Geochemistry of soil gas in the seismic fault zone produced by the Wenchuan Ms 8.0 earthquake, southwestern China
© Zhou et al; licensee BioMed Central Ltd. 2010
Received: 21 June 2010
Accepted: 6 December 2010
Published: 6 December 2010
The spatio-temporal variations of soil gas in the seismic fault zone produced by the 12 May 2008 Wenchuan Ms 8.0 earthquake were investigated based on the field measurements of soil gas concentrations after the main shock. Concentrations of He, H2, CO2, CH4, O2, N2, Rn, and Hg in soil gas were measured in the field at eight short profiles across the seismic rupture zone in June and December 2008 and July 2009. Soil-gas concentrations of more than 800 sampling sites were obtained. The data showed that the magnitudes of the He and H2 anomalies of three surveys declined significantly with decreasing strength of the aftershocks with time. The maximum concentrations of He and H2 (40 and 279.4 ppm, respectively) were found in three replicates at the south part of the rupture zone close to the epicenter. The spatio-temporal variations of CO2, Rn, and Hg concentrations differed obviously between the north and south parts of the fault zone. The maximum He and H2 concentrations in Jun 2008 occurred near the parts of the rupture zone where vertical displacements were larger. The anomalies of He, H2, CO2, Rn, and Hg concentrations could be related to the variation in the regional stress field and the aftershock activity.
The MS 8.0 Wenchuan earthquake of 12 May 2008 produced a 285-km long surface rupture zone along the pre-existing Yingxiu-Beichuan, Guanxian-Anxian, and Qingchuan faults, which indicated the faults were reactivated. The maximum thrust slip distance was estimated to be about 10 m, accompanied by 9 m of shortening across the rupture zone . Most of the large aftershocks were distributed in the north and south parts of the Longmenshan fault zone. The dominant focal depths of the aftershocks were between 5 and 20 km, and the depth of the main shock was 16.0 km. The focal depth distribution in some areas was characterized by high-angle westward dipping. The rupture mode of the main shock was characterized by reverse faulting in the south and with a large strike-slip component in the north .
The spatial and temporal patterns of deep-source gas leakage can be investigated by measuring soil gas in the faulted zones. The variations of soil-gas concentrations can serve as useful tools for monitoring earthquakes. The short-term decrease of helium concentrations in soil gas along the San Andreas Fault in central California was well-correlated with aftershocks . The sudden increase in CO2 and Rn concentrations at the Mariánské Láznĕ fault in the NW Bohemian swarm quake region might indicate an increase of fault permeability caused by stress redistribution, resulting in the opening of migration pathways . Across two fault segments that ruptured during the magnitude 7.5 Landers earthquake in 1992, anomalously high radon concentrations were found in the fractures three weeks after the earthquake . In parts of southeastern Ghana, In the highly faulted area, radon activity up to 115.00 k Bq/m3 was measured, on the contrary in non-faulted areas radon activity was less than 20.00 k Bq m3 . The concentrations of He, Rn, CO2, and N2 in soil gas clearly showed anomalous values along the fault of Hsincheng in the Hsinchu area of Taiwan . High H2 concentrations of up to 3% were observed in soil gas along a strike of the Yamasaki fault .
The compositions and distributions of soil gases in a fault zone are affected by many factors, such as agrologic, biogenic, and meteorological factors, especially gas leakage from deep faults . Therefore, the anomaly variation of soil gas concentrations induced by the earthquake is difficult to distinguish. The goals of this paper are to correlate the spatio-temporal variations of soil gas along the seismic rupture zone of the Wenchuan Ms 8.0 earthquake with the aftershocks and to try to couple the geochemical field with the crustal stress field.
