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Dynamics of oxidized and reduced iron in a northern hardwood forest

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Abstract

Iron (Fe) is ubiquitous in forest ecosystems and its cycle is thought to influence the development of soil, particularly Spodosols (podsolization), and the biogeochemistry of macronutrients such as carbon (C), nitrogen (N), and phosphorus (P), as well as many trace metals. The cycle of Fe in northern hardwood forests remains poorly understood. To address some of these uncertainties, we constructed a biogeochemical budget of Fe for a small catchment at the Hubbard Brook Experimental Forest in the White Mountains of New Hampshire, USA. Horizonal, temporal, and elevational patterns of concentrations and fluxes of oxidized and reduced Fe species were assessed in leaf litter, soil, soil solution, and stream water. The chemistry of dissolved Fe was evaluated in the context of its relationship with dissolved organic carbon, pH, and dissolved oxygen. Soil solution fluxes of Fe were highest in the organic (Oa, 52.5 mol ha−1 year−1) horizon and decreased with depth in the mineral (Bh, 50.5 mol ha−1 year−1, and Bs, 19.7 mol ha−1 year−1) horizons, consistent with podsolization theories predicting immobilization of Fe following downward transport to mineral soils. The export of Fe in stream water (1.8 mol ha−1 year−1) was lower than precipitation input (3.5 mol ha−1 year−1). The low stream flux indicates most Fe in drainage waters was immobilized in the soil and retained in the watershed. The portion of total Fe as Fe(II) was ~10–60% in soil solutions, seemingly high for soils that are considered to be well-drained, oxidizing environments. Organic complexes likely stabilized Fe(II) in solution under oxidizing conditions that would otherwise promote considerably higher Fe(III)-to-Fe(II) ratios. Our study indicates that there are organic matter-derived sources of dissolved Fe(II) as well as substantial mobilization of Fe(II), possibly the result of the reduction of Fe-bearing soil minerals.

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References

  • Aber JD, Federer CA (1992) A generalized, lumped-parameter model of photosynthesis, evapotranspiration, and net primary production in temperate and boreal forest ecosystems. Oecologia 92:463–474

    Article  Google Scholar 

  • Bloomfield C (1953) A study of podsolization. Part I. The mobilization of iron and aluminum by Scots Pine needles. J Soil Sci 4:5–23

    Article  Google Scholar 

  • Boudot JP, Brahim ABH, Steiman R, Seiglemurandi F (1989) Biodegradation of synthetic organo-metallic complexes of iron and aluminum with selected metal to carbon ratios. Soil Biol Biochem 21(7):961–966

    Article  Google Scholar 

  • Buerge IJ, Hug SJ (1998) Influence of organic ligands on chromium(VI) reduction by iron(II). Environ Sci Technol 32(14):2092–2099

    Article  Google Scholar 

  • Buol SW, Southard RJ, Graham RC, McDaniel PA (2003) Soil genesis and classification. Iowa State Press, Ames, IA

    Google Scholar 

  • Campbell JL, Hornbeck JW, McDowell WH, Buso DC, Shanley JB, Likens GE (2000) Dissolved organic nitrogen budgets for upland, forested ecosystems in New England. Biogeochemistry 49(2):123–142

    Article  Google Scholar 

  • Chacon N, Silver WL, Dubinsky EA, Cusack DF (2006) Iron reduction and soil phosphorus solubilization in humid tropical forests soils: the roles of labile carbon pools and an electron shuttle compound. Biogeochemistry 78(1):67–84

    Article  Google Scholar 

  • Chaney RF, Brown JC, Tiffin LO (1972) Obligatory reduction of ferric chelates in iron uptake by soybeans. Plant Physiol 50:208–213

    Article  Google Scholar 

  • Chen J, Gu BH, Royer RA, Burgos WD (2003) The roles of natural organic matter in chemical and microbial reduction of ferric iron. Sci Total Environ 307(1–3):167–178

    Article  Google Scholar 

  • Chorover J, Amistadi MK (2001) Reaction of forest floor organic matter goethite, birnessite and smectite surfaces. Geochim Cosmochim Acta 65(1):95–109

    Article  Google Scholar 

  • Clesceri LS, Greenberg AE, Eaton AD (eds) (1998) Standard methods for the examination of water and wastewater. American Public Health Association, Washington, D.C

    Google Scholar 

  • Dahlgren RA, Ugolini FC (1989) Aluminum fractionation of soil solutions from unperturbed and tephra-treated Spodosols, Cascade Range, Washington, USA. Soil Sci Soc Am J 53(2):559–566

    Article  Google Scholar 

  • Davidson EA, Chorover J, Dail DB (2003) A mechanism of abiotic immobilization of nitrate in forest ecosystems: the ferrous wheel hypothesis. Glob Change Biol 9(2):228–236

