A Yale- led study finds that agricultural liming (adding crushed limestone) in the Mississippi River Basin has acted as a net carbon sink, removing more CO₂ than it emits.

The practice, long used by farmers to raise soil pH, reduce acidity, and boost crop yields, covers a vast region: the Mississippi River Basin spans about 41% of the contiguous U.S. and includes roughly 65% of U.S. cropland.

Researchers, led by geochemist Tim Jesper Suhrhoff (Yale Center for Natural Carbon Capture), analyzed more than a century of data (roughly 1900- 2015) on river chemistry, fertilizer use, atmospheric pollution, and liming rates, combined with geochemical modeling.

Conventional accounting (including IPCC guidelines) treats liming as a CO₂ source because the carbon in limestone can be released as CO₂ when it reacts with strong acids in soil.

The new work argues this is incomplete: soil acidity from nitrogen fertilizers and fossil- fuel pollution is the main driver of those emissions. Without liming, the acids would still react with natural soil alkalinity and release CO₂.

In the presence of liming, much of the reaction instead forms bicarbonate that is exported by rivers (including the Mississippi) and can ultimately sequester carbon in the ocean for long periods. Compared with a no- liming scenario, liming in the basin removed an estimated 300- 400 million tonnes of CO₂.

Efficacy has improved since the 1930s as liming rates rose; current removal is estimated at about 75% of the theoretical maximum.

The study (published in Nature) concludes that liming aligns climate benefits with agronomic ones (higher yields, potentially lower nitrous- oxide emissions). It suggests policy and emissions inventories should attribute emissions to acid inputs rather than to liming itself, and that strategies such as adding silicate rock first to neutralize acidity could further enhance carbon removal.

The linked phys.org article appears to cover this same research (the URL slug matches the topic and timing). Related earlier work from the Yale group has also highlighted liming’s dual role in soil management and carbon cycling.

Silicate weathering is the natural chemical breakdown of silicate minerals (e.g., those in basalt, olivine, or other igneous rocks) by carbonic acid formed when atmospheric CO₂ dissolves in water.

The simplified reaction consumes CO₂ and produces bicarbonate ions (HCO₃⁻) plus dissolved cations such as Ca²⁺, Mg²⁺, K⁺, and Si:

$$\mathrm{CaSiO_3 + 2CO_2 + H_2O \to Ca^{2+} + 2HCO_3^- + SiO_2}$$

(Similar reactions occur for magnesium and other silicates.) The bicarbonate is ultimately transported to rivers and oceans, where the carbon can remain sequestered for thousands to hundreds of thousands of years. Natural silicate weathering already removes roughly 0.5 Gt CO₂ per year globally; enhanced rock weathering (ERW) accelerates it by crushing silicate rocks into fine powder and spreading them on soils (especially agricultural land).

Primary climate benefit: Carbon dioxide removal (CDR)

ERW converts atmospheric CO₂ into stable bicarbonate that is stored in groundwater and the ocean on intergenerational to geological timescales.

Field trials (e.g., U.S. Corn Belt maize-soybean rotations) have measured cumulative CDR potentials of ~10.5 t CO₂ ha⁻¹ over four years at application rates of ~50 t ha⁻¹ yr⁻¹ of basalt.

Modeling studies project that widespread deployment on U.S. farmland could deliver 0.16–0.30 Gt CO₂ yr⁻¹ by 2050 (rising further by 2070), and global estimates often fall in the 0.5–2 Gt CO₂ yr⁻¹ range under ambitious scenarios (after accounting for mining, grinding, and transport emissions).

Unlike carbonate liming (which can release some of its own carbon under acidic conditions), pure silicate minerals contain no carbon of their own, so the alkalinity they generate is more fully atmospheric in origin. Silicates can therefore act as a clearer net sink and are sometimes proposed as a complement or partial replacement for agricultural lime.

Agronomic and soil- health co -benefits

Soil pH regulation: Silicate dissolution neutralizes acidity, raising pH in a manner similar to traditional liming. This improves nutrient availability, reduces aluminum toxicity, and supports healthier microbial communities.

Nutrient release: Weathering supplies plant- available calcium, magnesium, potassium, phosphorus, silicon, and micronutrients. Field studies show elevated concentrations of these elements in soil and crops, partially offsetting the need for synthetic fertilizers.

Crop yield increases: Trials report 12- 16% higher maize and soybean yields, with similar gains for other crops (e.g., sugarcane, miscanthus). Silicon uptake can also strengthen plant tissues, improving resistance to pests, pathogens, and drought.

Reduced nitrous oxide (N₂O) emissions: Better soil conditions and higher pH can lower emissions of this potent greenhouse gas, improving the overall greenhouse- gas balance of ERW by tens of percent in some simulations.

Additional ecosystem effects: Higher silicon in runoff can favor diatoms over harmful algal blooms (reducing eutrophication risk). Downstream alkalinity can help buffer ocean acidification. Some studies also note modest reductions in surface ozone in agricultural regions, which further supports yields.

Relation to the Mississippi River Basin and liming context

In the recent Nature study on agricultural liming, the authors note that silicates are already used for pH management and have attracted strong interest as enhanced- weathering feedstocks. Because silicates do not carry their own carbonate carbon, they avoid some of the accounting complexities of limestone while still providing the same agronomic benefits (pH correction and nutrient release). Modeling and field work in the U.S. Midwest (including the Corn Belt portion of the Mississippi basin) indicate that combining or sequencing silicate and carbonate amendments could optimize both yield and long- term carbon removal.

