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Fluorescent DOC characteristics are related to streamflow and pasture cover in streams of a mixed landscape

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A growing body of research suggests that different land use activities may alter both the quantity and quality of dissolved organic carbon (DOC) exported from terrestrial landscapes. However, little is known about DOC from mixed-use landscapes where hydrology varies seasonally. This study examined how DOC and chemical properties of stream water were related to land use, drainage area, and streamflow in mixed-use landscape in the Willamette River Basin, Oregon. Stream water samples were collected at roughly monthly intervals over three water years from 21 sites whose drainage areas ranged from 1 to > 11,000 km2 and included pasture, forest, and developed land uses. DOC properties were characterized using PARAFAC (parallel factor) analyses of 3-D excitation and emission matrices (EEMs). We used the Cory-McKnight (CM) model, and we also developed a model unique to our samples. Thirteen components were identified using the CM model, and these were highly correlated with, and similar with respect to excitation and emission to the three components identified in our site-specific model. Fluorescent components of DOC were related to discharge and land cover, but not to drainage area. In our model, one component (C1) appeared to be associated with terrestrial detritus and was greater in streamflow from sites with forest/developed cover than from sites with high pasture cover. A second component (C2) was greater in streamflow from high-pasture sites than from high-forest sites. C2 was strongly correlated with a protein component identified in the CM model, and therefore we attributed this second component to more microbially-processed DOC. C1 increased significantly with discharge for both land covers, suggesting that periods of high flow produce less microbially-processed DOC from more surficial flow. C2 decreased significantly with discharge for both land covers, suggesting that deeper hydrologic flow paths produce more soil-associated, microbially processed DOC. SUVA254, often used as an index of chemical quality and aromaticity of DOC, was related only to streamflow but not land use, suggesting that while the chemistry of DOC differed among land use types as detected by EEMs analysis, the aromaticity of the DOC did not differ. The CM model and our site-specific model provided consistent results: those components that were highest in high pasture sites were also highest at low flow and appeared to be more microbially processed; components that were highest in low pasture sites were also greatest at high flow and appeared to reflect less microbially processed DOC. Taken together, these findings are consistent with a conceptual model of how differences in DOC chemistry among landscape types reflect differences in plant litter input chemistry, hydrologic connectivity, and degree of microbial processing. Such changes in DOC quality with land-use change can affect foodweb dynamics in receiving waters and change the balance between carbon storage and carbon flux to the atmosphere, and they imply that even non-intensive agricultural land use can have significant effects on terrestrial-aquatic carbon processes.

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References

  • Ågren A, Haei M, Köhler SJ, Bishop K, Laudon H (2010) Regulation of stream water dissolved organic carbon (DOC) concentrations during snowmelt; the role of discharge, winter climate and memory effects. Biogeosciences 7:2901–2913

    Article  Google Scholar 

  • Andersson CA, Bro R (2000) The N-way Toolbox for MATLAB. Chemom Intell Lab Syst 52:1–4

    Article  Google Scholar 

  • Asano Y, Compton JE, Church MR (2006) Hydrologic flowpaths influence inorganic and organic nutrient leaching in a forest soil. Biogeochemistry 81:191–204

    Article  Google Scholar 

  • Autio I, Soinne H, Helin J, Asmala E, Hoikkala L (2016) Effect of catchment land use and soil type on the concentration, quality, and bacterial degradation of riverine dissolved organic matter. Ambio 45:331–349

    Article  Google Scholar 

  • Burns MA, Barnard HR, Gabor RS, McKnight DM, Brooks PD (2016) Dissolved organic matter transport reflects hillslope to stream connectivity during snowmelt in a montane catchment. Water Resour Res 52:4905–4923

    Article  Google Scholar 

  • Cade-Menun BJ, Bell G, Baker-Ismail S, Fouli Y, Hodder K, McMartin DW, Perez-Valdivia C, Wu K (2013) Nutrient loss from Saskatchewan cropland and pasture in spring snowmelt runoff. Can J Soil Sci 93:445–458

