Christopher Fuller is a Emeritus Scientist for the USGS Water Resources Mission Area. His research characterizes processes and mechanisms of metal sorption reactions through field studies and lab experiments to better understand the metal transport and natural attenuation in mine contaminated systems and to better understand geochemical processes affecting bioavailability of metal contaminants to aquatic organisms.
Professional societies/affiliations/committees/editorial boards
American Geophysical Union
American Chemical Society
Geochemical Society
Professional Experience
Professional Studies/Experience
2019 - current: Scientist Emeritus
2018 - 2019: Research Hydrologist (Geochemistry), Hydrological-Ecological Interactions Branch, Earth Surface Processes Division, Water Mission Area, U.S. Geological Survey
1982 - 2017: Research Hydrologist (Geochemistry), National Research Program, Western Region, U.S. Geological Survey
1976 - 1982: Research Technician, Unversity of Southern California
Education and Certifications
Education
1976: BS Chemistry, SUNY Oswego
1982: MS Geology, emphasis in Marine Geochemistry, University of Southern California
Honors and Awards
Honors, awards, recognition, elected offices
May 1996: Editors Citation for Excellence in Manuscript Review for the Soil Science Society of America Journal
May 2003. STAR award for instrumental role in developing cooperative project with BLM at the Fry Canyon permeable reactive barrier demonstration site.
November 2006 Superior Service Award
October 2007. STAR award “Chris has done an outstanding job in age dating over 90 lake sediment cores collected from Great Salt Lake in a very short time frame to accommodate a Utah Water Science Center cooperator. This work was published in Applied Geochemistry.
June 2014 Superior Service Award
Science and Products
Minerals Science Team
Study Reveals Processes that Control Uranium Bioavailability in a Freshwater Snail—Relevance to Aquatic Biota in the Grand Canyon Area
Biogeochemical data of water, sediments, periphyton, and macroinvertebrates collected from springs in and near Grand Canyon National Park, Arizona (ver. 4.0, October 2022)
Data acquired in laboratory experiments conducted with the stonefly Zapada sp. and the ephemerellid mayflies Drunella sp. and Ephemerella tibialis to characterize uptake and surface adsorption after short aqueous exposures to uranium, 2017-2019
Geochemical data including mercury for subsamples of deep cores from the Cache Creek Settling Basin, Yolo County, California
Urban sediment and fallout radionuclide input characteristics of Dead Run watershed in Catonsville, Maryland for 2017-2018 (ver. 1.1, March 2020)
Hydrologic, biogeochemical, and radon data collected within and adjacent to the Little Wind River near Riverton, Wyoming
Aquatic insect accumulation of uranium at spring outflows in the Grand Canyon region as influenced by aqueous and sediment geochemistry and biological factors: Implications for monitoring
Interaction of a legacy groundwater contaminant plume with the Little Wind River from 2015 through 2017, Riverton Processing site, Wyoming
Sediment sources and sealed-pavement area drive polycyclic aromatic hydrocarbon and metal occurrence in urban streams
Influence of permafrost type and site history on losses of permafrost carbon after thaw
A 450-year record of environmental change from Castle Lake, California (USA), inferred from diatoms and organic geochemistry
Transport and speciation of uranium in groundwater-surface water systems impacted by legacy milling operations
Uranium bioaccumulation dynamics in the mayfly Neocloeon triangulifer and application to site-specific prediction
Pavement alters delivery of sediment and fallout radionuclides to urbanstreams
Combining sediment fingerprinting with age-dating sediment using fallout radionuclides for an agricultural stream, Walnut Creek, Iowa, USA
Competitive interactions among H, CU, and Zn ion moderate aqueous uptake of Cu and Zn by an aquatic insect
Carbon accumulation and vertical accretion in a restored vs. historic salt marsh in southern Puget Sound, Washington, United States
The approaching obsolescence of 137Cs dating of wetland soils in North America
Science and Products
- Science
Minerals Science Team
The Minerals Integrated Science Team focuses on contaminant exposures in the environment that might originate from mineral resource activities including, transportation, storage, extraction and waste management. Perceived health risks to humans and other organisms will be distinguished from actual risks, if any. If actual risks are identified the science produced by this team can inform how to...Study Reveals Processes that Control Uranium Bioavailability in a Freshwater Snail—Relevance to Aquatic Biota in the Grand Canyon Area
Scientists refined an existing speciation model to identify key biogeochemical processes controlling dissolved uranium bioavailability to a freshwater snail. This information is important to advance current understanding and prediction of the ecological risk posed by uranium mining to freshwater ecosystems, including federally managed lands such as in the Grand Canyon area. - Data
