{"entry_id": "1aab8801-66a5-42a3-9e8d-2706df6f1d0e", "infos": [{"txt": "sink caused by enhanced chemical weathering in the Rongbuk glacier runoff at the initial ablation, Mt.", "language": "english", "position": {"atoms": [{"position_id": 0, "txt": "sink caused by enhanced chemical weathering in the Rongbuk glacier runoff at the initial ablation, Mt.", "x": "//title"}]}, "tags": [], "label": "O", "web_segment_id": 0, "global_sentence_id": 0, "edu_l1_label": "EDU_O"}, {"txt": " Qomolangma (Everest)", "language": "english", "position": {"atoms": [{"position_id": 0, "txt": " Qomolangma (Everest)", "x": "//title"}]}, "tags": [], "label": "O", "web_segment_id": 0, "global_sentence_id": 1, "edu_l1_label": "EDU_O"}, {"txt": "<img https://sdfestaticassets-us-east-1.sciencedirectassets.com/prod/fa1c8b2301a14e2a58982c67ebe341e7af7fd8fc/image/elsevier-non-solus.svg", "language": "english", "position": {"atoms": [{"position_id": 123, "txt": "<img 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{"position_id": 815, "txt": " sink caused by enhanced chemical weathering in the Rongbuk glacier runoff at the initial ablation, Mt.", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/h1/span/sub"}]}, "tags": ["h1"], "label": "article_title", "web_segment_id": 5, "global_sentence_id": 6, "edu_l1_label": "BOT"}, {"txt": " Qomolangma (Everest)", "language": "english", "position": {"atoms": [{"position_id": 816, "txt": " Qomolangma (Everest)", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/h1/span/sub"}]}, "tags": ["h1"], "label": "article_title", "web_segment_id": 5, "global_sentence_id": 7, "edu_l1_label": "EDU_O"}, {"txt": "Author links open overlay panel, , , , , , ", "language": "english", "position": {"atoms": [{"position_id": 818, "txt": "Author links open overlay panel", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[3]/div[1]/div[2]/div/span"}, {"position_id": 820, "txt": ", , , , , , ", "x": 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Rongbuk Glacier meltwater runoff (RBM) acts as a significant CO", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sub[1]"}, {"position_id": 831, "txt": "2", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sub[2]"}, {"position_id": 833, "txt": " sink (−13.73 ± 9.56 mmol/m", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sub[2]"}, {"position_id": 835, "txt": "2", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sup[1]"}, {"position_id": 837, "txt": "/d) on the north slope of the Mountain Qomolangma (Everest), using floating chamber from 66 field observations at five sites conducted in May 2023, during the early ablation stage, primarily driven by chemical weathering processes.", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sup[1]"}]}, "tags": [], "label": "abstract", "web_segment_id": 8, "global_sentence_id": 11, "edu_l1_label": "IOS"}, {"txt": " Both the CO2 efflux rate (FCO2, mmol/m2/d) and the partial pressure of CO2 (pCO2, μatm) exhibited significant spatial and temporal variation.", "language": "english", "position": {"atoms": [{"position_id": 838, "txt": " Both the CO", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sup[1]"}, {"position_id": 840, "txt": "2", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sub[3]"}, {"position_id": 842, "txt": " efflux rate (FCO", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sub[3]"}, {"position_id": 844, "txt": "2", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sub[4]"}, {"position_id": 846, "txt": ", mmol/m", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sub[4]"}, {"position_id": 848, "txt": "2", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sup[2]"}, {"position_id": 850, "txt": "/d) and the partial pressure of CO", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sup[2]"}, {"position_id": 852, "txt": "2", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sub[5]"}, {"position_id": 854, "txt": " (", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sub[5]"}, {"position_id": 856, "txt": "p", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/em"}, {"position_id": 858, "txt": "CO", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/em"}, {"position_id": 860, "txt": "2", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sub[6]"}, {"position_id": 862, "txt": ", μatm) exhibited significant spatial and temporal variation.", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sub[6]"}]}, "tags": ["em"], "label": "abstract", "web_segment_id": 8, "global_sentence_id": 12, "edu_l1_label": "IOS"}, {"txt": " Under the influence of glacial microbial metabolisms and hydrological processes, FCO2 (−6.62 ± 7.01 mmol/m2/d) was significantly higher at night than during the day (−14.85 ± 9.22 mmol/m2/d).", "language": "english", "position": {"atoms": [{"position_id": 863, "txt": " Under the influence of glacial microbial metabolisms and hydrological processes, FCO", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sub[6]"}, {"position_id": 865, "txt": "2", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sub[7]"}, {"position_id": 867, "txt": " (−6.62 ± 7.01 mmol/m", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sub[7]"}, {"position_id": 869, "txt": "2", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sup[3]"}, {"position_id": 871, "txt": "/d) was significantly higher at night than during the day (−14.85 ± 9.22 mmol/m", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sup[3]"}, {"position_id": 873, "txt": "2", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sup[4]"}, {"position_id": 875, "txt": "/d).", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[5]/div[2]/div[1]/div/div/sup[4]"}]}, "tags": [], "label": "abstract", "web_segment_id": 8, "global_sentence_id": 13, "edu_l1_label": "IOS"}, {"txt": " As the meltwater flows downstream, the CO2 sink capacity gradually diminishes due to reduced glacial influence and increased external carbon sources.", "language": 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{"txt": " The