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- Sulfate_crust abstract "Sulfate crust is a zone observed in the axial (central) parts of burning coal dumps and related sites. It is a zone built mainly by anhydrous sulfate minerals, such as godovikovite and millosevichite. The outer zone can easily be hydrated giving rise to minerals like tschermigite and alunogen. The zone forms due to interaction with hot (even around 600 °C) coal-derived gases (mainly NH3 and SO3) with the "sterile" material (i.e. shales and other rocks serving as the source of Al3+, Fe3+, Ca2+ and other cations) in case of the lack of vents for the gases to escape into the atmosphere.".
- Sulfate_crust wikiPageID "19387740".
- Sulfate_crust wikiPageLength "1333".
- Sulfate_crust wikiPageOutDegree "14".
- Sulfate_crust wikiPageRevisionID "496890647".
- Sulfate_crust wikiPageWikiLink Alunogen.
- Sulfate_crust wikiPageWikiLink Ammonia.
- Sulfate_crust wikiPageWikiLink Category:Coal_mining.
- Sulfate_crust wikiPageWikiLink Category:Combustion.
- Sulfate_crust wikiPageWikiLink Category:Sulfate_minerals.
- Sulfate_crust wikiPageWikiLink Coal.
- Sulfate_crust wikiPageWikiLink Coal_Fire,_Alabama.
- Sulfate_crust wikiPageWikiLink Coal_fire.
- Sulfate_crust wikiPageWikiLink Coal_seam_fire.
- Sulfate_crust wikiPageWikiLink Godovikovite.
- Sulfate_crust wikiPageWikiLink Millosevichite.
- Sulfate_crust wikiPageWikiLink Sulfate.
- Sulfate_crust wikiPageWikiLink Sulfur_trioxide.
- Sulfate_crust wikiPageWikiLink Tschermigite.
- Sulfate_crust wikiPageWikiLinkText "sulfate crust".
- Sulfate_crust hasPhotoCollection Sulfate_crust.
- Sulfate_crust wikiPageUsesTemplate Template:Chemistry-stub.
- Sulfate_crust wikiPageUsesTemplate Template:Mining-stub.
- Sulfate_crust wikiPageUsesTemplate Template:Sulfate-mineral-stub.
- Sulfate_crust subject Category:Coal_mining.
- Sulfate_crust subject Category:Combustion.
- Sulfate_crust subject Category:Sulfate_minerals.
- Sulfate_crust hypernym Zone.
- Sulfate_crust type Settlement.
- Sulfate_crust type Process.
- Sulfate_crust type Sulfate.
- Sulfate_crust comment "Sulfate crust is a zone observed in the axial (central) parts of burning coal dumps and related sites. It is a zone built mainly by anhydrous sulfate minerals, such as godovikovite and millosevichite. The outer zone can easily be hydrated giving rise to minerals like tschermigite and alunogen. The zone forms due to interaction with hot (even around 600 °C) coal-derived gases (mainly NH3 and SO3) with the "sterile" material (i.e.".
- Sulfate_crust label "Sulfate crust".
- Sulfate_crust sameAs m.04n5kmy.
- Sulfate_crust sameAs Q7636189.
- Sulfate_crust sameAs Q7636189.
- Sulfate_crust wasDerivedFrom Sulfate_crust?oldid=496890647.
- Sulfate_crust isPrimaryTopicOf Sulfate_crust.