2. Geological setting
The Longmenshan fault zone (LFZ) consists of the Maoxian-Wenchuan fault, the Qingchuan fault, the Beichuan-Yingxiu fault, and the Penxian-Guanxian fault from west to east, and is located at the east margin of the Qinghai-Tibetan Plateau. These faults with a northeast-southwest strike began to develop in the Triassic. Due to episodic movements during the Meso-Cenozoic, especially since the Late Cenozoic, accompanied by eastward extrusion of the Qinghai-Tibet Plateau, the middle and southern segments of the LFZ underwent strong compression and the basement was detached, which formed impressive thrust nappe structures and klippen swarms on the eastern margin of the Qinghai-Tibet Plateau . The LFZ penetrates the Moho. Strata in the fault zone are predominantly Palaeozoic and Lower Mesozoic flysch and carbonate, with some intermediate layers of volcanic rocks. Many great earthquakes have been recorded along the Longmenshan fault zone. For instance, two Ms 7.2 earthquakes occurred between Songpan and Pingwu, north of Sichuan Province on August 16 and 23, 1976. An Ms 7.5 earthquake occurred at Diexi town, Maoxian county, Sichuan Province on August 25, 1933 .
The first soil-gas survey was performed from 20 Jun to 3 Jul in 2008; 196 samples were measured at five sites (SXG, BL, YH, LG and PT, Figure 1). The second and third surveys were carried out at eight sites (SXG, XYD, BL, YH, HW, LG and PT, NB, Figure 1) in the same areas from 16 to 31 Dec in 2008 and from 16 Jul to 31 Aug in 2009, and 331 and 301 samples were measured, respectively. Three or four parallel profiles at each of eight sampling sites were analyzed. Soil gas was sampled along profiles at distances of about 5 to 20 m, and the distances were shortened to 2.5 m near the fault scarps. He, H2, N2, O2, CO2, CH4, Rn, and Hg concentrations of 828 soil-gas samples were analyzed.
The traditional method was employed to sample soil gases . Three holes strike of 0.8 m deep and 2.3 cm in diameter at 0.5 m lateral intervals were drilled in the ground at each sampling site. Three Teflon tube probes strike of 80 cm long and 2.3 cm in diameter were inserted into the holes. The concentration of elemental mercury in the soil was analyzed in the field with a portable RA-915+ Zeeman Mercury Analyzer and the error of measurement was 2 ng/m3. The soil gas from two holes was continuously pumped through the analyzer cell at a rate of 2 L/min. Data were recorded on the portable computer with a response time of 1 sec. 222Rn concentration was measured in the field using a RAD7 Radon Detector. Soil gas was pumped at flow rate of 1 L/min from another probe into the internal accumulation chamber where electrostatic collection of alpha-emitters with spectral analysis took place. Alpha emissions with energy of 6.002 MeV were attributed to 218Po decay, allowing 222Rn activity to be produced . Three concentrations of radon were performed each with 5 minute integration time. The results in units of Bq/m3 were determined by the mean value of three measurements with an error of ± 5%. The concentrations of He, H2, N2, O2, CO2 and CH4 in soil gas were measured in the field by an Agilent 3000 Micro GC with an error of ± 5%.
Data were displayed as the contour line maps obtained by computer-processed 'kringing' interpolation method in the SURFER 8.0 software package.
4. Results and discussion
4.1. Statistical analysis
The statistical data of soil gas concentrations in the seismic fault zone
Number of samples
Loadings for Varimax-rotated factor matrix in two factor model
4.2. The relationship between co-seismic rupture and soil gas
Anomalies of He, H2, CO2, Rn, Hg, and N2/O2 in soil gas displayed complex characteristics (Figure 3). The spatial distributions of soil gas concentrations clearly showed higher values near the fault scarps because co-seismic ruptures usually enhance the permeability of rock and soil, favoring gas emission and resulting in ''halo'' anomalies. At many sites, isolated points with high concentration values (''spotty anomalies'') were frequently observed . The multiple ''spot anomalies'' along fault scarps probably mainly resulted from the differences in fault and soil features from place to place (Figure 3). The fault scarps observed upon the alluvial terrace, where unconsolidated deposits overlie basement rock, showed a complex morphology with a folding structure . The bimodal feature of the anomalies of soil gas crossing the fault scarps may be caused by emission and atmospheric dilution of the soil gas on the fault scarps (Figure 3).
