ミシシッピ川流域で硝酸汚染が20年で減少(Study shows 20-year decline in nitrate pollution)

2026-03-02 イリノイ大学アーバナ・シャンペーン校

イリノイ大学アーバナ・シャンペーン校を中心とする研究チームは、ミシシッピ・アチャファラヤ川流域(MARB)の217流域を対象に2000~2020年の窒素収支を分析し、河川中の硝酸塩汚染が過去20年間で減少していることを明らかにした。研究では窒素収支指標NANI(Net Anthropogenic Nitrogen Inputs)を用い、肥料使用、作物による窒素固定、大気沈着、食料・飼料の輸出入などを統合して評価した。その結果、硝酸塩濃度の低下は肥料削減ではなく、大気中の窒素酸化物排出の減少や、改良されたトウモロコシ品種による窒素利用効率の向上が主因であることが示された。窒素流入の減少はメキシコ湾の低酸素「デッドゾーン」縮小にも寄与すると期待される。研究は水質改善に向けた農業管理や大気汚染対策の重要性を示している。

ミシシッピ川流域で硝酸汚染が20年で減少(Study shows 20-year decline in nitrate pollution)
A map of the watershed areas sampled in the study.

<関連情報>

ミシシッピ川流域における陸上窒素収支と河川硝酸態窒素収量の2000年から2020年までの変動 Changes in Terrestrial N Budgets and Riverine Nitrate-N Yields from Mississippi River Basin Watersheds 2000 to 2020

Gregory F. McIsaac, Dennis P. Swaney, Alejandra Botero-Acosta, and Robert W. Howarth
Ocean-Land-Atmosphere Research  Published:16 Feb 2026
DOI:https://doi.org/10.34133/olar.0131

Abstract

The Mississippi–Atchafalaya River Basin (MARB) drains approximately 40% of the continental United States and discharges into the Northern Gulf of Mexico, where a large area of benthic hypoxia forms in late summer, largely in response to N loads from the MARB. Trend analysis revealed changes in nitrate-N (NO3-N) loads in MARB subbasins from 2000 to 2020, although causes are uncertain. Net anthropogenic N inputs (NANI), the net of estimated N inputs and outputs from human activities, has been correlated with riverine N loads in many regions worldwide. Here, we incorporate reported changes in crop N content and biological N fixation into NANI estimates and investigate correlations with flow-normalized (FN) riverine N yields from 217 watersheds in the MARB. Reductions in crop N content in corn and soybean influenced values of NANI but had little influence on NANI correlations with riverine FN NO3-N, which generally ranged from 0.5 to 0.7. In the late 1990s and early 2000s, NANI values and FN NO3-N yields were generally high for watersheds with a high percentage of cultivated cropland and tile drainage; by 2020, both NANI and FN NO3-N yields from these watersheds had declined. The magnitude of the decline in FN NO3-N yields from watersheds with greater than 20% tile drainage averaged 552 kg N km−2 year−1. In these watersheds, the largest reductions in NANI were due to greater N harvest in maize and wheat with little change in N fertilizer, and a reduction in atmospheric N deposition.

1902環境測定
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