山火事後のリン移動性を左右する要因を解明 (Mobility of Phosphorus Following Wildfire Depends on Vegetation and Burn Severity)

2026-08-18 パシフィック・ノースウェスト国立研究所(PNNL)

米国エネルギー省パシフィック・ノースウェスト国立研究所(PNNL)の研究チームは、山火事後のリン(P)の移動性が、植生の種類と焼失程度(burn severity)によって大きく左右されることを明らかにした。リンは生態系の生産性や水質に影響を与える重要な栄養塩であり、山火事後には土壌から河川や湖沼へ流出しやすくなる。本研究では、異なる植生タイプと焼失強度の条件下でリンの挙動を調査した結果、高強度の火災を受けた地域ほどリンの可溶化と流出リスクが高まることが確認された。また、植生の種類によって土壌中のリンの保持能力や火災後の放出量に差があり、リン移動の程度が大きく異なることが示された。これらの知見は、山火事後の栄養塩流出による水質悪化や富栄養化リスクの予測精度向上に貢献するとともに、流域管理や森林再生計画の策定に重要な科学的基盤を提供するものである。

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燃焼の深刻度と植生の種類がリンの濃度、分子組成、および移動を制御する Burn severity and vegetation type control phosphorus concentration, molecular composition, and mobilization

Morgan E. Barnes, J. Alan Roebuck Jr., Samantha Grieger, Paul J. Aronstein, Vanessa A. Garayburu-Caruso, Kathleen Munson, Robert P. Young, Kevin D. Bladon, John D. Bailey, Emily B. Graham, Lupita Renteria, Peggy A. O’Day, Timothy D. Scheibe, and Allison N. Myers-Pigg
Biogeosciences  Published:10 Sep 2025
DOI:https://doi.org/10.5194/bg-22-4491-2025

山火事後のリン移動性を左右する要因を解明 (Mobility of Phosphorus Following Wildfire Depends on Vegetation and Burn Severity)

Abstract

Shifting phosphorus (P) dynamics after wildfires can have cascading impacts from terrestrial to aquatic environments. However, it is unclear whether shifts in P composition or P concentration are responsible for changes in P dynamics post-fire. We used laboratory leaching experiments of Douglas fir forest and sagebrush shrubland chars to examine how the potential mobility of P compounds is influenced by different burn severities. Burning produced a 6.9- and 29-fold increase in particulate P mobilization but a 3.8- and 30.5-fold decrease in aqueous P released for Douglas fir forest and sagebrush shrubland, respectively. The mechanisms driving particulate- and dissolved-phase P compound mobilization were contrasting. Phosphorus compound mobilization in the particulate phase was controlled by solid char total P concentrations, while the aqueous phase was driven by solubility changes of molecular species. Nuclear magnetic resonance (NMR) and X-ray absorption near-edge structure (XANES) on the solid chars indicated that organic orthophosphate monoester and diester species were thermally mineralized to inorganic P moieties with burning in both vegetation types, which decreases P solubility. This coincided with the production of calcium- and magnesium-bound inorganic P compounds. With increasing burn severity there were systematic shifts in P concentration and composition – higher-severity chars mobilized P compounds in the particulate phase, although the magnitude of change was vegetation-specific. Our results indicate a post-fire transformation to both the composition of the solid charred material and how P compounds are mobilized, which may influence its environmental cycling and fate.

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