There is much joy to be had from
water.
It is not merely its awesome abundance and the variety of its forms that
are so joy inspiring, or even its essential role in the carving of our planet
and the evolution of life. For me, the joy is that
such rich properties can emerge from such a simple structure. Moreover, it
is not merely the richness of the simplicity of water that is such an
inspiration, for I also find deep satisfaction in the subtlety of its properties.
That these unusual properties are crucial to the emergence and persistence
of life is a dimension added to the pleasure of beholding water.
Water-be it the rolling Pacific Ocean or a droplet of morning mist, a craggy
glacier of a
snowflake,
a gas pulsing through the blades of a steam turbine or hanging in the air
as a major contribution to the global turmoil we call the
weather-is composed of water molecules. Every
water molecule in the world, and wherever else it occurs in the universe,
is identical. Each one consists of a central oxygen atom to which are attached
two hydrogen atoms. That is all. Oceans, life, and romance all stem from
this simple picture.
To see the potential for the formation of the Pacific Ocean in this minuscule
entity, we need to know some details about hydrogen, the lightest element
of all, and its companion element, oxygen. Atoms of hydrogen are very small;
they consist of a single positively charged proton for a nucleus, and that
proton is surrounded by a single electron. One advantage of being small is
that the nucleus of such an atom can penetrate close to the electrons of
other atoms. Hydrogen nuclei can wriggle into regions that bigger atoms cannot
reach. Moreover, because there is only one electron in a hydrogen atom, the
bright positive charge of the nucleus can blaze through the cloudlike electron's
misty negative charge, and there is, consequently, a strong attraction for
other electrons that happen to be nearby.
As for the oxygen atom, it is much bigger than a hydrogen atom. Nevertheless,
as atoms go, it is still quite small compared to those of other elements,
such as sulfur, chlorine, and even carbon and nitrogen. Its smallness stems
from the strong positive charge of the oxygen nucleus, which draws its electron
close to itself. Additionally, because it is so small and yet has a strongly
charged nucleus, an oxygen atom can draw toward itself the electrons of other
atoms. In particular, it can draw in the electrons of any atoms to which
it is bonded.
In water, an oxygen atom is bonded to two small hydrogen atoms. The central
oxygen atom sucks in the electrons of the oxygen-hydrogen links, and so partially
denudes the hydrogen still further of their electrons. The oxygen atom thereby
becomes oxygen rich and the hydrogen atoms become electron poor. Consequently,
the oxygen atom has a vestigial negative charge (arising from its being bloated
with electrons) and the hydrogen atoms acquire a vestigial positive charge
because the positive charge of the nucleus is no longer canceled by the
surrounding electrons (for they have been partially sucked away). The resulting
distribution of charge-oxygen negative and hydrogen positive-coupled with
the small size of the hydrogen atoms, is at the root of water's extraordinary
properties.
Another feature that conspires with the distribution of electrons and results
in oceans is the shape of the water molecule. It is an angular, open-V-shaped
molecule, with the oxygen atom at the apex of the V. The important feature
of this shape, which can be rationalized by examining how electrons are arranged
around the central oxygen atom, is that one side of the oxygen atom is exposed,
and that exposed side is rich in electrons.
Now we shall see how these features bubble out into the real world of phenomena
and tangible properties. Most important of all is the ability of one water
molecule to stick to another water molecule. The electron-rich region of
the oxygen atom is the site of negative electric charge; the partially denuded
hydrogen atom of a neighboring molecule
is the site of positive charge, and the opposite charges attract
one another. The special link between the two water molecules mediated by
a hydrogen atom in this way is called a hydrogen bond. It is one of the most
important intermolecular links in the world, for its effects range from the
operation of the genetic code (the two strands of the
DNA double helix are linked together by hydrogen
bonds), through the toughness of wood (for the ribbons of cellulose are clamped
rigidly together face-to-face by the sturdy and numerous hydrogen bonds between
them), and-the point of our concern-with the properties of water. For a water
molecule is so light that if it were not for the hydrogen bonds that can
form between its molecules, then water would be a gas, and instead of puddles,
lakes, and oceans of precious liquid, there would be a humid sky full of
gaseous water and barren ground beneath.
