School of Environmental Science and Engineering, Shaanxi University of Science and Technology, Xi'an, 710021, China; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, 710061, China; Tanggula Cryosphere and Environment Observation Station, Lanzhou, 730000, China; State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China.
School of Environmental Science and Engineering, Shaanxi University of Science and Technology, Xi'an, 710021, China.
Environ Res. 2023 Jan 1;216(Pt 3):114680. doi: 10.1016/j.envres.2022.114680. Epub 2022 Nov 1.
Carbonaceous matter (CM) (such as water-insoluble organic carbon (WIOC), black carbon (BC), and water-soluble organic carbon (WSOC)) has a significant impact on the carbon cycle and radiative forcing (RF) of glacier. Precipitation samples and glacier's snow/ice samples (snowpit, surface snow, and granular ice) (Xiao dongkemadi Glacier) were collected at the Dongkemadi River Basin (DRB) in the central Tibetan Plateau (TP) between May and October 2016 to investigate the characteristics and roles of CM in the TP River Basin. WIOC, BC, and WSOC concentrations in precipitation were relatively higher than that in snowpit, but lower than that in surface snow/ice, with the wet deposition fluxes of 0.10 ± 0.002, 0.04 ± 0.001, and 0.12 ± 0.002 g C m yr at DRB, respectively. The positive matrix factorization model identified four major sources (biomass burning source, secondary precursors, secondary aerosol, and dust source) of CM in precipitation at DRB. Two source areas (South Asia and the interior of TP) contributing to the pollution at DRB were identified using a potential source contribution function model, a concentration-weighted trajectory method, and the back-trajectory model. Moreover, the light-absorption by WSOC in the ultraviolet region was 23.0%, 12.1%, and 3.4% relative to the estimated total light-absorption in precipitation, snowpit, and surface snow/ice, respectively. Optical indices analysis revealed that WSOC in snowpit samples presented higher molecular weight, while presented higher aromatic and higher molecule sizes in surface snow/ice and precipitation samples, respectively. RF by WSOC relative to that of BC was estimated to be 17.6 ± 17.6% for precipitation, 10.9 ± 5.8% for snowpit, and 10.7 ± 11.6% for surface snow/ice, respectively, during the melt season in the central TP River Basin. These results help us understand how CM affects glaciers, and they can be utilized to create policies and recommendations that efficiently reduce emissions.
碳质物质(CM)(如不溶性有机碳(WIOC)、黑碳(BC)和水溶性有机碳(WSOC))对冰川的碳循环和辐射强迫(RF)有重大影响。2016 年 5 月至 10 月,在青藏高原中部的东科马迪流域(DRB)采集了降水和冰川雪/冰样本(雪坑、表面雪和粒状冰),以研究 CM 在 TP 流域的特征和作用。降水、雪坑、表面雪/冰中的 WIOC、BC 和 WSOC 浓度相对较高,但低于表面雪/冰中的浓度,DRB 的湿沉降通量分别为 0.10±0.002、0.04±0.001 和 0.12±0.002 g C m yr。正矩阵因子模型识别出 DRB 降水 CM 的四个主要来源(生物质燃烧源、二次前体、二次气溶胶和粉尘源)。利用潜在源贡献函数模型、浓度加权轨迹法和后轨迹模型,确定了对 DRB 地区污染有贡献的两个源区(南亚和青藏高原内部)。此外,WSOC 在紫外区的吸光度分别为降水、雪坑和表面雪/冰中总吸光度的 23.0%、12.1%和 3.4%。光学指数分析表明,雪坑样品中的 WSOC 具有更高的分子量,而表面雪/冰和降水样品中的 WSOC 分别具有更高的芳香度和更大的分子量。估计青藏高原中部流域融雪季节 WSOC 相对于 BC 的 RF 分别为降水的 17.6±17.6%、雪坑的 10.9±5.8%和表面雪/冰的 10.7±11.6%。这些结果有助于我们了解 CM 如何影响冰川,并可用于制定有效减少排放的政策和建议。