A climate change solution thats right under our feet Asmeret Asefaw Berhe

So one of the most important solutions

to the global challenge
posed by climate change

lies right under our foot every day.

It’s soil.

Soil’s just the thin veil
that covers the surface of land,

but it has the power to shape
our planet’s destiny.

See, a six-foot or so of soil,

loose soil material
that covers the earth’s surface,

represents the difference between life
and lifelessness in the earth system,

and it can also help us
combat climate change

if we can only stop treating it like dirt.

(Laughter)

Climate change is happening,

the earth’s atmosphere is warming,

because of the increasing amount
of greenhouse gases

we keep releasing into the atmosphere.

You all know that.

But what I assume you might not have heard

is that one of the most important things
our human society could do

to address climate change

lies right there in the soil.

I’m a soil scientist who has been
studying soil since I was 18,

because I’m interested in unlocking
the secrets of soil

and helping people understand this
really important climate change solution.

So here are the facts about climate.

The concentration of carbon dioxide
in the earth’s atmosphere

has increased by 40 percent

just in the last 150 years or so.

Human actions are now releasing
9.4 billion metric tons of carbon

into the atmosphere,

from activities
such as burning fossil fuels

and intensive agricultural practices,

and other ways we change
the way we use land,

including deforestation.

But the concentration of carbon dioxide
that stays in the atmosphere

is only increasing by about half of that,

and that’s because half of the carbon
we keep releasing into the atmosphere

is currently being taken up
by land and the seas

through a process we know
as carbon sequestration.

So in essence, whatever consequence
you think we’re facing

from climate change right now,

we’re only experiencing the consequence
of 50 percent of our pollution,

because the natural ecosystems
are bailing us out.

But don’t get too comfortable,

because we have two major things
working against us right now.

One: unless we do something big,

and then fast,

emissions will continue to rise.

And second: the ability
of these natural ecosystems

to take up carbon dioxide
from the atmosphere

and sequester it in the natural habitats

is currently getting compromised,

as they’re experiencing serious
degradation because of human actions.

So it’s not entirely clear

that we will continue to get bailed out
by these natural ecosystems

if we continue on this
business-as-usual path that we’ve been.

Here’s where the soil comes in:

there is about three thousand billion
metric tons of carbon in the soil.

That’s roughly about 315 times
the amount of carbon

that we release
into the atmosphere currently.

And there’s twice more carbon in soil
than there is in vegetation and air.

Think about that for a second.

There’s more carbon in soil

than there is in all
of the world’s vegetation,

including the lush tropical rainforests
and the giant sequoias,

the expansive grasslands,

all of the cultivated systems,

and every kind of flora you can imagine
on the face of the earth,

plus all the carbon that’s currently
up in the atmosphere, combined,

and then twice over.

Hence, a very small change
in the amount of carbon stored in soil

can make a big difference
in maintenance of the earth’s atmosphere.

But soil’s not just simply
a storage box for carbon, though.

It operates more like a bank account,

and the amount of carbon
that’s in soil at any given time

is a function of the amount of carbon
coming in and out of the soil.

Carbon comes into the soil
through the process of photosynthesis,

when green plants take carbon dioxide
from the atmosphere

and use it to make their bodies,

and upon death,
their bodies enter the soil.

And carbon leaves the soil

and goes right back up into the atmosphere

when the bodies of those
formerly living organisms

decay in soil by the activity of microbes.

See, decomposition releases
carbon dioxide into the atmosphere,

as well as other greenhouse gases
such as methane and nitrous oxide,

but it also releases all the nutrients
we all need to survive.

One of the things that makes soil
such a fundamental component

of any climate change mitigation strategy

is because it represents
a long-term storage of carbon.

Carbon that would have lasted
maybe a year or two

in decaying residue
if it was left on the surface

can stay in soil for hundreds of years,
even thousands and more.

Soil biogeochemists like me

study exactly how the soil system
makes this possible,

by locking away the carbon
in physical association with minerals,

inside aggregates of soil minerals,

and formation of strong chemical bonds

that bind the carbon
to the surfaces of the minerals.

See when carbon is entrapped in soil,

in these kinds of associations
with soil minerals,

even the wiliest of the microbes
can’t easily degrade it.

And carbon that’s not degrading fast

is carbon that’s not going back
into the atmosphere as greenhouse gases.

