Kimberly R. Beisner
Kimberly Beisner is a Research Hydrologist for the New Mexico Water Science Center. She received a Master's of Science Degree in Geology from the University of Utah and a Bachelors of Science Degree in Geology from the University of Kansas.
Kimberly's USGS experience started in the Utah Water Science Center as a graduate student working on mercury and selenium associated with the Great Salt Lake and abandoned uranium mines in southern Utah. Following graduation, she joined the Arizona Water Science center where she has worked on geochemical studies related to the lands withdrawn from uranium mining near the Grand Canyon, water resources at Saguaro National Park, and stable isotope and noble gas evaluation groundwater of the Verde watershed to understand recharge elevation. She served as the New Mexico Water Quality specialist and is now a research hydrologist focused on multiple geochemical and anthropogenic tracers including per- and polyfluoroalkyl substances and continues to work with the Arizona Water Science Center in the Grand Canyon.
Professional Experience
2023 to present: Research Hydrologist, U.S. Geological Survey, New Mexico Water Science Center, Albuquerque, New Mexico
2017 to 2023: Water Chemistry Specialist, U.S. Geological Survey, New Mexico Water Science Center, Albuquerque, New Mexico
2008 to 2017: Hydrologist, U.S. Geological Survey, Arizona Water Science Center, Tucson, Arizona
2007 to 2008: Student Trainee, U.S. Geological Survey, Utah Science Center, Salt Lake City, Utah
Education and Certifications
M.S. Geology (2008), University of Utah (Thesis "Selenium and trace element mobility affected by periodic interruption of stratification in the Great Salt Lake, Utah")
B.S. Environmental Geology (2006), University of Kansas (Thesis "Short-term water-level fluctuations and long-term water-level decline at the Konza Prairie: Drought or Vegetation?")
Science and Products
Filter Total Items: 34
Geochemical assessment of groundwater in the Big Chino subbasin, Arizona, 2011–18
A geochemical characterization of groundwater in the Big Chino subbasin of Arizona was conducted by the U.S. Geological Survey, in cooperation with the City of Prescott, the Town of Prescott Valley, and the Salt River Project, to understand groundwater evolution through the study area and the source of water to springs along the gaining reach of the Verde River just downstream from its confluence
Authors
Kimberly R. Beisner, Casey J. R. Jones
Rethinking groundwater flow on the South Rim of the Grand Canyon, USA: Characterizing recharge sources and flow paths with environmental tracers
In the arid landscape south of the Grand Canyon, natural springs and seeps are a critical resource for endemic species and Native American tribes. Groundwater is potentially threatened by expanding populations, visitations, and mineral extraction activities. Environmental tracers including noble gases, stable isotopes of hydrogen and oxygen in water, tritium, and carbon-14 were used to characteriz
Authors
John E. Solder, Kimberly R. Beisner, Jessica R. Anderson, Donald J. Bills
Critical evaluation of stable isotope mixing end-members for estimating groundwater recharge sources: Case study from the South Rim of the Grand Canyon, Arizona, USA
Springs and groundwater seeps along the South Rim of the Grand Canyon serve an important function for the region’s ecosystems, residents (both human and wild animal), and economy. However, these springs and seeps are potentially vulnerable to contamination, increased groundwater extraction, or reduced recharge due to climate change. Protection of South Rim groundwater resources requires improved u
Authors
John E. Solder, Kimberly R. Beisner
Geochemical characterization of groundwater evolution south of Grand Canyon, Arizona (USA)
Better characterization of the geochemical evolution of groundwater south of Grand Canyon, Arizona (USA), is needed to understand natural conditions and assess potential effects from breccia-pipe uranium mining in the region. Geochemical signatures of groundwater at 28 sampling locations were evaluated; baseline concentrations for select trace elements (As, B, Ba, Cr, Li, Mo, Rb, Se, Sr, Th, Tl, U
Authors
Kimberly R. Beisner, John E. Solder, Fred D. Tillman, Jessica R. Anderson, Ronald C. Antweiler
Characterization and load estimation of polychlorinated biphenyls (PCBs) from selected Rio Grande tributary stormwater channels in the Albuquerque urbanized area, New Mexico, 2017–18
In cooperation with the New Mexico County of Bernalillo, the U.S. Geological Survey characterized potential polychlorinated biphenyl (PCB) concentration and estimated loading into the Rio Grande from watersheds that are under the county’s jurisdiction. Water and sediment samples were collected in 2017–18 from six sites within four stormwater drainage basins in the Albuquerque, New Mexico, urbanize
