Geology ReportsSearch

Geology topics

M.A. Beckwith

Publications and source records attributed to M.A. Beckwith.

2 recordsLinked to original sources

Concepts for monitoring water quality in the Spokane River Basin, northern Idaho and eastern Washington

Numerous environmental studies have been conducted in the Spokane River Basin over the past several decades by government agencies, academic institutions, and environmental engineering firms. Most of these efforts have focused on the environmental effects of more than a century of silver, lead, and zinc mining and oreprocessing activities in the South Fork Coeur d'Alene River valley in northern Idaho. Several studies also have assessed the water quality and potential for eutrophication of Coeur d'Alene and Long Lakes and the Coeur d'Alene, St. Joe, and Spokane Rivers. Because past investigations often were limited in scope and employed different approaches and methods, an integrated understanding of hydrologic, water-quality, and aquatic biological conditions still is lacking for the basin as a whole. Substantial resources are being spent for water-quality and naturalresource management, and for mitigating the adverse environmental effects of past mining activities in the basin. A water-quality monitoring network, integrated with the decision-making processes associated with these efforts, could be of considerable value. The purpose of such a monitoring network is to produce high-quality information on which to base sound water-quality and natural-resource management decisions and to assess the effectiveness of those decisions. A streamflow- and water-quality monitoring infrastructure already exists in the Spokane River Basin. This infrastructure consists of 20 lake-stage and streamflow-gaging stations, representing specific drainages or subdrainages and, in many cases, specific stream reaches or subreaches. These gaging stations are operated by the U.S. Geological Survey (USGS), several of them in cooperation with State and Federal agencies and a private utility company. Extensive streamflow data are available, some dating from the late 1800s. Water-quality data are also available from recent USGS cooperative studies in the Coeur d'Alene Lake watershed. A nutrient load/lake response (eutrophication) model has been developed for Coeur d'Alene Lake. Hydraulic models for estimating streamflow through the low-gradient reaches of the Coeur d'Alene and St. Joe Rivers have been developed. Trace-element concentrations and distributions in sediments in the lower South Fork and main-stem Coeur d'Alene River flood plain and the bed of Coeur d'Alene Lake have been assessed. Trace-element transport models have been developed for the lower Coeur d'Alene River system; estimates of annual load are available from the early 1990's to the present (1998). The USGS is monitoring traceelement concentrations and transport at seven gaging stations in the lower Coeur d'Alene River system and upper Spokane River, in cooperation with the U.S. Environmental Protection Agency. Fish and macroinvertebrate community assessment and tissue contaminant analyses at four Coeur d'Alene and St. Joe River gaging stations will begin in 1998, either as part of the Idaho Surface- Water Quality Ambient Monitoring Network operated by USGS in cooperation with the Idaho Division of Environmental Quality, or for the Northern Rockies Intermontane Basins (NROK) study of the USGS National Water-Quality Assessment (NAWQA) Program. Several gaging stations in the Spokane River Basin are being considered for routine sampling sites for the NROK NAWQA study. Several other sites also will be sampled for contaminants in bed sediment and fish tissue for the NROK study. Combined with appropriate sampling and data interpretation strategies, the existing USGS gaging-station network and data base could provide integrated water-quality information needed for sound environmental and resource-management decisions throughout the Spokane River Basin.

Idaho;Washington

Nutrient and trace-element enrichment of Coeur d'Alene Lake, Idaho

The limnological characteristics and geochemistry of lakebed sediments in Coeur d'Alene Lake, a 129-square-kilometer, natural lake in northern Idaho, were assessed during 1991-92 because of the possible interaction of nutrient enrichment with the highly enriched trace-element concentrations stored in the lakebed. The lake was classified as oligotrophic during 1991-92 on the basis of annual geometric mean concentrations, in micrograms per liter, of total phosphorus (4.1), total nitrogen (247), and chlorophyll-a (0.54). Despite its oligotrophy, the lake developed a substantial hypolimnetic dissolved-oxygen deficit in both years during the later stage of thermal stratification. The lake's current trophic state of oligotrophic differs from the mesotrophic ranking it received in 1975 during the National Eutrophication Survey. The shift in trophic state was consistent with nutrient-load reductions that have occurred within the lake's 9,690-square-kilometer drainage basin since the early 1970's. Approximately 85 percent of the lakebed's surface area was highly enriched in antimony, arsenic, cadmium, lead, mercury, silver, and zinc. Mean total concentrations, in milligrams per kilogram, for cadmium, lead, and zinc in the enriched lakebed sediments were, respectively, 62, 1,900, and 3,600. In contrast, the concentrations of cadmium, lead, and zinc in unenriched lakebed sediments in the lake's southern end were, respec- tively, 2.8, 24, and 110 milligrams per kilogram. The vast majority of the trace elements in the surficial and subsurface sediments were associated with ferric oxides, not sulfides as previously postulated. Under reducing conditions, such as within as anoxic hypolimnon, the ferric oxide- associated trace elements would be readily soluble and available for release into the overlying water column. (USGS)

Idaho