Abstract

A large portion of the global carbon pool is stored in peatlands, which are sensitive to a changing environment conditions. The hydrological loss of dissolved organic carbon (DOC) is believed to play a key role in determining the carbon balance in peatlands. Zoige peatland, the largest peat store in China, is experiencing climatic warming and drying as well as experiencing severe artificial drainage. Using a fully crossed factorial design, we experimentally manipulated temperature and controlled the water tables in large mesocosms containing intact peat monoliths. Specifically, we determined the impact of warming and water table position on the hydrological loss of DOC, the exported amounts, concentrations and qualities of DOC, and the discharge volume in Zoige peatland. Our results revealed that of the water table position had a greater impact on DOC export than the warming treatment, which showed no interactive effects with the water table treatment. Both DOC concentration and discharge volume were significantly increased when water table drawdown, while only the DOC concentration was significantly promoted by warming treatment. Annual DOC export was increased by 69% and 102% when the water table, controlled at 0 cm, was experimentally lowered by −10 cm and −20 cm. Increases in colored and aromatic constituents of DOC (measured by Abs254 nm, SUVA254 nm, Abs400 nm, and SUVA400 nm) were observed under the lower water tables and at the higher peat temperature. Our results provide an indication of the potential impacts of climatic change and anthropogenic drainage on the carbon cycle and/or water storage in a peatland and simultaneously imply the likelihood of potential damage to downstream ecosystems. Furthermore, our results highlight the need for local protection and sustainable development, as well as suggest that more research is required to better understand the impacts of climatic change and artificial disturbances on peatland degradation.

Highlights

  • Peat-accumulating wetlands provide waterlogged conditions where carbon accumulation is encouraged [1], and have huge carbon storage potential

  • All values were within the range (5–40 C m22 year21) found in the natural peatland [3], the results indicated that dissolved organic carbon (DOC) export would increase by 69% and 102% annually if the water table at 0 cm was lowered by 10 cm and 20 cm, respectively

  • We investigated the response of the hydrological export of DOC in Zoige peatland to changes in the water table level and temperature

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Summary

Introduction

Peat-accumulating wetlands provide waterlogged conditions where carbon accumulation is encouraged [1], and have huge carbon storage potential. There is increasing concern that carbon storage in peatlands is unstable and may be susceptible to water table drawdown and higher temperatures over the two centuries due to projected climatic change [2,3,4,5,6]. Zoige peatland covers an estimated area of 0.5 million hectares and accounts for 47.53% of the total organic carbon reserves in Chinese peatland. It accounts for the highest organic carbon accumulation of any peatland in China [14]

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