Weathering processes and pickeringite formation in a sulfidic schist: a consideration in acid precipitation neutralization studies
Journal Article
·
· Environ. Geol. (N.Y.); (United States)
OSTI ID:6813147
Extremely low abrasion pH values (2.8-3.3) characterize the weathering products of the Partridge Formation, a Middle-Ordovician metamorphosed, black, sulfidic shale. The local occurrence is observed of two sulfates that are rare in the Northeast: pickeringite and jarosite. X-ray diffraction studies of the weathering residues and the sulfate efflorescences have also identified dioctahedral and trioctahedral illite, kaolinite, vermiculite, and an 11-12 Angstrom phase, thought to be a type of randomly-interstratified biotite-vermiculite. From the mineralogical studies, qualitative weathering processes for the schist are formulated. A probable mechanism for the intense chemical weathering of the schist appears to be oxidation of iron sulfides to form iron oxide-hydroxides, sulfates, and sulfuric acid. This natural weathering process is proposed as an analog to anthropogenic low pH rock weathering resulting from acid precipitation. In the Northeast, natural weathering rates, may, in places, significantly affect the water chemistry and mineralogy used to quantify total (natural plus anthropogenic) weathering and leaching rates. 27 references, 4 figures.
- Research Organization:
- Univ. of Virginia, Charlottesville
- OSTI ID:
- 6813147
- Journal Information:
- Environ. Geol. (N.Y.); (United States), Journal Name: Environ. Geol. (N.Y.); (United States) Vol. 4; ISSN ENGED
- Country of Publication:
- United States
- Language:
- English
Similar Records
Pedogenesis of black shale-influenced soils of the Knobs region of eastern Kentucky
Non-systematic weathering profile in the Blue Ridge Mountains, N. C. : Role of geochemical variables
Kaolinite, smectite and K-rectorite in bentonites: relation to coal rank at Tulameen, British Columbia
Thesis/Dissertation
·
Sat Dec 31 23:00:00 EST 1988
·
OSTI ID:5884300
Non-systematic weathering profile in the Blue Ridge Mountains, N. C. : Role of geochemical variables
Conference
·
Tue Dec 31 23:00:00 EST 1991
· Geological Society of America, Abstracts with Programs; (United States)
·
OSTI ID:5690774
Kaolinite, smectite and K-rectorite in bentonites: relation to coal rank at Tulameen, British Columbia
Journal Article
·
Mon Dec 31 23:00:00 EST 1979
· Clays Clay Miner.; (United States)
·
OSTI ID:5243997
Related Subjects
500200* -- Environment
Atmospheric-- Chemicals Monitoring & Transport-- (-1989)
54 ENVIRONMENTAL SCIENCES
58 GEOSCIENCES
580100 -- Geology & Hydrology-- (-1989)
ACID RAIN
ATMOSPHERIC PRECIPITATIONS
CHALCOGENIDES
CHEMICAL REACTIONS
CHEMISTRY
COHERENT SCATTERING
COMPARATIVE EVALUATIONS
DEPOSITION
DIFFRACTION
HYDROGEN COMPOUNDS
INORGANIC ACIDS
IRON COMPOUNDS
IRON OXIDES
IRON SULFIDES
METAMORPHIC ROCKS
MINERALS
NATURAL OCCURRENCE
OXIDATION
OXIDES
OXYGEN COMPOUNDS
RAIN
ROCKS
SCATTERING
SCHISTS
SULFATE MINERALS
SULFIDES
SULFUR COMPOUNDS
SULFURIC ACID
TRANSITION ELEMENT COMPOUNDS
WATER CHEMISTRY
WEATHERING
X-RAY DIFFRACTION
Atmospheric-- Chemicals Monitoring & Transport-- (-1989)
54 ENVIRONMENTAL SCIENCES
58 GEOSCIENCES
580100 -- Geology & Hydrology-- (-1989)
ACID RAIN
ATMOSPHERIC PRECIPITATIONS
CHALCOGENIDES
CHEMICAL REACTIONS
CHEMISTRY
COHERENT SCATTERING
COMPARATIVE EVALUATIONS
DEPOSITION
DIFFRACTION
HYDROGEN COMPOUNDS
INORGANIC ACIDS
IRON COMPOUNDS
IRON OXIDES
IRON SULFIDES
METAMORPHIC ROCKS
MINERALS
NATURAL OCCURRENCE
OXIDATION
OXIDES
OXYGEN COMPOUNDS
RAIN
ROCKS
SCATTERING
SCHISTS
SULFATE MINERALS
SULFIDES
SULFUR COMPOUNDS
SULFURIC ACID
TRANSITION ELEMENT COMPOUNDS
WATER CHEMISTRY
WEATHERING
X-RAY DIFFRACTION