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1923年关东大地震:东京的毁灭

The 1923 M7.9 Kanto earthquake destroyed Tokyo and Yokohama, killing over 140,000. The firestorms were deadlier than the shaking itself.

The Setting: The Tokyo-Yokohama Metropolitan Region

In 1923, the Tokyo-Yokohama region was the economic and cultural heart of the Japanese empire, with a combined population of approximately 4 million people. Tokyo had been rebuilt and modernized since the Meiji Restoration of 1868, but the rapid urban growth of the late 19th and early 20th centuries had produced a dense fabric of wooden buildings — the traditional Japanese townhouse style of closely packed wooden structures — interspersed with newer brick and concrete commercial buildings. The region sits above the triple junction of the Philippine Sea, Pacific, and North American (or Eurasian) plates, one of the most complex tectonic configurations on Earth. The 俯冲带一个构造板块潜入另一板块之下并进入地幔的区域。俯冲带产生世界上最大的地震(8.5级以上),并伴有深海沟和火山弧。 of the Philippine Sea Plate beneath the Kanto region had produced destructive earthquakes previously: historical records documented major events in 818, 1703, and 1855. The geological concept of recurrence was beginning to emerge in Japanese science, and some scholars had warned of the next great Kanto earthquake, but no systematic building code enforcing seismic resistance existed in the city.

The Earthquake: September 1, 1923

At 11:58 AM on September 1, 1923 — a Saturday, when many households had cooking fires lit for lunch preparation — a M7.9 earthquake struck in Sagami Bay, approximately 90 kilometers south-southwest of Tokyo. The 震级量化地震所释放总能量的单一数值。震级每增加一个整数单位,释放的能量约增加31.6倍。 is estimated at M7.9 by modern analysis of 地震仪用于探测并记录地震波引起的地面运动的仪器。现代数字地震仪可探测到小于一纳米的位移。 records. The rupture occurred on the interface between the Philippine Sea Plate and the Eurasian Plate, with the seafloor of Sagami Bay lurching and generating both severe ground shaking and a 海啸由水下地震导致海底突然位移而产生的一系列海浪。海啸可以喷气机般的速度(时速700公里以上)穿越整个大洋盆地。 that struck the Sagami Bay coastline within minutes. In Yokohama, which was closer to the 震中地震发生在地下的震源正上方对应的地表位置,新闻报道中通常将其作为地震发生的位置。 and contained a large proportion of brick and stone commercial buildings, the initial shaking collapsed roughly 50 percent of all structures. In Tokyo, the shaking was severe but slightly less intense, and the primarily wooden building stock responded differently: wood is a relatively ductile material that tends to lean and sag rather than disintegrate in moderate shaking, though it ultimately fails at high intensities. The 海啸由水下地震导致海底突然位移而产生的一系列海浪。海啸可以喷气机般的速度(时速700公里以上)穿越整个大洋盆地。 generated by the rupture struck the Atami and Sagami Bay coast with waves up to 12 meters high, killing hundreds in coastal communities.

The Science: Fire as the Dominant Killer

The 1923 Great Kanto earthquake is historically unique in that fire — a 次生地震灾害由地震震动引发而非震动本身直接造成的灾害,包括海啸、滑坡、液化、火灾、水坝溃决及化学品泄漏等,其造成的损失往往超过震动本身。 — caused the majority of casualties rather than building collapse or 海啸由水下地震导致海底突然位移而产生的一系列海浪。海啸可以喷气机般的速度(时速700公里以上)穿越整个大洋盆地。. The timing of the earthquake at midday, when approximately 250,000 cooking fires were burning across the wooden cityscape, was decisive. More than 130 fires broke out simultaneously in Tokyo and Yokohama within minutes of the shaking. In the Shitamachi (Low City) districts of eastern Tokyo — flat, low-lying areas with dense wooden construction built on alluvial and 液化饱和松散土壤在强烈震动下暂时失去强度、表现如液体般的现象。可导致建筑物下沉、倾斜或陷入地下坍塌。-prone bay fill — fires spread rapidly. Water mains had been broken by the earthquake, and fire trucks could not navigate debris-filled streets. Winds of 15 to 20 meters per second from a nearby typhoon fanned the fires. The most catastrophic single event was the fire whirl that erupted in the Honjo Military Clothing Depot in eastern Tokyo, where approximately 40,000 people had gathered seeking refuge. A firestorm generated by the convergence of multiple fires created a fire whirl with temperatures exceeding 1,000 degrees Celsius that swept through the open space within minutes, killing approximately 38,000 people in a single location — the deadliest single event in any earthquake-related disaster in modern history. By the time the fires burned out two days later, approximately 381,000 buildings had been destroyed, roughly two-thirds of Tokyo's total building stock.