Correlative coefficient (CC) of mean and maximum concentrations of soil gas and vertical displacement of co-seismic rupture at eight sites from three measurements, respectively
CC (Mean concentration)
CC (Maximum concentration)
The distribution of Rn, CO2, and Hg concentrations in soil gas may be correlated primarily with the geological environment of fault rupture (Figure 3 Table 3). The decomposition of organic matter is an important source to soil gas CO2. CO2 in spring water at the Wenchuan Seismostation originated predominately from sedimentary organic matter . These sources of CO2 can mask the information of mantle degassing in some places . A generating mechanism of the Rn concentration anomalies in the co-seismic rupture was possibly enlargements of effective area of grain surface, porosity and radon emanation rates, which resulted from co-seismic cracking of rocks . The soils above the bedrock always contain a certain amount of 238U and 226Ra, which means that there is a potential source of 222Rn in soil gas . In the vapor phase, Hg is readily transported along permeable bedrock structures and through overlying soil cover. Therefore, higher values of Hg concentration occurred near the rupture zones. The background values of free mercury(0Hg) seemed to be more stable and the anomalous zones narrower than those of radon gas in the fault zone .
The concentrations of CO2 were obviously higher in the summer (June 2008, July 2009) than in the winter month (December 2008, Figure 4d). In July 2009, the increase of N2/O2 ratio was consistent with the CO2 concentrations at 8 sampling sites, which indicated that more CO2 was derived from lithosphere. The seasonal variations of CO2 concentrations in soil gas can be attributed to meteorological change, such as temperature, atmospheric pressure and humidity of air and soil . However, the observations most likely reflect changes in microbial activities in response to subsurface temperature variations .
The similar distribution of N2/O2, CO2, and Rn anomalies, combined with the results of factor analysis, indicated the CO2 acted as a "carrier" for Rn (Figure 3). Rn has essentially a shallow origin due to its short half-life. The Rn concentration is never high enough for it to form a gas stream by itself, so a carrier gas is required . In a wide range of geological settings, carrier gases (CO2, CH4 etc.) in the lithosphere may play a dominant role for no-diffusive transport and redistribution of trace gases (Rn, He and H2) toward the Earth's surface. However, some measured sites exhibited higher concentrations of carbon dioxide derived from biogenic sources, but no anomalies of other gases. The distribution of CO2, N2 and O2 in soil in the investigated area, was not matched well with He and H2, indicating He and H2 might migrate upwards by migration. In addition, the distribution of anomalous values of He and H2 matched well with the trace of the fault scarps, which may indicate that the crustal stress field severely affected the He and H2 transport in the fault zone.
4.3. The relationship between the aftershocks and soil gas
The magnitudes of the He and H2 anomalies of three surveys declined significantly with time (Figure 3a and 3b). The higher concentrations of He and H2 in soil gas in the fault zone in June 2008 strongly indicated that the Wenchuan Ms8.0 earthquake excited the release of gases from the fault zone (Figure 4a and 4b). Because crustal stress can accumulate at some part of the fault zone, helium emission can be enhanced. The spatial and temporal variations of helium anomalies, therefore, indicated variation of the stress field in the Longmenshan earthquake zone, as Zhu et al.  reported the intensity of helium emission could be related to the stress. The dramatic decrease in He and H2 concentrations in Jul 2009 may be due to reduction of permeability and porosity of rocks and soils in the rupture zone. Soil-gas He concentrations were higher in July 2009 at the XYD profile at which the co-seismogenic fault changes from reverse type to left-lateral strike-slip type.
