4 edition of Preliminary estimates of benthic fluxes of dissolved metals in Coeur d"Alene Lake, Idaho found in the catalog.
Preliminary estimates of benthic fluxes of dissolved metals in Coeur d"Alene Lake, Idaho
by U.S. Dept. of the Interior, U.S. Geological Survey in Seattle, WA
Written in English
|Statement||by Laurie S. Balistrieri.|
|Series||Open-file report -- 98-793., U.S. Geological Survey open-file report -- 98-793.|
|Contributions||Geological Survey (U.S.)|
|The Physical Object|
|Number of Pages||40|
Coordinator, Benthic-flux study of contaminants into the water column of Lake Coeur d'Alene, ID, USEPA-funded ( to ) CALFED Technical Review Panel, Contaminants Proposals (August ) Special Session Chairman, American Society of Limnology and . Get this from a library! Benthic flux of metals and nutrients into the water column of Lake Coeur d'Alene, Idaho: report of an August, , pilot study. [James S Kuwabara; Geological Survey (U.S.);] -- Water resource investigation, monitoring for minerials in Lake Coeur d'Alene, Idaho.
The mean benthic flux of ammonia over the period of study was ab ± 13, kg-N/yr. Advective flux estimates from the external exchange over the tidal cycle ranged from −50 to kg-N/yr of ammonia. This difference of nearly two orders of magnitude suggests that benthic flux is a major source of ammonia to the water column for. Development and Research: Determining the Benthic Flux of Dissolved Metals CLICK PHOTOS FOR AN ENLARGED VERSION Photos of a coring operation showing the deployment of the non-metallic coring device, capping of the core upon retrieval, and removal of the core tube in .
Preliminary estimates of benthic fluxes of dissolved metals in Coeur d'Alene Lake, Idaho, , Open-File Report Scenarios for historic San Francisco . The use of diffusive gradients in thin films (DGT) for predicting metal bioavailability was investigated by exposing the bivalve Tellina deltoidalis to an identical series of metal-contaminated sediments deployed simultaneously in the field and laboratory. To understand the differences in metal exposure occurring between laboratory- and field-based bioassays, we investigated changes in metal.
Minutes of the special convention of the fertilizer industry held at Washington, D.C., January 10, 1927 ...
Ground-water flow and water quality in the sand aquifer of Long Beach Peninsula, Washington
Forget Not Your-Blank Book
John Morgan,continental doctor.
Two thirteenth-century walnut angels.
Signal Corps today
Improvement in infant and perinatal mortality in the United States
The ladies friend
Secularisation of Indian mind
The benthic flux calculations indicate that the sediment is generally a source of dissolved Zn, Cu, Mn, and, possibly, Pb to the overlying water column. These benthic fluxes are compared with two other major sources of metals to Coeur d'Alene Lake-the Coeur d'Alene and St. Joe Rivers.
Preliminary estimates of benthic fluxes of dissolved metals in Coeur d'Alene Lake, Idaho: USGS Open-File Report [L. Balistrieri] on *FREE* shipping on qualifying offers. This report presents porewater and selected water column data collected from Coeur d'Alene Lake in September of Despite probable oxidation of the porewater samples during collection Author: L.
Balistrieri. While these data and calculations provide preliminary information on benthic metal fluxes in Coeur d’Alene Lake, further work is needed to verify their direction and magnitude. The benthic flux calculations indicate that the sediment is generally a source of dissolved Zn, Cu, Mn, and, possibly, Pb to the overlying water column.
Get this from a library. Preliminary estimates of benthic fluxes of dissolved metals in Coeur d'Alene Lake, Idaho. [Laurie S Balistrieri; Geological Survey (U.S.)]. CiteSeerX - Document Details (Isaac Councill, Lee Giles, Pradeep Teregowda): Preliminary estimates of benthic fluxes of dissolved metals in Coeur d’Alene Lake, Idaho.
Benthic fluxes of metals, particularly zinc, are significant sources of metals to the water column of Lake Coeur d'Alene (Kuwabara et al., ) and presumably also in the chain lakes (which are.
