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Enhanced rock weathering: biological climate change mitigation with
co-benefits for food security?
David J. Beerling
Published 5 April 2017.DOI: 10.1098/rsbl.2017.0149

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Under the Paris Agreement of the UN's 21st Conference of the Parties, over
100 nations signed up to the goal of keeping future warming within 2°C of
pre-industrial levels, and ideally below 1.5°C. Yet anthropogenic CO2
emissions,
mainly from combustion of fossil fuels, are now the highest they have been
in human history, and 30% higher than 1990 [1
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-1>].
Accumulation of CO2 and other human-caused greenhouse gases in the
atmosphere has already driven global warming of approximately 1°C. If
warming continues at the current rate, the aspirational target of 1.5°C
will be out of reach within 30 years.

The urgent need for developing methods to extract CO2 from air (so-called
negative emission technologies, NETs) that are safe and affordable, and
that can be scaled-up to augment efforts to reduce CO2 emissions, is
becoming increasingly well recognized and understood (e.g. [2
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-2>]).
Indeed, extensive modelling scenarios assessed by the Intergovernmental
Panel on Climate Change that give us more than a 50% chance of limiting
warming to less than 2°C assume substantial CO2 extraction is achievable
with bioenergy crops in combination with carbon capture and storage (BECCS)
in the second half the 21st Century [3
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-3>].
However, major assumptions about land availability, feasibility at scale,
and costs involved raise doubt about the promise and effectiveness of BECCS
[4 <http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-4>,5
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-5>].

A range of potential techniques for extracting CO2from the atmosphere is
being investigated that afford opportunities for mitigating and
ameliorating climate change (figure 1
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#F1>), each of
which also needs to be understood in terms of feasibility, cost and
acceptability [6
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-6>,7
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-7>]. The
papers in this mini-series address an underdeveloped NET, enhanced rock
weathering, with a particular focus on croplands managed for food
production and bioenergy. Weathering is a slow natural process removing CO2from
the atmosphere on long timescales of a million years or more. During
weathering, silicate rocks are chemically broken down to release base
cations and generate bicarbonate, which is ultimately transferred to the
oceans leading to carbonate precipitation on the seafloor. These processes
can be accelerated by amending soils with crushed calcium and
magnesium-bearing silicate rocks with a high reactive surface area to
deliver effective carbon sequestration in soils and the oceans [8
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-8>,9
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-9>].
Enhanced weathering is also co-deployable with forestry and crops used in
BECCS, enhancing its carbon sequestration potential and reducing costs.
Reduced atmospheric CO2, in combination with the production of soluble
alkalinity from weathered rocks, can help reduce ocean acidification to
protect coral reefs and marine fisheries [8
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-8>,9
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-9>].
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Figure 1.

Six common categories of negative emissions strategies for extracting CO2 from
the atmosphere. Reproduced with permission from [7
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-7>].

Kantola *et al.* [10
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-10>] deal
with the opportunities presented by row crop agricultural production of
food and bioenergy crops for enhancing rock weathering. They highlight
mechanisms by which enhanced weathering on agricultural lands could combat
soil acidification and nitrogen loss while providing plant-essential
nutrients, two negative consequences of intensive cropland farming.
Uncertainties in the long-term effects on soils and crops remain and can
only be addressed through long-term experiments and field trials
investigating feasibility and effectiveness. Nevertheless, with nearly 11%
of the terrestrial surface intensively managed for crop production,
enhanced weathering could offer an opportunity to employ these soils to
sequester atmospheric carbon at scale within a decade or two, while
benefitting crop production. Additionally, this would use land already in
production, thereby avoiding potential land use conflicts.

Edwards *et al.* [11
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-11>]
provide a complementary tropical cropland perspective, focusing on the
potential for deployment of enhanced weathering across over 680 million
hectares of tropical agriculture, with the warm climates and productive
crops substantially accelerating weathering. They identify potential
co-benefits including decreased soil acidification, reduced heavy metal
toxicity and increased phosphorus-supply of highly weathered nutrient-poor
tropical soils promoting higher crop yields. This may have the effect of
sparing forest for conservation, and reducing cultural eutrophication.
Recycling the substantial annual global production of silicate waste
resulting from human activities [12
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-12>]
would minimize the impacts of mining operations on the environment,
including deforestation, and reduce energy requirements for crushing and
transporting silicates. Negative consequences identified [11
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-11>]
include erosion of silicates into rivers and coral reefs that might
increase inorganic turbidity, sedimentation and pH, with unknown impacts
for biodiversity. They conclude by outlining a research agenda for
responsibly unlocking the potential of the tropics for carbon capture by
enhanced weathering, including assessment of the potential impacts on human
health, farmland, forest, stream-water chemistry and biodiversity.