The means of CO2, Rn and Hg concentrations were higher in the north parts than in the south parts of the co-seismic rupture (Figure 4d, e and 4f). Most of the large aftershocks were distributed in the north and south parts of the aftershock zone (Figure 1). The direction of the maximum principal stress gradually changed from near EW to near NW-SE along the main fault, and then turned to near EW at the utmost northern part of the main fault . The higher values of radon counts were recorded as the sand column was stressed . At the San Andreas Fault system between Santa Rosa and Cholame, the radon anomaly coincided reasonably well in time and space with larger local earthquakes above a threshold magnitude of about 4.0. These episodic radon changes may be caused by a changing outgassing rate in the fault zones in response to some episodic strain changes . The hydromechanical modeling study of the Matsushiro earthquake swarm shows a clear connection between earthquake rupture, deformation, stress, and permeability changes, as well as large-scale fluid flow related to degassing of CO2 in the shallow seismogenic crust . This extraordinary release of CO2 can cause a flash fluid pressure increase in the fault plane, and therefore, enhance earthquake slip or trigger aftershocks . Kang et al.  found that the spatial features of mercury are correlated not only with the magnitude of earthquakes and distance from the epicenter to the observational site, but also with the stress field and medium between the focus and the observational site. Gu et al.  found that soil-gas Hg in the epicentral area decreased rapidly after the Shunyi 4.5 earthquake in China. The anomalies of CO2, Rn, and Hg concentrations could be related to the variation in the regional stress field and the aftershock activity.
The results obtained from this study led to the following conclusions:
1. The concentrations of He, H2, CO2, Rn, and Hg in the soil gas showed obvious anomalies near the fault scarps.
2. The maximum He and H2 concentrations in Jun 2008 occurred near the parts of the rupture zone where vertical displacements were larger. The distribution of Rn, CO2, and Hg concentrations in soil gas may be correlated with the geological environment of fault rupture and meteorological change.
3. The magnitudes of the He and H2 anomalies of three surveys declined significantly with decreasing strength of the aftershocks with time. The maximum concentrations of He and H2 were found three times at the south part of the rupture zone close to the epicenter. The spatio-temporal variations of CO2, Rn, and Hg concentrations differed obviously between the north and south parts of the fault zone. The anomalies of He, H2, CO2, Rn, and Hg concentrations could be related to the variation in the regional stress field and the aftershock activity.
We are grateful to the Seismological Bureau of Sichuan Province and Prof. Fang Du for help in the field work. We sincerely thank the editor and reviewer for their valuable comments and grammar edits in improving the manuscript. This research was jointly supported by the National Science and Technology Support Program (the characteristics of gas geochemistry of Longmenshan faults, WFSD-10) and the Basic Science Research Plan of the Institute of Earthquake Science, China Earthquake Administration (The fluid geochemical survey of Wenchuan, 02092416).
- Lin A, Ren Z, Jia D, Wu X: Co-seismic thrusting rupture and slip distribution produced by the 2008 Mw 7.9 Wenchuan earthquake, China. Tectonophysics. 2009, 471: 203-215. 10.1016/j.tecto.2009.02.014.View ArticleGoogle Scholar
