Douglas A Burns
Doug is a Research Hydrologist currently working as the Coordinator of the Delaware River Basin Next Generation Water Observing System (NGWOS).
Doug holds an M.S. in Environmental Sciences from the Univ. of Virginia, and a Ph.D. in Water Resources Management from the State Univ. of New York, College of Environmental Science and Forestry. His disciplinary background is primarily in biogeochemistry and hydrology with a focus on understanding the processes that control the cycling of chemical elements through watersheds and ecosystems. An emphasis on the cycling of atmopsheric pollutants and their environmental effects is noteworthy. He has worked as a Research Hydrologist in the New York Water Science Center since 1987 on studies that include the effects of acid rain on ecosystems, the cycling of nitrogen in watersheds, and environmental mercury cycling. His investigations have also included the environmental effects of landscape disturbance such as suburban land use, climate change, and forest harvesting. A recent interest is studying the effects of ongoing and future climate change on streamflow, with an emphasis on high flows. He works collaboratively, often with several investigators from the USGS, and other agencies and universities. Study approaches applied include monitoring of water and soil chemistry, quantifying the rates of key cycling processes, experimental manipulations of landscapes, use of natural and applied isotope tracers, and statistical and process-level models. He is also active in professional societies, has organized conferences at regional, national, and international levels, and has served in leadership roles in many organizations and agencies. Other activities include chairing a proposal evaluation panel for a federal agency, working at the science-policy interface by serving as Director of the National Acid Precipitation Assessment Program, and serving on an EPA Clean Air Act Advisory Panel, as well as serving on program evaluation and advisory panels for several agencies and science organizations.
more about Douglas A Burns
Science and Products
Total mercury, methylmercury, and selected elements in soils of the Fishing Brook watershed, Hamilton County, New York, and the McTier Creek watershed, Aiken County, South Carolina, 2008
Dual nitrate isotopes in dry deposition: Utility for partitioning NOx source contributions to landscape nitrogen deposition
How does landscape structure influence catchment transit time across different geomorphic provinces?
Sources and transformations of nitrate from streams draining varying land uses: Evidence from dual isotope analysis
Effects of forest harvesting on ecosystem health in the headwaters of the New York City Water Supply, Catskill Mountains, New York
Catchment data for process conceptualization: Simply not enough?
Nitrogen immobilization by wood-chip application: Protecting water quality in a northern hardwood forest
Changes in stream chemistry and biology in response to reduced levels of acid deposition during 1987-2003 in the Neversink River Basin, Catskill Mountains
Factors controlling nitrogen release from two forested catchments with contrasting hydrochemical responses
Factors controlling soil water and stream water aluminum concentrations after a clearcut in a forested watershed with calcium-poor soils
Recent climate trends and implications for water resources in the Catskill Mountain region, New York, USA
Nitrogen isotopes as indicators of NOx source contributions to atmospheric nitrate deposition across the midwestern and northeastern United States
Non-USGS Publications**
66. Burns, D.A., Lawrence, G.B., and Murdoch, P.S., 1998, Catskill streams still susceptible to acid rain, Northeastern Geology and Environmental Sciences, 20: 294-298.
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
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Total mercury, methylmercury, and selected elements in soils of the Fishing Brook watershed, Hamilton County, New York, and the McTier Creek watershed, Aiken County, South Carolina, 2008
Mercury is an element of on-going concern for human and aquatic health. Mercury sequestered in upland and wetland soils represents a source that may contribute to mercury contamination in sensitive ecosystems. An improved understanding of mercury cycling in stream ecosystems requires identification and quantification of mercury speciation and transport dynamics in upland and wetland soils within aAuthorsLaurel G. Woodruff, William F. Cannon, Christopher D. Knightes, Francis H. Chapelle, Paul M. Bradley, Douglas A. Burns, Mark E. Brigham, Mark A. LoweryDual nitrate isotopes in dry deposition: Utility for partitioning NOx source contributions to landscape nitrogen deposition
Dry deposition is a major component of total atmospheric nitrogen deposition and thus an important source of bioavailable nitrogen to ecosystems. However, relative to wet deposition, less is known regarding the sources and spatial variability of dry deposition. This is in part due to difficulty in measuring dry deposition and associated deposition velocities. Passive sampling techniques offer poteAuthorsE.M. Elliott, Carol Kendall, E. W. Boyer, Douglas A. Burns, Gary Lear, H.E. Golden, K. Harlin, A. Bytnerowicz, T.J. Butler, R. GlatzHow does landscape structure influence catchment transit time across different geomorphic provinces?
