DISTRIBUTION OF WATER AT THE EARTH'S SURFACE
| Reservoir |
% of total |
| Oceans |
97.25 |
| Ice caps and glaciers |
2.05 |
| Groundwater |
0.68 |
| Ice caps and glaciers |
2.05 |
| Lakes |
0.01 |
| Soils |
0.005 |
| Atmosphere (as vapor) |
0.001 |
| Rivers |
0.0001 |
| Biosphere |
0.00004 |
| TOTAL |
100% |
Water: a polar solvent
The polar nature of H2O gives it special properties:
-
cohesion: the molecules stick together, producing high surface tension,
capillary action
-
adhesion: the molecules stick to other materials, causing wetting
of surfaces
-
heat capacity, (the amount of heat required to raise the temperature by
a given amount) is among the highest in nature
-
expansion on freezing, causes ice to float
-
high latent heat:
-
of fusion (solidification to ice): 80 cal/g
-
of evaporation: highest of any substance: 585 cal/g
Water can absorb a lot of heat.
Last modified: March 2010
Department of Oceanography
Send comments to: ta@soest.hawaii.edu