长白山天池火山含碳气体排放特征

doi:10.12196/j.issn.1000-3274.2024.03.013

地震 ›› 2024, Vol. 44 ›› Issue (3): 196-214.doi: 10.12196/j.issn.1000-3274.2024.03.013

长白山天池火山含碳气体排放特征

顾国辉^1,2, 盘晓东^1,2, 关升^1,2, 仲广培¹, 宋雨佳^1,2, 胡乐³, 李营³

1.吉林省地震局吉林长白山火山国家野外科学观测研究站, 吉林长春 130117;
2.中国地震局火山研究所, 吉林长春 130117;
3.中国地震局地震预测研究所, 北京 100036

收稿日期:2024-04-24 接受日期:2024-06-11 出版日期:2024-07-31 发布日期:2024-08-28
通讯作者: 盘晓东, 高级工程师。 E-mail: panxd1970@126.com
作者简介:顾国辉(1993-), 男, 安徽淮南人, 工程师, 主要从事流体地球化学研究。
基金资助:
地震科技星火计划项目(XH23013B、XH23012B); 吉林省科技发展计划项目(20230203132SF); 吉林省地震局青年科技发展课题(JZQ-202403); 中国地震局地震预测研究所基本科研业务费专项(CEAIEF20230205)

Characteristics of Carbonaceous Gas Emissions from Changbaishan Tianchi Volcano, Northeast China

GU Guo-hui^1,2, PAN Xiao-dong^1,2, GUAN Sheng^1,2, ZHONG Guang-pei¹, SONG Yu-jia^1,2, HU Le³, LI Ying³

1. Jilin Changbaishan Volcano National Observation and Research Station, Jilin Earthquake Agency, Changchun 130117, China;
2. Institute of Volcanology, China Earthquake Administration, Changchun 130117, China;
3. Institute of Earthquake Forecasting, China Earthquake Administration, Beijing 100036, China

Received:2024-04-24 Accepted:2024-06-11 Online:2024-07-31 Published:2024-08-28

摘要/Abstract

摘要： 查明火山气体释放的规模及空间分布特征, 对火山监测与喷发预测、评估地质源温室气体释放及气候环境变化等具有重要意义。本文采用密闭气室法观测土壤气浓度, 计算了长白山天池火山区CO₂和CH₄气体释放通量, 结合高光谱气体CO和CO₂分析了火山区不同区域气体释放特征及影响因素。结果表明: ①长白山天池火山区土壤CO₂通量范围为0.16～1051.39 g·m^-2·d^-1; CH₄通量值范围为-0.05～4.68 g·m^-2·d^-1。长白山天池火山区气体释放在空间上呈环带状分布特征, 火山口周缘气体释放较弱, 在聚龙温泉群、锦江温泉群和锥体海拔1800～2200 m范围内气体释放最为强烈。 ② 长白山天池火山含碳气体释放在地表和高光谱卫星观测的时间和空间上都有一定的相关性, 火山口上方气体释放最弱。 ③ 长白山天池火山含碳气体排放的空间差异可能受到火山口特殊条件、断裂构造、温泉地热储和岩浆作用的控制。

关键词: 长白山天池火山, 气体通量, 高光谱气体, 空间特征, 控制因素

Abstract: Identifying the scale and spatial distribution characteristics of volcanic gas releases is of great significance for volcano monitoring and eruption prediction, assessing greenhouse gas releases from geological sources, and understanding climate changes. This paper investigates the scale and spatial characterization of greenhouse gas release in the volcanic area of Changbaishan Tianchi using the accumulation chamber method and hyperspectral gas method. The results of the study showed that: ① CO₂ fluxes in the volcanic area of Changbaishan Tianchi were in the range of 0.16~1051.39 g·m^-2·d^-1; CH₄ flux values were -0.05~4.68 g·m^-2·d^-1. The gas release from Changbaishan Tianchi volcano was spatially characterized by a ring-band distribution, with weaker gas release at the periphery of the caldera, and the strongest gas release occurring in the Julong Hot Spring Group, Jinjiang Hot Spring Group, and the cone within the range of 1800~2200 m above sea level. ② The surface and hyperspectral satellite observations of carbonaceous gases release from Changbaishan Tianchi Volcano are correlated on both temporal and spatial scales. ③ Spatial differences in carbonaceous gas emissions from Changbaishan Tianchi volcano may be controlled by the special conditions of the caldera, fault tectonics, hot spring geothermal reservoirs, and magmatism.