CO2 emission from rivers and streams into the atmosphere is estimated between 0.56 and 3.56 petagrams (Pg) of C per year (Cole et al., 2007, Raymond et al., 2013, Sawakuchi et al., 2017).", "language": "english", "position": {"atoms": [{"position_id": 915, "txt": " The CO", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[6]/div[2]/section/div[1]/sub[1]"}, {"position_id": 917, "txt": "2", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[6]/div[2]/section/div[1]/sub[2]"}, {"position_id": 919, "txt": " emission from rivers and streams into the atmosphere is estimated between 0.56 and 3.56 petagrams (Pg) of C per year (Cole et al., 2007, Raymond et al., 2013, Sawakuchi et al., 2017).", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[6]/div[2]/section/div[1]/sub[2]"}]}, "tags": [], "label": "content", "web_segment_id": 12, "global_sentence_id": 23, "edu_l1_label": "IOS"}, {"txt": "Although this range is notable, it exceeds the amount of C transported from land to the ocean by rivers (0.70–0.95 Pg C yr−1) and is in equal proportion to the amount of organic carbon (OC) burial (0.6–3.6 Pg C yr−1) (Cole et al., 2007, Aufdenkampe et al., 2011, Raymond et al., 2013, Drake et al., 2018, Pilla et al., 2022).", "language": "english", "position": {"atoms": [{"position_id": 921, "txt": "Although this range is notable, it exceeds the amount of C transported from land to the ocean by rivers (0.70–0.95 Pg C yr", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[6]/div[2]/section/div[2]"}, {"position_id": 923, "txt": "−1", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[6]/div[2]/section/div[2]/sup[1]"}, {"position_id": 925, "txt": ") and is in equal proportion to the amount of organic carbon (OC) burial (0.6–3.6 Pg C yr", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[6]/div[2]/section/div[2]/sup[1]"}, {"position_id": 927, "txt": "−1", "x": 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erosion rate and fine-textured sediment cause glacier erosion to become a veritable mineral surface area production factory, which accelerates the process of chemical weathering (Anderson, 2007).", "language": "english", "position": {"atoms": [{"position_id": 938, "txt": " A high erosion rate and fine-textured sediment cause glacier erosion to become a veritable mineral surface area production factory, which accelerates the process of chemical weathering (Anderson, 2007).", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[6]/div[2]/section/div[2]/sub"}]}, "tags": [], "label": "content", "web_segment_id": 13, "global_sentence_id": 29, "edu_l1_label": "IOS"}, {"txt": "Glacier meltwater harbors multiple potential C sources, such as the dissolution of atmospheric gases, C trapped in ice bubbles, mechanical grinding and organic matter (OM) remineralization (Pain et al., 2021).", "language": "english", "position": {"atoms": [{"position_id": 940, "txt": "Glacier meltwater 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authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.", "language": "english", "position": {"atoms": [{"position_id": 1202, "txt": "The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[7]/div[2]/section[6]/section/div"}]}, "tags": [], "label": "content", "web_segment_id": 32, "global_sentence_id": 107, "edu_l1_label": "EDU_O"}, {"txt": "Acknowledgments", "language": "english", "position": {"atoms": [{"position_id": 1204, "txt": "Acknowledgments", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[7]/div[2]/section[7]/section/h2"}]}, "tags": ["h2"], "label": "title1", "web_segment_id": 33, "global_sentence_id": 108, "edu_l1_label": "IOS"}, {"txt": "The field work was greatly supported by the Qomolangma Station and South-East Tibetan Plateau Station, Chinese Academy of Sciences.", "language": "english", "position": {"atoms": [{"position_id": 1206, "txt": "The field work was greatly supported by the Qomolangma Station and South-East Tibetan Plateau Station, ", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[7]/div[2]/section[7]/section/div"}, {"position_id": 1208, "txt": "Chinese Academy of Sciences", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[7]/div[2]/section[7]/section/div/span[1]"}, {"position_id": 1210, "txt": ".", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[7]/div[2]/section[7]/section/div/span[1]"}]}, "tags": [], "label": "content", "web_segment_id": 34, "global_sentence_id": 109, "edu_l1_label": "EDU_O"}, {"txt": " This work is sponsored by the National Key R&D Program of China [Grant No. 2024YFF0808601], the TAR Scientific Program [Grant No. XZ202401JD0002], and the National Natural Science Foundation of China [Grant No. U23A2011 and 42203060].", "language": "english", "position": {"atoms": [{"position_id": 1211, "txt": " This work is sponsored by the ", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[7]/div[2]/section[7]/section/div/span[1]"}, {"position_id": 1213, "txt": "National Key R&D Program of China", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[7]/div[2]/section[7]/section/div/span[2]"}, {"position_id": 1215, "txt": " [Grant No. ", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[7]/div[2]/section[7]/section/div/span[2]"}, {"position_id": 1217, "txt": "2024YFF0808601", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[7]/div[2]/section[7]/section/div/span[3]"}, {"position_id": 1219, "txt": "], the TAR Scientific Program [Grant No. XZ202401JD0002], and the ", "x": "/html/body/div[1]/div/div/div/div/div[2]/div[2]/article/div[7]/div[2]/section[7]/section/div/span[3]"}, {"position_id": 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# Atmospheric CO2 sink caused by enhanced chemical weathering in the Rongbuk glacier runoff at the initial ablation, Mt. Qomolangma (Everest)
## Abstract
## Graphical abstract
## Introduction
## Section snippets
### Study area
### Physical and biochemical characteristics across RBM
### A comparison of the CO2 sink with other glacier-fed freshwater
## Conclusion
