2015年4月15日内蒙古阿拉善左旗MS5.8地震前后CH4和CO变化

地震 ›› 2019, Vol. 39 ›› Issue (4): 54-62.

2015年4月15日内蒙古阿拉善左旗M_S5.8地震前后CH₄和CO变化

李新艳^1,2, 崔月菊², 马禾青², 卫定军², 仵柯田^3,2

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.宁夏回族自治区地震局, 宁夏银川 750001;
3.中国地质大学(北京), 北京 100083

收稿日期:2018-07-06 出版日期:2019-10-31 发布日期:2019-10-30
通讯作者: 崔月菊, 副研究员。 E-mail: cehuicuiyueju@126.com
作者简介:李新艳(1986-), 女, 甘肃庆阳人, 工程师, 主要从事遥感地球化学研究。
基金资助:
中国地震局地震预测研究所基本科研业务费专项(2016IES010103); 国家自然科学基金项目(4137059); 中国地震局地震科技星火计划项目(XH16040Y)

Anomalies on the Changes of CH₄ and CO related to the15 April 2015 Alashan Zuoqi M_S5.8 Earthquakein the Inner Mongolia

LI Xin-yan^1,2, CUI Yue-ju², MA He-qing², WEI Ding-jun², WU Ke-tian^3,2

1.CEA Key Laboratory of Earthquake Prediction (Institute of Earthquake Forecasting), China Earthquake Administration, Beijing 100036, China;
2.Earthquake Agency of Ningxia Hui Autonomous Region,Yinchuan 750001, China;
3.China University of Geosciences (Beijing), Beijing 100083, China

Received:2018-07-06 Online:2019-10-31 Published:2019-10-30

摘要/Abstract

摘要： 基于卫星高光谱数据讨论鄂尔多斯西缘CH₄和CO气体背景场特征和2015年4月15日内蒙古阿拉善左旗M_S5.8地震前后气体异常变化。结果表明, CH₄和CO气体总量在时间上均存在显著的季节变化, 空间分布上受构造地质背景、地形地貌影响, 高值区位于银川、吉兰泰、河套断陷盆地。 2015年4月15日内蒙古阿拉善左旗M_S5.8地震当月, CH₄异常沿鄂尔多斯西缘断裂带呈线性展布, 地震前1周左右, 震中两侧油气田出现CH₄异常, 异常幅度达到6倍标准偏差, 与地震引起附近油气田CH₄逸出增加有关; CO异常空间分布与CH₄基本一致, 时间上滞后CH₄异常1周左右, 持续2周左右后消失。 CH₄和CO关系密切, CO异常部分源自CH₄氧化。

关键词: CH₄, CO, 异常指数, 地震

Abstract: The anomalies of TotCH4 and TotCO associated with the 15 April 2015 Alashan Zuoqi M_S5.8 earthquake were discussed based on the satellite hyper-spectrum data. The background in monthly and anomaly-index of TotCH4 and TotCO were calculated from AIRS standard 3 level product data in recent years (2003—2012). The results showed that the TotCH4 and TotCO backgrounds in the study area presented obviously seasonal variations in temporally. Spatially, the distributions of TotCH₄ and TotCO were affected by the tectonic geological background and topographic landform. The high values of TotCH₄ and TotCO were located in Yinchuan, Jilantai and Hetao fault-sinking basins. TotCH4 anomaly appeared linearly along western edge of Ordos fault in April, while TotCH₄ appeared in oil-gas-bearing basins on both sides of the epicenter about 1 week before the major shock with the maximum anomaly index reached 6. TotCO anomaly appeared when and after the main shock, and lasted for two weeks. And the spatial distribution of TotCO anomaly was consistent with the CH₄. There was a close relationship between CH₄ and CO. The CO anomaly was partly derived from the CH₄ oxidation.

