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建筑规范(地震)

定义

一套法律要求,规范建筑物的设计和建造以确保最低级别的地震安全。在大地震暴露新的脆弱性后进行更新。

示例

加州的建筑规范在1971年圣费尔南多地震后大幅加强。

相关指南

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Learn what causes earthquakes, how they occur along fault lines, and why some regions experience more seismic activity than others.

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软层问题:某些建筑物为何坍塌

Soft story buildings with open ground floors are deadly in earthquakes. Learn how to identify them and what retrofitting options exist.

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Unreinforced masonry buildings kill more people in earthquakes than any other type. Learn the risks and how communities address this deadly legacy.

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抗震设计原理

Modern earthquake-resistant design uses ductility, redundancy, and energy dissipation. Learn the engineering principles that save lives.

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如何评估建筑物的抗震安全性

Learn to assess your building's earthquake vulnerability. A practical guide to identifying structural risks and when to hire a professional.

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为你的家加固抗震

Earthquake retrofitting strengthens your home's foundation and framing. Learn the most effective upgrades and their costs for homeowners.

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木框架建筑的抗震能力

Wood frame construction performs well in earthquakes due to flexibility and light weight. Learn why wood is often the safest residential material.

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大地震后建筑规范的演变

Every major earthquake reveals building failures that reshape building codes. Trace the evolution of seismic design standards from 1906 to today.

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2010年海地地震:灾难和救援

The 2010 M7.0 Haiti earthquake killed over 200,000 people. Learn why the devastation was so extreme and the lessons for earthquake preparedness.

历史事件

常见问题解答

震中是地表上位于震源(地震破裂开始处)正上方的点。通常以经纬度坐标报告。最强的震动通常发生在震中附近,但当地土壤条件和断层几何形态可能使最大损害区域发生偏移。

地震仪(地震计)是检测和记录地震波引起的地面运动的仪器。现代宽频带地震仪可以检测到比原子宽度还小的运动。全球地震仪网络使科学家能够在几分钟内确定地震的位置和震级。

P波(纵波)是通过岩石传播最快的压缩波,最先到达地震台站。S波(横波)到达较晚但引起更大的地面震动。P波可以通过固体、液体和气体传播;S波只能通过固体传播。两者之间的时间差有助于确定地震的距离。

震源是地球内部地震破裂开始的点。它由经度、纬度和深度来描述。震源与其正上方地表之间的垂直距离即为地震深度,这对地表感受到的震动强度有很大影响。

地震学是研究地震和地震波在地球内部传播的科学学科。它包括地震检测、定位和特征描述、地球内部结构、地震危险性评估和地震工程。地震学家利用全球地震仪网络的数据来研究这些现象。