But the benefit of carbon sequestration

is not just limited
to climate change mitigation.

Soil that stores large amounts of carbon
is healthy, fertile, soft.

It’s malleable. It’s workable.

It makes it like a sponge.

It can hold on to
a lot of water and nutrients.

Healthy and fertile soils like this

support the most dynamic, abundant
and diverse habitat for living things

that we know of anywhere
on the earth system.

It makes life possible for everything
from the tiniest of the microbes,

such as bacteria and fungi,

all the way to higher plants,

and fulfills the food, feed
and fiber needs for all animals,

including you and I.

So at this point, you would assume
that we should be treating soil

like the precious resource that it is.

Unfortunately, that’s not the case.

Soils around the world are experiencing
unprecedented rates of degradation

through a variety of human actions
that include deforestation,

intensive agricultural production systems,

overgrazing,

excessive application
of agricultural chemicals,

erosion and similar things.

Half of the world’s soils
are currently considered degraded.

Soil degradation is bad for many reasons,

but let me just tell you a couple.

One: degraded soils have diminished
potential to support plant productivity.

And hence, by degrading soil,

we’re compromising our own abilities
to provide the food and other resources

that we need for us

and every member of living things
on the face of the earth.

And second:

soil use and degradation,
just in the last 200 years or so,

has released 12 times more carbon
into the atmosphere

compared to the rate at
which we’re releasing carbon

into the atmosphere right now.

I’m afraid there’s even more bad news.

This is a story of soils
at high latitudes.

Peatlands in polar environments

store about a third
of the global soil carbon reserves.

These peatlands have
a permanently frozen ground underneath,

the permafrost,

and the carbon was able to build up
in these soils over long periods of time

because even though plants are able
to photosynthesize during the short,

warm summer months,

the environment quickly
turns cold and dark,

and then microbes are not able
to efficiently break down the residue.

So the soil carbon bank
in these polar environments

built up over hundreds
of thousands of years.

But right now, with atmospheric warming,

the permafrost is thawing and draining.

And when permafrost thaws and drains,

it makes it possible
for microbes to come in

and rather quickly
decompose all this carbon,

with the potential to release hundreds
of billions of metric tons of carbon

into the atmosphere
in the form of greenhouse gases.

And this release of additional
greenhouse gases into the atmosphere

will only contribute to further warming

that makes this predicament even worse,

as it starts a self-reinforcing
positive feedback loop

that could go on and on and on,

dramatically changing our climate future.

Fortunately, I can also tell you
that there is a solution

for these two wicked problems
of soil degradation and climate change.

Just like we created these problems,

we do know the solution,

and the solution lies
in simultaneously working

to address these two things together,

through what we call
climate-smart land management practices.

What do I mean here?

I mean managing land
in a way that’s smart

about maximizing
how much carbon we store in soil.

And we can accomplish this

by putting in place
deep-rooted perennial plants,

putting back forests whenever possible,

reducing tillage and other disturbances
from agricultural practices,

including optimizing the use
of agricultural chemicals and grazing

and even adding carbon to soil,
whenever possible,

from recycled resources
such as compost and even human waste.

This kind of land stewardship
is not a radical idea.

It’s what made it possible
for fertile soils

to be able to support human civilizations
since time immemorial.

In fact, some are doing it just right now.

There’s a global effort underway
to accomplish exactly this goal.

This effort that started in France
is known as the “4 per 1000” effort,

and it sets an aspirational goal

to increase the amount of carbon
stored in soil by 0.4 percent annually,

using the same kind of climate-smart
land management practices

I mentioned earlier.

And if this effort’s fully successful,

it can offset a third
of the global emissions

of fossil-fuel-derived carbon
into the atmosphere.

But even if this effort
is not fully successful,

but we just start heading
in that direction,

we still end up with soils
that are healthier, more fertile,

are able to produce all the food
and resources that we need

for human populations and more,

and also soils that are better capable

of sequestering carbon dioxide
from the atmosphere

and helping with
climate change mitigation.

I’m pretty sure that’s what politicians
call a win-win solution.

And we all can have a role to play here.

We can start by treating the soil
with the respect that it deserves:

respect for its ability
as the basis of all life on earth,

respect for its ability to serve
as a carbon bank

and respect for its ability
to control our climate.

And if we do so,

we can then simultaneously address

two of the most pressing
global challenges of our time:

climate change and soil degradation.