Key words: Changbaishan Tianchi volcano, Gas fluxes, Hyperspectral gas, Spatial characteristics, Controlling factor

中图分类号:

P317.6

顾国辉, 盘晓东, 关升, 仲广培, 宋雨佳, 胡乐, 李营. 长白山天池火山含碳气体排放特征[J]. 地震, 2024, 44(3): 196-214.

GU Guo-hui, PAN Xiao-dong, GUAN Sheng, ZHONG Guang-pei, SONG Yu-jia, HU Le, LI Ying. Characteristics of Carbonaceous Gas Emissions from Changbaishan Tianchi Volcano, Northeast China[J]. EARTHQUAKE, 2024, 44(3): 196-214.

参考文献

[1] 高清武. 长白山天池火山水热活动及气体释放特征[J]. 地球学报, 2004, 25(3): 345-350.
GAO Qing-wu. Volcanic hydrothermal activities and gas-releasing characteristics of the Tianchi lake region, Changbai Mountains[J]. Acta Geoscientica Sinica, 2004, 25(3): 345-350 (in Chinese).
[2] 郭正府, 张茂亮, 孙玉涛, 等. 火山温室气体释放通量与观测的研究进展[J]. 矿物岩石地球化学通报, 2015, 34(4): 690-700.
GUO Zheng-fu, ZHANG Mao-liang, SUN Yu-tao, et al. Research advances in greenhouse gases degassing from Cenozoic volcanic active fields[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2015, 34(4): 690-700 (in Chinese).
[3] 李婷. 长白山天池火山的气体地球化学特征与成因[D]. 长春: 吉林大学, 2015.
LI Ting. The geochemical characteristics and origins of the gases in Changbaishan Tianchi volcanic region[D]. Changchun: Jilin University, 2015 (in Chinese).
[4] 赵文斌, 郭正府, 刘嘉麒, 等. 中国东北新生代火山区CO₂释放规模与成因[J]. 岩石学报, 2021, 37(4): 1255-1269.
ZHAO Wen-bin, GUO Zheng-fu, LIU Jia-qi, et al. Fluxes and genesis of carbon dioxide emissions from Cenozoic volcanic fields in NE China[J]. Acta Petrologica Sinica, 2021, 37(4): 1255-1269 (in Chinese).
[5] 刘嘉麒. 中国东北地区新生代火山幕[J]. 岩石学报, 1988(1): 1-10.
LIU Jia-qi. The Cenozoic volcanic episodes in Northeast China[J]. Acta Petrologica Sinica. 1988(1): 1-10 (in Chinese).
[6] 杨清福, 史兰斌, 陈孝德, 等. 长白山天池火山一次近代喷发物的特征[J]. 地震地质, 2006, 28(1): 71-83.
YANG Qing-fu, SHI Lan-bin, CHEN Xiao-de, et al. Characteristics of recent ejecta of the Changbaishan Tianchi volcano, China[J]. Seismology and Geology, 2006, 28(1): 71-83 (in Chinese).
[7] Xu J, Liu G, Wu J, et al. Recent unrest of Changbaishan volcano, Northeast China: A precursor of a future eruption?[J]. Geophysical Research Letters, 2012, 39(16): 16305.
[8] Xu J, Pan B, Liu T, et al. Climatic impact of the millennium eruption of Changbaishan volcano in China: New insights from high-precision radiocarbon wiggle-match dating[J]. Geophysical Research Letters, 2013, 40(1): 54-59.
[9] Wei H, Liu G, Gill J. Review of eruptive activity at Tianchi volcano, Changbaishan, Northeast China: implications for possible future eruptions[J]. Bulletin of Volcanology, 2013, 75(4): 1-14.
[10] 刘国明. 利用背景噪声研究地震波速度变化及其在长白山火山监测中的应用[J]. 地震地质, 2015, 37(2): 576-587.