Authors
Zachary M. Shephard, Kathleen E. Conn, Kimberly R. Beisner, Alanna D. Jornigan, Christina F. Bryant
Brackish groundwater and its potential as a resource in the southwestern United States
Secure, reliable, and sustainable water resources are fundamental to food production, energy independence, and the health of humans and ecosystems. But the large-scale development of fresh groundwater resources has stressed aquifers in some areas, causing declines in the amount of groundwater in storage and decreases in discharge to surface-water bodies like rivers and springs (Reilly and others,
Authors
David W. Anning, Kimberly R. Beisner, Angela P. Paul, Jennifer S. Stanton, Susan A. Thiros
Geochemical characterization and modeling of regional groundwater contributing to the Verde River, Arizona between Mormon Pocket and the USGS Clarkdale gage
We use synoptic surveys of stream discharge, stable isotopes, and dissolved noble gases to identify the source of groundwater discharge to the Verde River in central Arizona. The Verde River more than doubles in discharge in Mormon Pocket over a 1.4 km distance that includes three discrete locations of visible spring input to the river and other diffuse groundwater inputs. A detailed study of th
Authors
Kimberly R. Beisner, W. Payton Gardner, Andrew G. Hunt
Assessment of geochemical and hydrologic conditions near Old Yuma Mine in Saguaro National Park, Arizona, 2014–17
The Old Yuma Mine is an abandoned copper, lead, zinc, silver, and gold mine located within the boundaries of Saguaro National Park, Tucson Mountain District, Arizona. This study analyzed the geochemistry of sediments associated with the Old Yuma Mine and assessed hydrologic and geochemical conditions of groundwater to evaluate the area surrounding the Old Yuma Mine. The purpose of the study was to
Authors
Kimberly R. Beisner, Floyd Gray
Geochemical characterization of groundwater discharging from springs north of the Grand Canyon, Arizona, 2009–2016
A geochemical study was conducted on 37 springs discharging from the Toroweap Formation, Coconino Sandstone, Hermit Formation, Supai Group, and Redwall Limestone north of the Grand Canyon near areas of breccia-pipe uranium mining. Baseline concentrations were established for the elements As, B, Li, Se, SiO2, Sr, Tl, U, and V. Three springs exceeded U.S. Environmental Protection Agency drinking wat
Authors
Kimberly R. Beisner, Fred D. Tillman, Jessica R. Anderson, Ronald C. Antweiler, Donald J. Bills
Geochemistry and hydrology of perched groundwater springs: assessing elevated uranium concentrations at Pigeon Spring relative to nearby Pigeon Mine, Arizona (USA)
The processes that affect water chemistry as the water flows from recharge areas through breccia-pipe uranium deposits in the Grand Canyon region of the southwestern United States are not well understood. Pigeon Spring had elevated uranium in 1982 (44 μg/L), compared to other perched springs (2.7–18 μg/L), prior to mining operations at the nearby Pigeon Mine. Perched groundwater springs in an area
Authors
Kimberly R. Beisner, Nicholas V. Paretti, Fred D. Tillman, David L. Naftz, Donald J. Bills, Katherine Walton-Day, Tanya J. Gallegos
Analysis of stable isotope ratios (δ18O and δ2H) in precipitation of the Verde River watershed, Arizona 2003 through 2014
Stable isotope delta values (δ18O and δ2H) of precipitation can vary with elevation, and quantification of the precipitation elevation gradient can be used to predict recharge elevation within a watershed. Precipitation samples were analyzed for stable isotope delta values between 2003 and 2014 from the Verde River watershed of north-central Arizona. Results indicate a significant decrease in summ
Authors
Kimberly R. Beisner, Nicholas V. Paretti, Rachel S. Tucci
Initial characterization of the groundwater system near the Lower Colorado Water Supply Project, Imperial Valley, California
In 2009, the U.S. Geological Survey, in cooperation with the city of Needles, began a study of the hydrogeology along the All-American Canal, which conveys water from the Colorado River to the Imperial Valley. The focus of this study was to gain a better understanding of the effect of lining the All-American Canal, and other management actions, on future total dissolved solids concentrations in gr
Authors
Alissa L. Coes, Michael Land, Jill N. Densmore, Michael T. Landrum, Kimberly R. Beisner, Jeffrey R. Kennedy, Jamie P. Macy, Fred D. Tillman
Non-USGS Publications**
Beisner, K.R., Paretti, N., Tillman, F.D., Naftz, D.L., Bills, D., Walton-Day, K., Gallegos, T.J., (2016) Assessing Pigeon uranium mine waste geochemistry for comparison with nearby perched groundwater springs: Geological Society of America Abstracts with Programs vol. 48, no. 7 paper no. 269-7.
