Distributive Features of Dissolved Organic Carbon in Aquatic Systems in the Source Area of the Yellow River on the Northeastern Qinghai–Tibet Plateau, China

Frontiers in Earth Science

Sergey S. Marchenko¹  Raul D. Serban²  Huijun Jin³  Xiaoying Li³  Shuhui Gao⁴  Sihai Liang⁶  Qiang Ma⁷  Qingfeng Wang⁷  Yadong Huang⁷  Dongliang Luo⁷  Qingbai Wu⁷  Yuzhong Yang⁷  Yan Li⁷ 

[1] Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, United States;Institute for Alpine Environment, Eurac Research, Bolzano, Italy;Key Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, School of Forestry, Northeast Forestry University, Harbin, China;School of Civil Engineering, Lanzhou Jiaotong University, Lanzhou, China;School of Civil Engineering, Ministry of Education Observational and Research Station of Permafrost Geo-Environment in Northeast China, Institute of Cold-Regions Science and Engineering, Northeast Forestry University, Harbin, China;School of Water Resources and Environment, China University of Geosciences, Beijing, China;State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, China;

关键词: alpine permafrost;    source area of the Yellow River;    dissolved organic carbon;    DOC distribution;    aquatic systems;   

DOI  :  10.3389/feart.2022.892524

来源: DOAJ

【 摘 要 】

Dissolved organic carbon (DOC) is the main participant in carbon cycles through water pathways. Recent studies have highlighted the roles of aquatic systems in landscape and watershed carbon budgets. This study is based on 261 samples collected between 2016 and 2017, from individual water types (e.g., river/stream, lake/pond, icing/spring, snow/rain, groundwater/ice, and others) in the source area of the Yellow River (SAYR). These samples were analyzed for examining the distributive features of DOC in aquatic systems, especially in relation to environmental factors. It shows that: 1) DOC concentrations in permafrost-related waters (7.2–234.4 mg C·L−1) were often the highest among all aquatic DOC sources (lakes/ponds: 21.3 ± 34.1 mg C·L−1, rivers/streams: 4.3 ± 3.7 mg C·L−1, and groundwater: 1.8 ± 1.4 mg C·L−1); 2) the seasonality of riverine DOC showed declining features in 2016 and high in summer/autumn, followed by a spring freshet in 2017, and a close association with intra-annual precipitation modes; 3) the main controls of aquatic DOC are permafrost presence, precipitation, and NDVI, and they contribute to 38% of variances of environmental variables in affecting variations in aquatic DOC in the SAYR; and 4) a literature review on biodegradable DOC (BDOC) of varied aquatic DOC pools indicates the highest DOC concentrations (48–1,548 mg C·L−1) and BDOC (23–71%) of ground-ice meltwater. Thus, we suggest that in the SAYR, permafrost dynamics dominate aquatic DOC distribution, and permafrost thaw may alter aquatic DOC budgets, eventually becoming an additional source for atmospheric carbon emissions.

【 授权许可】

Unknown