Sliding mode fuzzy control: Theory and verification on a benchmark structure     

Saang Bum Kim  Chung Bang Yun 《地震工程与结构动力学》2000,29(11):1587-1608

A sliding mode fuzzy control (SMFC) algorithm is presented for vibration reduction of large structures. The rule base of the fuzzy inference engine is constructed based on the sliding mode control, which is one of the non‐linear control algorithms. In general, fuzziness of the controller makes the control system robust against the uncertainties in the system parameters and the input excitation, and the non‐linearity of the control rule makes the controller more effective than linear controllers. For verification of the present algorithm, a numerical study is carried out on the benchmark problem initiated by the ASCE Committee on Structural Control. To achieve a high level of realism, various aspects are considered such as actuator–structure interaction, sensor noise, actuator time delay, precision of the A/D and D/A converters, magnitude of control force, and order of control model. Performance of the SMFC is examined in comparison with those of other control algorithms such as H_{mixed 2/∞}, optimal polynomial control, neural networks control, and SMC, which were reported by other researchers. The results indicate that the present SMFC is efficient and attractive, since the vibration responses of the structure can be reduced very effectively and the design procedure is simple and convenient. Copyright © 2000 John Wiley & Sons, Ltd.  相似文献   

土的连续级配方程在粗粒料中的应用     

郭万里  朱俊高  余挺  金伟 《岩土力学》2018,39(10):3661-3667

粗粒料的级配对其物理力学性质具有重要影响。土体的级配通常用级配曲线来表示,级配方程则是对土体级配曲线的定量描述。利用土的连续级配方程,对各种粗粒料级配的适用性进行了验证,进一步总结了土石坝工程中粗粒料级配参数的常用取值范围;同时,分析了利用该方程进行粗粒料配料计算的实用性。主要结论如下：粗粒料的级配参数常用取值范围集中在-2相似文献   

地下爆炸地震耦合效应的静态分析   总被引：1，自引：0，他引：1       下载免费PDF全文

朱号锋  靳平  肖卫国 《地震学报》2010,32(2):234-241

首先修正了地下爆炸地震耦合效应的准静态理论,然后利用改进之后的理论对剪切模量、材料强度、围压以及孔隙率不同的介质中地下爆炸的震源强度进行了分析.分析结果表明,对于密实硬岩介质来说,在其它条件不变的情况下,介质的剪切模量越大,震源强度越低;介质的强度越大,震源强度越低;震源强度随着埋深的增加而降低.而干燥多孔介质中的干孔隙率也对震源强度有重要影响.  相似文献   

Sedimentary Crust and Metallogeny of Granitoid Affinity: Implications from the Geotectonic Histories of the Circum‐Japan Sea Region,Central Andes and Southeastern Australia     

Kohei Sato 《Resource Geology》2012,62(4):329-351

Metallogeny of granitoid affinity was reviewed from the aspect of geotectonic history of the continental crust, particularly of the genesis of sedimentary crust involved in magmatism. The redox state of granitoids and related mineralization shows a remarkable contrast between the east and west sides of the Pacific Rim, but if examined closely, the reduced‐type and oxidized‐type granitoid provinces are juxtaposed in three regions: the circum‐Japan Sea region, the central Andes, and the Lachlan Fold Belt in southeastern Australia. Comparative study of these regions revealed that the reduced‐type magmatism associated with Sn mineralization generated in thick sedimentary crust which formed in three geotectonic environments: (i) accretionary terrane along a subduction zone (e.g. Jurassic East Asia), (ii) continental rift (e.g. Early Paleozoic Andes), and (iii) mega‐fan (e.g. Early Paleozoic southeastern Australia). A collisional orogen can provide large amounts of clastic sediment to these environments. The age gap between the magmatism and sedimentation varies depending on the tectonic evolution of individual regions. Thin sedimentary crust may not play an essential role for the reduced‐type magmatism. The oxidized‐type magmatism associated with porphyry Cu and other mineralization generated in the crust which was initially carbon‐free igneous crust or modified from sedimentary crust by magmatism. Subduction‐related basaltic magmas are relatively oxidized, and may enhance fO₂ conditions of granitoid activity. Repeated magmatism in a monotonous convergent margin may be favorable for porphyry Cu mineralization as exemplified in the eastern Pacific Rim.  相似文献   

Comparing landscape evolution models with quantitative field data at the millennial time scale in the Belgian loess belt     

A. J. A. M. Temme  I. Peeters  E. Buis  A. Veldkamp  G. Govers 《地球表面变化过程与地形》2011,36(10):1300-1312

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Multi‐process Late Quaternary landscape evolution modelling reveals lags in climate response over small spatial scales     

