高级搜索

首都圈西北部主要活动断裂土壤气中氢气（H2）地球化学特征

,  ,  ,  ,  ,  ,  ,  ,  ,  , 

downloadPDF

上一篇

下一篇

周晓成, 陈超, 吕超甲, 孙凤霞, 陈志, 仵柯田, 黄丹, 张冠亚, 张瑞鑫, 刘红, 崔月菊. 首都圈西北部主要活动断裂土壤气中氢气（H2）地球化学特征[J]. 环境化学, 2017, 36(5): 977-983. doi: 10.7524/j.issn.0254-6108.2017.05.2016090604
引用本文: 周晓成, 陈超, 吕超甲, 孙凤霞, 陈志, 仵柯田, 黄丹, 张冠亚, 张瑞鑫, 刘红, 崔月菊. 首都圈西北部主要活动断裂土壤气中氢气（H2）地球化学特征[J]. 环境化学, 2017, 36(5): 977-983. doi: 10.7524/j.issn.0254-6108.2017.05.2016090604
shu
ZHOU Xiaocheng, CHEN Chao, LYV Chaojia, SUN Fengxia, CHEN Zhi, WU Ketian, HUANG Dan, ZHANG Guanya, ZHANG Ruixin, LIU Hong, CUI Yueju. Gas geochemistry of H2 in soil gas from the main faults of northwest area of the capital region, China[J]. Environmental Chemistry, 2017, 36(5): 977-983. doi: 10.7524/j.issn.0254-6108.2017.05.2016090604
Citation: ZHOU Xiaocheng, CHEN Chao, LYV Chaojia, SUN Fengxia, CHEN Zhi, WU Ketian, HUANG Dan, ZHANG Guanya, ZHANG Ruixin, LIU Hong, CUI Yueju. Gas geochemistry of H2 in soil gas from the main faults of northwest area of the capital region, China[J]. Environmental Chemistry, 2017, 36(5): 977-983. doi: 10.7524/j.issn.0254-6108.2017.05.2016090604
shu

首都圈西北部主要活动断裂土壤气中氢气（H2）地球化学特征

  • 1.

    中国地震局地震预测重点实验室, 中国地震局地震预测研究所, 北京, 100036;

  • 2.

    四川省地震局康定地震台, 康定, 626000

  • 基金项目:

    中国地震局地震预测研究所基本科研业务费（2014IES010202，2014IES0402，2012IES0408，2016IES010103）和国家自然科学基金（41673106）资助

Gas geochemistry of H2 in soil gas from the main faults of northwest area of the capital region, China

  • 1.

    CEA Key Laboratory of Earthquake Prediction (Institute of Earthquake Science), China Earthquake Administration, Beijing, 100036, China;

  • 2.

    Kangding Seismic Station, Sichuan Earthquake Administration, Kangding, 626000, China

  • Fund Project: Supported by the National Science and Technology Support Program CEA Key Laboratory of Earthquake Prediction (2014IES010202, 2014IES0402, 2012IES0408, 2016IES010103) and the National Natural Science Foundation of China (41673106)

  • 摘要: 在首都圈西北部9条活动断裂上布置了17个土壤气氢气（H2）测区，土壤气H2浓度分别在2012年5月和2013年5月测量两次，测点共1105个.测量数据结果表明：（1）9条活动断裂上土壤气H2的浓度在断裂附近明显高于非断裂区域；（2）9条活动断裂上土壤气H2的浓度从西向东呈增大的趋势.首都圈西北部活动断裂带土壤气H2的释放会引起大气电离层的扰动，有关活动断裂带土壤气H2释放的进一步研究对大气环境变化研究有重要的意义.
    Abstract: H2 in soil gas was measured twice in seventeen sites in the nine faults in the northwest area of the capital region, China, in May 2012 and May 2013. The results indicated that the H2 concentrations in the soil gas from the nine faults had obvious anomalies. The H2 concentrations in soil gas increased from west to east in the nine faults in northwest of capital region. The release of H2 from faults would impact the ionosphere. It is very significant to carry on further study on the release of H2 from faults and its impact on atmospheric environment.
  • 加载中
  • [1] NOVELLI P C, LANG P M, MASARIE K A, et al. Molecular hydrogen in the troposphere: Global distribution and budget[J]. Journal of Geophysical Research, 1999, 104:30427-30444.
    [2] LIBERT M, BILDSTEIN O, ESNAULT L, et al. Molecular hydrogen: An abundant energy source for bacterial activity in nuclear waste repositories [J]. Physics and Chemistry of the Earth, 2011, 36:1616-1623.
    [3] WARE R H, ROECKEN C, WYSS M. The detection and interpretation of hydrogen in fault gases[J]. Pure and Applied Geophysics, 1984,122(2):392-402.
    [4] SHANGGUAN Z, HUO W. δD values of escaped H2 from hot springs at the Tengchong Rehai geothermal area and its origin [J]. Chinese Science Bulletin, 2002, 47(2):148-150.
    [5] MAYHEW L E, ELLISON E T, MCCOLLOM T M, et al. Hydrogen generation from low-temperature water-rock reactions[J]. Nature geoscience, 2013, 6: 577-584.
    [6] 杜乐天.地球排气作用的重大意义及研究进展[J].地质论评, 2005,51(2):174-180.