Beisner K, Naftz DL, Diaz X, Johnson G, Johnson WP. (2007) Oxidation of sequestered selenium in the water column of the Great Salt Lake, Utah, USA. Geological Society of America Abs. with Prog., vol 39, no 6, p 104.
Beisner K, Johnson WP, Naftz DL. (2006) Selenium re-suspension in the water column of the Great Salt Lake. Eos Trans. AGU, 87(52), Fall Meet. Suppl., Abstract H53A-0595.
**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.
Science and Products
Filter Total Items: 34
Geochemical assessment of groundwater in the Big Chino subbasin, Arizona, 2011–18
A geochemical characterization of groundwater in the Big Chino subbasin of Arizona was conducted by the U.S. Geological Survey, in cooperation with the City of Prescott, the Town of Prescott Valley, and the Salt River Project, to understand groundwater evolution through the study area and the source of water to springs along the gaining reach of the Verde River just downstream from its confluence
Authors
Kimberly R. Beisner, Casey J. R. Jones
Rethinking groundwater flow on the South Rim of the Grand Canyon, USA: Characterizing recharge sources and flow paths with environmental tracers
In the arid landscape south of the Grand Canyon, natural springs and seeps are a critical resource for endemic species and Native American tribes. Groundwater is potentially threatened by expanding populations, visitations, and mineral extraction activities. Environmental tracers including noble gases, stable isotopes of hydrogen and oxygen in water, tritium, and carbon-14 were used to characteriz
Authors
John E. Solder, Kimberly R. Beisner, Jessica R. Anderson, Donald J. Bills
Critical evaluation of stable isotope mixing end-members for estimating groundwater recharge sources: Case study from the South Rim of the Grand Canyon, Arizona, USA
Springs and groundwater seeps along the South Rim of the Grand Canyon serve an important function for the region’s ecosystems, residents (both human and wild animal), and economy. However, these springs and seeps are potentially vulnerable to contamination, increased groundwater extraction, or reduced recharge due to climate change. Protection of South Rim groundwater resources requires improved u
Authors
John E. Solder, Kimberly R. Beisner
Geochemical characterization of groundwater evolution south of Grand Canyon, Arizona (USA)
Better characterization of the geochemical evolution of groundwater south of Grand Canyon, Arizona (USA), is needed to understand natural conditions and assess potential effects from breccia-pipe uranium mining in the region. Geochemical signatures of groundwater at 28 sampling locations were evaluated; baseline concentrations for select trace elements (As, B, Ba, Cr, Li, Mo, Rb, Se, Sr, Th, Tl, U
Authors
Kimberly R. Beisner, John E. Solder, Fred D. Tillman, Jessica R. Anderson, Ronald C. Antweiler
Characterization and load estimation of polychlorinated biphenyls (PCBs) from selected Rio Grande tributary stormwater channels in the Albuquerque urbanized area, New Mexico, 2017–18
In cooperation with the New Mexico County of Bernalillo, the U.S. Geological Survey characterized potential polychlorinated biphenyl (PCB) concentration and estimated loading into the Rio Grande from watersheds that are under the county’s jurisdiction. Water and sediment samples were collected in 2017–18 from six sites within four stormwater drainage basins in the Albuquerque, New Mexico, urbanize
Authors
Zachary M. Shephard, Kathleen E. Conn, Kimberly R. Beisner, Alanna D. Jornigan, Christina F. Bryant
Brackish groundwater and its potential as a resource in the southwestern United States
Secure, reliable, and sustainable water resources are fundamental to food production, energy independence, and the health of humans and ecosystems. But the large-scale development of fresh groundwater resources has stressed aquifers in some areas, causing declines in the amount of groundwater in storage and decreases in discharge to surface-water bodies like rivers and springs (Reilly and others,
Authors
David W. Anning, Kimberly R. Beisner, Angela P. Paul, Jennifer S. Stanton, Susan A. Thiros
Geochemical characterization and modeling of regional groundwater contributing to the Verde River, Arizona between Mormon Pocket and the USGS Clarkdale gage