The Impact: 105,000 Dead, a City Leveled

The official death toll from the 1923 Great Kanto earthquake was approximately 105,385 confirmed deaths, with an additional 43,000 missing — figures that may underestimate actual mortality. Approximately 2 million people were left homeless. Yokohama, the region's primary international port, was almost completely destroyed. The economic losses were staggering: Japan's GDP declined significantly in the following year. The destruction of Tokyo and Yokohama's commercial districts set back Japan's industrial development by several years. Beyond the physical destruction, the disaster was accompanied by a wave of ethnic violence against Korean residents of the Tokyo area, with vigilante groups and some military units killing an estimated 6,000 Koreans based on false rumors that Koreans were poisoning wells and starting fires in the chaos following the earthquake — a dark chapter in Japanese history tied to the social breakdown that follows major 次生地震灾害由地震震动引发而非震动本身直接造成的灾害,包括海啸、滑坡、液化、火灾、水坝溃决及化学品泄漏等,其造成的损失往往超过震动本身。 disasters. 无筋砌体未配置钢筋加固的砖石或砌块结构,对地震震动极为脆弱。无筋砌体建筑是全球地震死亡人数中占比最高的建筑类型。 commercial buildings in both cities performed catastrophically in the shaking, reinforcing the emerging understanding that brick and stone construction required fundamental redesign for seismic regions.

The Response and Reconstruction

The Japanese imperial government's response was shaped by the scale of the disaster and the social instability that followed. The Army was mobilized to maintain order and begin debris removal. Relief supplies were distributed from unaffected provinces. The reconstruction of Tokyo under the direction of Home Minister Shinpei Goto was ambitious: Goto proposed a complete redesign of the city with wider boulevards, parks as fire breaks, and 抗震建筑规范为确保建筑物达到最低地震安全水平而制定的一套法律要求,涉及建筑的设计与施工,通常在重大地震暴露出新的薄弱环节后进行修订。 requirements for seismic resistance. The full plan was ultimately scaled back due to political and financial constraints, and reconstruction proceeded faster than the regulatory framework could be established, with much of Tokyo rebuilt in essentially its pre-earthquake wooden townhouse pattern. However, the earthquake did produce the first serious Japanese 抗震建筑规范为确保建筑物达到最低地震安全水平而制定的一套法律要求,涉及建筑的设计与施工,通常在重大地震暴露出新的薄弱环节后进行修订。 with seismic provisions: the Urban Building Law of 1924 introduced requirements for horizontal seismic loads in structural design, based on acceleration coefficients developed by Japanese engineers studying the damage patterns of the Great Kanto earthquake.