    DU L. Significance of Earth Degassing and Its Research Progress [J]. Geological Review, 2005, 51(2):174-180 (in Chinese).

    [7] 车用太,刘耀炜,何钄.断层带土壤气中H2观测-探索地震短临预报的新途径[J].地震,2015,35(4):1-10.

    CHE Y T, LIU Y W, HE L. Hydrogen monitoring in fault zone soil gas-A new approach to short/immediate earthquake prediction[J]. Earthquake, 2015, 35(4):1-10 (in Chinese).

    [8] 周晓成,王传远,柴炽章,等. 海原断裂带东南段土壤气体地球化学特征研究[J]. 地震地质, 2011,33(1):123-132.

    ZHOU X, WANG C, CHAI Z, et al. The geochemical characteristics of soil gas in the southeastern part of Haiyuan fault[J]. Seismology and Geology, 2011, 33(1):123-132 (in Chinese).

    [9] 周晓成,柴炽章,雷启云,等.银川隐伏断层带土壤气中H2地球化学特征[J].物探与化探,2013, 37(1):147-149.

    ZHOU X, CHAI C, LEI Q, et al. Geochemical characteristics of H2 in soil gas of Yinchuan buried fault belt [J]. Geophysical and Geochemical Exploration, 2013, 37(1):147-149 (in Chinese).

    [10] WIERBERG T, ERZINGER J. On the origin and spatial distribution of gas at seismogenic depths of the San Andreas Fault from drill mud gas analysis [J]. Applied Geochemistry, 2008, 23:1675-1690.
    [11] WAKITA H, NAKAMURA Y, KITA I, et al. Hydrogen release: New indicator of fault activity [J]. Science, 1980, 210:188-190.
    [12] SUGISAKI R, IDO M, TAKEDA H, et al. Origin of hydrogen and carbon dioxide in fault gases and its relation to fault activity[J]. Journal of Geology, 1983,91(3):239-258.
    [13] 邵济安, 赵谊, 张福松, 等.黑龙江省中西部地球排气与地震活动的探讨[J].岩石学报, 2010, 26(12): 3651-3656.

    SHAO J A, ZHAO Y, ZHANG F S, et al. Discussions on earth degassing and seismic activities in central west Heilongjiang Province[J]. Acta Petrologica Sinica, 2010, 26(12):3651-3656 (in Chinese).

    [14] POISSANT L,CONSTANT P, PI.OTE M, et al. The ebullition of hydrogen, carbon monoxide, methane, carbon dioxide and total gaseous mercury from the Cornwall Area of Concern [J]. Science of the Total Environment, 2007,381:256-262.
    [15] 周晓成,杜建国,陈志,等.地震地球化学研究进展[J]. 矿物岩石地球化学通报, 2012,31(4):15-18.

    ZHOU X, DU J, CHEN Z, et al. Advance review of seismic geochemistry[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2012,31(4):340-346 (in Chinese).

