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    Johnnie Moore

    Seasonal variations in stream inorganic geochemistry are not well documented or understood. We sampled two mining-impacted and two relatively pristine streams in western Montana over a 12-month period, collecting samples every 4 weeks,... more
    Seasonal variations in stream inorganic geochemistry are not well documented or understood. We sampled two mining-impacted and two relatively pristine streams in western Montana over a 12-month period, collecting samples every 4 weeks, with supplemental sampling (at least weekly) during spring runoff. We analyzed all samples for dissolved (operationally defined as <0.2 μm) and total recoverable concentrations. Generally, the trace
    Arsenic is a wide-spread contaminant of soils and sediments, and many watersheds worldwide regularly experience severe arsenic loading. While the toxicity of arsenic to plants and animals is well recognized, the geochemical and biological... more
    Arsenic is a wide-spread contaminant of soils and sediments, and many watersheds worldwide regularly experience severe arsenic loading. While the toxicity of arsenic to plants and animals is well recognized, the geochemical and biological transformations that alter its bioavailability in the environment are multifaceted and remain poorly understood. This communication provides a brief overview of our current understanding of the biogeochemistry of arsenic in circumneutral freshwater sediments, placing special emphasis on microbial transformations. Arsenic can reside in a number of oxidation states and complex ions. The common inorganic aqueous species at circumneutral pH are the negatively charged arsenates (H2As(V)O4(-) and Has(V)O4(2-)) and zero-charged arsenite (H3As(III)O3(0)). Arsenic undergoes diagenesis in response to both physical and biogeochemical processes. It accumulates in oxic sediments by adsorption on and/or co-precipitation with hydrous iron and manganese oxides. Bu...
    Arsenic behavior was examined in a contaminated stream by sampling the dissolved (<0.45 μm) arsenic and metals in surface water, shallow hyporheic zone water, and adjacent ground water. Surface water was oxic and slightly basic, and... more
    Arsenic behavior was examined in a contaminated stream by sampling the dissolved (<0.45 μm) arsenic and metals in surface water, shallow hyporheic zone water, and adjacent ground water. Surface water was oxic and slightly basic, and ground water was anoxic and ...
    Page 1. Mine waste contamination limits soil respiration rates: a case study using quantile regression Philip W. Ramsey a,*, Matthias C. Rilliga , Kevin P. Feris b , Johnnie N. Moore c , James E. Gannon a aMicrobial Ecology ...
    Before and during the first week of the March-April 1980 eruptions of Mount St. Helens, Washington, infrared thermal surveys were conducted to monitor the thermal activity of the volcano. The purpose was to determine if an increase in... more
    Before and during the first week of the March-April 1980 eruptions of Mount St. Helens, Washington, infrared thermal surveys were conducted to monitor the thermal activity of the volcano. The purpose was to determine if an increase in thermal activity had taken place since an earlier airborne survey in 1966. Nine months before the eruption there was no evidence of an increase in thermal activity. The survey during the first week of the 1980 eruptions indicated that little or no change in thermal activity had taken place up to 4 April. Temperatures of ejected ash and steam were low and never exceeded 15 degrees C directly above the vent.
    In this paper, we present results from a large number of experiments aimed at quantifying method and instrument uncertainty associated with laser diffraction analysis. We analyzed the size distribution of fine-grained sediment (< 1-50... more
    In this paper, we present results from a large number of experiments aimed at quantifying method and instrument uncertainty associated with laser diffraction analysis. We analyzed the size distribution of fine-grained sediment (< 1-50 µm) from Flathead Lake, Montana, along with samples ...
    ... YiQiang Zhang* and Johnnie N. Moore ... Microbial reduc-tion of selenate is a major process transferring Se from water to sediment (Bender et al., 1991; Oremland et al., 1989, 1990; Steinberg and Oremland, 1990; Tokunaga et al., 1996;... more
    ... YiQiang Zhang* and Johnnie N. Moore ... Microbial reduc-tion of selenate is a major process transferring Se from water to sediment (Bender et al., 1991; Oremland et al., 1989, 1990; Steinberg and Oremland, 1990; Tokunaga et al., 1996; Zhang and Moore, 1996). This reduction ...
    ... Eng., 11(3), 198–220. Moore, JN, and Landrigan, EM (1999). “Mobilization of metal-contaminated sediment by ice-jam floods.” Environ. Geol., 37(1–2), 96–101. Moore, JN, and Luoma, SN (1990). “Hazardous wastes from large-scale metal... more
    ... Eng., 11(3), 198–220. Moore, JN, and Landrigan, EM (1999). “Mobilization of metal-contaminated sediment by ice-jam floods.” Environ. Geol., 37(1–2), 96–101. Moore, JN, and Luoma, SN (1990). “Hazardous wastes from large-scale metal extraction: A case study.” Environ. Sci. ...
    ... P4C, 0.026 (4.9), 0.072 (13.6), 0.154 (29.0), 0.259 (48.8), 0.015 (2.8), 0.531, 0.511. P4C CNS h -1, 0.077 (2.6), 0.183 (6.2), 1.431 (48.5), 1.228 (41.6), 0.028 (1.0), 2.951, 3.052. P4C CNS h -2, 0.191 (3.9), 0.622 (12.6), 2.862... more
    ... P4C, 0.026 (4.9), 0.072 (13.6), 0.154 (29.0), 0.259 (48.8), 0.015 (2.8), 0.531, 0.511. P4C CNS h -1, 0.077 (2.6), 0.183 (6.2), 1.431 (48.5), 1.228 (41.6), 0.028 (1.0), 2.951, 3.052. P4C CNS h -2, 0.191 (3.9), 0.622 (12.6), 2.862 (58.1), 1.204 (24.4), 0.037 (0.8), 4.930, 4.912. a Soluble ...