LIU Guo-ming. Study of temporal seismic velocity changes from ambient seismic noise and its application to Changbaishan volcano monitoring[J]. Seismology and Geology, 2015, 37(2): 576-587 (in Chinese).
[11] Liu G, Li C, Peng Z, et al. The 2002—2005 Changbaishan volcanic unrest triggered by the 2002 M7.2 Wangqing deep focus earthquake[J]. Frontiers in Earth Science, 2021, 8: 599329.
[12] 上官志冠, 孙令昌, 孙凤民, 等. 长白山天池火山区深部流体成分及其稳定同位素组成[J]. 地质科学, 1996, 31(1): 54-64.
SHUANGGUAN Zhi-guan, SUN Ling-chang, SUN Feng-min, et al. Deep-seated fluid components and stable isotopic compositions in Tianchi volcanic area, Changbaishan Mountains[J]. Scientia Geologica Sinica, 1996, 31(1): 54-64 (in Chinese).
[13] 高玲, 上官志冠, 魏海泉, 等. 长白山天池火山近期气体地球化学的异常变化[J]. 地震地质, 2006, 28(3): 358-366.
GAO Ling, SHUANGGUAN Zhi-guan, WEI Hai-quan, et al. Recent geochemical changes of hot spring gases from Tianchi volcano area, Changbai Mountains, Northeast China[J]. Seismology and Geology, 2006, 28(3): 358-366 (in Chinese).
[14] 张茂亮, 郭正府, 成智慧, 等. 长白山火山区温泉温室气体排放通量研究[J]. 岩石学报, 2011, 27(10): 2898-2904.
ZHANG Mao-liang, GUO Zheng-fu, CHENG Zhi-hui, et al. Greenhouse gases flux estimation of hot springs in Changbaishan volcanic field, NE China[J]. Acta Petrologica Sinica, 2011, 27(10): 2898-2904 (in Chinese).
[15] 魏费翔, 许建东, 上官志冠, 等. 中国火山温泉气体地球化学特征及其在火山监测中的应用[J]. 震灾防御技术, 2018, 13(4): 938-949.
WEI Fei-xiang, XU Jian-dong, SHUANGGUAN Zhi-guan, et al. Geochemical characteristics of volcanic hot spring gas in China and its applications in volcanic monitoring[J]. Technology for Earthquake Disaster Prevention, 2018, 13(4): 938-949 (in Chinese).
[16] Wei F, Xu J, Kong Q, et al. Sources of CH₄ with variable carbon isotopes from Changbaishan volcano in NE China: Implications for the feeding system[J]. Journal of Volcanology and Geothermal Research, 2021, 419: 107355.
[17] Zhang M, Guo Z, Sano Y, et al. Stagnant subducted Pacific slab-derived CO₂ emissions: Insights into magma degassing at Changbaishan volcano, NE China[J]. Journal of Asian Earth Sciences, 2015, 106: 49-63.
[18] 赵文斌, 郭正府, 孙玉涛, 等. 火山区CO₂气体释放研究进展[J]. 矿物岩石地球化学通报, 2018, 37(4): 601-620.
ZHAO Wen-bin, GUO Zheng-fu, SUN Yu-tao, et al. Advances of the research on CO₂ degassing from volcanic fields[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2018, 37(4): 601-620 (in Chinese).
[19] Sun Y, Guo Z, Fortin D. Carbon dioxide emission from monogenetic volcanoes in the Mt. Changbai volcanic field, NE China[J]. International Geology Review, 2021, 63(14): 1803-1820.
[20] 刘若新, 樊祺诚, 郑祥身, 等. 长白山天池火山的岩浆演化[J]. 中国科学(D辑), 1998, 28(3): 226-231.
LIU Ruo-xin, FAN Qi-cheng, ZHENG Xiang-shen, et al. The magma evolution of Tianchi volcano, Changbaishan[J]. Science in China (Series D), 1998, 28(3): 226-231 (in Chinese).
