High Rainfall Inhibited Soil Respiration in an Asian Monsoon Forest in Taiwan

• Published in: Forests 2021-02, Vol.12 (2), p.239
• Main Authors: Yu, Jui-Chu, Chiang, Po-Neng, Lai, Yen-Jen, Tsai, Ming-Jer, Wang, Ya-Nan
• Format: Article
• Language: English
• Subjects: Annual rainfall; Asian monsoon; automated chamber; Automation; Biomass; Biosphere; Carbon; Carbon cycle; Carbon dioxide; Channel pores; Climate change; Ecosystems; Forest ecosystems; Forest soils; Forests; heterotrophic respiration; Monsoons; Photosynthesis; Plantations; Rain; Rain water; Rainfall; Respiration; Seasonal variations; Soil microorganisms; Soil moisture; Soil temperature; Temperature dependence; temperature sensitivity; Terrestrial ecosystems; Terrestrial environments
• ISSN: 1999-4907; 1999-4907
• DOI: 10.3390/f12020239

Soil respiration represents the second largest carbon flux, next to photosynthesis of the terrestrial biosphere, and thus plays a dual role in regional and global carbon cycles. However, soil respiration in Asian monsoon forests with high rainfall has rarely been studied. In this study, we continuously measured soil respiration using a 12-channel automated chamber system in a 61-year-old Japanese cedar forest in central Taiwan with annual rainfall greater than 2500 mm. A 4-year (2011–2014) continuous half-hourly dataset was used to quantify the influences of soil temperature and moisture, especially rainfall events, on both total soil respiration (Rs) and heterotrophic respiration (Rh). The annual mean Rs was approximately 10.8 t C ha−1 (ranging from 10.7 to 10.9) t C ha−1, with Rh contributing approximately 74.6% (ranging from 71.7% to 80.2%). Large seasonal variations in both Rs and Rh were primarily controlled by soil temperature. Over 45.8% of total annual rainfall amounts were provided by strong rainfall events (over 50 mm), and over 40% of rainfall events occurred during summers between 2012 and 2014. These strong rainfall events caused rainwater to enter soil pores and cover the soil surface, which resulted in limited soil microorganism activity and, consequently, restricted CO2 production. The mean Q10 values were 2.38 (ranging from 1.77 to 2.65) and 2.02 (ranging from 1.71 to 2.34) for Rs and Rh, respectively. The Q10 values in this study, which were lower than in global forest ecosystems, may imply that the interannual Rs values observed in this study that were caused by high rainfall were less temperature-dependent than the Rs levels in global forest ecosystems. Both Rs and Rh were negatively correlated with soil moisture, which indicated that the soil moisture levels in the studied forest were usually under saturated conditions. These results also provide the lack of data for respiration in the Asian monsoon region under high-rainfall conditions.