一般的な土壌処理が作物収量を改善し炭素を除去できることを確認(Researchers Confirm Common Soil Treatment Can Improve Farm Crop Yields and Remove Carbon)

2026-09-23 ジョージア工科大学

ジョージア工科大学などの研究者11人は、米国ミシシッピ川流域11州で約1世紀にわたって行われてきた農地への石灰施用(ライミング)が、長期的には大気中のCO₂を正味で除去する「炭素吸収源」になっていることを明らかにした。石灰石などの炭酸塩鉱物は土壌酸性度を中和し、その反応生成物が河川を通じて流域を移動するため、炭素の影響は農地だけでなく流域全体で評価する必要がある。研究チームは、農業・施肥記録と河川のアルカリ度など100年以上のデータを解析し、石灰施用による炭素除去効果を検証した。さらに農地の物理・化学過程を再現するモデルを構築し、モデル予測の約90%に相当する炭素除去効果が河川水質記録から確認された。土壌pH管理による作物生産性向上と炭素除去を両立できる可能性を示す研究である。

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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

一般的な土壌処理が作物収量を改善し炭素を除去できることを確認(Researchers Confirm Common Soil Treatment Can Improve Farm Crop Yields and Remove Carbon)

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.

1202農芸化学
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