日本地球惑星科学連合2014年大会

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セッション記号 A (大気海洋・環境科学) » A-HW 水文・陸水・地下水学・水環境

[A-HW29_2PM1] JapanFlux:水・物質循環における陸域生態系の役割

2014年5月2日(金) 14:15 〜 16:00 314 (3F)

コンビーナ:*平野 高司(北海道大学大学院農学研究院)、山野井 克己((独)森林総合研究所)、市井 和仁(福島大学共生システム理工学類)、三枝 信子(国立環境研究所)、座長:市井 和仁(海洋研究開発機構)

15:45 〜 16:00

[AHW29-07] 富士北麓カラマツ林における林床部CO2フラックスの連続測定

*寺本 宗正1梁 乃申1曾 継業1井手 玲子1三枝 信子1高橋 善幸1 (1.国立環境研究所地球環境研究センター)

キーワード:土壌呼吸, チャンバー, 林床植生, 光合成

Carbon fluxes of forest floor are thought to be important part of forest carbon dynamics. Multi-channel automated chamber system was installed to a larch forest site on the base of Mount Fuji in 2006 for continuous measurement of forest floor CO2 fluxes. We prepared soil chambers for measuring soil respiration (Rs) and heterotrophic respiration (Rh). Root trenching was applied to separate Rs and Rh. Net ecosystem exchange (NEE) on the forest floor was measured with plant chambers. In 2013, the average efflux of CO2 was 2.24, 1.81 and 2.11 μmol CO2 m-2 s-1 in Rs, Rh and NEE, respectively. Root respiration was estimated to occupy 80.7% of Rs. Plants of forest floor was suggested to absorb about 5.9% of CO2 in Rs, and it meant that the amount of carbon fixed by those plants was relatively low. There was little rain in summer time (July-August), and forest floor CO2 fluxes were decreased due to decreased soil moisture. Q10 was 2.49 and 2.87 in Rs and Rh, respectively. Soil respiration was estimated to be 8.48 tC ha-1 yr-1, and the forest floor was seen as 7.98 tC ha-1 yr-1 carbon source.