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Bulletin of the New Zealand Society for Earthquake Engineering最新文献

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The estimated PGA map of the Mw6.4 2006 Yogyakarta Indonesia earthquake, constructed from the Modified Mercalli intensity IMM 2006年印尼日惹Mw6.4地震的估计PGA地图,由修正的Mercalli强度IMM构建
IF 1.7 Q3 Earth and Planetary Sciences Pub Date : 2018-06-30 DOI: 10.5459/BNZSEE.51.2.92-104
Widodo Pawirodikromo
Many moderate and strong earthquakes have occurred in Indonesia. However, since ground motion records are unavailable, a concise earthquake peak ground acceleration (PGA) map has never before been constructed. Several efforts have been made to construct PGA maps after the Mw6.4 2006 Yogyakarta earthquake, i.e. earthquake PGA maps by researchers [1–4]. However, due to their use of completely different earthquake sources, methods of analysis and by using exclusion criteria of ground motion prediction equations (GMPE), the maps differed greatly and did not match the actual structural damage found in the field. Estimation of a 2006 Yogyakarta earthquake PGA map became possible after field surveying of the Imm conducted by Wijaya [5]. The estimated PGA map was constructed based on the isoseimic lines, intensity prediction equation (IPE) by Wijaya [5] and peak ground acceleration at YOGI and BJI station control points, as published by Elnashai et al [6]. A set of most recent GMPEs were chosen, as they closely predicted the PGA at two control points. An Extrapolation Method was developed in which the PGA between YOGI and BJI stations would be extrapolated to all data points in the field to yield the 2006 Yogyakarta seismic PGA map. Result of the investigation indicated that the pattern of the new PGA map does not form a circle with radius R, but occurs longitudinally following the direction of the Opak River fault trace and closely follows the pattern of Imm map and damage to buildings in the field. It was found that the maximum upperbound PGA reached ±0.50-0.51g and it did not occur at the epicenter area but instead took place in relatively deep soil deposit approximately ±2 km west of the Opak River fault.
印尼发生了多次中强地震。然而,由于地面运动记录不可用,以前从未构建过简明的地震峰值地面加速度(PGA)图。在2006年日惹6.4级地震后,研究人员已经做出了一些努力来构建PGA地图,即地震PGA地图[1-4]。然而,由于使用了完全不同的震源、分析方法和地震动预测方程的排除标准,这些地图差异很大,与现场发现的实际结构损伤不匹配。在Wijaya对Imm进行实地调查后,对2006年日惹地震PGA地图的估计成为可能[5]。根据Elnashai等人[6]发表的等压线、Wijaya[5]的强度预测方程(IPE)以及YOGI和BJI站控制点的峰值地面加速度,构建了估计的PGA地图。选择了一组最新的GMPE,因为它们在两个控制点上密切预测了PGA。开发了一种外推方法,将YOGI和BJI站之间的PGA外推到现场的所有数据点,以生成2006年日惹地震PGA图。调查结果表明,新的PGA地图的模式没有形成半径为R的圆圈,而是沿着Opak河断层线的方向纵向出现,并密切遵循Imm地图的模式和对现场建筑物的损坏。研究发现,最大上限PGA达到±0.50-0.51g,它没有发生在震中地区,而是发生在Opak河断层以西约±2km的相对较深的土壤沉积物中。
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引用次数: 2
Passive direction displacement dependent damping (D3) device 被动方向位移相关阻尼(D3)装置
IF 1.7 Q3 Earth and Planetary Sciences Pub Date : 2018-06-30 DOI: 10.5459/BNZSEE.51.2.105-112
N. K. Hazaveh, G. Rodgers, J. Chase, S. Pampanin
Viscous fluid damping has been used worldwide to provide energy dissipation to structures during earthquakes. Semi-active dissipation devices have also shown significant potential to re-shape structural hysteresis behaviour and thus provide significant response and damage reduction. However, semi-active devices are far more complex and costly than passive devices, and thus potentially less robust over time. Ideally, a passive device design would provide the unique response behaviour of a semi-active device, but in a far more robust and low-cost device. This study presents the design, development and characterization of a passive Direction and Displacement Dependent viscous damping (D3) device. It can provide viscous damping in any single quadrant of the force-displacement hysteresis loop and any two in combination. Previously, this behaviour could only be obtained with a semi-active device. The D3 device is developed from a typical viscous damper, which is tested to evaluate the baseline of orifice sizing, force levels and velocity dependence. This prototype viscous damper is then modified in clear steps to produce a device with the desired single quadrant hysteresis loop. The overall results provide the design approach, device characterization and validation for this novel device design.