    Article  Google Scholar 

  • De Coninck F (1980) Major mechanisms in the formation of spodic horizons. Geoderma 24:101–128

    Article  Google Scholar 

  • Dittman JA, Driscoll CT, Groffman PM, Fahey TJ (2007) Dynamics of nitrogen and dissolved organic carbon at the Hubbard Brook Experimental Forest. Ecology 88(5):1153–1166

    Article  Google Scholar 

  • Driscoll CT, Fuller RD, Simone DM (1988a) Longitudinal variations in trace-metal concentrations in a northern forested ecosystem. J Environ Qual 17(1):101–107

    Article  Google Scholar 

  • Driscoll CT, Johnson NM, Likens GE, Feller MC (1988b) Effects of acidic deposition on the chemistry of headwater streams––a comparison between Hubbard Brook, New Hampshire, and Jamieson creek, British Columbia. Water Resour Res 24(2):195–200

    Article  Google Scholar 

  • Drobner E, Huber H, Wachtershauser G, Rose D, Stetter KO (1990) Pyrite formation linked with hydrogen evolution under anaerobic conditions. Nature 346(6286):742–744

    Article  Google Scholar 

  • Fahey TJ, Siccama TG, Driscoll CT, Likens GE, Campbell J, Johnson CE, Battles JJ, Aber JD, Cole JJ, Fisk MC, Groffman PM, Hamburg SP, Holmes RT, Schwarz PA, Yanai RD (2005) The biogeochemistry of carbon at Hubbard Brook. Biogeochemistry 75(1):109–176

    Article  Google Scholar 

  • Federer CA, Hornbeck JW, Tritton LM, Martin CW, Pierce RS, Smith CT (1989) Long-term depletion of calcium and other nutrients in eastern United States forests. Environ Manage 13(5):593–601

    Article  Google Scholar 

  • Fimmen RL, Richter DD, Vasudevan D, Williams MA, West LT (2008) Rhizogenic Fe-C redox cycling: a hypothetical biogeochemical mechanism that drives crustal weathering in upland soils. Biogeochemistry 87(2):127–141

    Article  Google Scholar 

  • Fuller RD, David MB, Driscoll CT (1985) Sulfate adsorption relationships in forested Spodosols of the northeastern USA. Soil Sci Soc Am J 49(4):1034–1040

    Article  Google Scholar 

  • Gosz JR, Likens GE, Bormann FH (1972) Nutrient content of litterfall on the Hubbard Brook Experimental. Ecology 53:769–784

    Article  Google Scholar 

  • Gosz JR, Likens GE, Bormann FH (1976) Organic matter and nutrient dynamics of the forest and forest floor in the Hubbard Brook Forest, New Hampshire. Oecologia 22:305–320

    Article  Google Scholar 

  • Groffman PM, Driscoll CT, Fahey TJ, Hardy JP, Fitzhugh RD, Tierney GL (2001) Effects of mild winter freezing on soil nitrogen and carbon dynamics in a northern hardwood forest. Biogeochemistry 56(2):191–213

    Article  Google Scholar 

  • Gu BH, Schmitt J, Chen ZH, Liang LY, McCarthy JF (1994) Adsorption and desorption of natural organic matter on iron-oxide: mechanisms and models. Environ Sci Technol 28(1):38–46

    Article  Google Scholar 

  • Harrison RB, Johnson DW, Todd DE (1989) Sulfate adsorption and desorption reversibility in a variety of forest soils. J Environ Qual 18(4):419–426

    Article  Google Scholar 

  • Heinrichs H, Mayer R (1977) Distribution and cycling of major and trace elements in two central European forest ecosystems. J Environ Qual 6:402–407

    Article  Google Scholar 

  • Jersak J, Amundson R, Brimhall G (1995) A mass-balance analysis of podzolization––examples from the northeastern United States. Geoderma 66(1–2):15–42

    Article  Google Scholar 

  • Johnson NM, Driscoll CT, Eaton JS, Likens GE, McDowell WH (1981) Acid rain, dissolved aluminum and chemical weathering at the Hubbard Brook Experimental Forest, New Hampshire. Geochim Cosmochim Acta 45:1421–1437

    Article  Google Scholar 

  • Johnson CE, Driscoll CT, Siccama TG, Likens GE (2000) Element fluxes and landscape position in a northern hardwood forest watershed ecosystem. Ecosystems 3(2):159–184

    Article  Google Scholar 

  • Jones RH, Segal DS, Sharitz RR (1994) Cation dynamics in bottomland hardwood forest litter. Am Midl Nat 131(2):248–256

