Water (H2O) is a polar inorganic compound that is at room temperature a tasteless and odorless liquid, which is nearly colorless apart from an inherent hint of blue. It is by far the most studied chemical compound and is described as the "universal solvent" and the "solvent of life." It is the most abundant substance on the surface of Earth and the only common substance to exist as a solid, liquid, and gas on Earth's surface. It is also the third most abundant molecule in the universe (behind molecular hydrogen and carbon monoxide.
Water molecules form hydrogen bonds with
each other and are strongly polar. This polarity allows it to dissociate ions in
salts and bond to other polar substances such as alcohols and acids, thus
dissolving them. Its hydrogen bonding causes its many unique properties, such
as having a solid form less dense than its liquid form, a relatively high boiling
point of 100 C for its molar mass, and a high heat capacity.
Water is amphoteric, meaning that it can
exhibit properties of an acid or a base, depending on the pH of the solution
that it is in; it readily produces both H+ and OH− ions. Related to its amphoteric character, it
undergoes self-ionization. The product
of the activities, or approximately, the concentrations of H+ and
OH− is a constant, so their respective concentrations are inversely
proportional to each other.
Geochemistry
The action of water on rock over long
periods of time typically leads to weathering and water erosion, physical
processes that convert solid rocks and minerals into soil and sediment, but
under some conditions chemical reactions with water occur as well, resulting in
metasomatism or mineral hydration, a type of chemical alteration of a rock
which produces clay minerals. It also
occurs when Portland cement hardens.
Water ice can form clathrate compounds,
known as clathrate hydrates, with a variety of small molecules that can be
embedded in its spacious crystal lattice. The most notable of these is methane
clathrate, 4CH4·23H2O, naturally found in large quantities on the
ocean floor.
Acidity in
nature
Rain is generally mildly acidic, with a
pH between 5.2 and 5.8 if not having any acid stronger than carbon dioxide. If high amounts of nitrogen and sulfur oxides
are present in the air, they too will dissolve into the cloud and raindrops,
producing acid rain.
History
Henry Cavendish showed that water was
composed of oxygen and hydrogen in 1781.
The first decomposition of water into hydrogen and oxygen, by electrolysis,
was done in 1800 by English chemist William Nicholson and Anthony Carlisle. In 1805, Joseph Louis Gay-Lussac and Alexander
von Humboldt showed that water is composed of two parts hydrogen and one part
oxygen.
Gilbert Newton Lewis isolated the first
sample of pure heavy water in 1933.
The properties of water have
historically been used to define various temperature scales. Notably, the Kelvin, Celsius, Rankine, and Fahrenheit
scales were, or currently are, defined by the freezing and boiling points of
water. The less common scales of Delisle, Newton, Réaumur and Rømer were
defined similarly. The triple point of water is a more commonly used standard
point today.
See much more at: https://en.wikipedia.org/wiki/Properties_of_water
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