Probabilistic critical excitation for MDOF elastic–plastic structures on compliant ground     

Izuru Takewaki 《地震工程与结构动力学》2001,30(9):1345-1360

Earthquake ground motions and their effects on structural responses are very uncertain even with the present knowledge. It is therefore desirable to develop a robust structural design method taking into account these uncertainties. Critical excitation approaches are promising and a new random critical excitation method is proposed for MDOF elastic–plastic shear‐building structures on compliant ground. The power (area of power spectral density (PSD) function) and the intensity (magnitude of PSD function) are fixed and the critical excitation is found under these restrictions. In contrast to linear elastic structures, transfer functions and simple expressions for response evaluation cannot be defined in elastic–plastic structures and difficulties arise in describing the peak responses except by laborious elastic–plastic time‐history response analysis. Statistical equivalent linearization is used to estimate the elastic–plastic stochastic peak responses approximately. The critical excitation responses are obtained for several examples and compared with those of the corresponding recorded earthquake ground motion. Copyright © 2001 John Wiley & Sons, Ltd.  相似文献   

近20年来热带印度洋与热带太平洋海气系统相互作用特征的诊断研究   总被引：14，自引：4，他引：14       下载免费PDF全文

殷永红  史历  倪允琪 《大气科学》2001,25(3):355-371

利用1979年1月～1998年12月的月平均海表温度(SST)、向外长波辐射(OLR)和l000hPa纬向风速等NCEP/NCAR再分析资料，对近20年来热带印度洋与太平洋海温异常(SSTA)及相关的环流特征量进行综合分析和研究，发现热带印度洋的内部耦合动力特征模态—偶极子模的强度，存在着年代间的差异，80年代偏弱，90年代偏强。热带印度洋与热带太平洋海气耦合系统之间存在着相互作用，80年代热带印度洋的SSTA主要是对太平洋ENSO的响应，90年代太平洋ENSO的异常发展在一定程度上是受印度洋偶极子模态异常活跃影响的结果。从观测资料诊断分析的角度，找出了90年代后ZC耦合模式对ENSO事件预报失败的可能原因。  相似文献   

新月形沙丘迎风坡气流加速模拟   总被引：5，自引：8，他引：5  

李恒鹏  李波  陈广庭 《中国沙漠》2001,21(1):24-27

迎风坡气流加速是决定新月形沙丘发育和形态的动力因子，研究这一加速过程的定量关系有利于认识沙丘的发育、沙丘的形态、沙丘的运动等。通过大量的野外实测数据和前人的理论分析，得出沙丘迎风坡气流加速量主要和沙丘坡度、迎风坡前来流风速以及沙丘高度有关，并建立了新月形沙丘迎风坡气流加速和沙丘形态特征的定量关系。根据这一关系得了在风力较强的风沙环境中，沙丘坡度较小；在风力较弱的风沙环境中，沙丘坡度较陡。地表粗糙度越大，迎风坡坡度越陡。沙丘地貌发育高度存在一上限，这一上限与边界层厚度有关。  相似文献   

全球陆地生态系统与大气之间碳交换的模拟研究   总被引：31，自引：1，他引：31  

李银鹏  季劲钧 《地理学报》2001,56(4):379-389

利用陆面物理过程和植被生理生态过程完全动态耦合的大气植被相互作用模式 (AVIM) ,对全球陆地生态系统的净初级生产力进行模拟。全球陆地生态系统植被分为 1 3类 ,土壤质地分为 7类 ,确定了各种植被和土壤的模式参数。采用全球陆地 0 .5× 0 .5网格点气候平均资料 ;以 30分钟为步长进行积分。并用全球不同地区各种植被类型的 1 9个 NPP观测样点数据校准模型。AVIM模拟全球陆地生态系统 NPP的主要模拟结果如下 :全球陆地生态系统净初级生产力 (NPP)总量约为 60 .72 Gt Cyr- 1。分析了不同植被类型的 NPP分布 ,模式较好地模拟了全球陆地生态系统净初级生产力的纬向分布和区域分布的差异 ,模拟出中国植被生产力的分布特征。陆地生态系统净初级生产力与温度、降水和辐射等气候因素在不同地区有不同程度相关性 ,北方针叶林地区气候因子与 NPP的相关性明显 ,反映出植被对环境因子的不同响应及其物候特征。赤道热带雨林地区NPP与气候因子的相关性不明显。  相似文献   

Relationship between erosion and sediment yield in drainage basins of loess gully-hilly areas     

Chen Hao 《地理学报(英文版)》2001,11(1):71-79

From a long-term point of view, the balance between erosion and sediment yield in a drainage system can basically realize, i.e., the delivery ratio can be close to 1. However, substantial variations among individual rainfall events or between annual delivery ratio exist, causing frequent sediment retaining or re-erosion and re-delivery of the retained sediments in a short period of time. Thus the delivery ratio will be < 1 or > 1. The sediment delivery ratio is closely related to the spatial distribution of rainfall and magnitude of rise and fall of peak flood and that of runoff depth in the drainage system. Delivery ratio of single event in a drainage system and changes of delivery capacity of silt-laden runoff in various classes of gullies can be expressed by transformation mechanism of shear force of a single rainstorm event with flood resulting from increase and decrease of peak flood per unit area.  相似文献   

