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  2. Acid sulfate soil - Wikipedia

    en.wikipedia.org/wiki/Acid_sulfate_soil

    Sulfuric material refers to soil material that has a pH of less than 4 owing to the oxidation of sulfidic material. [ 27 ] Sulfidic material refers to “soil materials containing detectable inorganic sulfides (≥0.01% sulfidic sulfur) that can exist as horizons or layers at least 30 mm thick or as surficial features”, [ 27 ] and is further ...

  3. Pyrrhotite - Wikipedia

    en.wikipedia.org/wiki/Pyrrhotite

    Also, the mineral pyrite is both the most common and most abundant sulfide mineral in the Earth's crust. [6] If rocks containing pyrite undergo metamorphism, there is a gradual release of volatile components like water and sulfur from pyrite. [6] The loss of sulfur causes pyrite to recrystallize into pyrrhotite. [6]

  4. Template : List of oxidation states of the elements/doc

    en.wikipedia.org/wiki/Template:List_of_oxidation...

    See also: oxidation states in {{infobox element}} [ edit ] The oxidation states are also maintained in articles of the elements (of course), and systematically in the table {{ Infobox element/symbol-to-oxidation-state }}

  5. Smartsheet - Wikipedia

    en.wikipedia.org/wiki/Smartsheet

    As information is updated, other smartsheets tracking the same task, project or data-point are updated automatically. [7] [8] The service also has alerts for when a task deadline is coming up, [9] [11] and keeps track of document versions. [5] Smartsheet can import data from Microsoft Office or Google applications.

  6. Jarosite - Wikipedia

    en.wikipedia.org/wiki/Jarosite

    On Earth, jarosite is mainly associated with the ultimate stage of pyrite oxidation in clay environment, and can also be found in mine tailings waste where acidic conditions prevail. Against all expectations, jarosite has also been fortuitously discovered in minute quantities in the form of small dust particles in ice cores recovered from a ...

  7. Mineralization (soil science) - Wikipedia

    en.wikipedia.org/wiki/Mineralization_(soil_science)

    In general, organic matter contacting soil has too little nitrogen to support the biosynthetic needs of the decomposing soil microbial population. If the C:N ratio of the decomposing organic matter is above circa 30:1 then the decomposing microbes may absorb nitrogen in mineral form as, e. g., ammonium or nitrates. This mineral nitrogen is said ...

  8. Pyrite - Wikipedia

    en.wikipedia.org/wiki/Pyrite

    Pyrite oxidation is sufficiently exothermic that underground coal mines in high-sulfur coal seams have occasionally had serious problems with spontaneous combustion. [47] The solution is the use of buffer blasting and the use of various sealing or cladding agents to hermetically seal the mined-out areas to exclude oxygen.

  9. London Clay - Wikipedia

    en.wikipedia.org/wiki/London_Clay

    Pyrite oxidation produces insoluble brown iron oxyhydroxide and sulfuric acid leading to the formation of relatively soluble gypsum (CaSO 4 ·2H 2 O, calcium sulfate dihydrate). This latter is more soluble and mobile than iron oxides and can further recrystallize to form larger crystals sometimes called selenite (coming from the moon , but not ...