Changes in lead and zinc lability during weathering-induced acidification of desert mine tailings: Coupling chemical and micro-scale analyses

Sarah M. Hayes, Scott A. White, Thomas L. Thompson, Raina Margaret Maier, Jon Chorover

Research output: Contribution to journalArticle

30 Citations (Scopus)

Abstract

Desert mine tailings may accumulate toxic metals in the near surface centimeters because of low water through-flux rates. Along with other constraints, metal toxicity precludes natural plant colonization even over decadal time scales. Since unconsolidated particles can be subjected to transport by wind and water erosion, potentially resulting in direct human and ecosystem exposure, there is a need to know how the lability and form of metals change in the tailings weathering environment. A combination of chemical extractions, X-ray diffraction, micro-X-ray fluorescence spectroscopy, and micro-Raman spectroscopy were employed to study Pb and Zn contamination in surficial arid mine tailings from the Arizona Klondyke State Superfund Site. Initial site characterization indicated a wide range in pH (2.5-8.0) in the surficial tailings pile. Ligand-promoted (DTPA) extractions, used to assess plant-available metal pools, showed decreasing available Zn and Mn with progressive tailings acidification. Aluminum shows the inverse trend, and Pb and Fe show more complex pH dependence. Since the tailings derive from a common source and parent mineralogy, it is presumed that variations in pH and "bio-available" metal concentrations result from associated variation in particle-scale geochemistry. Four sub-samples, ranging in pH from 2.6 to 5.4, were subjected to further characterization to elucidate micro-scale controls on metal mobility. With acidification, total Pb (ranging from 5 to 13 g kg-1) was increasingly associated with Fe and S in plumbojarosite aggregates. For Zn, both total (0.4-6 g kg-1) and labile fractions decreased with decreasing pH. Zinc was found to be primarily associated with the secondary Mn phases manjiroite and chalcophanite. The results suggest that progressive tailings acidification diminishes the overall lability of the total Pb and Zn pools.

Original languageEnglish (US)
Pages (from-to)2234-2245
Number of pages12
JournalApplied Geochemistry
Volume24
Issue number12
DOIs
StatePublished - Dec 2009

Fingerprint

Acidification
Tailings
Weathering
tailings
acidification
Zinc
weathering
desert
Lead
zinc
Metals
metal
chalcophanite
Pentetic Acid
Geochemistry
Superfund
site characterization
Mineralogy
fluorescence spectroscopy
Water

ASJC Scopus subject areas

  • Environmental Chemistry
  • Pollution
  • Geochemistry and Petrology

Cite this

Changes in lead and zinc lability during weathering-induced acidification of desert mine tailings : Coupling chemical and micro-scale analyses. / Hayes, Sarah M.; White, Scott A.; Thompson, Thomas L.; Maier, Raina Margaret; Chorover, Jon.

In: Applied Geochemistry, Vol. 24, No. 12, 12.2009, p. 2234-2245.

Research output: Contribution to journalArticle

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