When.com Web Search

Search results

    138.00+1.26 (+0.92%)

    at Fri, May 31, 2024, 4:00PM EDT - U.S. markets closed

    Delayed Quote

    • Open 137.18
    • High 138.02
    • Low 136.10
    • Prev. Close 136.74
    • 52 Wk. High 142.30
    • 52 Wk. Low 110.07
    • P/E 20.84
    • Mkt. Cap N/A
  1. Results From The WOW.Com Content Network
  2. Alcohol by volume - Wikipedia

    en.wikipedia.org/wiki/Alcohol_by_volume

    Alcohol by volume (abbreviated as alc/vol or ABV) is a standard measure of how much alcohol is contained in a given volume of an alcoholic beverage (expressed as a volume percent ). [1] [2] [3] It is defined as the number of millilitres (mL) of pure ethanol present in 100 mL (3.5 imp fl oz; 3.4 US fl oz) of solution at 20 °C (68 °F).

  3. Water table - Wikipedia

    en.wikipedia.org/wiki/Water_table

    Water table. Cross-section of a hillslope depicting the vadose zone, capillary fringe, water table, and the phreatic or saturated zone. (Source: United States Geological Survey .) The water table is the upper surface of the zone of saturation. The zone of saturation is where the pores and fractures of the ground are saturated with groundwater ...

  4. Dissociation constant - Wikipedia

    en.wikipedia.org/wiki/Dissociation_constant

    Dissociation constant. In chemistry, biochemistry, and pharmacology, a dissociation constant ( KD) is a specific type of equilibrium constant that measures the propensity of a larger object to separate (dissociate) reversibly into smaller components, as when a complex falls apart into its component molecules, or when a salt splits up into its ...

  5. Water distribution on Earth - Wikipedia

    en.wikipedia.org/wiki/Water_distribution_on_Earth

    Typically, fresh water is defined as water with a salinity of less than 1% that of the oceans – i.e. below around 0.35‰. Water with a salinity between this level and 1‰ is typically referred to as marginal water because it is marginal for many uses by humans and animals. The ratio of salt water to fresh water on Earth is around 50:1.

  6. Groundwater - Wikipedia

    en.wikipedia.org/wiki/Groundwater

    Definition. Groundwater is fresh water located in the subsurface pore space of soil and rocks.It is also water that is flowing within aquifers below the water table.Sometimes it is useful to make a distinction between groundwater that is closely associated with surface water, and deep groundwater in an aquifer (called "fossil water" if it infiltrated into the ground millennia ago).

  7. Solubility - Wikipedia

    en.wikipedia.org/wiki/Solubility

    The solution was initially prepared at 20 °C and then stored for 2 days at 4 °C. In chemistry, solubility is the ability of a substance, the solute, to form a solution with another substance, the solvent. Insolubility is the opposite property, the inability of the solute to form such a solution. The extent of the solubility of a substance in ...

  8. Total dissolved solids - Wikipedia

    en.wikipedia.org/wiki/Total_dissolved_solids

    Total dissolved solids ( TDS) is a measure of the dissolved combined content of all inorganic and organic substances present in a liquid in molecular, ionized, or micro-granular ( colloidal sol) suspended form. TDS are often measured in parts per million (ppm). TDS in water can be measured using a digital meter.

  9. Alcohol proof - Wikipedia

    en.wikipedia.org/wiki/Alcohol_proof

    The proof system in the United States was established around 1848 and was based on percent alcohol rather than specific gravity. Fifty percent alcohol by volume was defined as 100 proof. [4] Note that this is different from 50% volume fraction (expressed as a percentage); the latter does not take into account change in volume on mixing, whereas ...

  10. Sieve analysis - Wikipedia

    en.wikipedia.org/wiki/Sieve_analysis

    The cumulative percent passing of the aggregate is found by subtracting the percent retained from 100%. %Cumulative Passing = 100% - %Cumulative Retained. The values are then plotted on a graph with cumulative percent passing on the y axis and logarithmic sieve size on the x axis.

  11. Salinity - Wikipedia

    en.wikipedia.org/wiki/Salinity

    A river or lake water with a salinity of around 70 mg/L will typically have a specific conductivity at 25 °C of between 80 and 130 μS/cm. The actual ratio depends on the ions present. The actual conductivity usually changes by about 2% per degree Celsius, so the measured conductivity at 5 °C might only be in the range of 50–80 μS/cm.