    Article  Google Scholar 

  • Kabata-Pendias A, Pendias H (1984) Trace elements in soils and plants. CRC Press, Boca Raton, FL

    Google Scholar 

  • Kieber RJ, Williams K, Willey JD, Skrabal S, Avery GB (2001) Iron speciation in coastal rainwater: concentration and deposition to seawater. Mar Chem 73(2):83–95

    Article  Google Scholar 

  • Killingbeck KT (1985) Autumnal resorption and accretion of trace-metals in gallery forest trees. Ecology 66(1):283–286

    Article  Google Scholar 

  • Koseoglu AT, Acikgoz V (1995) Determination of iron chlorosis with extractable iron analysis in peach leaves. J Plant Nutr 18(1):153–161

    Article  Google Scholar 

  • Lawrence GB, Fuller RD, Driscoll CT (1986) Spatial relationships of aluminum chemistry in the streams of the Hubbard Brook Experimental Forest, New Hampshire. Biogeochemistry 2(2):115–135

    Article  Google Scholar 

  • Likens GE, Bormann FH, Pierce RS, Eaton JS, Johnson NM (1977) Biogeochemistry of a forested ecosystem. Springer-Verlag, New York

    Google Scholar 

  • Lovley DR, Coates JD, BluntHarris EL, Phillips EJP, Woodward JC (1996) Humic substances as electron acceptors for microbial respiration. Nature 382(6590):445–448

    Article  Google Scholar 

  • Lundstrom US, van Breemen N, Bain DC, van Hees PAW, Giesler R, Gustafsson JP, Ilvesniemi H, Karltun E, Melkerud PA, Olsson M, Riise G, Wahlberg O, Bergelin A, Bishop K, Finlay R, Jongmans AG, Magnusson T, Mannerkoski H, Nordgren A, Nyberg L, Starr M, Strand LT (2000) Advances in understanding the podzolization process resulting from a multidisciplinary study of three coniferous forest soils in the Nordic Countries. Geoderma 94(2–4):335–353

    Article  Google Scholar 

  • McDowell WH, Wood T (1984) Podzolization––soil processes control dissolved organic-carbon concentrations in stream water. Soil Sci 137(1):23–32

    Article  Google Scholar 

  • McKeague JA, Ross GJ, Gamble, DS (1978) Properties, criteria of classification and genesis of podzolic soils in Canada. In: Mahaney WC (ed) Conference on quaternary research, Norwich. Quaternary soils, vol 3, pp 27–60

  • Nason A, McElroy WD (1963) Modes of action of the essential mineral elements. In: Stewart FC (ed) Plant physiology. Academic Press, New York

    Google Scholar 

  • Palmer SM, Driscoll CT, Johnson CE (2004) Long-term trends in soil solution and stream water chemistry at the Hubbard Brook Experimental Forest: relationship with landscape position. Biogeochemistry 68(1):51–70

    Article  Google Scholar 

  • Parekh PP, Chang AC (1981) Trace element concentrations in summer aerosols at rural sites in New York State and their possible sources. Atmos Environ 15:1717–1725

    Article  Google Scholar 

  • Parker GG (1983) Throughfall and stemflow in the forest nutrient cycle. Adv Ecol Res 13:57–133

    Article  Google Scholar 

  • Peretyazhko T, Sposito G (2005) Iron(III) reduction and phosphorous solubilization in humid tropical forest soils. Geochim Cosmochim Acta 69(14):3643–3652

    Article  Google Scholar 

  • Petras RJ (1996) Iron, zinc, and lead fractions in a northern hardwood forest Spodosol. Masters Thesis. Syracuse University, Syracuse, NY

  • Pinton R, Veranini Z, Nannipieri P (2007) The rhizosphere: biochemistry and organic substances at the soil-plant interface. CRC Rpess, Boca Raton, FL

    Book  Google Scholar 

  • Rochette EA, Cleary RJ (2004) Iron speciation of in situ solutions from an episaturated spodosol. Commun Soil Sci Plan 35(3–4):345–367

    Article  Google Scholar 

  • Sauer D, Sponagel H, Sommer M, Giani L, Jahn R, Stahr K (2007) Review article Podzol: soil of the year 2007. A review on its genesis, occurrence, and functions. J Plant Nutr Soil Sci 170(5):581–597

    Article  Google Scholar 

  • Schlesinger WH (1997) Biogeochemistry: an analysis of global change. Academic Press, San Diego

    Google Scholar 

  • Schnitzer M, Skinner SIM (1963) Organo-metallic interactions in soil: 1. Reactions between a number of metal ions and the organic matter of the Podzol Bh horizon. Soil Sci 96:86–94