湘西金矿尾矿—水相互作用：1．环境地球化学效应   总被引：8，自引：2，他引：8  

谭凯旋  王岳军  郭锋  谢焱石 《矿物学报》2001,21(1):53-58

湘西金矿在生产过程中产生了大量的尾矿。该区尾矿－水相互作用强烈，并引起了尾矿中重金属元素的释放、迁移和对水体－土壤、蔬菜等表生环境的重金属污染。污染程度较大的元素均为Au、Sb、As、Cd、Hg、W等，与尾矿中元素的富集特征相一致。尾矿中重金属元素的水迁移能力由大到小顺序为Au、Cd、W、Sb、Pb、As、Zn、Cu。元素的生物吸收系数由大至小顺序为Cd、Au、Zn、Hg、Sb、Cu、Pb、As、W。植物中金属元素浓度主要受土壤中的浓度、植物种类和吸收的影响。  相似文献   

Identification of soil–structure interaction effect in base-isolated bridges from earthquake records     

M. T. A. Chaudhary  M. Ab  Y. Fujino 《Soil Dynamics and Earthquake Engineering》2001,21(8):713-725

Identification of system parameters with the help of records made on base-isolated bridge during earthquakes provides an excellent opportunity to study the performance of the various components of such bridge systems. Using a two-stage system identification methodology for non-classically damped systems, modal and structural parameters of four base-isolated bridges are reliably identified using acceleration data recorded during 18 earthquakes. Physical stiffness of reinforced concrete columns, dynamic properties of soil and foundation impedance are found by available theoretical models in conjunction with pertinent information from the recorded accelerographs. Soil–structure interaction (SSI) effect in these bridges is examined by comparing the identified and physical stiffness of the sub-structure components. It is found that SSI is relatively pronounced in bridges founded in weaker soils and is more strongly related to the ratio of pier flexural stiffness and horizontal foundation stiffness than soil shear modulus, G_s, alone. However, substantial reduction in G_s is observed for moderate seismic excitation and this effect should be taken into account while computing foundation impedance.  相似文献   

Seasonal and event-scale variations in solute chemistry for four Sierra Nevada catchments     

JoAnn M. Holloway  Randy A. Dahlgren 《Journal of Hydrology》2001,250(1-4):106-121

Hydrobiogeochemical processes controlling stream water chemistry were examined in four small (<5 km²) catchments having contrasting bedrock lithologies in the western Sierra Nevada foothills of California. The Mediterranean climate with its cool/wet and hot/dry cycle produces strong seasonal patterns in hydrological, biological and geochemical processes. Stream water solutes fall into three general groups according to seasonal fluctuation in concentration: strong, rainy season minimum–dry season maximum (Cl⁻, SO₄²⁻, base cations); weak, rainy season minimum–dry season maximum (Si); and rainy season maximum–dry season minimum (NO₃⁻ and K⁺). Solute dynamics in soil solutions and stream water suggest that mixing of drainage waters from bedrock and soil sources regulate stream water solute concentrations. Patterns are further altered by the leaching of solutes accumulated in the soil over the summer period of desiccation and the temporal discoupling of nutrient cycles that occurs due to differences in the timing between vegetation growth (late spring) and leaching (early winter). Solute concentrations are remarkably similar between watersheds with varying bedrock types, with the exception of nitrate, sulfate and bicarbonate. Three watersheds have nitrogen-bearing metasedimentary bedrock that contributes to elevated nitrate concentrations in stream waters. Watersheds whose bedrock includes mineralized veins of sulfide and carbonate minerals similarly have greater sulfate and bicarbonate concentrations in stream water. Hydrobiogeochemical processes are highly dynamic at the seasonal and storm-event temporal scales and spatially complex at the watershed scale making management of stream water chemical composition, such as nitrate concentrations, very challenging.  相似文献   

Evolving Spatial Form of Urban‐Rural Interaction in the Pearl River Delta,China     

George C. S. Lin 《The Professional geographer》2001,53(1):56-70

Much of the development literature and the theory of urban transition have been based on an arbitrary division of production space into city and countryside. Despite growing recognition of the need for an integrated approach to urban‐rural relations, controversial issues related to the definition and measurement of the phenomenon remain unresolved. This case study of spatial transformation in China's Pearl River Delta analyzes with greater precision the geographic extent and functional attributes of a zone of urban‐rural interaction located outside and between major metropolitan centers. This zone has been the spatial focus of industrial and commercial development, although most of its population remains officially classified as “agricultural.” The peri‐urban zone was initially left behind by the central cities in terms of its contribution to the regional economy. After a decade of postreform development, this zone has moved ahead of the central cities and become the region's main destination for in‐migrants and foreign investment. The growth of the zone of urban‐rural interaction outside the central cities has absorbed a significant amount of the increased urban population, but it has not brought about a reduction of regional economic inequality because of the persistence of a backward economy in the periphery. Theoretical questions are raised concerning the validity of several fundamental assumptions underlying the conventional model of urban transition.  相似文献   

离散气候系统中的周期与混沌   总被引：1，自引：0，他引：1       下载免费PDF全文

曹鸿兴  王永中 《应用气象学报》1995,6(3):311-319

从零维气候模式导出了一个非线性映象公式，对由该公式表征的气候系统的平衡态和稳定域进行了研究。通过迭代计算揭露海洋热贮存C对气候系统的调控作用。计算结果表明，存在一个控制气候系统行为的很窄的C值敏感区；当C值大于敏感区上界时，气候系统趋向平衡态，即现代气候；当C值小于敏感区下界时，系统失稳。在敏感区内则呈现出周期与混沌行为，且随着C的增加，勾画出通过周期倍分岔通向混沌的道路。  相似文献