ミシシッピ川流域の農地への石灰施用、主要な炭素吸収源となることが研究で判明(Adding limestone to Mississippi River Basin farmlands acts as a major carbon sink, study finds)

2026-09-23 イェール大学

イェール大学主導の研究は、米国ミシシッピ川流域の農地で行われてきた石灰施用(ライミング)が、長期的にはCO₂の純吸収源として機能することを示した。120年以上の農業・環境記録を解析した結果、石灰を土壌に施すことで酸性土壌を改良すると同時に、土壌中のCO₂と反応して安定した重炭酸イオンを形成し、地下水や河川を通じて海洋へ炭素を運ぶ過程が明らかになった。1900年以降、同流域では推定3~4億トンのCO₂が除去されたという。従来の温室効果ガス排出量算定では、施用した石灰に含まれる炭素からのCO₂排出が重視されていたが、本研究は石灰を施さなかった場合に生じる土壌酸性化なども考慮すると、長期的には正味の炭素除去になると示した。ただし効果は土壌酸性度、緩衝能、水文条件など地域によって異なる。

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農業における石灰施用は、ミシシッピ川流域における炭素吸収源である Agricultural liming is a carbon sink in the Mississippi River Basin

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
Nature  Published:23 September 2026
DOI:https://doi.org/10.1038/s41586-026-11040-2

ミシシッピ川流域の農地への石灰施用、主要な炭素吸収源となることが研究で判明(Adding limestone to Mississippi River Basin farmlands acts as a major carbon sink, study finds)

Abstract

Application of carbonate minerals to arable lands, known as agricultural liming, is a long-standing practice for counteracting soil acidification1,2,3. 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.

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