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Geochemical characteristics of the mud volcano fluids in southwestern Taiwan and their possible linkage to elevated arsenic concentration in Chianan plain groundwater

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Abstract

Fluid and mud samples were collected from Wushanting (WST), Hsiaokunshui (HKS), Yenshuikeng (YSK), Kuantzeling (KZL), and Kunshuiping (KSP) mud volcanoes of southwestern Taiwan. Concentrations of major ions and trace elements in mud volcanic fluids were analyzed to find the possible linkage to elevated arsenic (As) concentrations in the Chianan plain groundwater. The elevated Na+, K+, and Cl concentrations indicated possible marine origin of the fluids. The trace element concentrations in the mud volcanic fluids were generally low, but the As concentrations were up to 0.12 mg/L. High contents of As, Fe, and Mn were observed in the mud samples. Saturation index calculations indicated that both carbonate and oxide minerals acted as potential sinks for As in the mud volcanic fluids. Arsenic in the dewatering fluids and muds may be transported by the subsurface flow and surface streams as suspended solids and eventually deposited in the Chianan plain aquifers. Under reducing conditions, As may be released from the host minerals (such as Fe- and Mn-oxides/hydroxides), thereby causing widespread groundwater As pollution.

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References

  • Alain K, Thomas H, Florin M, Marcus E, Tina T, Martin K (2006) Microbiological investigation of methane- and hydrocarbon-discharging mud volcanoes in the Carpathian Mountains, Romania. Environ Microbiol 8:574–590

    Article  Google Scholar 

  • Bethke CM (1996) Geochemical reaction modeling. Oxford University Press, New York

    Google Scholar 

  • Brown K (1990) The nature and hydrogeologic significance of mud diapirs and diatremes for accretionary systems. J Geophys Res 95:8969–8982

    Article  Google Scholar 

  • Carson B, Screaton EJ (1998) Fluid flow in accretionary prisms: evidence for focused, time-variable discharge. Rev Geophys 36:329–351

    Article  Google Scholar 

  • Chang CP, Angelier J, Huang CY (2000) Origin and evolution of a melange: the active plate boundary and suture zone of the Longitudinal Valley, Taiwan. Tectonophys 325:43–62

    Article  Google Scholar 

  • Craig H (1966) Isotopic composition and origin of the Red Sea and Salton Sea geothermal brines. Science 154:1544–1548

    Article  Google Scholar 

  • Dia AN, Castrec M, Boulègue J, Comeau P (1999) Trinidad mud volcanoes: where do the expelled fluids come from? Geochim Cosmochim Acta 63:1023–1038

    Article  Google Scholar 

  • Dimitrov LI (2002) Mud volcanoes—the most important pathway for degassing deeply buried sediments. Earth Sci Rev 59:49–76

    Article  Google Scholar 

  • Drever JI (1988) The Geochemistry of Natural Waters, 2nd ed. Prentice Hall, Englewood Cliffs

    Google Scholar 

  • Duchi V, Minissale A, Vaselli O, Ancillotti M (1995) Hydrogeochemistry of the Campania Region in Southern Italy. J Volcanol Geoth Res 67:313–328

    Article  Google Scholar 

  • Gieskes JM, You CF, Lee T, Yui TF, Chen HW (1992) Hydrogeochemistry of mud volcanoes in Taiwan. Acta Geol Taiwan 30:79–88

    Google Scholar 

  • Klute A (1986) Method of soil analysis, part 1: physical and mineralogical methods. American Society of Agronomy, Madison, Wisconsin

    Google Scholar 

  • Kohl B, Roberts HH (1994) Fossil foraminifera from four active mud volcanoes in the Gulf of Mexico. Geo Mar Lett 14:126–134

    Article  Google Scholar 

  • Kopf AJ (2002) Significance of mud volcanism. Rev Geophys 40:1005

    Article  Google Scholar 

  • Li YH (1976) Denudation of Taiwan island since Pliocene epoch. Geology 4:105–107

    Article  Google Scholar 

  • Liu C-C, Jean J-S, Nath B, Lee M-K, Hor L-I, Lin K-H, Maity JP (2009) Geochemical characteristics of the fluids and muds from two southern Taiwan mud volcanoes: Implications for water–sediment interaction and groundwater arsenic enrichment. Appl Geochem 24:1793–1802

    Article  Google Scholar 

  • Liu C-C, Maity JP, Jean J-S, Sracek O, Kar S, Li Z, Bundschuh J (2011) Biogeochemical interactions amoung the arsenic, iron, humic substance, and bacterial activity in mud volcano in southern Taiwan. J Environ Sci Health Part A (accepted for publication)

  • Martin JB, Kastner M, Egeberg PK (1995) Origins of saline fluids at convergent margins. In: Taylor B, Natland J (eds) Active margins and marginal basins of the western pacific, vol 88. AGU Geophysical Monograph Series, Washington, pp 219–239

    Chapter  Google Scholar 

  • Milkov AV (2000) Worldwide distribution of submarine mud volcanoes and associated gas hydrates. Mar Geol 167:29–42

    Article  Google Scholar 

  • Minissale A, Magro G, Martinelli G, Vaselli O, Tassi GF (2000) Fluid geochemical transect in the Northern Apennines (central-northern Italy): fluid genesis and migration and tectonic implications. Tectonophys 319:199–222

    Article  Google Scholar 

  • Nath B, Jean J-S, Lee M-K, Yang H-J, Liu C-C (2008) Geochemistry of high arsenic groundwater in Chia-Nan plain, Southwestern Taiwan: possible sources and reactive transport of arsenic. J Contam Hydrol 99:85–96

