Skip to main content
Log in

Vulnerability of headwater catchment resources to incidences of 210Pb excess and 137Cs radionuclide fallout

  • Original Article
  • Published:
Environmental Geology

Abstract

Recent identification of elevated excess 210Pb (≤302.6 mBq L−1) and 137Cs (≤111.3 mBq L−1) activity in drinking water wells up to 20 m depth indicates some transport of airborne radionuclide fallout beyond soils in the Shaker Village catchment, Maine. Estimated airborne mass loading 210Pbex fluxes of about 0.9 mBq m−3, canvass this headwater catchment and may be sufficient to pose risks to unprotected shallow wells. Inventories of 210Pbex and 137Cs in pond sediments indicate maximum median activities of 943 mBq g−1 and 40.0 mBq g−1, respectively. Calculated 210Pbex fluxes in the catchment soils range from 0.62–0.78 Bq cm−2 year−1 and yield a mean residence time of near 140 years. Measured 137Cs activity up to 51.1 mBq g−1 occurs in sediments at least to 5 m depth. Assumed particle transport in groundwater with apparent 85Kr ages less than 5 years BP (2005) may explain the correlation between these particle-reactive radionuclides and elevated activity in some drinking water wells.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11

Similar content being viewed by others

References

  • Appleby PG, Nolan PJ, Gifford DW, Godfrey MJ, Oldfield F, Anderson NJ, Battarbee RW (1986) 210Pb dating by low gamma background counting. Hydrobiologia 141:21–27

    Article  Google Scholar 

  • Appleby PG, Oldfield F (1992) Application of lead-210 to sedimentation studies. In: Ivanovich M, Harmon RS (eds) Uranium-series Disequilibrium. Clarendon Press, Oxford, pp 731–778

    Google Scholar 

  • Beven K, Germann P (1982) Macropores and water flow in soil. Water Resour Res 18:1311–1325

    Article  Google Scholar 

  • Campbell BL, Loughran RJ, Elliot GL (1982) Cesium-137 as an indicator of geomorphic processes in a drainage basin. J Aust Geogr Stud 20:1–49

    Google Scholar 

  • Cember H (1992) Introduction to health physics. McGraw Hill, New York

    Google Scholar 

  • Chesser K, Rodgers BE, Wickliffe JK, Gaschak S, Chizhevsky I, Phillips CJ, Baker RJ (2001) Accumulation of 137cesium and 90strontium from abiotic and biotic sources in rodents at Chernobyl, Ukraine. Environ Toxic Chem 20:1927–1935

    Article  Google Scholar 

  • Doering C, Akber R, Heijnis H (2006) Vertical distributions of 210Pb excess, 7Be and 137Cs in selected grass covered soils in Southeast Queensland, Australia. J Environ Radioact 87:135–147

    Article  Google Scholar 

  • Domenico PA, Schwartz FW (1990) Physical and chemical hydrogeology. Wiley, New York

    Google Scholar 

  • Easthouse KB, Mulder J, Christophersen N, Seip HM (1992) Dissolved organic carbon fractions in soil and stream water during variable hydrological conditions at Birkenes, southern Norway. Water Resour Res 28:1585–1596

    Article  Google Scholar 

  • Fisenne IM (1994) Lead-210 in animal and human bone: a new analytical method. Environ Int 20:627–632

    Article  Google Scholar 

  • Hess CT, Weiffenbach CV, Norton SA (1983) Environmental radon and cancer correlations in Maine. Health Phys 45:339–348

    Article  Google Scholar 

  • Ho EC, Measday DF (2005) A simple model for describing the concentration of 212Pb in the atmosphere. J Environ Radioact 78:289–309

    Article  Google Scholar 

  • Holtzman RB (1963) Lead-210 (RaD) and polonium-210 (RaF) in potable waters in Illinois. In: Adams JS, Lowder WM (eds) The natural radiation environment. University of Chicago Press, Chicago, pp 227–237