Despite an increasing number of empirical investigations of catchment transit times (TTs), virtually all are based on individual catchments and there are few attempts to synthesize understanding across different geographical regions. Uniquely, this paper examines data from 55 catchments in five geomorphic provinces in northern temperate regions (Scotland, United States of America and Sweden). TheAuthorsD. Tetzlaff, J. Seibert, K.J. McGuire, H. Laudon, Douglas A. Burns, S.M. Dunn, C. SoulsbySources and transformations of nitrate from streams draining varying land uses: Evidence from dual isotope analysis
Knowledge of key sources and biogeochemical processes that affect the transport of nitrate (NO3-) in streams can inform watershed management strategies for controlling downstream eutrophication. We applied dual isotope analysis of NO3- to determine the dominant sources and processes that affect NO3- concentrations in six stream/river watersheds of different land uses. Samples were collected monthlAuthorsDouglas A. Burns, E. W. Boyer, E.M. Elliott, C. KendallEffects of forest harvesting on ecosystem health in the headwaters of the New York City Water Supply, Catskill Mountains, New York
The effects of forest clearcutting and selective harvesting on forest soils, soil and stream water chemistry, forest regrowth, and aquatic communities were studied in four small headwater catchments. This research was conducted to identify the sensitivity of forested ecosystems to forest disturbance in the northeastern United States. The study area was in the headwaters of the Neversink ReservoirAuthorsMichael R. McHale, Peter S. Murdoch, Douglas A. Burns, Barry P. BaldigoCatchment data for process conceptualization: Simply not enough?
[No abstract available]AuthorsC. Soulsby, C. Neal, H. Laudon, Douglas A. Burns, P. Merot, M. Bonell, S.M. Dunn, D. TetzlaffNitrogen immobilization by wood-chip application: Protecting water quality in a northern hardwood forest
Forest harvesting disrupts the nitrogen cycle, which may affect stream water quality by increasing nitrate concentrations, reducing pH and acid neutralizing capacity, and mobilizing aluminum and base cations. We tested the application of wood chips derived from logging slash to increase immobilization of N after harvesting, which should reduce nitrate flux to streams. In August 2004, a stand of noAuthorsP.M. Homyak, R.D. Yanai, Douglas A. Burns, R.D. Briggs, R.H. GermainChanges in stream chemistry and biology in response to reduced levels of acid deposition during 1987-2003 in the Neversink River Basin, Catskill Mountains
Atmospheric acid deposition has decreased in the northeastern United States since the 1970s, resulting in modest increases in pH, acid-neutralizing capacity (ANC), and decreases in inorganic monomeric aluminum (AlIM) concentrations since stream chemistry monitoring began in the 1980s in the acid-sensitive upper Neversink River basin in the Catskill Mountains of New York. Stream pH has increased byAuthorsDouglas A. Burns, K. Riva-Murray, R.W. Bode, S. PassyFactors controlling nitrogen release from two forested catchments with contrasting hydrochemical responses
Quantifying biogeochemical cycles of nitrogen (N) and the associated fluxes to surface waters remains challenging, given the need to deal with spatial and temporal variability and to characterize complex and heterogeneous landscapes. We focused our study on catchments S14 and S15 located in the Adirondack Mountains of New York, USA, which have similar topographic and hydrologic characteristics butAuthorsS.F. Christopher, M.J. Mitchell, Michael McHale, E. W. Boyer, Douglas A. Burns, C. KendallFactors controlling soil water and stream water aluminum concentrations after a clearcut in a forested watershed with calcium-poor soils