- Huang Y, Wu J, Zhang T, Zhang D: Relocation of the M8.0 Wenchuan earthquake and its aftershock sequence. Science in China (Series D). 2008, 51 (12): 1703-1711. 10.1007/s11430-008-0135-z.View ArticleGoogle Scholar
- Reimer GM: Prediction of Central California earthquakes from soil-gas helium fluctuations. Pageoph. 1984, 122: 369-375. 10.1007/BF00874605.View ArticleGoogle Scholar
- Weinlich FH, Faber E, Boušková A, Horálek J, Teschner M, Poggenburg J: Seismically induced variations in Mariánské Láznĕ fault gas composition in the NW Bohemian swarm quake region, Czech Republic-A continuous gas monitoring. Tectonophysics. 2006, 421 (1-2): 89-110. 10.1016/j.tecto.2006.04.012.View ArticleGoogle Scholar
- King CY, King BS, Evans WC, Zhang W: Spatial radon anomalies on active faults in California. Applied Geochemistry. 1996, 11: 497-510. 10.1016/0883-2927(96)00003-0.View ArticleGoogle Scholar
- Amponsah P, Banoeng-Yakubo B, Andam A, Asiedu D: Soil radon concentration along fault systems in parts of south eastern Ghana. Journal of African Earth Sciences. 2008, 51: 39-48. 10.1016/j.jafrearsci.2007.11.004.View ArticleGoogle Scholar
- Walia V, Yang TF, Hong WL, Lin SJ, Fu CC, Wen KL, Chen CH: Geochemical variation of soil-gas composition for fault trace and earthquake precursory studies along the Hsincheng fault in NW Taiwan. Applied Radiation and Isotopes. 2009, 67: 1855-1863. 10.1016/j.apradiso.2009.07.004.View ArticleGoogle Scholar
- Wakita H, Nakamura Y, Kita I, Fujii N, Notsu K: Hydrogen release: new Indicator of fault activity. Science. 1980, 210: 188-190. 10.1126/science.210.4466.188.View ArticleGoogle Scholar
- Toutain JP, Baubron JC: Gas geochemistry and seismotectonics: a review. Tectonophysics. 1999, 304: 1-27. 10.1016/S0040-1951(98)00295-9.View ArticleGoogle Scholar
- Burchfiel BC, Chen Z, Liu Y, Royden LH: Tectonics of the Longmen Shan and Adjacent regions, central China. International Geology Review. 1995, 37: 661-735. 10.1080/00206819509465424.View ArticleGoogle Scholar
- Tang R, Han W: Earthquake and active fault in Sichuan. 1993, Seismological Press, Beijing, 7-272.Google Scholar
- Zhou X, Guo W, Du J, Wang C, Liu L: The geochemical characteristics of radon and mercury in the soil gas of buried faults in the Hohhot district. Earthquake. 2007, 27 (1): 70-76. (in Chinese with English abstract)Google Scholar
- Burton M, Neri M, Condarelli D: High spatial resolution radon measurements reveal hidden active faults on Mt. Etna. Geophysical Research Letters. 2004, 31: L07618-7627. 10.1029/2003GL019181.View ArticleGoogle Scholar
- Ciotoli G, Lombardi S, Annunziatellis A: Geostatistical analysis of soil gas data in a high seismic intermontane basin: Fucino Plain, central Italy. Journal of Geophysical Research. 2007, 112: 23-10.1029/2005JB004044. B05407View ArticleGoogle Scholar
- Novelli PC, Lang PM, Masarie KA, Hurst DF, Myers R, Elkins JW: Molecular hydrogen in the troposphere: Global distribution and budget. Journal of Geophysical Research. 1999, 104 (D23): 30427-30444. 10.1029/1999JD900788.View ArticleGoogle Scholar
- Sinclair AJ: A fundamental approach to threshold estimation in exploration geochemistry: Probability plots revisited. Journal of Geochemical Exploration. 1991, 41: 1-22. 10.1016/0375-6742(91)90071-2.View ArticleGoogle Scholar
- Etiope G, Martinelli G: Migration of carrier and trace gases in the geosphere: An overview. Physics of the Earth and Planetary Interiors. 2002, 129: 185-204. 10.1016/S0031-9201(01)00292-8.View ArticleGoogle Scholar
- Du J, Cheng W, Zhang Y, Jie C, Guan Z, Liu W, Bai L: Helium and carbon isotopic compositions of thermal springs in the earthquake zone of Sichuan, Southwestern China. Journal of Asian Earth Sciences. 2006, 26: 533-539. 10.1016/j.jseaes.2004.11.006.View ArticleGoogle Scholar