Key words: CH₄, CO, Anomaly-index, earthquake

中图分类号:

P315.7

李新艳, 崔月菊, 马禾青, 卫定军, 仵柯田. 2015年4月15日内蒙古阿拉善左旗M_S5.8地震前后CH₄和CO变化[J]. 地震, 2019, 39(4): 54-62.

LI Xin-yan, CUI Yue-ju, MA He-qing, WEI Ding-jun, WU Ke-tian. Anomalies on the Changes of CH₄ and CO related to the15 April 2015 Alashan Zuoqi M_S5.8 Earthquakein the Inner Mongolia[J]. EARTHQUAKE, 2019, 39(4): 54-62.

参考文献

[1] King C Y. Gas geochemistry applied to earthquake prediction: an overview[J]. Journal of Geophysical Research, 1986, 91(B12): 12269-12281.
[2] King C Y, Zhang W, Zhang Z C. Earthquake-induced groundwater and gas changes[J]. Pure and Applied Geophysics, 2006, 163(4): 633-645.
[3] Toutain J P, Baubron J C. Gas geochemistry and seismotectonics: a review[J]. Tectonophysics, 1999, 304(1-2): 1-27.
[4] Denman K L. Coupling s between changes in the climates system and biogeochemistry[A]. In : Solomon S ed. Climate change 2007: The physical science basis. Contribution of working group I to the four the assessment report of the intergovernmental panel on climate change[C]. Cambridge University. Press, Cambridge, UK, 2007, 7: 499-587.
[5] Etiope G. Natural emissions of methane from geological seepage in Europe[J]. Atmospheric Environment, 2009 , 43(7): 1430-1443.
[6] 岳中琦. 汶川地震与山崩地裂的极高压甲烷天然气成因和机理[J]. 地学前缘, 2013, 20(6): 15-20.
[7] 卢振权, 强祖基, 吴必豪. 南海临震前卫星热红外增温异常原因初探[J]. 地球学报, 2002, 23(1): 42-46.
[8] 黄福林, 张训华, 夏响华, 等. 中国东部和海域低层大气甲烷及其同系物分布[J]. 科学通报, 1998, 43(16): 1767-1771.
[9] Li Y, Du J G, Wang F K, et al. Geochemical characteristics of soil gas in the Yanhuai Basin, northern China[J]. Earthquake Science, 2009, 22(1): 93-100.
[10] 王杰, 张雄, 潘黎黎, 等. 芦山地震(M_S7.0)前甲烷释放与大气增温异常[J]. 地学前缘, 2013, 20(6): 29-35.
[11] 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.
[12] 崔月菊, 杜建国, 荆凤, 等. 2008年汶川M_S8.0地震前后川西含碳气体卫星高光谱特征[J]. 地震学报, 2016, 40(3): 448-457.
[13] 周凌晞, 温玉璞, 李金龙. 瓦里关山大气CO本底变化[J]. 环境科学学报, 2004, 24(4): 637-642.
[14] Daniel J S, Solomon S. On the climate forcing of carbon monoxide[J]. Journal of Geophysical Research, 1998, 103(D11): 13249-13260.
[15] Singh R P, Kumar J S, Zlotnicki J, et al. Satellite detection of carbon monoxide emission prior to the Gujarat earthquake of 26 January 2001[J]. Applied Geochemistry, 2010, 25(4): 580-585
[16] Cui Y, Du J, Zhang D, et al. Anomalies of total column CO and O₃associated with great earthquakes in recent years[J]. Natural Hazards and Earth System Sciences, 2013, 13: 2513-2519, 140.
[17] 孙玉涛, 崔月菊, 刘永梅, 等. 苏门答腊两次M＞8.0地震前后CO和O₃气体地球化学异常与地面验证[J]. 地震研究, 2014, 37(4): 222-227.
[18] 张国民, 马宏生, 王辉, 等. 中国大陆活动地块与强震活动关系[J]. 中国科学: 地球科学, 2004, 34(7): 591-599.
[19] 刘建辉, 张培震, 郑德文, 等. 贺兰山晚新生代隆升的剥露特征及隆升模式[J]. 中国科学: 地球科学, 2010, 4(1): 50-60.
[20] 韩晓明, 刘芳, 张帆, 等. 2015年阿拉善左旗M_S5.8地震的震源机制和重新定位[J]. 地震学报, 2015, 37(6): 1059-1063.
[21] 吴晓智, 王桂君, 郑民, 等. 雅布赖盆地构造演化与油气聚集[J]. 地质科学, 2015, 50(1): 74-87.