[21] 刘嘉麒, 陈双双, 郭文峰, 等. 长白山火山研究进展[J]. 矿物岩石地球化学通报, 2015, 34(4): 710-723.
LIU Jia-qi, CHEN Shuang-shuang, GUO Wen-feng, et al. Research advances in the Mt. Changbai volcano[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2015, 34(4): 710-723 (in Chinese).
[22] Lei J, Xie F, Fan Q, et al. Seismic imaging of the deep structure under the Chinese volcanoes: An overview[J]. Physics of the Earth and Planetary Interiors, 2013, 224: 104-123.
[23] Chiodini G, Marini L. Hydrothermal gas equilibria: The H₂O-H₂-CO₂-CO-CH₄ system[J]. Geochimica et Cosmochimica Acta, 1998, 62(15): 2673-2687.
[24] Mazot A, Taran Y. CO₂ flux from the volcanic lake of El Chichón (Mexico)[J]. Geofísica Internacional, 2009, 48(1): 73-83.
[25] Mazot A, Rouwet D, Taran Y, et al. CO₂ and He degassing at El Chichón volcano, Chiapas, Mexico: Gas flux, origin and relationship with local and regional tectonics[J]. Bulletin of Volcanology, 2011, 73(4): 423-441.
[26] Sun Y, Guo Z, Liu J, et al. CO₂ diffuse emission from maar lake: An example in Changbai volcanic field, NE China[J]. Journal of Volcanology and Geothermal Research, 2018, 349: 146-162.
[27] Raich J W, Schlesinger W H. The global carbon dioxide flux in soil respiration and its relationship to vegetation and climate[J]. Tellus B, 1992, 44(2): 81-99.
[28] Raich J W, Tufekciogul A. Vegetation and soil respiration: Correlations and controls[J]. Biogeochemistry, 2000, 48: 71-90.
[29] Chiodini G, Baldini A, Barberi F, et al. Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy[J]. Journal of Geophysical Research: Solid Earth, 2007, 112(B12): B12204.
[30] Yazaki Y, Mariko S, Koizumi H. Carbon dynamics and budget in a Miscanthus sinensis grassland in Japan[J]. Ecological Research, 2004, 19(5): 511-520.
[31] Zencak Z, Borgen A, Reth M, et al. Evaluation of four mass spectrometric methods for the gas chromatographic analysis of polychlorinated n-alkanes[J]. Journal of Chromatography A, 2005, 1067(1-2): 295-301.
[32] Bowling D R, Pataki D E, Randerson J T. Carbon isotopes in terrestrial ecosystem pools and CO₂ fluxes[J]. New Phytologist, 2008, 178(1): 24-40.
[33] Chiodini G, Caliro S, Cardellini C, et al. Carbon isotopic composition of soil CO₂ efflux, a powerful method to discriminate different sources feeding soil CO₂ degassing in volcanic-hydrothermal areas[J]. Earth and Planetary Science Letters, 2008, 274(3-4): 372-379.
[34] 尹海霞. 长白山区不同立地条件下土壤温室气体排放的对比研究[D]. 长春: 东北师范大学, 2014.
YIN Hai-xia. Comparison of greenhouse gas emissions under different site conditions in Changbai Mountain area[D]. Changchun: Northeast Normal University, 2014 (in Chinese).
