Dihydrogen Monoxide is responsible for many facts of life
that we take for granted.
The beach is typically cooler than the inland regions.
The ocean is cold even when the temperature on the beach is
hot.
Small bugs can walk on water.
You can slightly overfill a glass with water, and it won’t
overflow.
Dry porous materials draw up water.
Ice floats.
We sweat to cool down.
It feels hotter on a hot, humid day than on a hot, dry day.
The explanations for all these things comes down to the
unique molecule that is water. Water is made of two hydrogen atoms and one
oxygen atom. When they bond, the oxygen atom is more electronegative (ie
electron hungry) than the hydrogen atoms, so the electrons of both Hydrogens
tend to spend their time around the Oxygen atom. This results in a slight
positive charge on each of the hydrogens that isn’t quite a proper charge, but
a positive dipole. The oxygen likewise has two negative dipoles.
So on each water molecule there are four dipoles- and
because the elements in question are hydrogen and oxygen, the intermolecular
bonds that are formed between the positive dipole of Hydrogen and the negative
dipole of Oxygen are H-bonds.
Because of the ease with which water can break and form weak
intermolecular bonds, it has a heat capacity of 4.184 joules/ gram Celsius.
This means that to heat one gram of water up one degree Celsius, it takes 4.184
joules.
So:
The beach is typically cooler than the inland regions
because the ocean and the water vapor from the ocean take won’t heat up as
easily.
The ocean is cold even when the temperature on the beach is
hot because the sand has a lower heat capacity than water does.
Small bugs walk on water because h-bonds allow for cohesion
of water molecules and thus a surface tension that, when treaded upon with the
fuzzy feet of small bugs, can hold the bug’s weight.
You can slightly overfill a glass with water, and it won’t
overflow because water has such strong cohesive properties that it can sit on
top of itself when there is no surface to adhere to. The same property can be
observed on a wet penny.
You can also place a toothpick on an overfilled penny and
observe the strength of water’s surface tension, which makes it easier to
visualize how water bugs walk on water.
Dry porous materials draw up water because some water is
attracted to the stronger bonds of the material (adhesion), and the rest of the water tags
along because the water molecules are cohesive due to their h-bonds.
Ice floats because water freezes in a hexagonal lattice
shape that is less dense than the h-bonded liquid structure.
We sweat to cool down because the heat that allows sweat to
evaporate comes from our body.
It feels hotter on a hot, humid day than on a hot, dry day
because if there is water vapor pressure in the air, it is harder for your sweat
to evaporate (think boiling water in high atmospheric pressures), no matter how much body heat you have. You literally can’t cool
down as efficiently. On a hot humid day, drinking water can sub in for the
cooling effects of sweating.


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