粘性流体阻尼已在世界范围内用于在地震期间为结构提供能量耗散。半主动耗散装置也显示出重塑结构磁滞行为的巨大潜力,从而提供显著的响应和减少损伤。然而,半主动装置远比被动装置复杂和昂贵,因此随着时间的推移,其鲁棒性可能会降低。理想情况下,无源器件设计将提供半主动器件的独特响应行为,但在一个更坚固和低成本的器件中。本研究介绍了被动方向和位移相关粘性阻尼(D3)装置的设计、开发和表征。它可以在力-位移滞后回路的任何单个象限以及任何两个象限的组合中提供粘性阻尼。以前,这种行为只能通过半主动装置获得。D3装置是由一个典型的粘性阻尼器开发的,该阻尼器经过测试以评估孔口尺寸、力水平和速度相关性的基线。然后,对这个原型粘性阻尼器进行明确的步骤修改,以生产出具有所需单象限磁滞回线的装置。总体结果为这种新型器件设计提供了设计方法、器件表征和验证。
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引用次数: 3
Experimental in-plane performance of insulated concrete and brick masonry wall panels retrofitted using polymer composites 聚合物复合材料改性隔热混凝土和砖砌体墙板的面内性能试验
IF 1.7 Q3 Earth and Planetary Sciences Pub Date : 2018-06-30 DOI: 10.5459/BNZSEE.51.2.85-91
N. Ismail, T. El-Maaddawy, A. Najmal, N. Khattak
Masonry infilled reinforced concrete frame buildings built prior to the introduction of modern seismic provisions have been observed to undergo damage in and around the masonry infill walls during most recent moderate to severe earthquakes. Fibre reinforced cementitious matrix (FRCM) is one of several retrofitting options available to limit such earthquake induced damage to infill walls. An experimental program was undertaken herein to experimentally investigate the effectiveness of FRCM as a strengthening solution for vintage (i.e. built between 1880 and 1930) un-reinforced brick masonry (URM) and insulated concrete masonry (IMU) infill walls. A total of 16 masonry assemblages were tested under in-plane diagonal load, of these 8 were constructed replicating vintage URM whereas the remainder were constructed using modern IMU. IMU is a preferred masonry type in hot and humid regions owing to its superior insulting capability. Different polymer fabrics (i.e., carbon, glass and basalt) were applied over both faces of test walls, with two replicate test walls receiving the same FRCM strengthening details. One test wall of each masonry type was tested as-built to serve as a control specimen for comparison. One wall of each masonry type received two layers of basalt FRCM. The investigated aspects included stress-strain behaviour, stiffness, and ductility. Shear strength increment observed due to single layer of FRCM application was 422-778% for vintage URM and 307-415% for modern IMU. FRCM also substantially increased the ductility capacity of the masonry assemblages.
在引入现代抗震措施之前建造的砖石填充钢筋混凝土框架建筑,在最近的中重度地震中,砖石填充墙内部和周围都受到了破坏。纤维增强胶凝基质(FRCM)是几种可用于限制地震引起的填充墙损伤的改造选择之一。本文进行了一项实验计划,以实验研究FRCM作为加固老式(即建于1880年至1930年之间)无增强砖砌体(URM)和绝缘混凝土砌体(IMU)填充墙的有效性。共有16个砌体组合在平面内对角荷载下进行了测试,其中8个是复制老式URM建造的,其余的是使用现代IMU建造的。IMU具有优异的保温性能,是湿热地区首选的砌体类型。不同的聚合物织物(即碳、玻璃和玄武岩)被应用于测试墙的两面,两个重复的测试墙接受相同的FRCM强化细节。每个砌体类型的一个试验墙进行了测试,作为对照试件进行比较。每种砌体类型的一面墙均采用两层玄武岩FRCM。研究的方面包括应力-应变行为,刚度和延性。由于单层FRCM的应用而观察到的抗剪强度增加在复古URM中为422-778%,在现代IMU中为307-415%。FRCM还大大提高了砌体组合体的延性能力。
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引用次数: 5
Performance of churches during the Darfield earthquake of September 4, 2010 2010年9月4日达菲尔德地震期间教堂的表演
IF 1.7 Q3 Earth and Planetary Sciences Pub Date : 2010-12-31 DOI: 10.5459/BNZSEE.43.4.374-381
M. Anagnostopoulou, M. Bruneau, H. Gavin
This paper focuses on the structural behaviour and types of failure of churches located in the general Canterbury area following the Darfield earthquake of September 04, 2010. Given the variability in architectural styles, structural systems and properties of underlying soils, different patterns of damage were identified including out-of-plane gable failures, collapse of bell towers and cracking due to liquefaction and ground settlement. An architectural and historical landmark of Christchurch, the Christchurch Cathedral, suffered insignificant damage during the earthquake mainly because of its seismic retrofitting during 2006-2007. However many other church structures required retrofitting and supporting measures to avoid additional damage.
本文重点研究了2010年9月4日达菲尔德地震后坎特伯雷地区教堂的结构行为和破坏类型。考虑到建筑风格、结构体系和下垫土性质的可变性,确定了不同的破坏模式,包括面外山墙破坏、钟楼倒塌以及液化和地面沉降引起的裂缝。基督城的建筑和历史地标,基督城大教堂,在地震中遭受了轻微的破坏,主要是因为它在2006-2007年期间进行了抗震改造。然而,许多其他教堂结构需要改造和配套措施,以避免额外的破坏。
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引用次数: 10
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Bulletin of the New Zealand Society for Earthquake Engineering
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