Biogeochemical data of water, sediments, periphyton, and macroinvertebrates collected from springs in and near Grand Canyon National Park, Arizona (ver. 4.0, October 2022)
The U.S. Geological Survey is studying uranium and associated trace element bioaccumulation in aquatic invertebrates across a gradient of dissolved uranium concentrations in spring outflow pools and creeks in the Grand Canyon and adjacent watershed. This data release makes available data from sampling campaigns in April 2016, April 2017, and in April 2019. Data collected include: (1) major ion, trData acquired in laboratory experiments conducted with the stonefly Zapada sp. and the ephemerellid mayflies Drunella sp. and Ephemerella tibialis to characterize uptake and surface adsorption after short aqueous exposures to uranium, 2017-2019
Little is known about the underlying mechanisms governing uranium (U) bioaccumulation in aquatic insects, especially the influence of surface adsorption on the measured U concentrations (Henry et al. 2020). U.S. Geological Survey scientists are conducting experiments to parameterize conditional rate constants for aqueous U uptake and to quantify desorption of weakly bound U from insect's integumenGeochemical data including mercury for subsamples of deep cores from the Cache Creek Settling Basin, Yolo County, California
Sediment cores were collected in the Cache Creek Settling Basin (CCSB), Yolo County, California, during October 2011 at 10 locations (borehole sites) and during August 2012 at 5 other locations. Total core depths ranged from approximately 4.6 to 13.7 meters (15 to 45 feet), with penetration to about 9.1 meters (30 feet) at most locations. Detailed subsampling (3-centimeter intervals) was done at tUrban sediment and fallout radionuclide input characteristics of Dead Run watershed in Catonsville, Maryland for 2017-2018 (ver. 1.1, March 2020)
This metadata record documents two comma delimited tables that contain information on fallout radionuclides and urban sediments within Dead Run watershed in Catonsville, Baltimore County, Maryland. Measurements include radiological activity for rainwater and sediment samples, sediment particle size information, suspended sediment concentration measurements, elemental composition of sediments, andHydrologic, biogeochemical, and radon data collected within and adjacent to the Little Wind River near Riverton, Wyoming
The U.S. Geological Survey is studying the interaction of a contaminated groundwater plume enriched in uranium and other trace elements with water, sediment, and biota along a 3 km reach of the Little Wind River in central Wyoming. The source of the contaminants is from a reclaimed uranium mill site near Riverton, Wyoming. The study is being done in collaboration with the Department of Energy, Uni - Multimedia
- Publications
Filter Total Items: 82
Aquatic insect accumulation of uranium at spring outflows in the Grand Canyon region as influenced by aqueous and sediment geochemistry and biological factors: Implications for monitoring
Potential adverse ecological effects of expanded uranium (U) mining within the Grand Canyon region motivated studies to better understand U exposure and risk to endemic species. This study documents U exposures and analyzes geochemical and biological factors affecting U bioaccumulation at spring-fed systems within the Grand Canyon region. The principal objective was to determine if aqueous U was bAuthorsDaniel J. Cain, Marie-Noële Croteau, Christopher C. Fuller, David Barasch, Kimberly R. Beisner, Kate M. Campbell, Deborah Stoliker, Edward J. SchenkInteraction of a legacy groundwater contaminant plume with the Little Wind River from 2015 through 2017, Riverton Processing site, Wyoming
The Riverton Processing site was a uranium mill 4 kilometers southwest of Riverton, Wyoming, that prepared uranium ore for nuclear reactors and weapons from 1958 to 1963. The U.S. Department of Energy completed surface remediation of the uranium tailings in 1989; however, groundwater below and downgradient from the tailings site and nearby Little Wind River was not remediated. Beginning in 2010, aAuthorsDavid L. Naftz, Christopher C. Fuller, Robert L. Runkel, John Solder, W. Payton Gardner, Neil Terry, Martin A. Briggs, Terry M. Short, Daniel J. Cain, William L Dam, Patrick A. Byrne, James R. CampbellSediment sources and sealed-pavement area drive polycyclic aromatic hydrocarbon and metal occurrence in urban streams
Metals and polycyclic aromatic hydrocarbons (PAHs) are common pollutants in urban streambed sediment, yet their occurrence is highly variable and difficult to predict. To investigate sources of PAHs and metals to streambed sediment, we sampled pavement dust, soil, and streambed sediment in 10 urban watersheds in three regions of the United States and applied a fallout-radionuclide-based sediment-sAuthorsPeter C. Van Metre, Barbara Mahler, Sharon L. Qi, Allen Gellis, Christopher C. Fuller, Travis S. SchmidtInfluence of permafrost type and site history on losses of permafrost carbon after thaw