Just as hydrogen bonds between water molecules trap them into forming a liquid
even at warm everyday temperatures, so they also help to form the rigid solid
ice at only slightly lower temperatures. However, when ice forms from liquid
water, something rather odd happens, an oddness that is also life preserving.
When the temperature is lowered, the water molecules of a liquid are shaken
and jostled less vigorously, and hydrogen bonds can form more extensively
and survive for longer. As a result, the molecules cease flowing readily
as a liquid, and a stable solid forms instead. Now the shape of the molecule
comes into play. An oxygen atom in the V-shaped water molecule has room to
accommodate two hydrogen bonds, one to each of two neighboring molecules.
Each oxygen atom now participates in four bonds-two ordinary oxygen-hydrogen
bonds, and two hydrogen bonds to neighbors-and these four bonds point toward
the corners of a tetrahedron. This arrangement, which is continued neighbor
after neighbor through the solid, results in a very open structure for ice,
and the water molecules are held apart as well as held together, like an
open scaffold of atoms and bonds. When ice melts, this open structure collapses
and forms a denser liquid. When water freezes, the collapsed structure of
the liquid unfurls and expands into an open structure.
In other words, almost uniquely among substances, the solid form (ice) is
less dense than the liquid form. One consequence of this peculiarity is that
ice forms and floats on the surface of lakes. This feature is life preserving,
because the film of ice helps to protect the water below from the freezing
effect of the air above, and marine life can survive and flourish even though
the temperature is low enough to freeze the surface layers of water.
The hydrogen bonds in water and the tightness with which they bind molecule
to molecule are also responsible for other features of water. The color of
water in bulk, which gives our planet its singular hue, can be traced to
them; so can the film that forms on the surface of the liquid and which curves
it into droplets. Water's considerable heat capacity (its ability to store
energy supplied as heat) is another consequence of these bonds, and this
characteristic is put to use in domestic central heating systems, where a
little water can be used to pump a great deal of energy around a house.
Another extraordinary feature of water is its ability to dissolve so much.
This characteristic also stems from the peculiar arrangement of electric
charges and atoms in a water molecule. Many compounds consist of ions, or
electrically charged atoms.
Common salt,
sodium chloride, for instance, consists of positively charged sodium ions
and negatively charged chloride ions. In the solid, each positive ion is
surrounded by negative ions, and each negative ion is surrounded by positive
ions. Water, though, with its system of positive and negative charges, can
emulate both types of these surrounding ions. Thus, when exposed to water,
the sodium ions of a crystal can become surrounded by water molecules that
present their negatively charged oxygen atoms toward them, and thereby emulate
chloride ions. Similarly, chloride ions can become surrounded by positively
charged hydrogen atoms of the water molecules, which emulate the effect of
sodium ions in the original crystal. Each type of ion is seduced; the sodium
ions float off surrounded by water molecules emulating chloride ions, and
the chloride ions float off surrounded by water molecules using their hydrogen
atoms to emulate sodium ions. Water has a peculiarly strong ability to act
in this way, which is why it is such a good solvent (or, in some circumstances,
when it corrodes, a highly dangerous chemical). It is this ability of water
that carves landscapes from stone. It transports nutrients through the soil
and brings them into plants. Water pervades our bodies, and through its ability
to support the free motion of ions and other molecules that it dissolves,
provides an environment for life.
Water is truly a remarkable substance; so slight in structure, yet so huge
in physical and chemical stature. That so meager an entity can behave so
grandly is a microcosm of modern science, which seeks giants of simplicity
and thereby adds joy to our appreciation of this wonderful world.
PETER ATKINS has been a Fellow of Lincoln College, Oxford University; university lecturer in physical chemistry since 1965; and visiting professor in a number of institutions, including universities in France, Japan, China, New Zealand, and Israel. He was awarded the Meldola Medal of the Royal Society of Chemistry in 1969, and an honorary degree from the University of Utrecht for his contributions to chemistry. His books include Physical Chemistry; Inorganic Chemistry; and General Chemistry. In addition, he has written a number of books on science for the general public, including The Second Law; Molecules; and Atoms, Electrons, and Change. His interests extend to cosmology and the deep contribution of science to culture. His overriding focus is on the communication of science, and he seeks to share the thrill and pleasure that scientific insights provide.
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