Seismic performance of chevron-configured special concentrically braced frames with yielding beams     

Hayato Asada  Andrew D. Sen  Tao Li  Jeffrey W. Berman  Dawn E. Lehman  Charles W. Roeder 《地震工程与结构动力学》2020,49(15):1619-1639

Current seismic design requirements for special concentrically braced frames (SCBFs) in chevron configurations require that the beams supporting the braces be designed to resist the demands resulting from the simultaneous yielding of the tension brace and degraded, post-buckling strength of the compression brace. Recent research, including large-scale experiments and detailed finite-element analyses, has demonstrated that limited beam yielding is not detrimental to chevron braced frame behavior and actually increases the story drift at which the braces fracture. These findings have resulted in new expressions for computing beam demands in chevron SCBFs that reduce the demand in the tension brace to be equal to the expected compressive capacity at buckling of the compression brace. In turn, the resultant force on the beam is reduced as is the required size of the beam. Further study was undertaken to investigate the seismic performance of buildings with SCBFs, including chevron SCBFs with and without yielding beams and X-braced frames. Prototype three- and nine-story braced frames were designed using all three framing systems, that is, chevron, chevron with yielding beams, and X SCBFs, resulting in six building frames. The nonlinear dynamic response was studied for ground motions simulating two different seismic hazard levels. The results were used to characterize the seismic performance in terms of the probability of salient damage states including brace fracture, beam vertical deformation, and collapse. The results demonstrate that the seismic performance of chevron SCBFs with limited beam yielding performs as well as or better than the conventionally designed chevron and X SCBFs.  相似文献   

一种地电阻率场地干扰的快速检测方法     

侯博文  谢佳兴  刘庆华  宋建锁 《地震地磁观测与研究》2020,41(4):78-82

对2018年洛阳地震台地电阻率观测区域出现的1次典型漏电干扰进行分析。经初步分析、干扰源模拟定位、干扰源现场调查等,确定干扰源的位置。通过对此次干扰的分析与排查,归纳总结出一种便利、快速的干扰检测定位方法。  相似文献   

Pleistocene deposits at Stoke Goldington,in the valley of the Great Ouse,UK     

C. P. Green  G. R. Coope  R. L. Jones  D. H. Keen  D. Q. Bowen  A. P. Currant  D. T. Holyoak  M. Ivanovich  J. E. Robinson  R. J. Rogerson  R. C. Young 《第四纪科学杂志》1996,11(1):59-87

At Stoke Goldington in the valley of the Great Ouse in Buckinghamshire a river terrace at a height of about 7 m above the floodplain is underlain by fluvial sediments representing climatic fluctuations in the late Middle Pleistocene. Near the base of the succession, at a level only 1 m above the modern floodplain, a fossil assemblage, including pollen, plant macrofossils, molluscs, insects and ostracods, provides evidence for the local development of herb-rich grassland under temperate climatic conditions. The fossil record, amino-acid racemisation ratios and uranium disequilibrium dating all suggest deposition of this material during Oxygen Isotope Stage 7. The deposits containing the temperate assemblage are immediately overlain by typical cold-climate gravels of the Great Ouse. These have been subjected to a later cut-and-fill episode, with the fill accumulating in cool climatic conditions. The cut-and-fill episode was succeeded by aggradation, forming the overlying terrace surface. Amino-acid racemisation ratios indicate that the fill was emplaced, and the terrace surface created, during or after Oxygen Isotope Stage 5. © 1996 John Wiley & Sons, Ltd.  相似文献   

B, Sr, O and H Isotopic Compositions of Formation Waters from the Bachu Bulge in the Tarim Basin     

CAI Chunfang PENG Licai MEI Bowen XIAO Yingkai 《《地质学报》英文版》2006,80(4):550-556

In order to elucidate the origin and migration of basinal brines in the Bachu Bulge, Tarim Basin, we have carried out analyses on chemical composition, and boron, hydrogen and oxygen isotopes of formation waters together with the XRD of clay minerals from the Paleozoic strata. The waters show Ca, B, Li and Sr enrichment and SO4 depletion in the Carboniferous and Ordovician and K enrichment in part of the Ordovician relative to seawater. The relationship between δD and δ^18O shows that all the data of the waters decline towards the Global Meteoric Water Line with the intersection of them close to the present-day local meteoric water, suggesting that modern meteoric water has mixed with evaporated seawater. The ^87Sr/^86Sr ratios range from 0.7090 to 0.7011, significantly higher than those of the contemporary seawater. The δ^11B values range from ＋19.7 to ＋32.3‰, showing a decrease with the depth and B concentrations. The results suggest that isotopically distinct B and Sr were derived from external sources. However, since the percentages of illite are shown to increase with depth among clay minerals in the study area, i.e., illite is due to precipitation rather than leaching during deeper burial, it is unlikely for illite to have contributed a significant amount of B to the waters. Thus, B with low δ^11B values is interpreted to have been added mainly from thermal degradation of kerogen or the basalts in the Cambrian and Lower Ordovician.  相似文献   