The 24 ha Dry Creek watershed in the Catskill Mountains of southeastern New York State USA was clearcut during the winter of 1996-1997. The interactions among acidity, nitrate (NO3- ), aluminum (Al), and calcium (Ca2+) in streamwater, soil water, and groundwater were evaluated to determine how they affected the speciation, solubility, and concentrations of Al after the harvest. Watershed soils werAuthorsM.R. McHale, Douglas A. Burns, G. B. Lawrence, Peter S. MurdochRecent climate trends and implications for water resources in the Catskill Mountain region, New York, USA
Climate scientists have concluded that the earth’s surface air temperature warmed by 0.6 °C during the 20th century, and that warming induced by increasing concentrations of greenhouse gases is likely to continue in the 21st century, accompanied by changes in the hydrologic cycle. Climate change has important implications in the Catskill region of southeastern New York State, because the region isAuthorsDouglas A. Burns, Julian Klaus, Michael R. McHaleNitrogen isotopes as indicators of NOx source contributions to atmospheric nitrate deposition across the midwestern and northeastern United States
Global inputs of NOx are dominated by fossil fuel combustion from both stationary and vehicular sources and far exceed natural NOx sources. However, elucidating NOx sources to any given location remains a difficult challenge, despite the need for this information to develop sound regulatory and mitigation strategies. We present results from a regional-scale study of nitrogen isotopes (δ15N) in wetAuthorsEmily M. Elliott, Carol Kendall, Scott D. Wankel, Douglas A. Burns, E. W. Boyer, K. Harlin, Daniel J Bain, T.J. ButlerNon-USGS Publications**
Harpold, A.A., Burns, D.A., Walter, T., Shaw, S.B., and Steenhuis, T.S., 2010, Relating hydrogeomorphologic properties to stream buffering chemistry in the Neversink River Watershed, New York State, USA, Hydrological Processes, 24: 3759-3771.Vidon, P., Allan, C., Burns, D., Duval, T., Gurwick, N., Inamdar, S., Lowrance, R., Okay, J., Scott, D., Sebestyen, S., 2010, Hot spots and hot moments in riparian zones: Potential for improved water quality management, Journal of the American Water Resources Association, 46: 278-298.Kerr, J.G., Eimers, M.C., Creed, I.F., Adams, M.B., Beall, F., Burns, D., Campbell, J.L., Christopher, S.F., Clair, T.A., Couchesne, F., Duchense, L., Fernandez, I., Houle, D., Jeffries, D.S., Likens, G.E., Mitchell, M.J., Shanley, J., Yao, H., 2012, The effect of seasonal drying on sulphate dynamics in streams across southeastern Canada and the northeastern USA, Biogeochemistry, 111: 393-409.Burns, D.A., Blett, T., Haeuber, R., Pardo, L., 2008, Critical loads as a policy tool for protecting ecosystems from the effects of air pollutants, Frontiers of Ecology and the Environment, 6: 156-159.Elliott, E.M., Kendall, C., Boyer, E.W., Burns, D.A., Wankel, S.D., Bain, D.J., Harlin, K., Butler, T.J., Carlton, R., 2007, An isotopic tracer of stationary source NOx emissions across the midwestern and northeastern United States, Environmental Science and Technology, 41: 7661-7667.Burns, D.A., Plummer, L.N., McDonnell, J.J., Busenberg, E., Casile, G.C., Kendall, C., Hooper, R.P., Freer, J.E., Peters, N.E., Beven, K., and Schlosser, P., 2003, The geochemical evolution of groundwater in a forested Piedmont catchment, Ground Water, 41: 913-925.Burns, D.A., and Nguyen, L., 2002, Nitrate movement and removal along a shallow groundwater flow path in a riparian wetland within a sheep-grazed pastoral catchment: results of a tracer study, New Zealand Journal of Marine and Freshwater Research, 36: 371-385.Vitvar, T., Burns, D.A., Lawrence, G.B., McDonnell, J.J., and Wolock, D.M., 2002, Estimation of groundwater residence times in watersheds from the recession of the runoff-hydrograph: method and application in the Neversink watershed, Catskill Mountains, New York, Hydrological Processes, 16: 1871-1877.Burns, D.A., Lawrence, G.B., and Murdoch, P.S., 1998, Catskill streams still susceptible to acid rain, Eos, Transactions, American Geophysical Union, 79: 197, 200-201.