[22] 高山林, 韩庆军, 杨华. 鄂尔多斯盆地燕山运动及其与油气关系[J]. 吉林大学学报, 2000, 30(4): 353-358.
[23] 方双喜, 周凌晞, 许林, 等. 我国4个WMO/GAW 本底站大气CH₄浓度及变化特征[J]. 环境科学, 2012, 33(9): 2917-2923.
[24] 梅秀萍, 邵志刚, 张浪平, 等. 南北地震带北段强震破裂空段的地震危险性研究[J]. 地震学报, 2012, 34(4): 509-525.
[25] Aumann H H, Chahine M T, Gautier C, et al. AIRS/AMSU/HSB on the Aqua mission: Design, science objectives, data products and processing system[J]. IEEE Transactions on Geoscience and Remote Sensing, 2003, 41(2): 253-264.
[26] Won Y-I. Readme document for AIRS Level-3 version 5 standard products: Daily (AIRH3STD, AIRX3STD, AIRS3STD) 8-days (AIRH3ST8, AIRX3ST8, AIRS3ST8) & monthly (AIRH3STM, AIRX3STM, AIRS3STM). 2008, http:∥disc.sci.gsfc.nasa.gov/AIRS/documentation/readmes/README.AIR-3ST.pdf.
[27] Melsheimer C, Verdes C, Buehler S A, et al. Intercomparison of general purpose clear sky atmospheric radiative transfer models for the millimeter sub millimeter spectral range[J]. Radio Science, 2016, 40(1): 1-25.
[28] Adushkin V V, Kudryavtsev V P. Estimating the global flux of methane into the atmosphere and its seasonal variations[J]. Izvestiya Atmospheric & Oceanic Physics, 2013, 49(2): 128-136.
[29] Tramutoli V. Robust AVHRR Techniques (RAT) for environmental monitoring: theory and applications, in Earth Surface Remote Sensing II[J]. Proc. SPIE, 1998, 3496: 101-113.
[30] Tramutoli V, Di Bello G, Pergola N. Robust satellite techniques for remote sensing of seismically active areas[J]. Annali Di Geofisica, 2001, 44(2): 295-312.
[31] Cui Y, Ouzounov D, Hatzopoulos N, et al. Satellite observation of CH₄ and CO anomalies associated with the Wenchuan M_S8.0 and Lushan M_S7.0 earthquakes in China[J]. Chemical Geology, 2017, 469: 185-191.
[32] Artuso F, Chamard P, Piacentino S, et al. Influence of transport and trends in atmospheric CO₂ at Lampedusa[J]. Atmospheric Environment, 2009, 43(19) : 3044-3051.
[33] Martinelli G, Dadomo A. Factors constraining the geographic distribution of earthquake geochemical and fluid-related precursors[J]. Chemical Geology, 2017, 469: 176-184.
[34] Asadzadeh S, de Souza Filho C S. Spectral remote sensing for onshore seepage characterization: A critical overview[J]. Earth Science Reviews, 2017, 168.
[35] 秦瑜, 赵春生. 大气化学基础[M]. 北京: 气象出版社, 2003, 168-170.
[36] Horowitz L W, Walters S, Mauzerall D L, et al. A global simulation of tropospheric ozone and related tracers: Description and evaluation of MOZART, version 2[J]. Journal of Geophysical Research, 2003, D24(108): 4784, doi:10.1029/2002JD002853.
[37] 崔月菊, 李静, 王燕艳, 等. 地震遥感气体地球化学研究进展[J]. 地球科学进展, 2015, 30(2): 284-294.
[38] McConnell J C, McElroy M B, Wofsy S C. Natural sources of atmospheric CO[J]. Nature, 1971, 233: 187-188.
[39] Fishman J, Seiler W. Correlative nature of ozone and carbon monoxide in the troposphere: implications for the tropospheric ozone budget[J]. Journal of Geophysical Research, 1983, 88(C6): 3662-3670.