    [16] ZHOU X, DU J, CHEN Z, et al. Geochemistry of soil gas in the seismic fault zone produced by the Wenchuan Ms 8.0 earthquake, southwestern China [J]. Geochemical Transactions,2010,11:5. doi:10.1186/1467-4866-11-5.
    [17] ZHOU X, CHEN Z, CUI Y. Environmental impact of CO2, Rn, Hg degassing from the rupture zones produced by Wenchuan Ms 8.0 earthquake in western Sichuan, China[J]. Environmental Geochemistry and Health, 2016, 38:1067-1082.
    [18] FU Z, LIU J, LIU G. On the long-term seismic hazard analysis in the Zhangjiakou-Penglai seismotectonic zone, China [J]. Tectonophysics, 2004,390:75-83.
    [19] GUO L, LI S, SUO Y, et al. Experimental study and active tectonics on the Zhangjiakou-Penglai fault zone across North China [J]. Journal of Asian Earth Sciences, 2015,114:18-27.
    [20] SHI W, CEN M, CHEN L, et al. Evolution of the late Cenozoic tectonic stress regime in the Shanxi Rift, central North China Plate inferred from new fault kinematic analysis [J]. Journal of Asian Earth Sciences, 2015,114:54-72.
    [21] 李西双,刘保华,华清峰,等.张家口-蓬莱断裂带渤海段晚第四纪活动特征[J].海洋科学进展,2009,27(3).332-347.

    Li S X, LIU B H,HUA Q F, et al. Characters of the Zhangjiakou-Penglai Fault Zone Activity in the Bohai Sea Since Late Quaternary[J]. Advances in Marine Science, 2009, 27(3):332-347 (in Chinese).

    [22] 徐杰,马宗晋,陈国光,等.中国大陆东部新构造期北西向断裂带的初步探讨[J].地学前缘,2003,10(Z1):193-198.

    XU J, MA Z J, CHEN G G, et al. NW Trending active fault zones of the eastern Chinese continent in neo tectonic time[J]. Earth Science Fronties (China University of Geosciences, Beijing), 2003, 10(Z1):193-198 (in Chinese).

    [23] 程绍平,杨桂枝,杨喆.延庆盆地北缘断裂带蚕房营段晚更新世晚期断层作用[J].地震地质, 1994,16(4):346-354.

    CHENG S P, YANG G Z, YANG Z. The latest Pleistocene faulting along the Canfangying segment of the fault zone along the northern margin of Yanqing Basin[J]. Seismolgy and Geology, 1994,16(4):346-354 (in Chinese).

    [24] 段瑞涛,方仲景.六棱山北麓断裂新活动特征[J].地震地质,1995,17(3):207-213.

    DUAN R, FANG Z. Neotectonic Characteristics of the northern piedmont fault of the Liuleng mountain[J]. Seismolgy and Geology, 1995,17(3):207-213 (in Chinese).

    [25] 冉勇康.我国几个典型地点的古地震细研究和大地震重复行为探讨[D].北京:中国地震局地质研究所学位论文,1997. RAN K. Detailed research of paleoearthquakes at several typical regions in China and exploration of recurrence behavior of large earthquakes[D]. Beijing:Institute of Geology, China Earthquake Administration, 1997 (in Chinese).
    [26] LI Y L, YANG J C, XIA Z K, et al. Tectonic geomorphology in the Shanxi Graben System, northern China[J]. Geomorphology, 1998, 23:77-89.
    [27] PAVLIDES S B, ZOUROS N C, FANG Z J, et al. Geometry, kinematics and morphotectonics of the Yanqing-Huailai active faults (Northern China) [J]. Tectonophysics, 1999, 308:99-118.
    [28] 徐锡伟,吴卫民,张先康,等.首都圈地区地壳最新构造变动与地震[M].北京:科学出版社.2002. XU X W,WU W M,ZHANG X K,et al. Neotectonic Movements and Seismology in the Crust of the Capital Region[M]. Beijing, Science Press, 2002 (in Chinese).
    [29] 谢富仁,张红艳,崔效锋,等.延怀盆地活动断裂运动与现代构造应力场[J].地震地质,2007,29(4):693-305.

    XIE F R, ZHANG H Y, CUI X F, et al. Active fault movement and recent tectonic stress field in Yanhuai basin[J]. Seismolgy and Geology, 2007,29(4):693-305 (in Chinese).

    [30] 周月玲,尤惠川.张家口断裂第四纪构造变形与活动性研究[J].震灾防御技术, 2010,5(2):157-166.

    Zhou Y L, YOU H C. Research on Quaternary Deformation and Activities of Zhangjiakou Fault, Hebei Province[J]. Technology for Earthquake Disaster Prevention, 2010,5(2):157-166 (in Chinese).

    [31] 徐伟,刘旭东,张世民.口泉断裂中段晚第四纪以来断错地貌及滑动速率确定[J]. 地震地质, 2011, 33(2):335-346.