The Legacy: Japan's Seismic Safety Culture

The 1923 Great Kanto earthquake is the founding event of Japan's modern seismic safety culture. September 1 is observed annually as Disaster Prevention Day in Japan, with nationwide earthquake drills on the anniversary. The earthquake motivated the development of the first seismic design provisions for buildings in the world, directly inspired earthquake engineering research programs at Japanese universities, and embedded earthquake preparedness as a core cultural value in Japanese society. The lesson that 次生地震灾害由地震震动引发而非震动本身直接造成的灾害,包括海啸、滑坡、液化、火灾、水坝溃决及化学品泄漏等,其造成的损失往往超过震动本身。 — in this case fire — can be more deadly than the earthquake itself shaped subsequent Japanese urban planning, with fire-break greenways, wider streets, and fire-resistant building materials incorporated into post-war Tokyo's layout. The 1923 disaster's influence on Japanese seismology, engineering, and 地震防灾准备为减轻地震影响而持续进行的规划与准备过程,包括固定家具、制定通讯计划、储备应急物资以及开展演练。 culture ultimately contributed to the dramatic difference in death tolls between the 1923 Great Kanto earthquake and the 2011 Tohoku earthquake — two events of comparable destructive intensity affecting the same metropolitan region, separated by 88 years of scientific and institutional progress.

相关术语

俯冲带
一个构造板块潜入另一板块之下并进入地幔的区域。俯冲带产生世界上最大的地震(8.5级以上),并伴有深海沟和火山弧。
地震仪
用于探测并记录地震波引起的地面运动的仪器。现代数字地震仪可探测到小于一纳米的位移。
地震防灾准备
为减轻地震影响而持续进行的规划与准备过程,包括固定家具、制定通讯计划、储备应急物资以及开展演练。
抗震建筑规范
为确保建筑物达到最低地震安全水平而制定的一套法律要求,涉及建筑的设计与施工,通常在重大地震暴露出新的薄弱环节后进行修订。
无筋砌体
未配置钢筋加固的砖石或砌块结构,对地震震动极为脆弱。无筋砌体建筑是全球地震死亡人数中占比最高的建筑类型。
次生地震灾害
由地震震动引发而非震动本身直接造成的灾害,包括海啸、滑坡、液化、火灾、水坝溃决及化学品泄漏等,其造成的损失往往超过震动本身。
海啸
由水下地震导致海底突然位移而产生的一系列海浪。海啸可以喷气机般的速度(时速700公里以上)穿越整个大洋盆地。
液化
饱和松散土壤在强烈震动下暂时失去强度、表现如液体般的现象。可导致建筑物下沉、倾斜或陷入地下坍塌。
震中
地震发生在地下的震源正上方对应的地表位置,新闻报道中通常将其作为地震发生的位置。
震级
量化地震所释放总能量的单一数值。震级每增加一个整数单位,释放的能量约增加31.6倍。

常见问题解答

地震准备的关键步骤:将重型家具和热水器固定在墙上;准备含有水、食物、手电筒、收音机和急救用品的应急包,至少够用3天以上;确定每个房间的安全位置(坚固桌子下方、远离窗户);练习“蹲下、掩护、抓紧”演练;了解如何关闭燃气和水阀。

如果在室内:蹲下、掩护、抓紧——双膝跪地,躲在坚固的桌子下面,紧紧抓住直到震动停止。不要跑到室外或站在门口。如果在室外:移到远离建筑物、电线和树木的开阔地带。如果在开车:靠边停车,留在车内。

地震预警(EEW)系统检测最先到达、破坏性较小的P波,并在更强的S波到达之前发送警报。ShakeAlert(美国)、J-Alert(日本)和SASMEX(墨西哥)等系统可以提供数秒到数十秒的预警——足够人们躲避、停止列车和关闭工业流程。

地震保险承保地震对建筑物和财物造成的损害,而标准的房屋保险通常不包含此项。是否需要取决于所在地区的地震风险、建筑结构类型以及承受地震损失的经济能力。在加利福尼亚和日本等高风险地区,强烈建议购买地震保险。

抗震建筑采用多种策略:吸收地震能量的柔性结构体系、将建筑与地面运动分离的基础隔震、钢筋混凝土和钢框架结构、抗侧力的剪力墙以及阻尼装置。现代建筑规范(IBC、欧洲规范8)根据当地地震危险性规定设计要求。

液化是指在地震震动过程中,饱和的松散土壤失去强度并表现得像液体一样的现象。这可能导致建筑物下沉、倾斜或倒塌,地下管道和储罐等结构物浮出地面。靠近水体、地下水位较高的砂质土壤最易发生液化。