    Google Scholar 

  • Hussey AM (1988) Lithotectonic stratigraphy, deformation, plutonism, and metamorphism, greater Casco Bay Region, Southeastern Maine. In: Marvinney R (ed) Studies in maine geology, v 1. Maine Geologic Survey, Augusta, pp 17–34

    Google Scholar 

  • Jaworowski Z (1969) Radioactive lead in the environment and in the human body. Atomic Energy Rev 7:3–45

    Google Scholar 

  • Klanminder J, Binder R, Emteryd O, Appleby PG, Grip H (2006) Estimating the mean residence time of lead in the organic horizon of boreal soils using 210-lead, stable lead and a soil chronosequence. Biogeochem 78:31–49

    Article  Google Scholar 

  • Koterba MT, Wilde FD, Lapham WW (1996) Updates to ground-water data-collection protocols and procedures for the national water-quality assessment program: collection and documentation of water-quality samples and related data. US Geological Survey Open-File Report 95–399

  • Krishnaswami S, Lal D, Martin JM, Meybeck M (1971) Geochronology of lake sediments. Earth Planet Sci Lett 11:407–414

    Article  Google Scholar 

  • Kung KJ (1990) Preferential flow in a sandy vadose zone: 2 Mechanism and implications. Geoderma 46:59–71

    Article  Google Scholar 

  • Malcolm RL (1985) Geochemistry of stream fulvic and humic substances. In: Aiken GR (ed) Humic substances in soil, sediment, and water. Wiley-Interscience, New York, pp 181–209

    Google Scholar 

  • Marcazzan GM, Caprioli E, Valli G, Veechi R (2003) Temporal variation of 212Pb concentration in outdoor air of Milan and comparison with 214Bi. J Environ Radioact 65:77–90

    Article  Google Scholar 

  • Mayer LM, Schick LL, Hardy KR, Wagal R, McCarthy J (2004) Organic matter in small mesopores in sediments and soils. Geochim Cosmochim Acta 68:3863–3872

    Article  Google Scholar 

  • McDowell IM, Hunt JR, Sitar N (1986) Particle transport through porous media. Water Resour Res 22:1901–1921

    Article  Google Scholar 

  • Moore WS (1984) Radium isotope measurements using germanium detectors. Nucl Instr Meth Phys Res 223:407–411

    Article  Google Scholar 

  • Murray AS, Marten R, Johnston A, Martin P (2005) Analysis for naturally occurring radionuclides in environmental concentrations by gamma spectrometry. J Radioanal Nucl Chem 115:263–288

    Google Scholar 

  • National Weather Service (2005) Annual meteorological data, Gray Station, Maine. http://www.weather.gov/view/national

  • Orton GJ, Reading HG (1993) Variability of deltaic processes in terms of sediment supply, with particular emphasis on grain size. Sedimentology 40:475–512

    Article  Google Scholar 

  • Porstendorfer J, Zock C, Reineking A (2000) Aerosol size distribution of radon progeny in outdoor air. J Environ Radioact 51:37–48

    Article  Google Scholar 

  • Ritchie JC, McHenry JR (1990) Application of radioactive fallout cesium-137 for measuring erosion and sediment accumulation rates and patterns: a review. J EnvironQual 19:215–233

    Google Scholar 

  • Robbins JA (1978) Geochemical and geophysical applications of radioactive lead. In: Nriagu JO (ed) Biogeochemistry of lead in the environment. Elsevier, Amsterdam, pp 285–393

    Google Scholar 

  • Robbins JA (ed) (1984) Geochronology of recent deposits. Chem Geol 44:1–348

    Google Scholar 

  • Robbins JA, Eadie BJ (1991) Seasonal cycling of trace elements 137Cs, 7Be, 239 + 240Pu in Lake Michigan. J Geophys Res 96:17081–17104

    Article  Google Scholar 

  • Salers JE, Hornberger GN (1996) The role of colloidal kaolinite in the transport of cesium through laboratory sand columns. Water Resourc Res 32:33–41