    Article  Google Scholar 

  • Cawley KM, Wolski P, Mladenov N, Jaffe R (2012) Dissolved organic matter biogeochemistry along a transect of the Okavango Delta, Botswana. Wetlands 32:475–486

    Article  Google Scholar 

  • Cawley KM, Campbell J, Zwilling M, Jaffé R (2014) Evaluation of forest disturbance legacy effects on dissolved organic matter characteristics in streams at the Hubbard Brook Experimental Forest, New Hampshire. Aquat Sci 76(4):611–622

    Article  Google Scholar 

  • CCAL (2014) Analytical detection levels. http://ccal.oregonstate.edu/detection. Accessed 8 Oct 2014

  • Coble PG (1996) Characterization of marine and terrestrial DOM in seawater using excitation-emission matrix spectroscopy. Mar Chem 51(4):325–346

    Article  Google Scholar 

  • Coble PG (2007) Marine optical biogeochemistry: the chemistry of Ocean color. Chem Rev 107:402–418

    Article  Google Scholar 

  • Cole JJ, Prairie YT, Caraco NF, McDowell WH, Tranvik LJ, Striegl RG, Duarte CM, Kortelainen P, Downing JA, Middleburg JJ, Melack J (2007) Plumbing the global carbon cycle: integrating inland waters into the terrestrial carbon budget. Ecosystems 10:172–185. https://doi.org/10.1007/s10021-006-9013-8

    Article  Google Scholar 

  • Cory RM, McKnight DM (2005) Fluorescence spectroscopy reveals ubiquitous presence of oxidized and reduced quinones in dissolved organic matter. Environ Sci Technol 39:8142–8149

    Article  Google Scholar 

  • Cory RM, Miller MP, McKnight DM, Guerard JJ, Miller PL (2010) Effect of instrument-specific response on the analysis of fulvic acid fluorescence spectra. Limnol Oceanogr 8:67–78

    Google Scholar 

  • Cory RM, Boyer EW, Mcknight DM (2011) In: Levia DF, Carlyle-Moses D, Tanaka T (eds) Forest hydrology and biogeochemistry, 1st edition. Springer, Dordrecht, pp 117–136

  • Dai KH, David MB, Vance GF (1996) Characterization of solid and dissolved carbon in a spruce-fir spodosol. Biogeochemistry 35:339–365

    Article  Google Scholar 

  • Ebert J (2013) Collecting 3-dimensional fluorescence scans. Page Fluorescence and LTER DOM Workshops. University of Colorado, Boulder, CO.

  • Erlandsson M, Cory N, Fölster J, Köhler S, Laudon H, Weyhenmeyer GA, Bishop K (2011) Increasing dissolved organic carbon redefines the extent of surface water acidification and helps resolve a classic controversy. Bioscience 61:614–618

    Article  Google Scholar 

  • Evans CD, Jones TG, Burden A, Ostle N, Zieliński P, Cooper MDA, Peacock M, Clark JM, Oulehle F, Cooper D, Freeman C (2012) Acidity controls on dissolved organic carbon mobility in organic soils. Glob Change Biol 18:3317–3331

    Article  Google Scholar 

  • Fellman JB, Miller MP, Corey R, D’Amore DV, White D (2009) Characterizing dissolved organic matter using PARAFAC modeling of fluorescence spectroscopy: a comparison of two models. Environ Sci Technol 43:6228–6234

    Article  Google Scholar 

  • Fuß T, Behounek B, Ulseth AJ, Singer GA (2017) Land use controls stream ecosystem metabolism by shifting dissolved organic matter and nutrient regimes. Freshw Biol 62:582–599

    Article  Google Scholar 

  • Graeber D, Boëchat IG, Encina-Montoya F, Esse C, Gelbrecht J, Goyenola G, Gücker B, Heinz M, Kronvang B, Meerhoff M, Nimptsch J, Pusch MT, Silva RCS, von Schiller D, Zwirnmann E (2015) Global effects of agriculture on fluvial dissolved organic matter. Sci Rep 5:16328