    XU W, LIU X D, ZHANG S M. Late quaternary faulted landforms and determination of slip rates of the middle part of Kouquan fault[J]. Seismolgy and Geology, 2011, 33(2):335-346 (in Chinese).

    [32] 王林, 田勤俭, 李德文, 等. 京西北蔚县-广灵半地堑盆地南缘断裂带的断层生长研究[J]. 地震地质, 2011, 33(4): 828-838.

    WANG L, TIAN Q J, LI D W, et al. the growth of the south margin fault of the Yuxuan-Guangling basin in Northwest Beijing area[J]. Seismolgy and Geology, 2011, 33(4): 828-838 (in Chinese).

    [33] 索艳慧,李三忠,刘鑫,等.中国东部NWW向活动断裂带构造特征:以张家口-蓬莱断裂带为例[J].岩石学报, 2013, 29(3): 953-966.

    SUO Y H, LI S Z, LIU X,et al. Structural characteristics of NWW-trending active fault zones in East China: A case study of the Zhangjiakou-Penglai Fault Zone[J]. Acta Petrologica Sinica, 2013, 29(3):953-966 (in Chinese).

    [34] CIOTOLI G, LOMBARDI S, ANNUNIATELLIS A. Geostatistical analysis of soil gas data in a high seismic intermontane basin: Fucino Plain, Central Italy [J]. Journal of Geophysical Research, 2007,112:B05407.
    [35] EVANS J P, FORSTER C B, GODDARD J V. Permeability of fault-related rocks, and implication for hydraulic structure of fault zones [J]. Journal of Structural Geology, 1997,19:1393-1404.
    [36] HERNÁNDEZ P, PÉREZ N, SALAZAR J, et al. Soil gas CO2, CH4 and H2 distribution in and around Las Cañadas caldera, Tenerife, Canary Islands, Spain[J]. Journal of Volcanology and Geothermal Research, 2000,103:425-438.
    [37] LIN L, HALL J, LIPPMANN-PIPKE J, et al. Radiolytic H2 in continental crust: Nuclear power for deep subsurface microbial communities[J]. Geochemistry Geophysics Geosystems, 2005, 6(7): 1-13.
    [38] KATAYAMA I, KUROSAKI I, HIRAUCHI K. Low silica activity for hydrogen generation during serpentinization: An example of natural serpentinites in the Mineoka ophiolite complex, central Japan [J]. Earth and Planetary Science Letters, 2010, 298:199-204.
    [39] KAMEDA J, SARUWATARI K, TANAKA H. H2 generation in wet grinding of granite and single-crystal powders and implications for H2 concentration on active faults [J]. Geophysical Research Letters, 2003, 30(20):2063.
    [40] KAMEDA J, SARUWATARI K, TANAKA H. H2 generation by dry grinding of kaolinite [J]. Journal of Colloid and Interface Science, 2004, 275:225-228.
    [41] KITA I, MATSUO S, WAKITA H. H2 generation by reaction between H2O and crushed rock: An experimental study on H2 degassing from the active fault zone [J]. Journal of Geophysical Research, 1982, 87(B13): 10789-10795.
    [42] KITA I, MATSUO S, WAKITA H, et al. D/H ratios of H2 in soil gases as an indicator of fault movements [J]. Geochemical Journal, 1980,14: 317-320.
    [43] LIBERT M, BILDSTEIN O, ESNAULT L, et al. Molecular hydrogen: An abundant energy source for bacterial activity in nuclear waste repositories [J]. Physics and Chemistry of the Earth, 2011, 36:1616-1623.
    [44] 胡勐乾,邓志辉,陆远忠,等.三维数值模拟在华北地区现今构造变形分析中的应用[J]. 地震地质, 2014, 36(1): 148-165.

    HU M Q, DENG Z H, LU Y Z, et al. Contemporary tectonic deformation in north China by using three-dimensional simulation[J]. Seismolgy and Geology, 2014, 36(1): 148-165 (in Chinese).

    [45] EHHALT D H. Gas phase chemistry of the troposphere, in Global Aspects of Atmospheric Chemistry, edited by R. Sellner [M]. New York, Springer, 1999, 21-109.
    [46] HAUGLUSTAINE D A, EHHALT D H. A three-dimensional model of molecular hydrogen in the troposphere [J]. Journal of Geophysical Research, 2002,107:(D17):ACH4-1—ACH4-16.
    [47] WARWICK N J, BEKKI S, NISBET E G, et al. Impact of a hydrogen economy on the stratosphere and troposphere studied in a 2-D model [J]. Geophysical Research Letters, 2004,31(5):325-341.
    [48] 汪四成,方涵先,杨升高,等.H2释放扰动电离层的数值模拟[J].大气科学学报,2013,36(4):499-503.

