Publications
All of our publications are accessible through the USGS Publication Warehouse. Publications by scientists of the Oregon Water Science Center are listed below.
Filter Total Items: 786
A synoptic approach for analyzing erosion as a guide to land-use planning A synoptic approach for analyzing erosion as a guide to land-use planning
A synoptic approach has been devised to delineate the relationships that exist' between physiographic factors, land-use activities, and resultant erosional problems. The approach involves the development of an erosional-depositional province map and a numerical impact matrix for rating the potential for erosional problems. The province map is prepared by collating data on the natural...
Authors
William M. Brown, Walter G. Hines, David A. Rickert, Gary L. Beach
Ground water in Myrtle Creek - Glendale area, Douglas County, Oregon Ground water in Myrtle Creek - Glendale area, Douglas County, Oregon
The Myrtle Creek-Glendale area covers about 400 mi2 (1,000 km2 in Douglas County in southwestern Oregon. Although the geologic formations of the area have low permeabilities and generally yield small amounts of water to wells, ground water is the chief source of water for domestic usse in rural parts of the area not served by public supplies. A well capable of yielding 5 to 10 gal/min (0...
Authors
F. J. Frank
Water-quality data from five Oregon stream basins Water-quality data from five Oregon stream basins
The U.S. Geological Survey collected water-quality data in five Oregon stream basins during summer low-flow conditions in 1977 and 1978. During the two sampling periods, a total of 18 different sites were sampled. Several sites were sampled twice in 1977, and some sites were sampled in both 1977 and 1978. Included in the sampling were diel trace of dissolved oxygen, temperature, specific
Authors
Timothy L. Miller
Water availability and flood hazards in the John Day Fossil Beds National Monument, Oregon Water availability and flood hazards in the John Day Fossil Beds National Monument, Oregon
The rock formations of the John Day Fossil Beds National Monument area are aquifers that can be expected to yield less than 10 gallons of water per minute to wells. The most permeable of the geologic units is the alluvium that occurs at low elevations along the John Day River and most of the smaller streams. Wells in the alluvial deposits can be expected to yield adequate water supplies...
Authors
Frank J. Frank, E. A. Oster
Benthic invertebrates, periphyton, and bottom material and their trace-metal concentrations in Salmon Creek basin, Clark County, Washington Benthic invertebrates, periphyton, and bottom material and their trace-metal concentrations in Salmon Creek basin, Clark County, Washington
In 1978, data were collected for identification and quantification of benthic invertebrates, periphyton, and bottom material and their trace-metals concentrations from three sites in Salmon Creek basin, Wash. Metal analyses included arsenic, cadmium, chromium, copper, lead, zinc, selenium, and mercury. Physical data collected included water temperature, dissolved oxygen, pH, discharge...
Authors
Amy C. White, Stuart W. McKenzie
Ground-water data in the Baker County-northern Malheur County area, Oregon Ground-water data in the Baker County-northern Malheur County area, Oregon
Ground-water data for the Baker County-northern Malheur area, Oregon, are tabulated for the Bureau of Land Management. The data include well and spring records, a well-location map, drillers' logs of wells, observation-well hydrographs, and chemical analyses of ground-water samples. The reported yields of wells and springs in the area ranged from less than 1 to 2,500 gallons per minute...
Authors
C. A. Collins
Steady-state dissolved oxygen model of the Willamette River, Oregon Steady-state dissolved oxygen model of the Willamette River, Oregon
For nearly half a century the Willamette River in Oregon experienced severe dissolved-oxygen problems related to large loads of organically rich waste waters from industries and municipalities. Since the mid-1950 's dissolved oxygen quality has gradually improved owing to low-flow augmentation, the achievement of basinwide secondary treatment, and the use of other waste-management...
Authors
Stuart W. McKenzie, W. G. Hines, D. A. Rickert, F. A. Rinella
Storm-water data for Bear Creek basin, Jackson County, Oregon 1977-78 Storm-water data for Bear Creek basin, Jackson County, Oregon 1977-78
Storm-water-quality samples were collected from four subbasins in the Bear Creek basin in southern Oregon. These subbasins vary in drainage size, channel slope, effective impervious area, and land use. Automatic waterquality samplers and precipitation and discharge gages were set up in each of the four subbasins. During the period October 1977 through May 1978, 19 sets of samples...
Authors
Loren A. Wittenberg
Sediment sources and Holocene sedimentation history in Tillamook Bay, Oregon; data and preliminary interpretations Sediment sources and Holocene sedimentation history in Tillamook Bay, Oregon; data and preliminary interpretations
Surface and core sediments from Tillamook Bay, Oregon, have been analyzed to determine modern and Holocene sediment sources and sedimentation history. Heavy mineral analyses established three sediment sources: (1) the five major rivers draining the volcanic and associated sedimentary rocks of the Coast Range, (2) small streams draining the sedimentary uplands that form the shoreline...
Authors
Jerry L. Glenn
Monitoring water-quality during pilot-dredging operations in the Willamette and Columbia Rivers, Oregon Monitoring water-quality during pilot-dredging operations in the Willamette and Columbia Rivers, Oregon
Water quality was monitored in the Willamette and Columbia Rivers during a pilot dredging operation on December 16, 1977. Monitoring included in-situ measurements of pH, temperature, dissolved oxygen, and conductivity in the Willamette and Columbia Rivers; analyses of dissolved ammonia, dissolved manganese, suspended-sediment concentration and particle size, loss on ignition, and total...
Authors
Joseph F. Rinella, Stuart W. McKenzie
Rainfall-runoff data for selected basins, Portland, Oregon, and Vancouver, Washington, 1973-77 Rainfall-runoff data for selected basins, Portland, Oregon, and Vancouver, Washington, 1973-77
In the Portland-Vancouver area, storms and floods are presently being studied in 16 basins with drainage areas ranging from 0.21 to 6.63 square miles and with various basin slopes, degrees of imperviousness, and mixes of land use. Fanno Creek basin in Portland has the longest period of rainfall-runoff record, starting in 1973; Tryon Creek basin in Portland is next with a record starting...
Authors
Antonius Laenen, Gary L. Solin
Hydrologic data in Bear Creek Basin and western Jackson County, Oregon, 1976-77 Hydrologic data in Bear Creek Basin and western Jackson County, Oregon, 1976-77
To determine irrigation return flow impacts on Meyer Creek and Griffin Creek, 12 sites were sampled prior to and during the irrigation season. Thirty-three sets of samples, consisting of irrigation inflow and outflow samples on farms, were collected to determine if the use of irrigation water was improving or degrading the water quality. One hundred fifty visits were made to tributaries...
Authors
Loren A. Wittenberg, Stuart W. McKenzie