- Kameda J, Saruwatari K, Tanaka H, Tsunomori F: Mechanisms of hydrogen generation during the mechanochemical treatment of biotite within D2O media. Earth Planets Space. 2004, 56: 1241-1245.View ArticleGoogle Scholar
- Dogan T, Mori T, Tsunomori F, Notsu K: Soil H2 and CO2 surveys at several active faults in Japan. Pure and Applied Geophysics. 2007, 12 (164): 2449-2463. 10.1007/s00024-007-0277-5.View ArticleGoogle Scholar
- Wang Z, Fukao Y, Pei S: Structural control of rupturing of the Mw 7.9 2008 Wenchuan Earthquake, China. Earth and Planetary Science Letters. 2009, 279 (1-2): 131-138. 10.1016/j.epsl.2008.12.038.View ArticleGoogle Scholar
- Holub RF, Brady BT: The effect of stress on radon emanation from rock. Journal of Geophysical Research. 1981, 86 (B3): 1776-1784. 10.1029/JB086iB03p01776.View ArticleGoogle Scholar
- Jönsson G, Baixeras C, Devantier R, Enge W, Font L, Freyer K, Ghose R, Treutler HC: Soil radon levels measured with SSNTD's and the soil radium content. Radiation Measurements. 1999, 31 (1-6): 291-294.View ArticleGoogle Scholar
- Wang G, Liu C, Wang J, Liu W, Zhang P: The use of soil mercury and radon gas surveys to assist the detection of concealed faults in Fuzhou City, China. Environmental Geology. 2006, 51: 83-90. 10.1007/s00254-006-0306-1.View ArticleGoogle Scholar
- Hinkle M: Environmental conditions affecting concentrations of He, CO2, O2 and N2 in soil gases. Applied Geochemistry. 1994, 9: 53-63. 10.1016/0883-2927(94)90052-3.View ArticleGoogle Scholar
- Deyo BG, Robbins GA, Binkhors GK: Use of portable oxygen and carbon dioxide detectors to screen soil gas for subsurface gasoline contamination. Ground Water. 1993, 31 (4): 598-604. 10.1111/j.1745-6584.1993.tb00593.x.View ArticleGoogle Scholar
- King C, Zhang W, Zhang Z: Earthquake-induced Groundwater and Gas Changes. Pure and Applied Geophysics. 2006, 163 (4): 633-645. 10.1007/s00024-006-0049-7.View ArticleGoogle Scholar
- Zhu M, Zhou R, Yin D, Gao Y, Zhang F: Stress emission of helium and argon in coal seams. Science in China (Series D). 2003, 46 (6): 547-560. 10.1360/03yd9048.View ArticleGoogle Scholar
- Wang QC, Chen ZL, Zheng SH: Spatial segmentation characteristic of focal mechanism of aftershock sequence of Wenchuan Earthquake. Chinese Science Bulletin. 2009, 54: 2263-2270. 10.1007/s11434-009-0367-0.View ArticleGoogle Scholar
- Chyi LL, Quick TJ, Yang TF, Chen CH: Soil gas radon spectra and earthquakes. Terrestrial Atmospheric and Oceanic Sciences. 2005, 16: 763-774.Google Scholar
- King CY: Episodic Radon changes in subsurface soil gas along active faults and possible relation to earthquakes. Journal of Geophysical Research. 1980, 85 (B6): 3065-3078.0. 10.1029/JB085iB06p03065.View ArticleGoogle Scholar
- Cappa F, Rutqvist J, Yamamoto K: Modeling crustal deformation and rupture processes related to upwelling of deep CO2 rich fluids during the 1965-1967 Matsushiro Earthquake Swarm in Japan. LBNL-2308E. Journal of Geophysical Research. 2009, 114: B10304-10.1029/2009JB006398.View ArticleGoogle Scholar
- Famin V, Nakashima S, Boullier A, Fujimoto K, Hirono T: Earthquakes produce carbon dioxide in crustal faults. Earth and Planetary Science Letters. 2008, 265 (3-4): 487-497. 10.1016/j.epsl.2007.10.041.View ArticleGoogle Scholar
- Kang C, Du J, Li S: Anomaly characteristics of mercury associated with moderately strong earthquake. Earthquake. 1999, 19 (4): 352-358. (in Chinese with English abstract)Google Scholar
- Gu Y, Lin Y, Zhang P: Application of gas geochemical method to prediction of seismic trend after mainshock. Earthquake. 2001, 21 (2): 101-104. (in Chinese with English abstract)Google Scholar
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