Zobrazeno 1 - 10
of 56
pro vyhledávání: '"John L. Jambor"'
Publikováno v:
Applied Geochemistry. 57:178-193
The long-term influence of a shallow water cover limiting sulfide-mineral oxidation was examined in tailings deposited near the end of operation in 1951 of the former Sherritt-Gordon Zn–Cu mine (Sherridon, Manitoba, Canada). Surface-water, pore-wat
Autor:
J.G. Bain, Matthew B.J. Lindsay, John L. Jambor, David W. Blowes, Carol J. Ptacek, Michael C. Moncur
Publikováno v:
Applied Geochemistry. 57:157-177
Tailings generated during processing of sulfide ores represent a substantial risk to water resources. The oxidation of sulfide minerals within tailings deposits can generate low-quality water containing elevated concentrations of SO 4 , Fe, and assoc
Autor:
Brenda L. Bailey, David W. Blowes, John L. Jambor, David C. Sego, Lianna J.D. Smith, Leslie Smith
Publikováno v:
Applied Geochemistry. 36:210-221
Three large-scale experimental waste rock piles (test piles) were constructed and instrumented at the Diavik Diamond Mine in the Northwest Territories, Canada, as part of an integrated field and laboratory study to measure and compare physical and ge
Autor:
John L. Jambor, David W. Blowes, Leslie Smith, Lianna J.D. Smith, David C. Sego, Matthew Neuner
Publikováno v:
Applied Geochemistry. 36:200-209
Three large-scale instrumented waste rock piles were constructed at the Diavik Diamond Mine in the Northwest Territories, Canada. These experimental waste rock piles (test piles) are 15 m high and are part of an integrated field and laboratory resear
Autor:
Kerry G. Lear, Carol J. Ptacek, David W. Blowes, John L. Jambor, Matthew B.J. Lindsay, Peter D. Condon
Publikováno v:
Applied Geochemistry. 24:2212-2221
Mineralogical, geochemical and microbial characterization of tailings solids from the Greens Creek Mine, Juneau, Alaska, was performed to evaluate mechanisms controlling aqueous geochemistry of near-neutral pH pore water and drainage. Core samples of
Publikováno v:
Applied Geochemistry. 24:2362-2373
Pyrite and pyrrhotite are the principal minerals that generate acid drainage in mine wastes. Low-pH conditions derived from Fe-sulfide oxidation result in the mobilization of contaminant metals (such as Zn, Cd, Ni and Cr) and metalloids (such as As)
Autor:
Josef Vajdak, Jiří Sejkora, Frank C. Hawthorne, Joel D. Grice, Mark A. Cooper, John L. Jambor
Publikováno v:
The Canadian Mineralogist. 47:159-164
Burgessite, Co 2 (H 2 O) 4 [AsO 3 (OH)] 2 (H 2 O), is a new mineral species of supergene origin from the Keeley mine, South Lorrain Township, Timiskaming District, Ontario, Canada. Burgessite forms rosettes up to 0.8 mm across consisting of prismatic
Autor:
William S. Wise, Michael Kokinos, Andrew C. Roberts, John L. Jambor, Joel D. Grice, Mati Raudsepp, J. Viñals
Publikováno v:
The Canadian Mineralogist. 46:205-217
The new mineral species barahonaite-(Fe) and barahonaite-(Al), simplified as (Ca,Cu,Na,Fe 3+ ,Al) 12 Fe 3+ 2 (AsO 4 ) 8 (OH) x · n H 2 O and (Ca,Cu,Na,Al) 12 Al 2 (AsO 4 ) 8 (OH) x · n H 2 O, respectively, occur at the Dolores prospect in Murcia Pr
Publikováno v:
Environmental Geology. 52:1019-1031
Static tests typically are used in the initial stage of environmental assessments to predict the potential for acid mine drainage, and also are used to monitor waste disposal at active mining operations. The neutralization potential (NP) of 19 sedime
Publikováno v:
Applied Geochemistry. 21:1799-1817
Release of acid drainage from mine-waste disposal areas is a problem of international scale. Contaminated surface water, derived from mine wastes, orginates both as direct surface runoff and, indirectly, as subsurface groundwater flow. At Camp Lake,