华东地区能见度时空变化特征及影响因子分析     

董芳淑  廉丽姝  孙博雯  程禛  朱艳冰 《气象科技》2023,51(4):510-519

为探究华东地区能见度变化情况,利用1973—2020年的能见度数据、2014—2019年的气象要素和污染物浓度数据,采用趋势分析、经验正交函数(Empirical Orthogonal Function, EOF)分解、相关分析的方法,分析了能见度时空变化特征及影响因子。结果表明：(1)1973—2020年能见度呈显著(p<0.01)下降趋势,变化倾向率为-1.315 km/10a,季节之间存在差异,夏、秋季能见度下降速率较大分别为1.681 km/10a、1.443 km/10a;冬、春季下降幅度相对较小分别为1.092 km/10a、1.091 km/10a。其中,1973—2012年能见度呈显著(p<0.01)下降趋势,变化倾向率为-1.204 km/10a, 2013—2020年能见度呈不显著(p>0.05)增加趋势,变化倾向率为2.229 km/10a,近8年(2013—2020年)来能见度存在明显改善。(2)华东地区南部、北部能见度较好,中部能见度较差。EOF分解第1模态表明华东地区能见度整体变化趋势一致,第2模态具有明显的区域差异。(3)能见度与相对湿度...  相似文献   

二氧化碳羽流地热系统的碳封存经济分析          下载免费PDF全文

付雷  马鑫  刁玉杰  郑博文  郑长远  刘廷  邵炜 《中国地质》2022,49(5):1374-1384

【研究目的】 二氧化碳羽流地热系统（CPGS）在取热的同时可实现CO₂地质封存，在碳达峰与碳中和背景下，CPGS碳封存的经济性是众多学者关注的要点。【研究方法】 以松辽盆地泉头组为例，采用数值模拟方法对比分析了注入压力、井间距与回注温度对热提取率的影响，在供暖情景下，计算了CPGS供暖效益与碳封存成本，并与常规水热型地热系统供暖效益进行了对比。【研究结果】 受携热介质转变与热突破影响，CPGS开采井温度呈现“降低-稳定-降低”的趋势，其中井间距对开采井温降影响显著，井间距越小开采井温降越明显；热提取率与回注压力呈现正相关性，与回注温度呈现负相关性，井间距对热提取率影响不显著；CPGS与常规水热型地热系统相比，采热量呈现“高-低-高”三个阶段，其中回注压力越小、回注温度与储层温度越接近，实现CPGS较水介质多采热能所需的时间越短。【结论】 仅考虑CO₂价格与取热效益，供暖收益抵消部分碳封存成本后，井间距对CO₂封存单位成本影响最为显著，井间距越小，CO₂封存单位成本降低越迅速，在注采井间距300 m条件下，持续开采30 a后CO₂封存单位成本可降至160元/t。  相似文献   

日间对流边界层中的非局地动量混合          下载免费PDF全文

赵昭  周博闻 《气象科学》2021,41(5):631-643

日间对流边界层最显著的结构特征是在热力作用下所形成的组织化对流。与小尺度湍涡不同的是，组织化对流具有边界层尺度的垂直相干性，可实现垂直贯穿边界层的非局地物质和能量传输。本文针对对流边界层中的动量混合，探究组织化对流对动量输送的贡献。以高精度大涡模拟数据为研究资料，通过傅里叶变换、本征正交分解和经验模态分解3种滤波方法，分离组织化对流和背景湍涡，计算与两者相关的非局地和局地动量通量，发现与组织化对流相关的非局地动量通量是总通量的重要组成部分，并主导混合层中的垂直动量输送。而后，基于协谱和相位谱分析，探究组织化对流的空间结构对动量传输的影响，发现在热力主导的不稳定环境中，单体型环流结构对动量的传输效率较低。而在风切较强的近中性环境中，滚涡型组织化结构可使垂直和水平流向扰动速度的相位差减小，从而提升动量传输效率。研究结果表明，边界层方案需要包含非局地动量通量项，其参数化应考虑整体稳定度对传输效率的影响。  相似文献