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Virginia Polytechnic Institute and State University

Relative rates of reaction of pyrite and marcasite with ferric iron at low pH

Abstract

dc:description.abstract

The relative reactivities of pulverized samples (100-200 mesh) of 3 marcasite and 7 pyrite specimens from various sources were determined at 25°C and pH = 2.0 in ferric chloride solutions with initial ferric iron concentrations of 10⁻³ molal. The rate of the reaction: FeS₂ + 14Fe³⁺ + 8H₂O = 15Fe²⁺ + 2SO₄²⁻ + 16H⁺ was determined by calculating the rate of reduction of aqueous ferric ion from measured oxidation-reduction potentials. The reaction follows the rate law: -d m<sub>Fe³⁺</sub> / dt = k (A/M) m<sub>Fe³⁺</sub> where m<sub>Fe³⁺</sub> is the molal concentration of uncomplexed ferric iron, k is the rate constant and A/M is the surface area of reacting solid to mass of solution ratio. The measured rate constants, k, range from 1.0x10⁻⁴ to 2.7x10⁻⁴ sec⁻¹ ±5%, with lower-temperature/early diagenetic pyrite having the smallest rate constants, marcasite intermediate, and pyrite of higher-temperature hydrothermal and metamorphic origin having the greatest rate constants. Geologically, these small relative differences between the rate constants are not significant, so the fundamental reactivities of marcasite and pyrite are not appreciably different. The activation energy of the reaction for a hydrothermal pyrite in the temperature interval of 25 to 50°C is 92 kJ mol⁻¹. The BET-measured specific surface area for lower-temperature/ early diagenetic pyrite is an order of magnitude greater than that for pyrite of higher-temperature origin. Consequently, since the lower-temperature types have a much greater A/M ratio, they will appear to be more reactive per unit mass than the higher temperature types.

Degree

thesis:*
Name thesis:degree_name
Master of Science
Level thesis:degree_level
masters
Discipline thesis:degree_discipline
Geology
Department dc:contributor.department
Geology
Grantor dc:publisher
Virginia Polytechnic Institute and State University
Year dc:date.issued
1982

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Wiersma, Cynthia Leigh

Rights

dc:rights
Statement dc:rights
  • In Copyright
Language dc:language.iso
en_US

Identifiers

dc:identifier.*
Handle dc:identifier.uri
http://hdl.handle.net/10919/82891
OAI identifier oai:identifier
oai:vtechworks.lib.vt.edu:10919/82891

Chain of custody

source
Harvested from
Virginia Tech
Base URL
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Last updated
2026-07-22
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citation

Wiersma, Cynthia Leigh. Relative rates of reaction of pyrite and marcasite with ferric iron at low pH. masters thesis, Virginia Polytechnic Institute and State University, 1982. http://hdl.handle.net/10919/82891