有确定的关系。当具有内外双重不可逆时，相应公式只是对内可逆时的公式用不可逆系数I进行修正，即用ITL代替原公式中的TL即可。给出了计算实例，并通过实例计算分析了内不可逆系数、热源温度对最大输出功率、热效率的影响及循环压缩比、预胀比对热效率的影响。本文的研究对内燃机的设计和性能评估有理论意义。     

喀什地区盐渍土基本工程性质试验研究

我国盐渍土分布范围较广，各地区盐渍土的成因、组成及特征有明显的区域特点。通过室内物理力学性质试验，系统分析喀什地区天然盐渍土的盐渍化程度、液限、塑限、土样类别、最优含水量、最大干密度，可为盐渍土工程提供参考。     

丁坝错口距离的最优值、极限值研究

丁坝的布置方法直接影响到工程的效果,其关键是利用丁坝的坝后回流区。本文通过理论分析和水槽实验,提出了两岸丁坝在适当错口布置时整治范围增大的看法。获得了错口距离的最优值、极限值。错口坝的回流长度与宽度,回流与主流的分界边线的计算公式,计算结果与实验值吻合较好。     

Carbonate chemistry dynamics and carbon dioxide fluxes across the atmosphere–ice–water interfaces in the Arctic Ocean: Pacific sector of the Arctic

Climatic changes in the Northern Hemisphere have led to remarkable environmental changes in the Arctic Ocean, which is surrounded by permafrost. These changes include significant shrinking of sea-ice cover in summer, increased time between sea-ice break-up and freeze-up, and Arctic surface water freshening and warming associated with melting sea-ice, thawing permafrost, and increased runoff. These changes are commonly attributed to the greenhouse effect resulting from increased atmospheric carbon dioxide (CO₂) concentration and other non-CO₂ radiatively active gases (methane, nitrous oxide). The greenhouse effect should be most pronounced in the Arctic where the largest air CO₂ concentrations and winter–summer variations in the world for a clean background environment were detected. However, the air–land–shelf interaction in the Arctic has a substantial impact on the composition of the overlying atmosphere; as the permafrost thaws, a significant amount of old terrestrial carbon becomes available for biogeochemical cycling and oxidation to CO₂. The Arctic Ocean's role in determining regional CO₂ balance has been ignored, because of its small size (only  4% of the world ocean area) and because its continuous sea-ice cover is considered to impede gaseous exchange with the atmosphere so efficiently that no global climate models include CO₂ exchange over sea-ice. In this paper we show that: (1) the Arctic shelf seas (the Laptev and East-Siberian seas) may become a strong source of atmospheric CO₂ because of oxidation of bio-available eroded terrestrial carbon and river transport; (2) the Chukchi Sea shelf exhibits the strong uptake of atmospheric CO₂; (3) the sea-ice melt ponds and open brine channels form an important spring/summer air CO₂ sink that also must be included in any Arctic regional CO₂ budget. Both the direction and amount of CO₂ transfer between air and sea during open water season may be different from transfer during freezing and thawing, or during winter when CO₂ accumulates beneath Arctic sea-ice; (4) direct measurements beneath the sea ice gave two initial results. First, a drastic pCO₂ decrease from 410 μatm to 288 μatm, which was recorded in February–March beneath the fast ice near Barrow using the SAMI-CO₂ sensor, may reflect increased photosynthetic activity beneath sea-ice just after polar sunrise. Second, new measurements made in summer 2005 beneath the sea ice in the Central Basin show relatively high values of pCO₂ ranging between 425 μatm and 475 μatm, values, which are larger than the mean atmospheric value in the Arctic in summertime. The sources of those high values are supposed to be: high rates of bacterial respiration, import of the Upper Halocline Water (UHW) from the Chukchi Sea (CS) where values of pCO₂ range between 400 and 600 μatm, a contribution from the Lena river plume, or any combination of these sources.     

极限平衡法与有限元法结合分析平阿高速公路高边坡稳定性

结合平安至阿岱高速公路高边坡工程实例,先用极限平衡法计算得出边坡的稳定安全系数,再用有限元法分析边坡的应力、应变和位移,这两种方法相结合既能反映边坡的稳定和变形之间的关系,又能用安全系数来评价边坡的稳定性。采用预应力锚索等加固,高边坡处于稳定状态。     

顺置式吊杆锚固区受力特性与极限承载力研究

为掌握顺桥向设置的吊杆锚固区在吊杆力作用下的受力特性和极限承载力,以某在建斜拉-自锚式悬索组合体系桥为依托工程,利用ANSYS软件建立壳单元空间有限元模型,对锚固区在最不利荷载作用下的受力性能进行研究;并分别采用线弹性及非线性分析方法对吊杆锚固区极限承载力进行分析,讨论构件的受力情况。结果表明:在最不利荷载作用下,钢锚箱及钢锚梁应力较横隔板应力小;除钢锚梁与横隔板焊接处应力集中现象显著外,各构件应力分布较均匀;各构件顺桥向变形较大。不同极限承载力分析方法表明,此类结构采用壳单元建模进行极限承载力分析时应仅考虑材料非线性。建议在此类结构设计时,对于横隔板刚度不足问题应给予足够重视。