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Summary
| Description |
English: Acid mine drainage flowing away from collapsed entrance to the Davis Mine pyrite mine near Rowe, Massachusetts, USA. The mine was active from 1882 to 1911, after which the mine filled with water and began generating acidic drainage (Becerra et al., 2009). Near the mine entrance, drainage pH is near 2, and outside of the waste rock area, pH ranges from about 4.5 to 6 (Becerra et al., 2009). |
| Date | |
| Source | Own work |
| Author | Microbialmatt |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 17:46, 16 December 2022 |
| 2,048 × 1,536 (1.54 MB) | Microbialmatt | Uploaded own work with UploadWizard |
File usage
The following pages on the English Wikipedia use this file (pages on other projects are not listed):
- AAG Gold Medal
- Ankaramite
- Aqueous geochemistry
- Bacterial oxidation
- Bailey Distinguished Member Award
- Base-richness
- Bermuda Atlantic Time-series Study
- Chemical Geology
- Chondritic uniform reservoir
- Conodont Alteration Index
- Cottonseed meal
- Cyclic salt
- Davis, Massachusetts
- Dopplerite
- Effluent spreading
- Environmental Chemistry (journal)
- European Association of Geochemistry
- Feather meal
- Ferrallitisation
- Fish emulsion
- Geochemical Journal
- Geochemical Ocean Sections Study
- Geochemical Perspectives Letters
- Houtermans Award
- Incompatible element
- Incongruent melting
- Institute of Geochemistry
- Intermediate composition
- Journal of Environmental Radioactivity
- Kinetic fractionation
- Marine Chemistry (journal)
- Maturity (geology)
- Max Planck Institute for Biogeochemistry
- Oligosaprobe
- Olive mill pomace
- Pedocal
- Per meg
- Pit water
- Podsolisation
- Quartz-dolerite
- Recrystallization (geology)
- Regional geochemistry
- SUPER HI-CAT
- SedDB
- Sericitic alteration
- Tellus B
- Temperature–salinity diagram
- Total boron
- V. M. Goldschmidt Award
- Van Krevelen diagram
- Water-use efficiency
- Wehrlite
- Δ15N
- Template:Geochem-journal-stub
- Template:Geochem-stub
Global file usage
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