    Seepage of metal-rich water from tailings ponds in the Clark Fork River Basin, a Supe@nd Complex ... 001 3-936)(/9O/O924-1278$02.5O/O 0 1990 American Chemical Society ... Johnnie N. Moore University of Montana Missoula, MT 59812 Samuel N.... more
    Seepage of metal-rich water from tailings ponds in the Clark Fork River Basin, a Supe@nd Complex ... 001 3-936)(/9O/O924-1278$02.5O/O 0 1990 American Chemical Society ... Johnnie N. Moore University of Montana Missoula, MT 59812 Samuel N. Luoma US. Geological Survey ...
    ... Zhang, † Johnnie N. Moore, ‡ and William T. Frankenberger, Jr.* †. Department of Environmental Sciences, University of California, Riverside, California 92521-0424, and Department of Geology, University of Montana, Missoula, Montana... more
    ... Zhang, † Johnnie N. Moore, ‡ and William T. Frankenberger, Jr.* †. Department of Environmental Sciences, University of California, Riverside, California 92521-0424, and Department of Geology, University of Montana, Missoula, Montana 59812-1019. Environ. Sci. Technol. ...
    ... relatively uncontaminated surface water (Figure 1). Three hydrostratigraphic units are present within the flood plain along Silver Bow Creek. ... ion concen-trations in the surface and groundwater can identify potential conservative... more
    ... relatively uncontaminated surface water (Figure 1). Three hydrostratigraphic units are present within the flood plain along Silver Bow Creek. ... ion concen-trations in the surface and groundwater can identify potential conservative constituents (Table 1). These cal-culations were ...
    ... Coarse-Grained River Floodplain Sediment: Clark Fork River, Montana, USA JOHNNIE N. MOORE, EDWARD J. BROOK, and CAROLYN JOHNS Department of Geology University of Montana Missoula, Montana 59812, USA ... 2, 107-115 © 1989... more
    ... Coarse-Grained River Floodplain Sediment: Clark Fork River, Montana, USA JOHNNIE N. MOORE, EDWARD J. BROOK, and CAROLYN JOHNS Department of Geology University of Montana Missoula, Montana 59812, USA ... 2, 107-115 © 1989 Springer-Verlag New York Inc. ...
    ABSTRACT Analytical transmission electron microscopy (aTEM) and flow field flow fractionation (FlFFF) coupled to multi-angle laser light scattering (MALLS) and high-resolution inductively coupled plasma mass spectroscopy (HR-ICPMS) were... more
    ABSTRACT Analytical transmission electron microscopy (aTEM) and flow field flow fractionation (FlFFF) coupled to multi-angle laser light scattering (MALLS) and high-resolution inductively coupled plasma mass spectroscopy (HR-ICPMS) were utilised to elucidate relationships between trace metals and nanoparticles in contaminated sediment. Samples were obtained from the Clark Fork River (Montana, USA), where a large-scale dam removal project has released reservoir sediment contaminated with toxic trace metals (namely Pb, Zn, Cu and As) which had accumulated from a century of mining activities upstream. An aqueous extraction method was used to recover nanoparticles from the sediment for examination; FlFFF results indicate that the toxic metals are held in the nano-size fraction of the sediment and their peak shapes and size distributions correlate best with those for Fe and Ti. TEM data confirms this on a single nanoparticle scale; the toxic metals were found almost exclusively associated with nano-size oxide minerals, most commonly brookite, goethite and lepidocrocite. © 2010 CSIRO.
    ABSTRACT Metal concentrations were determined in benthic biota, fish livers, water, and fine-grained sediment through 215 km of an intermontane river system (Blackfoot River, Montana, USA) affected by headwater inputs of acid-mine... more
    ABSTRACT Metal concentrations were determined in benthic biota, fish livers, water, and fine-grained sediment through 215 km of an intermontane river system (Blackfoot River, Montana, USA) affected by headwater inputs of acid-mine effluent. Solute and particulate contaminants decreased rapidly downstream from headwater sources, but some extended through an extensive marsh system. Particulate contaminants penetrated through the marsh system, effectively resulting in food web contamination downstream of the marshes. Metals differed in their bioavailability within and below the marsh system. Cadmium was most consistently accumulated in the food web, and the general order of downstream mobilization of bioavailable metals appears to be Cd, Zn > Cu > As, Ni. Depauperate benthic communities and reduced fish populations occurred coincident with the sediment contamination.
    ... Elevated metal concentrations in the floodplain of the Clark Fork River originate from tailings deposited onto the floodplain predominantly as overbank deposits and as point bars adjacent to abandoned channels ... Ee : :; : : 2.57 : :... more
    ... Elevated metal concentrations in the floodplain of the Clark Fork River originate from tailings deposited onto the floodplain predominantly as overbank deposits and as point bars adjacent to abandoned channels ... Ee : :; : : 2.57 : : :: 0.82 3.65 : : :::1.49: .:: ; 0.628 :. ...
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