| Type of Document |
Master's Thesis |
| Author |
Li, Yanqing
|
| URN |
etd-06102009-063129 |
| Title |
Electrochemical studies of pyrite and galena |
| Degree |
Master of Science |
| Department |
Mining and Minerals Engineering |
| Advisory Committee |
| Advisor Name |
Title |
| No Advisors Found |
|
| Keywords |
|
| Date of Defense |
1994-05-05 |
| Availability |
restricted |
Abstract
The major objective of this work was to investigate the initial oxidation behavior
of pyrite in order to better understand how mine wastes containing pyrite generate acid
water. It was found that a unique potential exists at which a fresh surface of pyrite
undergoes neither oxidation nor reduction. This potential is pH dependent and is referred
to as the "stable" potential. The stable potential was found to be 0 V at pH 4.6 and -0.3
V at pH 9.2. Fresh, unoxidized pyrite surfaces were obtained by fracturing under the
electrolyte while holding at the stable potentials. The initial oxidation behavior of pure
pyrite was investigated using cyclic voltammetry technique by beginning potential sweeps
from the stable potential and sweeping in the positive-going or negative-going direction.
The effects of semiconducting properties of pyrite on its electrochemical behavior
were studied by photocurrent measurement. The results indicate that pyrite samples fronl
Peru and Spain are all highly n-type. A spontaneous depletion layer is formed on the
fresh surfaces of n-type pyrite. The depletion layer is attributed to an intrinsic, acceptorlike
surface state. Charge storage in this surface state pins the band edge over a wide
potential range, accounting for the metallic-like electrochemical behavior that has been
reported for pyrite. Electrochemical and photocurrent measurements were also conducted
on galena for comparison with pyrite. The results indicate that galena samples from the
same cluster have varying semiconducting properties, ranging from nearly intrinsic to
highly n-type. Abrasion introduces defects in the surface of pyrite and galena, which
strongly decrease the magnitude of photocurrent.
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