66. Burns, D.A., Lawrence, G.B., and Murdoch, P.S., 1998, Catskill streams still susceptible to acid rain, Northeastern Geology and Environmental Sciences, 20: 294-298.Driscoll, C.T., Cirmo, C.P., Fahey, T.J., Blette, V.L., Bukaveckas, P.A., Burns, D.A., Gubala, C.P., Leopold, D.J., Newton, R.M., Raynal, D.J., Schofield, C.L., Yavitt, J.B., and Porcella, D.B., 1996, The experimental watershed liming study: Comparison of lake and watershed neutralization strategies, Biogeochemistry, 32: 143-174.McDonnell, J.J., Freer, J., Hooper, R., Kendall, C., Burns, D., Beven, K., and Peters, J., 1996, New method developed for studying flow on hillslopes, Eos, Transactions, American Geophysical Union, 77: 465 and 472.Clair, T.C., Burns, D.A., Perez, I.R., Blais, J., and Percy, K., 2011, Ecosystems, in: Technical Challenges of Multipollutant Air Quality Management, Hidy, G., Brook, J.R., Demerjian, K.L., Molina, L.T., Pennell, W.T., and Scheffe, R. (eds.), Springer, Dordrecht, Netherlands, Ch. 6, p. 139-229.Nguyen, L., Rutherford, K., and Burns, D., 1999, Denitrification and nitrate removal in two contrasting riparian wetlands, in: Proceedings of the 20th New Zealand Land Treatment Collective Technical Session, M. Tomer, M Robinson, and G Gielen (eds.), New Plymouth, New Zealand, p. 127-131.Kendall, C., Silva, S.R., Chang, C.C.Y., Burns, D.A.., Campbell, D.H., and Shanley, J.B., 1996, Use of the d18O and d15N of nitrate to determine sources of nitrate in early spring runoff in forested catchments, in: Isotopes in Water Resources Management, Proceedings of the Symposium on Isotopes in Water Resources Management, March 20-24, 1995, Volume 1, IAEA-SM-336/29, International Atomic Energy Agency, Vienna, Austria, p. 167-176.Kendall, C., Campbell, D.H., Burns, D.A., Shanley, J.B., Silva, S.R., Chang, C.C.Y., 1995, Tracing sources of nitrate in snowmelt runoff using the oxygen and nitrogen isotopic compositions of nitrate, in: Biogeochemistry of Seasonally Snow-Covered Catchments, K.A. Tonnessen, M.W. Williams, M. Trantner, M. (eds.), International Association of Hydrological Sciences Proceedings, July 3-14, 1995, Boulder, CO, I.A.H.S. Publication 228, Wallingford, U.K., p. 339-347.Hendrey, G.R., Galloway, J.N., Norton, S.A., Schofield, C.L., Burns, D.A., and Shaffer, P.W., 1980, Sensitivity of the eastern United States to acid precipitation impacts on surface waters, in: Drablos, D., and Tollan, A. (eds.), Ecological Impact of Acid Precipitation, SNSF Proceedings, Oslo, p. 216-217.Allen, G., Burns, D.A., Negra, C., and Thurston, G.D., 2009, Indicator measurements for assessing the impacts of anthropogenic air pollutants on human health and ecosystems, EM: The Magazine for Environmental Managers, Oct. 2009, p. 20-25, Air and Waste Management Association, Pittsburgh, PA.Burns, D.A., 2005, What do hydrologists mean when they use the term flushing? Hydrological Processes, 19: 1325-1327.**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.