We use synoptic surveys of stream discharge, stable isotopes, and dissolved noble gases to identify the source of groundwater discharge to the Verde River in central Arizona. The Verde River more than doubles in discharge in Mormon Pocket over a 1.4 km distance that includes three discrete locations of visible spring input to the river and other diffuse groundwater inputs. A detailed study of th
Authors
Kimberly R. Beisner, W. Payton Gardner, Andrew G. Hunt
Assessment of geochemical and hydrologic conditions near Old Yuma Mine in Saguaro National Park, Arizona, 2014–17
The Old Yuma Mine is an abandoned copper, lead, zinc, silver, and gold mine located within the boundaries of Saguaro National Park, Tucson Mountain District, Arizona. This study analyzed the geochemistry of sediments associated with the Old Yuma Mine and assessed hydrologic and geochemical conditions of groundwater to evaluate the area surrounding the Old Yuma Mine. The purpose of the study was to
Authors
Kimberly R. Beisner, Floyd Gray
Geochemical characterization of groundwater discharging from springs north of the Grand Canyon, Arizona, 2009–2016
A geochemical study was conducted on 37 springs discharging from the Toroweap Formation, Coconino Sandstone, Hermit Formation, Supai Group, and Redwall Limestone north of the Grand Canyon near areas of breccia-pipe uranium mining. Baseline concentrations were established for the elements As, B, Li, Se, SiO2, Sr, Tl, U, and V. Three springs exceeded U.S. Environmental Protection Agency drinking wat
Authors
Kimberly R. Beisner, Fred D. Tillman, Jessica R. Anderson, Ronald C. Antweiler, Donald J. Bills
Geochemistry and hydrology of perched groundwater springs: assessing elevated uranium concentrations at Pigeon Spring relative to nearby Pigeon Mine, Arizona (USA)
The processes that affect water chemistry as the water flows from recharge areas through breccia-pipe uranium deposits in the Grand Canyon region of the southwestern United States are not well understood. Pigeon Spring had elevated uranium in 1982 (44 μg/L), compared to other perched springs (2.7–18 μg/L), prior to mining operations at the nearby Pigeon Mine. Perched groundwater springs in an area
Authors
Kimberly R. Beisner, Nicholas V. Paretti, Fred D. Tillman, David L. Naftz, Donald J. Bills, Katherine Walton-Day, Tanya J. Gallegos
Analysis of stable isotope ratios (δ18O and δ2H) in precipitation of the Verde River watershed, Arizona 2003 through 2014
Stable isotope delta values (δ18O and δ2H) of precipitation can vary with elevation, and quantification of the precipitation elevation gradient can be used to predict recharge elevation within a watershed. Precipitation samples were analyzed for stable isotope delta values between 2003 and 2014 from the Verde River watershed of north-central Arizona. Results indicate a significant decrease in summ
Authors
Kimberly R. Beisner, Nicholas V. Paretti, Rachel S. Tucci
Initial characterization of the groundwater system near the Lower Colorado Water Supply Project, Imperial Valley, California
In 2009, the U.S. Geological Survey, in cooperation with the city of Needles, began a study of the hydrogeology along the All-American Canal, which conveys water from the Colorado River to the Imperial Valley. The focus of this study was to gain a better understanding of the effect of lining the All-American Canal, and other management actions, on future total dissolved solids concentrations in gr
Authors
Alissa L. Coes, Michael Land, Jill N. Densmore, Michael T. Landrum, Kimberly R. Beisner, Jeffrey R. Kennedy, Jamie P. Macy, Fred D. Tillman
Non-USGS Publications**
Beisner, K.R., Paretti, N., Tillman, F.D., Naftz, D.L., Bills, D., Walton-Day, K., Gallegos, T.J., (2016) Assessing Pigeon uranium mine waste geochemistry for comparison with nearby perched groundwater springs: Geological Society of America Abstracts with Programs vol. 48, no. 7 paper no. 269-7.
Beisner K, Naftz DL, Diaz X, Johnson G, Johnson WP. (2007) Oxidation of sequestered selenium in the water column of the Great Salt Lake, Utah, USA. Geological Society of America Abs. with Prog., vol 39, no 6, p 104.
Beisner K, Johnson WP, Naftz DL. (2006) Selenium re-suspension in the water column of the Great Salt Lake. Eos Trans. AGU, 87(52), Fall Meet. Suppl., Abstract H53A-0595.
**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.