We quantified permafrost peat plateau and post-thaw carbon (C) stocks across a chronosequence in Interior Alaska to evaluate the amount of C lost with thaw. Macrofossil reconstructions revealed three stratigraphic layers of peat: (1) a base layer of fen/marsh peat, (2) peat from a forested peat plateau (with permafrost) and, (3) collapse-scar bog peat (at sites where permafrost thaw has occurred).AuthorsKristen L. Manies, Miriam C. Jones, Mark Waldrop, Mary-Catherine Leewis, Christopher C. Fuller, Robert S. Cornman, Kristen HoefkeA 450-year record of environmental change from Castle Lake, California (USA), inferred from diatoms and organic geochemistry
A 39-cm sediment core from Castle Lake, California (USA) spans the last ~ 450 years and was analyzed for diatoms and organic geochemistry (δ15N, δ13C, and C:N), with the goal of determining sensitivity to natural climate variation and twentieth century anthropogenic effects. Castle Lake is a subalpine, nitrogen-limited lake with ~ 5 months of annual ice cover. Human impacts include light recreatioAuthorsPaula Noble, Gary A. McGaughey, Michael R. Rosen, Christopher C. Fuller, Marco A. Aquino-López, Sudeep ChandraTransport and speciation of uranium in groundwater-surface water systems impacted by legacy milling operations
Growing worldwide concern over uranium contamination of groundwater resources has placed an emphasis on understanding uranium transport dynamics and potential toxicity in groundwater-surface water systems. In this study, we utilized novel in-situ sampling methods to establish the location and magnitude of contaminated groundwater entry into a receiving surface water environment, and to investigateAuthorsPatrick A. Byrne, Christopher C. Fuller, David L. Naftz, Robert L. Runkel, Niklas J Lehto, William L DamUranium bioaccumulation dynamics in the mayfly Neocloeon triangulifer and application to site-specific prediction
Little is known about the underlying mechanisms governing the bioaccumulation of uranium (U) in aquatic insects. We experimentally parameterized conditional rate constants for aqueous U uptake, dietary U uptake, and U elimination for the aquatic baetid mayfly Neocloeon triangulifer. Results showed that this species accumulates U from both the surrounding water and diet, with waterborne uptake prevAuthorsBrianna L. Henry, Marie-Noële Croteau, David Walters, Janet L. Miller, Daniel J. Cain, Christopher C. FullerPavement alters delivery of sediment and fallout radionuclides to urbanstreams
Sediment from urban impervious surfaces has the potential to be an important vector for contaminants, particularly where stormwater culverts and other buried channels draining large impervious areas exit from underground pipes into open channels. To better understand urban sediment sources and their relation to fallout radionuclides, we collected samples of rainfall, urban sediment (pavement sedimAuthorsAllen Gellis, Christopher C. Fuller, Peter C. Van Metre, Barbara Mahler, C. Welty, Andrew Miller, Lucas A Nibert, Zachary Clifton, Jeremy Malen, J.T. KemperCombining sediment fingerprinting with age-dating sediment using fallout radionuclides for an agricultural stream, Walnut Creek, Iowa, USA
PurposeThe main purpose of this study was to demonstrate the utility of the sediment fingerprinting approach to apportion surface-derived sediment, and then age date that portion using short-lived fallout radionuclides. In systems where a large mass of mobile sediment is in channel storage, age dating provides an understanding of the transfer of sediment through the watershed and the time scales oAuthorsAllen Gellis, Christopher C. Fuller, Peter C. Van Metre, Christopher T. Filstrup, Kevin Cole, Timur SabitovCompetitive interactions among H, CU, and Zn ion moderate aqueous uptake of Cu and Zn by an aquatic insect
The absorption of aqueous copper (Cu) and zinc (Zn) by aquatic insects, a group widely used to assess water quality, is unresolved. This study examined interactions among Cu, Zn, and protons that potentially moderate Cu and Zn uptake by the acid-tolerant stonefly Zapada sp. Saturation uptake kinetics was imposed to identify competitive mechanisms. Decreasing pH reduced the maximum transport capaciAuthorsDaniel J. Cain, Marie-Noële Croteau, Christopher C. FullerCarbon accumulation and vertical accretion in a restored vs. historic salt marsh in southern Puget Sound, Washington, United States
Few comparisons exist between vertical accretion (VA) and carbon accumulation rates (CARs), in restored vs. historic (i.e., reference) marshes. Here we compare these processes in a formerly diked, sparsely vegetated, restored salt marsh (Six Gill Slough, SG), whose surface is subsided relative to the tidal frame, to an adjacent, relatively pristine, historic salt marsh (Animal Slough, AS). Six sAuthorsJudith Z. Drexler, Isa Woo, Christopher C. Fuller, Glynnis NakaiThe approaching obsolescence of 137Cs dating of wetland soils in North America
The peak fallout in 1963 of the radionuclide 137Cs has been used to date lake, reservoir, continental shelf, and wetland sedimentary deposits. In wetlands such dating is used to project the ability of wetlands to keep pace with sea level rise and develop strategies for mitigating carbon pollution using biological carbon sequestration. Here we demonstrate that reliable 137Cs profiles are increasingAuthorsJudith Z. Drexler, Christopher C. Fuller, Stacey A. Archfield