    Article  Google Scholar 

  • Hood E, Williams MW, McKnight DM (2005) Sources of dissolved organic matter (DOM) in a Rocky Mountain stream using chemical fractionation and stable isotopes. Biogeochemistry 74:231–255

    Article  Google Scholar 

  • Hosen JD, McDonough OT, Febria CM, Palmer MA (2014) Dissolved organic matter quality and bioavailability changes across an urbanization gradient in headwater streams. Environ Sci Technol 48:7817–7824

    Article  Google Scholar 

  • Hruška J, Krám P, McDowell WH, Oulehle F (2009) Increased dissolved organic carbon (DOC) in Central European streams is driven by reductions in ionic strength rather than climate change or decreasing acidity. Environ Sci Technol 43:4320–4326

    Article  Google Scholar 

  • Huang W, Chen RF (2009) Sources and transformations of chromophoric dissolved organic matter in the Neponset River Watershed. J Geophys Res 114:G00F05

    Article  Google Scholar 

  • Inamdar S, Singh S, Dutta S, Levia D, Mitchell M, Scott D, Bais H, McHale P (2011) Fluorescence characteristics and sources of dissolved organic matter for stream water during storm events in a forested mid-Atlantic watershed. J Geophys Res 116:G03043

    Article  Google Scholar 

  • Jin S, Yang L, Danielson P, Homer C, Fry J, Xian G (2013) A comprehensive change detection method for updating the National Land Cover Database to circa 2011. Remote Sens Environ 132:159–175

    Article  Google Scholar 

  • Johnson M, Couto E, Abdo M, Lehmann J (2011) Fluorescence index as an indicator of dissolved organic carbon quality in hydrologic flowpaths of forested tropical watersheds. Biogeochemistry 105:149–157

    Article  Google Scholar 

  • Kalbitz K, Schwesig D, Schmerwitz J, Kaiser K, Haumaier L, Glaser B, Ellerbrock R, Leinweber P (2003) Changes in properties of soil-derived dissolved organic matter induced by biodegradation. Soil Biol Biochem 35:1129–1142

    Article  Google Scholar 

  • Kramer MG, Lajtha K, Aufdenkampe AK (2017) Depth trends of soil organic matter C: N and 15 N natural abundance controlled by association with minerals. Biogeochemistry 136:237–248

    Article  Google Scholar 

  • Larsen LG, Aiken GR, Harvey JW, Noe GB, Crimaldi JP (2010) Using fluorescence spectroscopy to trace seasonal DOM dynamics, disturbance effects, and hydrologic transport in the Florida Everglades. J Geophys Res 115:G03001

    Article  Google Scholar 

  • Laudon H, Köhler S, Buffam I (2004) Seasonal TOC export from seven boreal catchments in northern Sweden. Aquat Sci 66:223–230

    Article  Google Scholar 

  • Lawaetz AJ, Stedmon CA (2009) Fluorescence intensity calibration using the Raman scatter peak of water. Appl Spectrosc 63:936–940

    Article  Google Scholar 

  • Lee BS (2015) Hydrologic and land cover effects on sources and fate of in-stream flourescent dissolved organic matter. PhD Dissertation, Oregon State University

  • Lee BS, Lajtha K (2016) Hydrologic and forest management controls on dissolved organic matter characteristics in headwater streams of old-growth forests in the Oregon Cascades. For Ecol Manag 380:11–22

    Article  Google Scholar 

  • Lu YH, Bauer JE, Canuel EA, Chambers RM, Yamashita Y, Jaffé R, Barrett A (2014) Effects of land use on sources and ages of inorganic and organic carbon in temperate headwater streams. Biogeochemistry 119:275–292

    Article  Google Scholar 

  • Mann PJ, Davydova A, Zimov N, Spencer RGM, Davydov S, Bulygina E, Zimov S, Holmes RM (2012) Controls on the composition and lability of dissolved organic matter in Siberia’s Kolyma River basin. J Geophys Res 117:1–15

    Article  Google Scholar 

  • Mann PJ, Spencer RGM, Dinga BJ, Poulsen JR, Hernes PJ, Fiske G, Salter ME, Wang ZA, Hoering KA, Six J, Holmes RM (2014) The biogeochemistry of carbon across a gradient of streams and rivers within the Congo Basin. J Geophys Res 119:2013JG002442

    Google Scholar 

  • McKay L, Bondelid T, Dewald T, Johnston J, Moore R, Rea A (2012) NHDPlus version 2: user guide. United States Environmental Protection Agency, Washington, D.C.