And in the process, we would be able
to provide food and nutritional security

to our growing human family.

Thank you.

(Applause)

因此

,应对气候变化带来的全球挑战的最重要解决方案之一

每天都在我们脚下。

是土壤。

土壤只是
覆盖陆地表面的薄薄的面纱,

但它具有塑造
我们星球命运的力量。

看,六英尺左右的土壤

,覆盖地球表面的松散土壤材料,

代表
着地球系统中生与死的区别,

如果我们不能像对待泥土一样对待它,它还可以帮助我们应对气候变化 .

(笑声)

气候变化正在发生

,地球大气正在变暖,

因为

我们不断向大气中释放越来越多的温室气体。

你们都知道。

但我想你可能没有听说过


我们人类社会可以

为应对气候变化做的最重要的事情之一

就在土壤中。

我是一名土壤科学家,
从 18 岁起就开始研究土壤,

因为我有兴趣解开
土壤的秘密

并帮助人们了解这一
非常重要的气候变化解决方案。

所以这里是关于气候的事实。

仅在过去 150 年左右
,地球大气中的二氧化碳浓度

就增加了 40%

人类行为现在正在向大气释放
94 亿吨碳

这些碳来自燃烧化石燃料

和集约农业实践等活动,

以及
我们改变土地使用方式的其他方式,

包括森林砍伐。

但是
留在大气中的二氧化碳浓度

只增加了大约一半

,这是因为
我们不断释放到大气

中的碳的一半目前正在

通过我们
称为碳的过程被陆地和海洋吸收 封存。

所以从本质上讲,无论
你认为我们

现在面临气候变化带来

的后果,我们只经历
了 50% 污染的后果,

因为自然生态系统
正在拯救我们。

但是不要太自在,

因为我们现在有两件主要的
事情对我们不利。

一:除非我们做大事,

然后快速,

排放量将继续上升。

第二:
这些自然生态系统从大气

中吸收二氧化碳

并将其隔离在自然栖息地的

能力目前正在受到损害,

因为它们正在经历
人类活动的严重退化。

因此,

如果我们继续
走我们一直以来的一切如常的道路,我们是否会继续得到这些自然生态系统的救助并不完全清楚。

这就是土壤的来源:土壤

中约有 3000
亿吨碳。

这大约

是我们
目前释放到大气中的碳量的 315 倍。

土壤中的碳
含量是植被和空气中的两倍。

这点考虑一下吧。

土壤中的碳含量


世界上所有植被中的碳含量都多,

包括茂密的热带雨林
和巨大的红杉

、广阔的草原、

所有的耕作系统

以及
地球表面上你能想象到的各种植物,

加上目前在大气中的所有碳
,加起来,

然后是两倍。

因此,
土壤中储存的碳量的一个非常小的变化

可以
对地球大气的维护产生很大的影响。

但是,土壤不仅仅是
碳的储存箱。

它的运作更像是一个银行账户,

在任何给定时间,土壤中

的碳量都是进出土壤的碳量的函数


通过光合作用进入土壤,

当绿色植物
从大气中吸收二氧化碳

并利用它制造身体

时,
它们的身体在死亡时进入土壤。

当那些
以前的生物体

在土壤中因微生物的活动而腐烂时,碳会离开土壤并直接回到大气中。

看,分解会
向大气中释放二氧化碳,

以及甲烷和一氧化二氮等其他温室气体,

但它也会释放
我们生存所需的所有营养物质。

使土壤

成为任何减缓气候变化战略的基本组成部分的

原因之一是它代表
了碳的长期储存。 如果将其留在表面上

,可能会在腐烂残留物中持续
一两年的碳

可以在土壤中停留数百年,
甚至数千年甚至更长时间。

像我这样的土壤生物地球化学家

研究土壤系统是如何
使这成为可能的,方法

是锁定
与矿物质物理结合的碳

、土壤矿物质的内部聚集体,

以及形成

将碳结合
到矿物质表面的强化学键。

看看碳何时被困在土壤中,


与土壤矿物质的这些关联中,

即使是最狡猾的微生物
也无法轻易降解它。

不会快速降解

的碳是不会
作为温室气体回到大气中的碳。

但碳封存的好处

不仅
限于减缓气候变化。

储存大量碳的土壤
健康、肥沃、柔软。

它具有延展性。 这是可行的。

它使它像海绵一样。

它可以
保持大量的水分和营养。

像这样健康肥沃的土壤为我们所知的地球系统上任何地方的生物

提供了最有活力、最丰富
、最多样化的栖息

地。

它使
从最微小的微生物(

如细菌和真菌)

