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  2. Water distribution on Earth - Wikipedia

    en.wikipedia.org/wiki/Water_distribution_on_Earth

    The vast bulk of the water on Earth is saline or salt water, with an average salinity of 35‰ (or 3.5%, roughly equivalent to 34 grams of salts in 1 kg of seawater), though this varies slightly according to the amount of runoff received from surrounding land. In all, water from oceans and marginal seas, saline groundwater and water from saline ...

  3. Seawater - Wikipedia

    en.wikipedia.org/wiki/Seawater

    Seawater, or sea water, is water from a sea or ocean. On average, seawater in the world's oceans has a salinity of about 3.5% (35 g/L, 35 ppt, 600 mM). This means that every kilogram (roughly one liter by volume) of seawater has approximately 35 grams (1.2 oz) of dissolved salts (predominantly sodium ( Na+. ) ions ).

  4. Alcohol by volume - Wikipedia

    en.wikipedia.org/wiki/Alcohol_by_volume

    However, because of the miscibility of alcohol and water, the conversion factor is not constant but rather depends upon the concentration of alcohol. At 0% and 100% alc/vol is equal to ABW, but at values in between alc/vol is always higher, up to ~13% higher around 60% ABV.

  5. Particle-size distribution - Wikipedia

    en.wikipedia.org/wiki/Particle-size_distribution

    e. In granulometry, the particle-size distribution ( PSD) of a powder, or granular material, or particles dispersed in fluid, is a list of values or a mathematical function that defines the relative amount, typically by mass, of particles present according to size. [1]

  6. Runoff (hydrology) - Wikipedia

    en.wikipedia.org/wiki/Runoff_(hydrology)

    Surface runoff (also known as overland flow or terrestrial runoff) is the unconfined flow of water over the ground surface, in contrast to channel runoff (or stream flow ). It occurs when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil.

  7. Salinity - Wikipedia

    en.wikipedia.org/wiki/Salinity

    Salinity (/ s ə ˈ l ɪ n ɪ t i /) is the saltiness or amount of salt dissolved in a body of water, called saline water (see also soil salinity). It is usually measured in g/L or g/kg (grams of salt per liter/kilogram of water; the latter is dimensionless and equal to ‰).

  8. Total dissolved solids - Wikipedia

    en.wikipedia.org/wiki/Total_dissolved_solids

    Water can be classified by the level of total dissolved solids (TDS) in the water: Fresh water : TDS is less than 1,000 ppm Brackish water : TDS = 1,000 to 10,000 ppm

  9. REI Is Offering Up to 50% Off Editor-Fave Hoka and New ... - AOL

    www.aol.com/rei-offering-50-off-editor-164400900...

    For example, the Fresh Foam 880 v12 is available for 50 percent off in the women’s pink and white version, and for 21 or 50 percent off (depending on the color you choose) for the men’s version.

  10. Water - Wikipedia

    en.wikipedia.org/wiki/Water

    See also: Frost weathering. Water differs from most liquids in that it becomes less dense as it freezes. [d] In 1 atm pressure, it reaches its maximum density of 999.972 kg/m 3 (62.4262 lb/cu ft) at 3.98 °C (39.16 °F), or almost 1,000 kg/m 3 (62.43 lb/cu ft) at almost 4 °C (39 °F).

  11. Water–cement ratio - Wikipedia

    en.wikipedia.org/wiki/Water–cement_ratio

    The water-to-cement ratio is the ratio between the weights of water and cement in a concrete mix. For proper hydration, this ratio (commonly called the w/c ratio) should be about 0.30, assuming no contribution to hydration from external water sources. ^ De Boevere, M.J. (7 July 2021).

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