[35] Chiodini G, Frondini F, Cardellini C, et al. CO₂ degassing and energy release at Solfatara volcano, Campi Flegrei, Italy[J]. Journal of Geophysical Research: Solid Earth, 2001, 106(B8): 16213-16221.
[36] Bridgham S D, Updegraff K, Pastor J. Carbon, nitrogen, and phosphorus mineralization in northern wetlands[J]. Ecology, 1998, 79(5): 1545-1561.
[37] Kaye J P, Burke I C, Mosier A R, et al. Methane and nitrous oxide fluxes from urban soils to the atmosphere[J]. Ecological Applications, 2004, 14(4): 975-981.
[38] 崔月菊, 杜建国, 李营, 等. 张渤地震带高光谱气体地球化学特征[J]. 地球科学进展, 2016, 31(1): 59-65.
CUI Yue-ju, DU Jian-guo, LI Ying, et al. Gas geochemical characteristics of the Zhang-Bo seismic zone extracted from hyper-spectral data[J]. Advances in Earth Science, 2016, 31(1): 59-65 (in Chinese).
[39] 崔月菊, 杜建国, 陈杨, 等. 汶川M_S8.0地震前后龙门山断裂带CO和CH₄排气增强[J]. 地震研究, 2016, 39(2): 239-245.
CUI Yue-ju, DU Jian-guo, CHEN Yang, et al. Increasing of CO and CH₄ gas emission at Longmenshan fault zone before and after Wenchuan M_S8.0 earthquake[J]. Journal of Seismological Research, 2016, 39(2): 239-245 (in Chinese).
[40] 赵容生. 长白山地热系统汽-液两相循环机理及成因模式[D]. 吉林: 吉林大学, 2019.
ZHAO Rong-sheng. The mechanism and genetic model of vapor-liquid circulation processes in Changbai mountain two-phase geothermal system[D]. Jilin: Jilin University, 2019 (in Chinese).
[41] 张春山, 吴满路, 张重远, 等. 长白山地区现今地应力测量结果与应力状态分析[J]. 地球物理学报, 2016, 59(3): 922-930.
ZHANG Chun-shan, WU Man-lu, ZHANG Chong-yuan, et al. Measurement of present-day stress and analysis of stress state in the Changbaishan mountains of Jilin Province[J]. Chinese Journal of Geophysics, 2016, 59(3): 922-930 (in Chinese).
[42] 陈棋福, 艾印双, 陈赟. 长白山火山区深部结构探测的研究进展与展望[J]. 中国科学: 地球科学, 2019, 49(5): 778-795.
CHEN Qi-fu, AI Yin-shuang, CHEN Yun. Overview of deep structures under the Changbaishan volcanic area in Northeast China[J]. Science China Earth Sciences, 2019, 49(5): 778-795 (in Chinese).
[43] 仇根根, 裴发根, 方慧, 等. 长白山天池火山岩浆系统分析[J]. 地球物理学报, 2014, 57(10): 3466-3477.
QIU Gen-gen, PEI Fa-gen, FANG Hui, et al. Analysis of magma chamber at the Tianchi volcano area in Changbai Mountain[J]. Chinese Journal of Geophysics, 2014, 57(10): 3466-3477 (in Chinese).

长白山天池火山含碳气体排放特征

Characteristics of Carbonaceous Gas Emissions from Changbaishan Tianchi Volcano, Northeast China

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 3

编辑推荐

Metrics

本文评价

[1]	王琼, 王海涛, 唐兰兰, 宋春燕. 基于地震对应概率谱的多参数综合异常空间特征研究[J]. 地震, 2010, 30(1): 98-107.
[2]	任雪梅, 马禾青, 盛菊琴, 赵知军, 刘秀景. 1950年以来中国大陆5级以上地震原地(区)连发地震组的空间特征及意义[J]. 地震, 2005, 25(3): 95-101.
[3]	宋贯一. 地壳“轧展”效应对地震成因的解释[J]. 地震, 1998, 18(1): 89-96.