2015年4月15日内蒙古阿拉善左旗M_S5.8地震前后CH₄和CO变化

Anomalies on the Changes of CH₄ and CO related to the15 April 2015 Alashan Zuoqi M_S5.8 Earthquakein the Inner Mongolia

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	纪润池, 申旭辉, 张景发, 田云锋. 中小地震三维形变场重构方法研究与同震滑动分布反演以2016年5月22日定日M_W5.3地震为例[J]. 地震, 2019, 39(4): 84-97.
[2]	廖晓峰, 冯丽丽, 祁玉萍, 李霞. 地磁极化方法在阿拉善5.0级地震中的应用研究[J]. 地震, 2019, 39(4): 127-135.
[3]	汤兰荣, 曾新福, 董非非, 罗丽, 查小惠, 郭雨帆, 曾文敬. 华东地区地震空区预报效能评估[J]. 地震, 2019, 39(4): 136-146.
[4]	张希, 秦姗兰, 贾鹏, 李瑞莎. 2016年门源M_S6.4地震孕育—发生的地形变异常特征[J]. 地震, 2019, 39(4): 27-38.
[5]	刘兴旺, 袁道阳, 邵延秀, 张波, 柳煜. 祁连山北缘玉门—北大河断裂东段古地震特征[J]. 地震, 2019, 39(3): 1-10.
[6]	于吉鹏, 孟国杰, 苏小宁, Nikolay Shestakov, Mikhail Gerasimenko, Hiroaki Takahashi, Mako Ohzono, 刘泰, 李承涛. 基于GPS观测研究中国东北地区现今地壳形变特征[J]. 地震, 2019, 39(3): 11-27.
[7]	李伟, 储日升, 王烁帆. 2017年6月16日湖北秭归M_S4.3地震成因初探[J]. 地震, 2019, 39(3): 28-42.
[8]	闫坤, 王伟君, 王琼, 杨峰, 刘宁, 寇华东. 北天山中段微震活动检测及其活动性和孕震构造分析[J]. 地震, 2019, 39(3): 43-60.
[9]	杨江, 李营, 陈志, 孙凤霞, 赵建明, 李静, 王江. 唐山断裂带南西段和北东段土壤气Rn和CO₂浓度特征[J]. 地震, 2019, 39(3): 61-70.
[10]	黄继攀, 王新安, 雍珊珊, 王墨, 刘众. 2017年九寨沟7级地震前电磁扰动异常分析[J]. 地震, 2019, 39(3): 84-94.
[11]	宋锐, 刘静, 张学民, 何建辉. 2016年缅甸M7.2地震前中国区域电离层TEC扰动的时空分布[J]. 地震, 2019, 39(3): 95-105.
[12]	戴勇, 高立新, 姚丽, 朱培育, 格根, 王磊. 2013年岷县—漳县6.6级地震地磁垂直分量日变化低点时间空间分布特征[J]. 地震, 2019, 39(3): 106-114.
[13]	李利波, 付虹, 李琼, 何德强. 滇东北地区地震弱活动前兆异常特征研究[J]. 地震, 2019, 39(3): 115-126.
[14]	庞亚瑾, 程惠红, 董培育, 石耀霖. 天山北部强震活动对区域应力扰动的分析以2012年伊犁M6.6地震和2017年精河M6.6地震为例[J]. 地震, 2019, 39(3): 127-137.
[15]	孟真, 宋晓东. 龙门山断裂带周缘重复地震识别及其在台网定位评价中的应用[J]. 地震, 2019, 39(3): 166-177.