Zinc stable isotope fractionation upon accelerated oxidative weathering of sulfidic mine waste

Accelerated oxidative weathering in a reaction cell (ASTM D 5744 standard protocol) was performed over a 33week period on well characterized, sulfidic mine waste from the Kidd Creek Cu–Zn volcanogenic massive sulfide deposit, Canada. The cell leachate was monitored for physicochemical parameters, io...

Full description

Saved in:
Bibliographic Details
Published in:The Science of the total environment 2014-07, Vol.487, p.97-101
Main Authors: Matthies, R., Krahé, L., Blowes, D.W.
Format: Article
Language:English
Subjects:
Acid mine drainage
Applied sciences
Canada
Chemical Fractionation
Enrichment
Environmental Monitoring
Exact sciences and technology
Industrial Waste
Industrial wastewaters
Isotope fractionation
Isotope ratios
Isotopes
Kidd Creek
MC-ICP-MS
Minerals - analysis
Minerals - chemistry
Mining
Other industrial wastes. Sewage sludge
Oxidation
Oxidation-Reduction
Pollution
Signatures
Soil Pollutants - analysis
Soil Pollutants - chemistry
Sphalerite
Tailings
Wastes
Wastewaters
Water Pollutants, Chemical - analysis
Water Pollutants, Chemical - chemistry
Water treatment and pollution
Weather
Weathering
Zinc
Zinc - analysis
Zinc - chemistry
Zinc Isotopes - analysis
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:Accelerated oxidative weathering in a reaction cell (ASTM D 5744 standard protocol) was performed over a 33week period on well characterized, sulfidic mine waste from the Kidd Creek Cu–Zn volcanogenic massive sulfide deposit, Canada. The cell leachate was monitored for physicochemical parameters, ion concentrations and stable isotope ratios of zinc. Filtered zinc concentrations (
ISSN:0048-9697
1879-1026
DOI:10.1016/j.scitotenv.2014.04.020