Why do buildings fall in earthquakes Vicki V. May

Earthquakes have always been
a terrifying phenomenon,

and they’ve become more deadly
as our cities have grown,

with collapsing buildings posing
one of the largest risks.

Why do buildings collapse
in an earthquake,

and how can it be prevented?

If you’ve watched a lot of disaster films,

you might have the idea

that building collapse is caused directly
by the ground beneath them

shaking violently,
or even splitting apart.

But that’s not really how it works.

For one thing, most buildings
are not located right on a fault line,

and the shifting tectonic plates
go much deeper than building foundations.

So what’s actually going on?

In fact, the reality of earthquakes
and their effect on buildings

is a bit more complicated.

To make sense of it,
architects and engineers use models,

like a two-dimensional array of lines
representing columns and beams,

or a single line lollipop with circles
representing the building’s mass.

Even when simplified to this degree,
these models can be quite useful,

as predicting a building’s response
to an earthquake

is primarily a matter of physics.

Most collapses that occur
during earthquakes

aren’t actually caused
by the earthquake itself.

Instead, when the ground moves
beneath a building,

it displaces the foundation
and lower levels,

sending shock waves through
the rest of the structure

and causing it to vibrate back and forth.

The strength of this oscillation
depends on two main factors:

the building’s mass,
which is concentrated at the bottom,

and its stiffness,

which is the force required
to cause a certain amount of displacement.

Along with the building’s material type
and the shape of its columns,

stiffness is largely a matter of height.

Shorter buildings tend to be stiffer
and shift less,

while taller buildings are more flexible.

You might think that the solution
is to build shorter buildlings

so that they shift as little as possible.

But the 1985 Mexico City earthquake is
a good example of why that’s not the case.

During the quake,

many buildings between six
and fifteen stories tall collapsed.

What’s strange is that while shorter
buildings nearby did keep standing,

buildings taller than fifteen stories
were also less damaged,

and the midsized buildings that collapsed

were observed shaking far more violently
than the earthquake itself.

How is that possible?

The answer has to do with something
known as natural frequency.

In an oscillating system,

the frequency is how many back and forth
movement cycles occur within a second.

This is the inverse of the period,

which is how many seconds it takes
to complete one cycle.

And a building’s natural frequency,
determined by its mass and stiffness,

is the frequency that its vibrations
will tend to cluster around.

Increasing a building’s mass slows down
the rate at which it naturally vibrates,

while increasing stiffness
makes it vibrate faster.

So in the equation representing
their relationship,

stiffness and natural frequency
are proportional to one another,

while mass and natural frequency
are inversely proportional.

What happened in Mexico City
was an effect called resonance,

where the frequency
of the earthquake’s seismic waves

happen to match the natural frequency
of the midsized buildings.

Like a well-timed push on a swingset,

each additional seismic wave
amplified the building’s vibration

in its current direction,

causing it to swing even further back,
and so on,

eventually reaching a far greater extent
than the initial displacement.

Today, engineers work
with geologists and seismologists

to predict the frequency
of earthquake motions at building sites

in order to prevent
resonance-induced collapses,

taking into account factors
such as soil type and fault type,

as well as data from previous quakes.

Low frequencies of motion
will cause more damage to taller

and more flexible buildings,

while high frequencies of motion
pose more threat

to structures that
are shorter and stiffer.

Engineers have also devised ways
to abosrb shocks

and limit deformation
using innovative systems.

Base isolation uses flexible layers

to isolate the foundation’s displacement
from the rest of the building,

while tuned mass damper systems
cancel out resonance

by oscillating out of phase
with the natural frequency

to reduce vibrations.

In the end, it’s not the sturdiest
buildings that will remain standing

but the smartest ones.

地震一直是
一个可怕的现象,

随着我们城市的发展,地震变得更加致命

,倒塌的建筑物
构成了最大的风险之一。

为什么建筑物会
在地震中倒塌

,如何预防?

如果你看过很多灾难片,

你可能会有这样的想法

,建筑物倒塌是直接
由其下方的地面

剧烈震动,
甚至分裂造成的。

但这并不是真正的工作方式。

一方面,大多数建筑物
并不位于断层线上

,移动的构造板块
比建筑物地基要深得多。

那么究竟发生了什么?

事实上,地震的现实
及其对建筑物的影响

要复杂一些。

为了理解它,
建筑师和工程师使用模型,

例如
代表柱和梁的二维线阵列,

或者代表建筑物质量的带有圆圈的单线棒棒糖

即使简化到这种程度,
这些模型也非常有用,

因为预测建筑物
对地震

的响应主要是物理问题。

地震期间发生的大多数倒塌

实际上并不是
由地震本身引起的。

相反,当地面
在建筑物下方移动时,

它会移动地基
和较低的楼层,

从而通过
结构的其余部分发送冲击波

并使其来回振动。

这种振动的强度
取决于两个主要因素

:建筑物的质量
(集中在底部)

和刚度(

引起一定位移所需的力)

除了建筑物的材料类型
和柱子的形状外,

刚度在很大程度上也与高度有关。

较短的建筑物往往更坚固
且移动更少,

而较高的建筑物则更灵活。

您可能认为解决方案
是建造更短的建筑物,

以便它们尽可能少地移动。

但 1985 年墨西哥城地震就是
一个很好的例子,说明为什么情况并非如此。

地震期间,

许多六
至十五层高的建筑物倒塌。

奇怪的是,虽然
附近矮矮的

建筑物依然屹立不倒,但十五层以上的建筑物
受到的破坏也较小,

而且倒塌的中型建筑物的

震动
远比地震本身剧烈得多。

这怎么可能?

答案与
所谓的自然频率有关。

在振荡系统中

,频率是
在一秒钟内发生多少来回运动周期。

这是周期的倒数,


完成一个周期所需的秒数。

由其质量和刚度决定的建筑物的固有

频率是其
振动倾向于聚集的频率。

增加建筑物的质量会
减慢其自然振动的速度,

而增加刚度
会使其振动得更快。

所以在表示它们关系的方程中

刚度和固有
频率成正比,

而质量和固有
频率成反比。

墨西哥城发生的事情
是一种称为共振的效应,

地震的地震波

频率恰好与中型建筑物的自然频率
相匹配。

就像在秋千上适时推动一样,

每次额外的地震波都会
放大建筑物

在其当前方向上的振动,

使其摆动得更远,
依此类推,

最终达到比初始位移更大的程度

今天,工程师
与地质学家和地震学家

合作,预测
建筑工地的地震运动频率,

以防止
共振引起的倒塌,

同时考虑到
土壤类型和断层类型等因素,

以及以前地震的数据。

低频率的运动
将对更高

、更灵活的建筑物造成更大的破坏,

而高频率的运动

更短、更硬的结构构成更大的威胁。

工程师们还设计了使用创新系统
来吸收冲击

和限制变形的
方法。

基础隔离使用柔性

层将基础的位移
与建筑物的其余部分隔离,

而调谐质量阻尼器系统

通过与固有频率异相振荡来消除共振

以减少振动。

最终,能屹立不倒的不是最坚固的
建筑,

而是最聪明的建筑。