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December  3, 2020


Agricultural Soils and Climate Change Mitigation


Policymakers, scientists, farmers, and others takeholders
have debated the potential of agricultural soils to sequester
(store) carbon and help mitigate future climate change. This
dis cussion includes various approaches to agriculture-
referred to as carbon farming, regenerative agriculture,
farming for soil health, and farming forsoil carbon
sequestration-and theirpotential to increase agriculture's
role as a greenhouse gas (GHQ sink and reduce its role as a
GHG  source. GHGsinks  remove and store GHGs from the
atmosphere, and GHGsources  emit (release) them.
Figure I. Carbon Cycling in Agricultural Soils


Source: Figure created by CRS.
A    iulue A GCH G                      {rean ik
According to the Environmental Protection Agency (EPA),
the agriculture sector is a net emitter ofGHGs; agricultural
practices, including crop and livestock operations, currently
emit more GHGs  than they remove. The EPA's annual
Inventory ofUS. Greenhouse Gas Emissions andSinks
reports estimates of anthropogenic GHG emissions and
sinks in the United States,using internationally
standardized sectors. On the source side, the agriculture
sector's GHG emis sions -primarily methane and nitrous
oxide-include  those fromlivestockand soilmanagement.
The 2020 Inventory shows that in 2018, the agriculture
sector contributed about 10% of total U.S. GHG emissions.

The Inventory reports estimates of net emissions (emissions
minus removals) fromthe Land Use, Land-Use Change,
and Forestry sector (LULUCF)-primarily carbon dioxide
(C02) emissions and carbon storage. LULUCF includes net
emis s ions for fores tlands, agricultural croplands,
grasslands, andother land types. Data from2018 and prior
years indicate that U.S. croplands are a net GHG source and
grasslands area netsink. Land-use change, rather than land
use, largely shapes these p atterns-the conversion of other
land-usetypes to croplands (netemissions) and to
grasslands (net removals).

AgrkcLdtural Practces That Store Carbn
Soils store carbon in two basic forms: organic (derived
fromliving material, such as plant roots) andinorganic


(derived fromnonliving material, such as minerals). Soil
organic carbon (SOC) measures the carbon in soil organic
matter (SOM), which consists largely of soil microbes (i.e.,
bacteria and fungi), and decaying and decayedplant and
animal material. In addition to its role sequestering carbon,
SOM  is important to soil health and agricultural
productivity. Photosynthesis, decomposition, and
respiration are themajor factors in determining SOC levels
(Figure 1). Photosynthesis fixes atmospheric CO2 into plant
material, which can lead to increased SOC. Decomposition
of SOM  releases CO2 into the atmosphere and leaves a
small amount ofcarbonin the soil. Respiration of plants
and microbes releases CO2 into the atmosphere as a by-
product ofusing organic materials for energy and growth;
this process returns to the atmosphere some of the carbon
fixed through photosynthesis.
Agricultural practices have generally increased net GHG
emissions, but certain practices can reduce GHG emissions
in the atmosphere andincreasenet carbon storage in soils.
Such practices generally reduce soil exposure to air and
increase plant root growth. These practices include no-till
or reduced-till land management and use of cover crops,
compost, and manure. The combination of multiple
practices may further increase carbon storage in soils. The
adoption of carbon-sequestering practices depends on
factors that include requirements for equipment and labor
and vary widely in the United States (Table 1).

Table  I. Selected Carbon-Sequestering Management
Practices in Use in U.S. Croplands (2017)

                                Acres     % of Total
    Management   Practice     (millions)   Cropland
 No-Till (includes Rotational Till) 105      27%
 Reduced-Till                        98         25%
 Cover Crops                          15         4%
 Source: USDA, 201 7 Census ofAgriculture (COA), 20 19, Table 47.
 Note: Total U.S. cropland =396 million acres (COA,Table 1).

 Sc,  ntific D    a
 The carbon sequestration potential of agricultural soils has
been an active research area for decades. Some scientists
are optimistic and others advise caution when considering
agriculture's potential to measurably mitigate global GHG
emissions.
The utility and effectiveness of mitigating GHG emissions
via agriculture depends in part on the
  carbon-storage potential of agricultural soils,
  carbon-storing potential ofagricultural practices, and
  carbon storage over time.
Carbon-storage potential of agricultural soils. Recent
estimates suggest that over the past 12,000 years,human


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