到高等植物的一切都成为可能,


满足所有动物(

包括你和我)对食物、饲料和纤维的需求。

所以在这一点上,你 会
假设我们应该

像对待宝贵的资源一样对待土壤。

不幸的是,事实并非如此。

世界各地的土壤正在经历
前所未有的退化速度,

这些人类
行为包括砍伐森林、

集约化农业生产系统、

过度放牧、

过度
使用农药、

侵蚀和类似的事情。 目前

,世界上一半的土壤
被认为已经退化。

土壤退化不好的原因有很多,

但让我告诉你几个。

一:退化的土壤降低
了支持植物生产力的潜力。

因此,通过使土壤退化,

我们正在损害我们自己为我们和地球上的每一个生物成员
提供所需的食物和其他资源的能力

第二:

就在过去 200 年左右的时间里,土壤利用和退化

向大气中

释放的碳是我们

现在向大气中释放碳的速度的 12 倍。

恐怕还有更多的坏消息。

这是一个关于
高纬度土壤的故事。

极地环境中的泥炭地

储存
了全球约三分之一的土壤碳储量。

这些泥炭
地下面有永久冻土,

即永久冻土

,碳能够
在这些土壤中长时间积累,

因为即使植物能够
在短暂而

温暖的夏季进行光合作用

,环境也会迅速
变冷, 黑暗,

然后微生物
不能有效地分解残留物。

因此,这些极地环境中的土壤碳库已经

建立了
数十万年。

但是现在,随着大气变暖

,永久冻土正在融化和流失。

当永久冻土融化和排水时,

微生物可以进入

并迅速
分解所有这些碳,

并有可能以温室气体的形式将
数千亿公吨的碳释放

到大气
中。

而这种
向大气中释放额外的温室气体

只会导致进一步的变暖

,使这种困境变得更糟,

因为它开始了一个自我强化的
正反馈循环

,这个循环可能会一直持续下去,从而

极大地改变我们的气候未来。

幸运的是,我还可以告诉你
,土壤退化和气候变化

这两个棘手的问题是有解决办法的

就像我们制造了这些问题一样,

我们确实知道解决方案,

而解决方案在于

通过我们所谓的
气候智能型土地管理实践同时努力解决这两个问题。

我在这里是什么意思?

我的意思
是以一种聪明的方式管理土地,

最大限度地增加
我们在土壤中储存的碳量。

我们可以通过

种植根深蒂固的多年生植物、

尽可能恢复森林、

减少耕作和其他农业实践造成的干扰
来实现这一目标,

包括优化
农药和放牧的使用

,甚至尽可能在土壤中添加碳

从 回收资源
,如堆肥,甚至人类废物。

这种土地
管理并不是一个激进的想法。 自远古以来,

这就是
肥沃的土壤

能够支持人类文明的
原因。

事实上,有些人现在正在这样做。

全球正在
努力实现这一目标。

这项始于法国的努力
被称为“千分之四”努力

,它设定了一个雄心勃勃的目标

,即使用我提到的同一种气候智能型土地管理实践,每年将土壤中储存的碳量增加 0.4%

早些时候。

如果这项努力完全成功,

它可以抵消全球三分之一

的化石燃料衍生碳排放
到大气中。

但即使这项
努力没有完全成功,

但我们只是开始
朝着那个方向前进,

我们最终的土壤
仍然更健康、更肥沃

,能够生产
我们人类所需的所有食物和资源

等等,

以及能够更好地从大气

中隔离二氧化碳

并有助于
缓解气候变化的土壤。

我很确定这就是政客们
所说的双赢解决方案。

我们都可以在这里发挥作用。

我们可以首先以
应有的尊重对待土壤:尊重其

作为地球上所有生命基础的

能力,尊重其
作为碳银行

的能力,以及尊重其
控制气候的能力。

如果我们这样做,

我们就可以同时应对我们这个时代

最紧迫的两个
全球挑战:

气候变化和土壤退化。

在此过程中,我们将能够

为我们日益壮大的人类大家庭提供食物和营养保障。

谢谢你。

(掌声)