    Google Scholar 

  • McKnight DM, Boyer EW, Westerhoff PK, Doran PT, Kulbe T, Andersen DT (2001) Spectrofluorometric characterization of dissolved organic matter for indication of precursor organic material and aromaticity. Limonol Oceanogr 46:38–48

    Article  Google Scholar 

  • Miller MP, McKnight DM, Cory RM, Williams MW, Runkel RL (2006) Hyporheic exchange and fulvic acid redox reactions in an alpine stream/wetland ecosystem, colorado front range. Environ Sci Technol 40:5943–5949

    Article  Google Scholar 

  • Miller MP, Simone BE, McKnight DM, Cory RM, Williams MW, Boyer EW (2010) New light on a dark subject: comment. Aquat Sci 72:269–275

    Article  Google Scholar 

  • Monteith DT, Stoddard JL, Evans CD, Wit HAD, Forsius M, Høgåsen T, Wilander A, Skjelkvåle BL, Jeffries DS, Vuorenmaa J, Keller B, Kopácek J, Vesely J (2007) Dissolved organic carbon trends resulting from changes in atmospheric deposition chemistry. Nature 450:537–540

    Article  Google Scholar 

  • Morrison Erway M, Motter K, Karen B (2004) National Wadeable Stream Assessment: Water Chemistry Laboratory Manual (EPA841-B-04-008). U.S. Environmental Protection Agency, Office of Water and Office of Research and Development, Washington, D.C.

    Google Scholar 

  • O’Donnell JA, Aiken GR, Kane ES, Jones JB (2010) Source water controls on the character and origin of dissolved organic matter in streams of the Yukon River basin, Alaska. J Geophys Res 115:G03025

    Google Scholar 

  • Oni SK, Futter MN, Teutschbein C, Laudon H (2014) Cross-scale ensemble projections of dissolved organic carbon dynamics in boreal forest streams. Clim Dyn 42:2305–2321

    Article  Google Scholar 

  • Petrone KC (2010) Catchment export of carbon, nitrogen, and phosphorus across an agro-urban land use gradient, Swan-Canning River system, southwestern Australia. J Geophys Res 115:G01016

    Article  Google Scholar 

  • Schelker J, Eklöf K, Bishop K, Laudon H (2012) Effects of forestry operations on dissolved organic carbon concentrations and export in boreal first-order streams. J Geophys Res 117:G1

    Article  Google Scholar 

  • Singh S, Inamdar S, Scott D (2013) Comparison of two PARAFAC models of dissolved organic matter fluorescence for a mid-atlantic forested watershed in the USA. J Ecosyst. https://doi.org/10.1155/2013/532424

    Article  Google Scholar 

  • Singh S, Inamdar S, Mitchell M, McHale P (2014) Seasonal pattern of dissolved organic matter (DOM) in watershed sources: influence of hydrologic flow paths and autumn leaf fall. Biogeochemistry 118:321–337

    Article  Google Scholar 

  • Sollins P, Kramer MG, Swanston C, Lajtha K, Filley T, Aufdenkampe AK, Wagai R, Bowden RD (2009) Sequential density fractionation across soils of contrasting mineralogy: evidence for both microbial- and mineral-controlled soil organic matter stabilization. Biogeochemistry 96:209–231

    Article  Google Scholar 

  • Spencer RGM, Aiken GR, Wickland KP, Striegl RG, Hernes PJ (2008) Seasonal and spatial variability in dissolved organic matter quantity and composition from the Yukon River basin, Alaska. Global Biogeochem Cycles 22:1–13