Questions concerning the spatial scale of roll-out necessary to affect
atmospheric CO2, climate and ocean chemistry on decadal to century
timescales can only be addressed through Earth system modelling [8
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-8>,9
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-9>].
Central to these large-scale Earth system issues are robust numerical
models describing the geochemical weathering of crushed silicates by
climate in combination with the rooting systems of crop plants and their
associated soil microbes. In this context, Taylor *et al.* [13
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-13>]
review how current models represent the geochemical processes describing
the soil weathering CO2 sink. They highlight the need to bridge the gap
between the current generation of weathering models that typically neglect
agricultural processes and agricultural models simulating how land
management practices govern cropland soil chemistry and greenhouse gas
emissions that neglect weathering. Land use history and fertilizers are key
drivers of the physico-chemical characteristics of agricultural soils,
including pH. Capturing these interactions with crushed silicates will be
an important development of soil weathering models if they are to provide
powerful and flexible research tools for assessment of rates of enhanced
weathering, nutrient release, pH change and carbon capture.

Meysman & Montserrat [14
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-14>]
shift the focus to the marine realm by considering the potential for carbon
capture by applying crushed silicates directly into coastal environments.
The idea is that deliberately introducing fast-weathering silicate minerals
onto coastal sediments releases alkalinity into the overlying waters, thus
creating a coastal CO2 sink. As they point out, the concept is still at an
early stage and dedicated experiments need to (i) better constrain the
weathering rate under *in situ* conditions, and (ii) evaluate ecosystem
impacts arising from the liberation of weathered chemical products.

Ultimately, the public perception of any NET option may prove to be as
important as the underlying scientific evidence that builds the case for
deployment to combat climate change. If policymakers and governments
propose deployment, there has to public trust and acceptance of the
technology involved. Social science engagement is therefore critical to
understanding how society will perceive different NET options [15
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-15>]. How
might public groups in the UK, North America and non-western countries,
respond to and perceive potential risks and benefits of possible enhanced
weathering strategies as innovative responses to the climate change
problem? Pidgeon & Spence [16
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-16>]
report the first UK-wide assessment of the public's social perception of
enhanced terrestrial weathering. Their analyses provide an important
baseline for determining how this may change as the technology gains
prominence and for comparing the UK public with other parts of the world.
Encouragingly, it appears the public generally agree that scientists should
be able to conduct small-scale trials into enhanced weathering, provided
there is scientific independence, strict monitoring, risk minimization and
transparency of results.

Lawford-Smith & Currie [17
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-17>]
address some of the thorny ethical issues associated with developing
negative emissions options. They analyse the well-rehearsed moral hazard
argument in relation to questions of blame and responsibility for removing
the onus on developed countries to reduce fossil fuel emissions. Would
large-scale effective NETs deployed in the future lead to less mitigation
today [18
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-18>]?
Might, for example, it encourage society to think CO2 emissions can exceed
‘safe’ limits in the near-term with the promise that excess carbon will
pulled out of the atmosphere later? Given current lack of depth in our
understanding of the effectiveness of NETs, a safer working assumption
might be that they may not be deployable this century, forcing the urgency
of deeper near-term emission cuts to avoid locking in the worst effects of
future climate change.

Collectively, the papers in this mini-series suggest that enhanced
weathering has promise in providing climate and food security by capturing
carbon and improving crop yields, while decreasing fertilizer and pesticide
usage and costs. The collection is not in any way intended to be a
comprehensive treatment of the topic but rather to represent an
introduction to some of the key issues with an emphasis on biological
interactions; detailed treatment of enhanced weathering is given elsewhere [
19 <http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-19>].
The topic is, however, the focus of the newly established international
Leverhulme Centre for Climate Change Mitigation (http://www.lc3m.org/). The
new Centre aims to deliver transformative understanding of all aspects of
enhanced weathering with croplands as a strategic NET, including its
technical, environmental, economic and social viability, as highlighted in
a recent *Nature Geoscience* editorial [20
<http://rsbl.royalsocietypublishing.org/content/13/4/20170149#ref-20>]. It
aims to revolutionize climate change mitigation by linking it to the
substantive co-benefit of delivering resource-efficient sustainable food
security. Moving towards these goals will require fundamentally
understanding our ability to manipulate food/bioenergy production systems
to drive biogeochemical cycles that positively affect global CO2, climate
and ocean chemistry—a formidable challenge that underpins some climate
change mitigation strategies required by the Paris Agreement

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