    Article  Google Scholar 

  • Shanklin DE, Sidle WC, Ferguson ME (1995) Micro-purge low flow sampling of uranium-contaminated ground water at the Fernald Environmental Management Project. Ground Water Monitor Rev Summer 15:168–176

    Article  Google Scholar 

  • Sheets RW, Lawrence AE (1999) Temporal dynamics of airborne lead-210 in Missouri (USA): implications for geochronological methods. Environ Geol 38:343–348

    Article  Google Scholar 

  • Sidle WC (2006) Apparent 85Kr ages of groundwater within the Royal watershed, Maine, USA. J Environ Radioact 91:113–127

    Article  Google Scholar 

  • Sidle WC, Li P (2007) Submersible pump impacts on Pb constituents in residential wells. Environ Geochem Health. doi:10.1007/s10653-007-9090-4

  • Smith BM, Grune WN, Higgins FB, Terrill JG (1961) Natural radioactivity in ground water supplies in Maine and New Hampshire. J Amer Water Works Assoc 53:75–88

    Google Scholar 

  • Smith GW, Hunter LE (1989) Late Wisconsinan deglaciation of coastal Maine. In: Marvinney R (ed) Studies in Maine Geology, v 6. Maine Geologic Survey, Augusta, pp 13–32

    Google Scholar 

  • Tessier A, Campbell PC, Bisson M (1979) Evaluation of the APDC-MIBK extraction method for the atomic absorption analysis of trace metals in river water. Int J Environ Anal Chem 7:41–54

    Article  Google Scholar 

  • Turekian KK, Benninger LK, Dion ED (1983) Be-7 and Pb-210 total deposition fluxes at New Haven, Connecticut and at Bermuda. J Geophys Res 88:5411–5415

    Article  Google Scholar 

  • USEPA (2005) United States Environmental Protection Agency, National Primary Drinking Water Regulations. http://www.epa.gov/safewater/standards/standards.html

  • Veechi R, Marcazzan G, Valli G (2005) Seasonal variation of 210Pb activity concentration in outdoor air of Milan (Italy). J Environ Radioact 82:251–266

    Article  Google Scholar 

  • Wahlgren MA, Nelson DM, Chase EM (1978) Sediment trap methodology. US Department of Energy, Radiological and Environmental Research Division, Rept ANL-78-65, Part III Argonne National Laboratory, pp 77–79

  • Weddle TK (1997) Surficial geology of the Gray 7.5-minute quadrangle, Androscoggin and Cumberland counties, Maine. Maine Geologic Survey, OF Report 97-73, 1-10, with plate OF-97–58

  • Williams JS, Tepper DH, Tolman AL, Thompson WB (1987) Hydrogeology and Water Quality of Significant sand and Gravel Aquifers in Parts of Androscoggin, Cumberland, Cumberland, Oxford, and York Counties, Maine. Maine Geologic Survey OF Report 87-1a

  • Zapecza OS, Szabo Z (1986) Natural radioactivity in groundwater-a review. In Moody DW, Carr J, Chase EB, Paulsen RW (eds) National Water Summary-1986. US Geological Survey Water Supply Pap 2325

Download references

Acknowledgments

Without the full and gracious cooperation of homeowners and businesses in the region, this research would not be possible. Special thanks are given to the field crews through the years to complete an uninterrupted sampling record through all seasons. The cooperation of Maine Public Health is appreciated. Thanks to the USEPA Isotope Hydrology Laboratory (Cincinnati); D. Andrews, Dartmouth College; B. Craig, Oak Ridge National Laboratory; and R. Kolmar, Groundwater Research, Oxford, Ohio. Any opinions expressed in this paper are those of the author and do not, necessarily, reflect the official positions and policies of the USEPA. Any mention of products or trade names does not constitute recommendation by the USEPA.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to William Sidle.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Sidle, W. Vulnerability of headwater catchment resources to incidences of 210Pb excess and 137Cs radionuclide fallout. Environ Geol 57, 377–388 (2009). https://doi.org/10.1007/s00254-008-1306-0

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00254-008-1306-0

Keywords

Navigation