JpGU-AGU Joint Meeting 2020

Presentation information

[J] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-CG Complex & General

[A-CG54] Biogeochemical cycles in Land Ecosystem

convener:Tomomichi Kato(Research Faculty of Agriculture, Hokkaido University), Kazuhito Ichii(Chiba University), Takeshi Ise(FSERC, Kyoto University), Munemasa Teramoto(Arid Land Research Center, Tottori University)

[ACG54-02] Change in soil respiration rate of Sugi plantation for seven years

*Yukiko Abe1, Naishen Liang2, Jun Koarashi3, Mariko Atarashi-Andoh3, Munemasa Teramoto2, Shoji Hashimoto1,4, Takeshi Tange1 (1.Graduate School of Agricultural and Life Sciencies, The University of Tokyo, 2.Center for Global Environmental Research, National Institute for Environmental Studies, 3.Japan Atomic Energy Agency, 4.Forestry and Forest Products Research Institute)

Keywords:soil respiration rate, soil temperature, soil carbon content, density fractionation, fine root biomass

It is known that soil respiration rate has large spatial variation even within the same forest. We measured soil respiration rates at 21 points in a Cryptomeria japonica plantation of Tokyo University of Agriculture Okutama Forest, from January 2013 to August 2019, and examined temporal changes and factors of spatial variation. From the relationship between soil temperature at 5 cm depth and soil respiration rate, the soil respiration rate at each measured point at a soil temperature of 20 °C (R20) was estimated and compared. The observation showed that the measured points with higher R20 in 2013 tended to have higher R20 throughout the observation period, and the measured points with lower R20 in 2013 tended to show lower R20 throughout the seven years. There wasn’t significant correlation between the amount of carbon of the surface soil (0-30 cm in depth) and the soil respiration rate. However, the amount of light fraction (<1.6 g cm-3) of soil or fine root biomass of the surface soil had a significant positive correlation with the soil respiration rate. Since the light fraction of soil contains organic matter that is easily decomposed by microbes, the variation of the easily decomposable organic matter content was considered to be the cause of the spatial variation in soil respiration rate.