    Article  Google Scholar 

  • Senesi N, Sposito G (1989) Characterization and stability of transition-metal complexes of chestnut (Castanea-sativa L.) leaf litter. J Soil Sci 40(2):461–472

    Article  Google Scholar 

  • Senesi N, Sposito G, Bradford GR (1989) Iron, copper, and manganese complexation by forest leaf litter. Forest Sci 35(4):1040–1057

    Google Scholar 

  • Singer PC, Stumm W (1970) Acidic mine drainage: the rate-determining step. Science 167:1121

    Article  Google Scholar 

  • Smith WH, Siccama TG, Clark S (1986) Atmospheric deposition of heavy metals and forest health: an overview including a ten year budget for the input/output of seven heavy metals to a northern hardwood forest. In: Vol FWS-87-02. Virginia Polytechnic Institute and State University, Blacksburg, VA, p 27

  • Sollins P, Robertson GP, Uehara G (1988) Nutrient mobility in variable-charge and permanent-charge soils. Biogeochemistry 6(3):181–199

    Article  Google Scholar 

  • Sunda WG (2000) Trace metal-phytoplankton interactions. In: Lovely DK (ed) Environmental microbe-metal interactions. ASM Press, Washington

    Google Scholar 

  • Swanson KA, Johnson AH (1980) Trace metal budgets for a forested watershed in the New Jersey Pine Barrens. Water Resour Res 16:373–376

    Article  Google Scholar 

  • Thompson Y, Sandefur BC, Karathanasis AD, D’Angelo E (2009) Redox potential and seasonal porewater biogeochemistry of three mountain wetlands in Southeastern Kentucky, USA. Aquat Geochem 15(3):349–370

    Article  Google Scholar 

  • Tyler G (1981) Leaching of metals from the A-horizon of a spruce forest soil. Water Air Soil Pollut 15:353–360

    Article  Google Scholar 

  • Tyler G (2005) Changes in the concentrations of major, minor and rare-earth elements during leaf senescence and decomposition in a Fagus sylvatica forest. Forest Ecol Manag 206(1–3):167–177

    Article  Google Scholar 

  • Ussiri DAN, Johnson CE (2004) Sorption of organic carbon fractions by Spodosol mineral horizons. Soil Sci Soc Am J 68(1):253–262

    Article  Google Scholar 

  • Weber KA, Achenbach LA, Coates JD (2006) Microorganisms pumping iron: anaerobic microbial iron oxidation and reduction. Nat Rev Microbiol 4(10):752–764

    Article  Google Scholar 

  • Wilkin RT, Ptacek CJ (2002) Field measurement of geochemical redox parameters. In: Wilkin RT, Ludwig RD, Ford RG (eds) Workshop on monitoring oxidation-reduction processes for ground-water restoration. U.S. Environmental Protection Agency, Dallas, TX, Vol EPA/600/R-02/002. U.S. Environmental Protection Agency, pp 89–99

  • Willey JD, Kieber RJ, Seaton PJ, Miller C (2008) Rainwater as a source of Fe(II)-stabilizing ligands to seawater. Limnol Oceanogr 53(4):1678–1684

    Article  Google Scholar 

  • Yuan G, Lavkulich LM (1994) Phosphate sorption in relation to extractable iron and aluminum in Spodosols. Soil Sci Soc Am J 58(2):343–346

    Article  Google Scholar 

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Acknowledgements

This study was supported by the National Science Foundation (NSF) through the Long-Term Ecological Research (LTER) Program. The HBEF is a NSF LTER site. We would like to thank L. Martel, J. Towse, C. Wood, S. Quimby, C. Ortiz, E. Hunter, and M. Montesdeoca for assistance with field sampling and/or laboratory analysis. The Hubbard Brook Experimental Forest is administered by the USDA Forest Service, Northeastern Research Station, Newtown Square, Pennsylvania. The USDA Forest Service provides precipitation and hydrologic data for this study. This is contribution of the Hubbard Brook Ecosystem Study.

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Authors and Affiliations

  1. Department of Civil and Environmental Engineering, Syracuse University, 151 Link Hall, Syracuse, NY, 13244, USA

    Colin B. Fuss, Charles T. Driscoll, Chris E. Johnson & Robert J. Petras

  2. Department of Natural Resources, Cornell University, Ithaca, NY, 14853, USA

    Timothy J. Fahey

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  1. Colin B. Fuss
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  2. Charles T. Driscoll
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Correspondence to Colin B. Fuss.

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Fuss, C.B., Driscoll, C.T., Johnson, C.E. et al. Dynamics of oxidized and reduced iron in a northern hardwood forest. Biogeochemistry 104, 103–119 (2011). https://doi.org/10.1007/s10533-010-9490-x

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