森の中の水循環を追う(Following the water cycle in the forest)

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2023-03-21 スイス連邦工科大学チューリッヒ校(ETHZurich)

スイスのETHチューリッヒ大学の研究者らは、森林での水の貯蔵や輸送過程を調査しており、最近、森林の水循環において、枯れ木や落ち葉層が予想以上に大きな影響を持っていることを示した。この落ち葉層や枯れ木が、年間降雨量の1/5まで保持・蒸発させており、この水は土壌中に浸透することなく、植物には利用可能な水が少ないことを示している。
森林における水の循環の知識は、森林の干ばつに対する影響を理解するために不可欠である。

<関連情報>

林床のリターと枯れ木が降水循環を大きくする可能性 Potential for significant precipitation cycling by forest-floor litter and deadwood

Marius G. Floriancic, Scott T. Allen, Raphael Meier, Lucas Truniger, James W. Kirchner, Peter Molnar
Ecohydrology  Published: 17 October 2022
DOI:https://doi.org/10.1002/eco.2493

森の中の水循環を追う(Following the water cycle in the forest)

Abstract

The forest-floor litter layer can retain substantial volumes of water, thus affecting evaporation and soil-moisture dynamics. However, litter layer wetting/drying dynamics are often overlooked when estimating forest water budgets. Here, we present field and laboratory experiments characterizing water cycling in the forest-floor litter layer and outline its implications for subcanopy microclimatic conditions and for estimates of transpiration and recharge. Storage capacities of spruce needle litter and beech broadleaf litter averaged 3.1 and 1.9 mm, respectively, with drainage/evaporation timescales exceeding 2 days. Litter-removal experiments showed that litter reduced soil water recharge, reduced soil evaporation rates, and insulated against ground heat fluxes that impacted snowmelt. Deadwood stored ~0.7 mm of water, increasing with more advanced states of decomposition, and retained water for >7 days. Observed daily cycles in deadwood weight revealed decreasing water storage during daytime as evaporation progressed and increasing storage at night from condensation or absorption. Water evaporating from the forest-floor litter layer modulates the subcanopy microclimate by increasing humidity, decreasing temperature, and reducing VPD. Despite the relatively small litter storage capacity (<3.1 mm in comparison to ~102 mm for typical forest soil rooting zones), the litter layer alone retained and cycled 18% of annual precipitation, or 1/3 of annual evapotranspiration. These results suggest that overlooking litter interception may lead to substantial overestimates of recharge and transpiration in many forest ecosystems.

1304森林環境
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