    Wang S C, FANG H X,YANG S G, et al. Numerical simulation of ionoshperic modification by release[J].Transactions of Atmospheric Sciences, 2013,36(4):499-503 (in Chinese).

    [49] 闫雨龙,温彦平,冯新宇,等.太原市城区臭氧变化特征及影响因素[J].环境化学,2016,35(11):2261-2268.

    YAN Y L,WEN Y P,FENG X Y,et al. Variation and the influence factors of ozone in urban area in Taiyuan[J].Environmental Chemistry,2016,35(11):2261-2268(in Chinese).

    [50] FREUND F. Pre-earthquake signals: Underlying physical processes[J]. Journal of Asian Earth Sciences, 2011, 41:383-400.
  • 加载中
WeChat 点击查看大图
计量
  • 文章访问数:  1076
  • HTML全文浏览数:  1009
  • PDF下载数:  434
  • 施引文献:  0
出版历程
  • 收稿日期:  2016-09-06
  • 刊出日期:  2017-05-15
周晓成, 陈超, 吕超甲, 孙凤霞, 陈志, 仵柯田, 黄丹, 张冠亚, 张瑞鑫, 刘红, 崔月菊. 首都圈西北部主要活动断裂土壤气中氢气（H2）地球化学特征[J]. 环境化学, 2017, 36(5): 977-983. doi: 10.7524/j.issn.0254-6108.2017.05.2016090604
引用本文: 周晓成, 陈超, 吕超甲, 孙凤霞, 陈志, 仵柯田, 黄丹, 张冠亚, 张瑞鑫, 刘红, 崔月菊. 首都圈西北部主要活动断裂土壤气中氢气（H2）地球化学特征[J]. 环境化学, 2017, 36(5): 977-983. doi: 10.7524/j.issn.0254-6108.2017.05.2016090604
shu
ZHOU Xiaocheng, CHEN Chao, LYV Chaojia, SUN Fengxia, CHEN Zhi, WU Ketian, HUANG Dan, ZHANG Guanya, ZHANG Ruixin, LIU Hong, CUI Yueju. Gas geochemistry of H2 in soil gas from the main faults of northwest area of the capital region, China[J]. Environmental Chemistry, 2017, 36(5): 977-983. doi: 10.7524/j.issn.0254-6108.2017.05.2016090604
Citation: ZHOU Xiaocheng, CHEN Chao, LYV Chaojia, SUN Fengxia, CHEN Zhi, WU Ketian, HUANG Dan, ZHANG Guanya, ZHANG Ruixin, LIU Hong, CUI Yueju. Gas geochemistry of H2 in soil gas from the main faults of northwest area of the capital region, China[J]. Environmental Chemistry, 2017, 36(5): 977-983. doi: 10.7524/j.issn.0254-6108.2017.05.2016090604
shu

首都圈西北部主要活动断裂土壤气中氢气（H2）地球化学特征

  • 1.  中国地震局地震预测重点实验室, 中国地震局地震预测研究所, 北京, 100036;
  • 2.  四川省地震局康定地震台, 康定, 626000
  • 收稿日期:  2016-09-06
基金项目:

中国地震局地震预测研究所基本科研业务费（2014IES010202，2014IES0402，2012IES0408，2016IES010103）和国家自然科学基金（41673106）资助

摘要: 在首都圈西北部9条活动断裂上布置了17个土壤气氢气（H2）测区，土壤气H2浓度分别在2012年5月和2013年5月测量两次，测点共1105个.测量数据结果表明：（1）9条活动断裂上土壤气H2的浓度在断裂附近明显高于非断裂区域；（2）9条活动断裂上土壤气H2的浓度从西向东呈增大的趋势.首都圈西北部活动断裂带土壤气H2的释放会引起大气电离层的扰动，有关活动断裂带土壤气H2释放的进一步研究对大气环境变化研究有重要的意义.

English Abstract

    全文HTML

参考文献 (50)

返回顶部

目录

/

返回文章
返回

Copyright © 2019 中国科学院生态环境研究中心