Continuous measurement of soil carbon efflux with Forced Diffusion (FD)chambers in a tundra ecosystem of Alaska
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- Continuous measurement of soil carbon efflux with Forced Diffusion (FD)chambers in a tundra ecosystem of Alaska
- Other Titles
- 미국 알래스카 툰드라 생태계에서의 FD를 이용한 토양 탄소 플럭스 측정
- Kim, Yongwon
Lee, Bang Yong
- Environmental Sciences & Ecology
- FD chamber system; Soil CO2 efflux; Temperature; Thaw depth
- Issue Date
- Kim, Yongwon, et al. 2016. "Continuous measurement of soil carbon efflux with Forced Diffusion (FD)chambers in a tundra ecosystem of Alaska". SCIENCE OF THE TOTAL ENVIRONMENT, 566-567(1): 175-184.
- Soil is a significant source of CO2 emission to the atmosphere, and this process is accelerating at high latitudes due to rapidly changing climates. To investigate the sensitivity of soil CO2 emissions to high temporal frequency variations in climate, we performed continuous monitoring of soil CO2 efflux using Forced Diffusion (FD) chambers at half-hour intervals, across three representative Alaskan soil cover types with underlying permafrost. These siteswere established during the growing season of 2015, on the Seward Peninsula ofwestern Alaska. Our chamber system is conceptually similar to a dynamic chamber, though FD is more durable and water-resistant and consumes less power, lending itself to remote deployments. We first conducted methodological tests, testing different frequencies of measurement, and did not observe a significant difference between collecting data at 30-min and 10-min measurement intervals (averaged half-hourly) (p b 0.001). Temperature and thaw depth, meanwhile, are important parameters in influencing soil carbon emission. At the study sites, we observed cumulative soil CO2 emissions of 62.0, 126.3, and 133.5 gCm？2 for the growing period, in sphagnum, lichen, and tussock, respectively, corresponding to 83.8, 63.7, and 79.6% of annual carbon emissions. Growing season soil carbon emissions extrapolated over the region equated to 0.17 ± 0.06 MgC over the measurement period. Thiswas 47% higher than previous estimates fromcoarse-resolutionmanual chamber sampling, presumably because it better captured high efflux events. This finding demonstrates how differences in measurement method and frequency can impact interpretations of seasonal and annual soil carbon budgets. We conclude that annual CO2 efflux-measurements using FD chamber networks would be an effective means for quantifying growing and non-growing season soil carbon budgets, with optimal pairing with time-lapse imagery for tracking local and regional changes in environment and climate in a warming Arctic.
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