    Article  Google Scholar 

  • Parkhurst DL, Appelo CAJ (1999) User’s guide to PhreeqC (Version 2)—a computer program for speciation, batch-reaction, one-dimensional transport, and inverse geochemical calculations. Water-Resources Investigations Report US Geological Survey, Denver, Colorado, pp 99–4259

  • Plank T, Langmuir CH (1998) The chemical composition of subducting sediment and its consequences for the crust and mantle. Chem Geol 145:325–394

    Article  Google Scholar 

  • Planke S, Svensen H, Hovland M, Banks DA, Jamtveit B (2003) Mud and fluid migration in active mud volcanoes in Azerbaijan. Geo Mar Lett 23:258–268

    Article  Google Scholar 

  • Porowski A (2006) Origin of mineralized waters in the Central Carpathian Synclinorium, SE Poland. Studia Geologica Polonica 125:67

    Google Scholar 

  • Reza AHMS, Jean J-S, Yang H-J, Lee M-K, Hsu H-F, Liu C-C, Lee Y-C, Bundschuh J, Lin K-H, Lee C-Y (2011) A comparative study on arsenic and humic substances in alluvial aquifers of Bengal delta plain (NW Bangladesh), Chianan plain (SW Taiwan) and Lanyang plain (NE Taiwan) implication of arsenic mobilization mechanisms. Environ Geochem Health 33:235–258

    Article  Google Scholar 

  • Różański K, Aragus-Aguas L, Gonfiantini R (1993) Isotopic patterns in modern global precipitation. In: Stewart PK, Lohmann KC, McKenzie J, Savin S (eds) Climate Change in Continental Isotopic Records, vol 76. AGU Geophysical Monograph Series, Washington, pp 1–36

    Google Scholar 

  • Sheppard SMF (1986) Characterization and isotopic variations in natural waters. In: Valley JW, Taylor HP Jr, O’Neil JR (eds) Stable isotopes in high temperature geological processes, Rev Mineral Geochem 16:165–183

  • Smedley PL, Kinniburgh DG (2002) A review of the source, behavior and distribution of arsenic in natural waters. Appl Geochem 17:517–568

    Article  Google Scholar 

  • Suppe J (1980) Imbricated structure of western foothills belt, south central Taiwan. Petrol Geol Taiwan 30:163–176

    Google Scholar 

  • Teng L-S (1990) Geotectonic evolution of Late Cenozoic arc-continent collision in Taiwan. Tectonophys 183:57–76

    Article  Google Scholar 

  • Vogt PR, Gardner J, Crane K (1999) The Norwegian–Barents–Svalbard (NBS) continental margin: introducing a natural laboratory of mass wasting, hydrates and ascent of sediment pore water and methane. Geo Mar Lett 19:2–21

    Article  Google Scholar 

  • Wang C-H, Kuo C-H, Peng T-R, Chen W-F, Liu T-K, Chiang C-J, Liu W-C, Hung J-J (2001) Isotope characteristics of Taiwan Groundwaters. West Pac Earth Sci 1:415–428

    Google Scholar 

  • Wu C-M (1978) Characteristics of groundwater geology in the blackfoot disease endemic area. The Blackfoot Disease Prevention and Control Research Group of Taiwan, Provincial Health Department, Blackfoot Disease Research Report 5:1–24

  • Yakimov MM, Giuliano L, Crisafi E, Chernikova TN, Timmis KN, Golyshin PN (2002) Microbial community of a saline mud volcano at San Biagio-Belpasso, Mt. Etna (Italy). Environ Microbiol 4:249–256

    Article  Google Scholar 

  • Yang T-F, Yeh G-H, Fu C-C, Wang C-C, Lan T-F, Lee H-F, Chen C-H, Walia V, Sung Q-C (2004) Composition and exhalation flux of gases from mud volcanoes in Taiwan. Environ Geol 46:1003–1011

    Article  Google Scholar 

  • Yeh G-H (2003) Geochemistry and sources of mud-volcano fluids in Taiwan. MS dissertation, Institute of Oceanography, National Taiwan University, Taipei, Taiwan

  • Yeh G-H, Yang T-F, Chen J-C, Chen Y-G, Song, S-R (2005) Fluid geochemistry of mud volcanoes in Taiwan. In: Martinelli G, and Panahi B (eds) Mud volcanoes, Geodynamics and seismicity. NATO science series: IV. Earth Environ Sci 51:227–237

  • Yeh G-H, You C-F, Chen J-C, Yang T-F, Chen Y-G, Song S-R (2002) Fluid geochemistry of mud volcanoes at the accretionary prism in southern Taiwan. Goldschmidt Conference, Davos, Cambridge Publications, Cambridge, A862

  • You C-F, Gieskes JM, Lee T, Yui T-F, Chen H-W (2004) Geochemistry of mud volcano fluids in the Taiwan accretionary prism. Appl Geochem 19:695–707

    Article  Google Scholar 

  • Zuber A, Chowaniec J (2009) Diagenetic and other highly mineralized waters in the Polish Carpathians. Appl Geochem 24:1889–1900

    Article  Google Scholar 

Download references

Acknowledgments

The authors wish to thank National Science Council of Taiwan for partial financial support (NSC98-2627-M-006-004). Mr. Jiann-Hong Liu’s help in field work is gratefully acknowledged. We also thank anonymous reviewer for constructive comments to improve this manuscript.

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Correspondence to Jiin-Shuh Jean.

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Liu, CC., Maity, J.P., Jean, JS. et al. Geochemical characteristics of the mud volcano fluids in southwestern Taiwan and their possible linkage to elevated arsenic concentration in Chianan plain groundwater. Environ Earth Sci 66, 1513–1523 (2012). https://doi.org/10.1007/s12665-011-1391-3

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