Practical considerations

Benefits are greatest in warm, wet, acidic soils with active biological communities (roots and microbes accelerate dissolution). Application rates of tens of tonnes per hectare are typical. Life- cycle emissions from grinding and transport must be minimized (renewable energy helps), and potential release of trace metals is monitored; well- chosen basalts generally show low risk in trials. Measurement, reporting, and verification of the actual CDR remain active research areas because of soil heterogeneity and time lags.

In short, silicate weathering (especially when enhanced on farmland) offers durable carbon removal while delivering direct benefits to soil fertility, crop productivity, and other greenhouse- gas reductions, aligning climate action with existing agricultural practices.

Agricultural liming is a carbon sink in the Mississippi River Basin

Application of carbonate minerals (limestone or dolomite) to farmland, agricultural liming, is a long-established practice that counters soil acidification and boosts crop yields. Conventional greenhouse- gas accounting treats it as a net source of agricultural CO₂ emissions.

Using century-scale records of liming rates and anthropogenic acidity inputs across the Mississippi River Basin (MRB), the authors show that liming has instead acted as a net carbon sink over the past century. River alkalinity flux records indicate that roughly 90% of the ideal CO₂- removal potential of the lime applied since 1900 (≈ 0.44 Gt CO₂) has been realized at the catchment scale. A multi- decadal time lag occurs because of soil cation- exchange processes and solute transport. Reactive- transport modelling corroborates this: an initial emissions pulse (from neutralizing existing soil acidity pools) is followed by net CO₂ removal.

Current accounting frameworks use an incomplete counterfactual, they attribute emissions to the lime itself rather than to the anthropogenic strong acids (from fertilizers and fossil- fuel pollution) that drive CO₂ release. When evaluated against the proper counterfactual (acidity inputs without liming), liming is a net sink on decade- to- century timescales. The results imply that optimized soil- pH management can simultaneously cut agricultural greenhouse- gas emissions, raise yields, and improve soil health.

Key scientific points from the paper

Chemical basis of the conventional view
At low soil pH, carbonate dissolution releases CO₂:

$\mathrm{CaCO_3 + 2H^+ \to Ca^{2+} + CO_2 + H_2O}$

IPCC default methods essentially treat the carbon in applied lime as emitted; U.S. inventories use a lower emission factor (~50%).

Revised framework
The dominant driver of CO₂ release is the input of strong acids (nitric and sulfuric) from nitrogen fertilizers, manure, soil- organic- nitrogen mineralization, biological nitrogen fixation, and atmospheric deposition of SO₂/NOₓ oxidation products. These acids titrate existing alkalinity (bicarbonate) and force CO₂ out of the system regardless of whether lime is added. Adding lime supplies alkalinity that can form bicarbonate, which is exported downstream and ultimately sequesters atmospheric carbon.

Mississippi River Basin as the study system
The MRB covers ~41% of the contiguous U.S. land area and ~65% of its cropland, receives most U.S. agricultural lime, and has well-documented river chemistry. The authors compiled spatially explicit, century-long time series of acidity inputs (fertilizer/manure oxidation, atmospheric deposition, etc.) and lime additions. Cumulative acidity has exceeded lime- derived alkalinity by ~20 Tmol by 2015, but the excess is concentrated outside intensively limed Corn- Belt croplands.

Evidence for net sink

• Empirical river alkalinity fluxes.
• Gridded reactive- transport modelling (SCEPTER) comparing “acidity- only” vs. “acidity and lime” scenarios.
  Both approaches show that, after an early emissions pulse, liming produces a cumulative carbon sink on the order of hundreds of millions of tonnes of CO₂.

Implications
Emissions inventories and climate policy should attribute CO₂ release to acidity inputs rather than to liming. Better -aligned pH management (including possible pre- treatment with silicate rocks) can deliver agronomic benefits while contributing to carbon- dioxide removal.

The paper is open- access; a PDF download link is available on the Nature page. Authors include researchers affiliated with Yale (among others).

Journal information: Nature (2026) 

DOI: 10.1038/s41586-026-11040-2. www.nature.com/articles/s41586-026-11040-2

Provided: Yale University

Authors: Tim Jesper Suhrhoff,
Christopher T. Reinhard,
Yoshiki Kanzaki,
Samuel Shou-En Tsao,
Beck Woollen,
Tom Reershemius,
Samuel Shaheen,
James Saiers,
Shuang Zhang,
Peter A. Raymond &
Noah J. Planavsky

Abstract

Application of carbonate minerals to arable lands, known as agricultural liming, is a long-standing practice for counteracting soil acidification^1,2,3. Although liming boosts crop yields⁴, it is also considered a source of agricultural carbon dioxide (CO₂) emissions⁵. Here we show, using century-scale records of agricultural liming and anthropogenic acidity inputs for the Mississippi River Basin, that agricultural liming has acted as a net carbon sink over the past century. Records of river alkalinity fluxes suggest that approximately 90% of the ideal CO₂ removal potential of agricultural lime added since 1900 (approximately 0.44 GtCO₂) has been realized at the catchment scale, with a decadal-scale time lag owing to soil cation exchange and solute transport. These results are consistent with reactive transport modelling of soil cation throughput, which indicates that net CO₂ removal emerges after an initial emissions pulse associated with neutralization of soil acidity pools. Current accounting frameworks implicitly apply an incomplete counterfactual, attributing CO₂ emissions to lime addition rather than to the anthropogenic acidity inputs that drive CO₂ release. Evaluated against the counterfactual of anthropogenic acidity inputs, agricultural liming represents a net carbon sink in the Mississippi River Basin on decade-to-century timescales. These results suggest that optimized soil pH management can reduce agricultural greenhouse gas emissions while simultaneously improving crop yields and soil health.