    Article  Google Scholar 

  • Stedmon CA, Bro R (2008) Characterizing dissolved organic matter fluorescence with parallel factor analysis: a tutorial. Environ Res 6:572–579

    Google Scholar 

  • Stedmon CA, Markager S (2005) Resolving the variability in dissolved organic matter fluorescence in a temperate estuary and its catchment using PARAFAC analysis. Limonol Oceanogr 50:686–697

    Article  Google Scholar 

  • Stedmon CA, Markager S, Bro R (2003) Tracing dissolved organic matter in aquatic environments using a new approach to fluorescence spectroscopy. Mar Chem 82:239–254. https://doi.org/10.1016/S0304-4203(03)00072-0

    Article  Google Scholar 

  • Toosi ER, Schmidt JP, Castellano MJ (2014) Land use and hydrologic flowpaths interact to affect dissolved organic matter and nitrate dynamics. Biogeochemistry 120:89–104

    Article  Google Scholar 

  • Volk C, Kaplan LA, Robinson J, Johnson B, Wood L, Zhu HW, LeChevallier M (2005) Fluctuations of dissolved organic matter in river used for drinking water and impacts on conventional treatment plant performance. Environ Sci Technol 39:4258–4264

    Article  Google Scholar 

  • Weishaar JL, Aiken GR, Bergamaschi BA, Fram MS, Fujii R, Mopper K (2003) Evaluation of specific ultraviolet absorbance as an indicator of the chemical composition and reactivity of dissolved organic carbon. Environ Sci Technol 37:4702–4708

    Article  Google Scholar 

  • Williams CJ, Yamashita Y, Wilson HF, Jaffe R, Xenopoulos MA (2010) Unraveling the role of land use and microbial activity in shaping dissolved organic matter characteristics in stream ecosystems. Limnol Oceanogr 55:1159–1171

    Article  Google Scholar 

  • Williams CJ, Frost PC, Morales-Williams AM, Larson JH, Richardson WB, Chiandet AS, Xenopoulos MA (2016) Human activities cause distinct dissolved organic matter composition across freshwater ecosystems. Glob Change Biol 22:613–626

    Article  Google Scholar 

  • Wilson HF, Xenopoulos M (2008) Ecosystem and seasonal control of stream dissolved organic carbon along a gradient of land use. Ecosystems 11:555–568. https://doi.org/10.1007/s10021-008-9142-3

    Article  Google Scholar 

  • Wilson HF, Xenopoulos M (2009) Effects of agricultural land use on the composition of fluvial dissolved organic matter. Nat Geosci 2:37–41

    Article  Google Scholar 

  • Winterdahl M, Erlandsson M, Futter MN, Weyhenmeyer GA, Bishop K (2014) Intra-annual variability of organic carbon concentrations in running waters: Drivers along a climatic gradient. Global Biogeochem Cycles 28:451–464

    Article  Google Scholar 

  • Yamashita Y, Kloeppel BD, Knoepp J, Zausen GL, Jaffé R (2011) Effects of watershed history on dissolved organic matter characteristics in headwater streams. Ecosystems 14:1110–1122

    Article  Google Scholar 

  • Yano Y, Lajtha K, Sollins P, Caldwell B (2004) Chemical and seasonal controls on the dynamics of dissolved organic matter in a coniferous old-growth stand in the Pacific Northwest. USA. Biogeochemistry 71(2):197–223

    Article  Google Scholar 

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Acknowledgements

The study was partially funded by the Institute for Water and Watersheds, Dr. Michael Campana at Oregon State University, by NSF 1440409 to J. Jones, by NSF DEB 1257032 to K. Lajtha, and by NSF OCE 0962362 to A. E. White. We thank Katie Watkins-Brandt and Kathryn Motter for lab support.

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Correspondence to Baek Soo Lee.

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Lee, B.S., Lajtha, K., Jones, J.A. et al. Fluorescent DOC characteristics are related to streamflow and pasture cover in streams of a mixed landscape. Biogeochemistry 140, 317–340 (2018). https://doi.org/10.1007/s10533-018-0494-2

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