A. J. A. M. Temme  A. Veldkamp 《地球表面变化过程与地形》2009,34(4):573-589

Landscapes evolve in complex, non‐linear ways over Quaternary timespans. Integrated geomorphological field studies usually yield plausible hypotheses about timing and impact of process activity. Landscape Evolution Models (LEMs) have the potential to test and falsify these landscape evolution hypotheses. Despite this potential, LEMs have mainly been used with hypothetical data and rarely to simulate the evolution of an actual landscape. In this paper, we use a LEM (LAPSUS: LandscApe ProcesS modelling at mUlti dimensions and scaleS) to explore if it is possible to test and falsify conclusions of an earlier field study on 50 ka landscape evolution in Okhombe Valley, KwaZulu Natal, South Africa. In this LEM, five landscape processes interact without supervision: water driven erosion and deposition, creep, solifluction, biological weathering and frost weathering. Calibration matched model results to three types of qualitative fieldwork observations: individual process activity over time, relative process activity over time and net landscape changes over time. Results demonstrate that landscape evolution of the Okhombe valley can be plausibly simulated. A particularly interesting and persistent feature of model results are erosional and depositional phases that lag climatic drivers both by decades, and by several ka within a few hundred meters. The longer lag has not been reported for this spatial scale before and may be an effect of slow landscape‐soil‐vegetation feedbacks. The combined modelling and fieldwork results allow a more complete understanding of these responses to climate change and can fill in hiatuses in the stratigraphical record. Suggestions are made for methodological adaptations for future LEM studies. Copyright © 2009 John Wiley & Sons, Ltd.  相似文献   

A Sensitivity Study of Arctic Ice-Ocean Heat Exchange to the Three-Equation Boundary Condition Parametrization in CICE6     

Lei YU  Jiping LIU  Yongqi GAO  Qi SHU 《大气科学进展》2022,39(9):1398-1416

In this study, we perform a stand-alone sensitivity study using the Los Alamos Sea ice model version 6(CICE6) to investigate the model sensitivity to two Ice-Ocean(IO) boundary condition approaches. One is the two-equation approach that treats the freezing temperature as a function of the ocean mixed layer(ML) salinity, using two equations to parametrize the IO heat exchanges. Another approach uses the salinity of the IO interface to define the actual freezing temperature, so an equation describ...  相似文献   

等效源技术在低纬度地区航磁化极中的应用     

郭志宏 《城市地质》1997,9(2):14-22

参考国内外有关资料，本文尝试将双极子等效源技术应用到伟纬度地区的航磁化极中，首次对南海低纬度地区的一片航磁△Ｔ数据场进行了化极实算，获得了较好的效果，对解决低纬度地区的航磁化极问题做了一次有意义的探索。  相似文献   

湘中曹家坝大型钨矿床的主要矽卡岩矿物学特征及其地质意义   总被引：5，自引：1，他引：4  

张志远  谢桂青  朱乔乔  李伟  韩颖霄  王凤兰 《矿床地质》2016,35(2):335-348

矽卡岩矿物特征是确定矽卡岩矿床成因的关键证据之一。曹家坝钨矿床是湘中盆地新探明的大型钨矿床,矿体呈似层状产于中泥盆统棋梓桥组灰岩与跳马涧组碎屑岩之间硅钙界面附近。矿区内发育大量矽卡岩矿物,但是未见到岩浆岩。文章通过钻孔编录、矿物的显微特征和电子探针分析,确定了曹家坝钨矿床的成因类型。研究表明曹家坝钨成矿作用与矽卡岩关系密切;石榴子石存在早、晚2个阶段,早阶段石榴子石以钙铝榴石和钙铁榴石为主,晚阶段以钙铝榴石和铁铝榴石-锰铝榴石为主;辉石以钙铁辉石为主;绿泥石主要是铁镁绿泥石。根据矽卡岩的矿物特征,结合发育磁黄铁矿和伴生金矿化等特征,提出曹家坝钨矿床可能是还原性远端矽卡岩型钨矿床。  相似文献   

Reduced order observer based identification of base isolated buildings     

Satish?NagarajaiahEmail author  Prasad?Dharap 《地震工程与工程振动(英文版)》2003,2(2):237-244

The objective of this study is to identify system parameters from the recorded response of base isolated buildings, such as USC hospital building, during the 1994 Northridge earthquake. Full state measurements are not available for identification. Additionally, the response is nonlinear due to the yielding of the lead-rubber bearings. Two new approaches are presented in this paper to solve the aforementioned problems. First, a reduced order observer is used to estimate the unmeasured states. Second, a least squares technique with time segments is developed to identify the piece-wise linear system properties. The observer is used to estimate the initial conditions needed for the time segmented identification. A series of equivalent linear system parameters are identified in different time segments. It is shown that the change in system parameters, such as frequencies and damping ratios, due to nonlinear behavior of the lead-rubber bearings, are reliably estimated using the presented technique. It is shown that the response was reduced due to yielding of the lead-rubber bearings and period lengthening.  相似文献