William J Andrews, PhD
Bill Andrews is a Science Coordinator for the USGS Rocky Mountain Region. He has worked for the USGS since 1988. His previous positions in the USGS include Hydrologist, Webmaster, Water-Quality Specialist, Groundwater Specialist, Report Specialist, Section Chief, and Center Director.
Biography
Bill Andrews earned a Bachelor of Science Degree in Geology (College of William and Mary), a Master of Science Degree in Geology (Northern Illinois University), and a Doctoral Degree in Environmental Science (University of Oklahoma). He has served in a wide range of technical and supervisory roles at USGS offices in Florida, Minnesota, and Oklahoma and has assisted in several headquarters projects. Bill has lead-authored or coauthored 40 USGS-series publications, 11 journal papers, 17 conference abstracts or proceedings papers, and has given numerous talks about hydrology, emerging contaminants, relations between land uses and water quality, climate change, and induced seismicity. He currently serves as a Science Coordinator for the Rocky Mountain Region of the USGS, which involves reviewing and writing technical documents and publications, and reviewing center science programs.
Science and Products
Evaluation and trends of land cover, streamflow, and water quality in the North Canadian River Basin near Oklahoma City, Oklahoma, 1968-2009
The U.S. Geological Survey, in cooperation with the city of Oklahoma City, collected water-quality samples from the North Canadian River at the streamflow-gaging station near Harrah, Oklahoma (Harrah station), since 1968, and at an upstream streamflow-gaging station at Britton Road at Oklahoma City, Oklahoma (Britton Road station), since 1988....
Esralew, Rachel A.; Andrews, William J.; Smith, S. JerrodChanges in Selected Metals Concentrations from the Mid-1980s to the Mid-2000s in a Stream Draining the Picher Mining District of Oklahoma
After abandonment in the late 1960s, the Picher mining district of Oklahoma, once the largest source of lead and zinc in the world, continued to be affected by severe environmental degradation, with scattered subsidence and abundant toxic metals such as cadmium and lead seeping from flooded underground mine workings and seeping and running off...
Andrews, William J.; Masoner, Jason R.Challenges in design and construction of a large multi-cell passive treatment system for ferruginous lead-zinc mine waters
Artesian discharges of net alkaline, ferruginous waters from abandoned underground lead-zinc mines cause considerable surface water degradation at the Tar Creek Superfund Site, part of the historic Tri-State Mining District of Oklahoma, Kansas and Missouri. Two perennial borehole discharges, identified as the lowest elevation mine water discharge...
Nairn, Robert W.; Beisel, T.; Thomas, Robert C.; LaBar, Julie A.; Strevett, Keith A. ; Fuller, Daniel; Strosnider, William H.; Andrews, William J.; Bays, James; Knox, Robert C.Summary of surface-water quality data from the Illinois River Basin in Northeast Oklahoma, 1970-2007
The quality of streams in the Illinois River Basin of northeastern Oklahoma is potentially threatened by increased quantities of wastes discharged from increasing human populations, grazing of about 160,000 cattle, and confined animal feeding operations raising about 20 million chickens. Increasing numbers of humans and livestock in the basin...
Andrews, William J.; Becker, Mark F.; Smith, S. Jerrod; Tortorelli, Robert L.Selected metals in sediments and streams in the Oklahoma Part of the Tri-State Mining District, 2000-2006
The abandoned Tri-State mining district includes 1,188 square miles in northeastern Oklahoma, southeastern Kansas, and southwestern Missouri. The most productive part of the Tri-State mining district was the 40-square mile part in Oklahoma, commonly referred to as 'the Picher mining district' in north-central Ottawa County, Oklahoma. The Oklahoma...
Andrews, William J.; Becker, Mark F.; Mashburn, Shana L.; Smith, S. JerrodStreamflow, water quality, and metal loads from chat leachate and mine outflow into Tar Creek, Ottawa County, Oklahoma, 2005
Picher mining district is an abandoned lead and zinc mining area located in Ottawa County, northeastern Oklahoma. During the first half of the 20th century, the area was a primary producer of lead and zinc in the United States. Large accumulations of mine tailings, locally referred to as chat, produce leachate containing cadmium, iron, lead, and...
Cope, Caleb C.; Becker, Mark F.; Andrews, William J.; DeHay, KelliPreliminary assessment of time trends in bioavailable metals in the Tri-State lead/zinc mining district through analysis of tree cores
The Tri-State mining district in the central U.S. was a major source of zinc and lead from the early 1800s to 1970, producing 11.7 million tons of zinc, and 2.8 million tons of lead. Soils and streams in more than 70 square miles of the mining district and downstream areas are contaminated by metals. Little environmental monitoring was conducted...
Andrews, William J.; Nairn, Robert W.; Minarik, William G.Water-quality assessment of part of the Upper Mississippi River basin, Minnesota and Wisconsin - Ground-water quality along a flow system in the Twin Cities metropolitan area, Minnesota, 1997-98
As part of a national analysis of the effects of land use on ground-water quality for the National Water-Quality Assessment Program, the U.S. Geological Survey sampled wells along a flow system in surficial glacial aquifers in the northwestern part of the Twin Cities metropolitan area during 1997 and 1998. In addition, a reconnaissance steady-...
Andrews, William J.; Stark, James R.; Fong, Alison L.; Fallon, James D.Regional cooperation for water management, northern tier meeting—Iraqis, Jordanians, Lebanese, Syrians, and Turks
No abstract available.
Andrews, William J.; Ragep, SallyHydrology and ground-water quality in the mine workings within the Picher Mining District, Northeastern Oklahoma, 2002-03
The Picher mining district of northeastern Ottawa County, Oklahoma, was a major site of mining for lead and zinc ores in the first half of the 20th century. The primary source of lead and zinc were sulfide minerals disseminated in the cherty limestones and dolomites of the Boone Formation of Mississippian age, which comprises the Boone aquifer....
DeHay, Kelli L.; Andrews, William J.; Sughru, Michael P.Phosphorus concentrations, loads, and yields in the Illinois River Basin, Arkansas and Oklahoma, 1997-2001
The Illinois River and tributaries, Flint Creek and the Baron Fork, are designated scenic rivers in Oklahoma. Recent phosphorus increases in streams in the basin have resulted in the growth of excess algae, which have limited the aesthetic benefits of water bodies in the basin, especially the Illinois River and Lake Tenkiller. The Oklahoma Water...
Pickup, Barbara E.; Andrews, William J.; Haggard, Brian E.; Green, W. ReedGround-water quality in the Central High Plains Aquifer, Colorado, Kansas, New Mexico, Oklahoma, and Texas, 1999
A network of 74 randomly distributed domestic water-supply wells completed in the central High Plains aquifer was sampled and analyzed from April to August 1999 as part of the High Plains Regional Ground-Water Study conducted by the U. S. Geological Survey National Water-Quality Assessment Program to provide a broad-scale assessment of the ground-...
Becker, Mark F.; Bruce, Breton W.; Pope, Larry M.; Andrews, William J.