Preliminary estimates of benthic flux of dissolved metals in Coeur d’Alene Lake, Idaho. US Geological Survey Open File Report 98–, 40 pp. Google Scholar Balistrieri, L. S., Ortiz, R. Briggs, P. Elrick, K. and Edelmann. Metal(loid) Diagenesis in Mine-Impacted Sediments of Lake Coeur d'Alene, Idaho Article (PDF Available) in Environmental Science and Technology 40(8) May with Reads.
Balistrieri, L.S.: Preliminary estimates of benthic fluxes of dissolved metals in Coeur d'Alene Lake, Idaho. US Department of the Interior, US Geological Survey () Preliminary estimates of benthic fluxes of dissolved metals in Coeur d’Alene Lake, Idaho.
Open File Report R.B. CookEffect of mining and related activities on the sediment trace element geochemistry of Lake Coeur d’Alene, Idaho, USA, Part II: Subsurface sediments. Hydrol. Process., 9 (), pp. Woods, P.F.,Role of limnological processes in fate and transport of nitrogen and phosphorus loads delivered into Coeur d’Alene Lake and Lake Pend Oreille, Idaho, and Flathead Lake, Montana: U.S.
Geological Survey Professional Paper44 p. Sediments are active recipients of anthropogenic inputs, including heavy metals, but may be difficult to interpret without the use of numerical models that capture sediment-metal interactions and provide an accurate representation of the intricately coupled sedimentological, geochemical, and biological processes.
The focus of this study is to present a benchmark problem on heavy metal. Benthic flux of metals and nutrients into the water column of Lake Coeur d'Alene, Idaho: Report of an August,pilot study.
Water-Resources Investigations Report Calculated fluxes ranging from – × 10 8 atoms m −2 d −1 show that a completely independent estimate of benthic fluxes matches well with the average Ra flux derived from the water column Ra inventory ( ± × 10 8 atoms m −2 d −1), reinforcing the argument that benthic input is the primary source of Ra to the system.
Map of Coeur d’Alene Lake and sampling locations: (Site 1) St. Joe River inlet (47 ° ′ N ° ′ W), (Site 2) a water-column monitoring site between the St.
Joe and Coeur d. and calculations provide preliminary information on benthic metal fluxes in Coeur d’Alene Lake, further work is needed to verify their direction and magnitude. The benthic flux calculations indicate that the sediment is generally a source of dissolved Zn, Cu, Mn, and, possibly, Pb.
Coeur d'Alene Lake in northern Idaho is fed by two major rivers: the Coeur d'Alene River from the east and the St.
Joe River from the south, with the Spokane River as its outlet to the north. Benthic flux of metals – Flux estimates from both lander deployments and core-incubations, when averaged over the affected lake area, were of similar magnitude as the dissolved-metal flux from the Coeur d’Alene and St.
Joe Rivers even with oxygenated bottom waters in the lake (Table 9; Metals discussion). This is consistent. Estimates of nutrient fluxes. The vertical diffusional flux of dissolved nutrients from sediments to the overlying water may be calculated from the pore water dissolved gradients (dC/dZ) Z=0 across the sediment–water interface, according to Fick's law in one dimension (Azcue et al., ) represented by Eq.
A survey of heavy metal concentration in the sediments was carried out in order to estimate the extent and degree of heavy metal contamination in the southern part of the Coeur d'Alene lake.
INTRODUCTION During recent years, increased interest in the environment has resulted in consider- able attention being given to pollution caused by industry. A field study was conducted between August, to provide the first direct measurements of the benthic flux of dissolved (micron filtered) solutes between the bottom sediment and water column at two sites in Lake Coeur d'Alene, Idaho.
Trace metals (namely, cadmium, copper, manganese, mercury species, and zinc) and nutrients (namely, ammonia, nitrate plus nitrite, oxygen. Water chemistry. The Coeur d’Alene river and lake waters near Harrison are dilute Ca–SO 4 waters typically with Ca and SO 4 2-concentrations ranging 5–20 mg/L, and with Mg, Na and Cl concentrations generally a few mg/L or less.
The studies of Balistrieri,Winowiecki,Toevs et al., provide most of the available pore-water chemical analyses from Lake Coeur d’Alene.The waters and sediments of the Coeur d’Alene River (CdAR) in northern Idaho have been impacted by decades of mining operations within the Coeur d’Alene mining district.
Lake Coeur d’Alene (LCdA) is fed at the southernportion of thelakebythe St. Joe River and CdAR (Horowitz et .