NOTES
Links to summaries of key issues for each topic
VISUALS
Links to images employed in lectures on a topic-by-topic basis
TEXT
Link to chapter outlines at online learning center at McGraw Hill.
NOTES
Links to summaries of key issues for each topic
|
|
The Physical Properties of Water (contd.)
|
Notes on Topic:
The notes represent summaries of key issues
for each topic
They emphasize the terminology used to describe
the various phenomena.
| 1. Properties of Water
(contd.): |
| Learning Objectives: |
-
Understanding of the influences of water structure on its properties
-
Energetics of water, and variations associated with changes in state
|
| Structures of Ice and Water: |
-
Ice:
-
open network held together by H-bonds, which excludes salts
-
Water:
-
in part H-bonded clusters.
-
Water vapor:
-
Hydrogen bonds form (break) during condensation (evaporation).
-
Heat energy measured in calories:
-
1 cal = heat required to raise 1g water by 1°C.
-
melting/freezing (80 cal = latent heat of fusion)
-
warming/cooling from 0°C to 100°C (100 cal)
-
evaporation/condensation (540 cal = latent heat of vaporization).
-
Dew point:
-
condensation occurs
-
sublimation direct conversation of solid to gas.
-
Heat absorbed in two forms:
-
sensible heat in vibrational energy, which leads to temperature change
-
latent heat in H-bonds.
|
| Physical properties: |
-
Heat capacity:
-
high heat capacity (1 cal/g/°C; only NH3 higher)
-
changes little with heat absorption
-
vital in regulation of Earth's oceanic temperature
-
Cohesion:
-
H-bonds hold water together
-
Surface tension:
-
ordered layer at air/water interface
-
Viscosity:
-
resistance to flow, low for water
-
Compressibility:
-
Water almost incompressible.
-
Volume reduced by only 1.7% at 400 atm (4km)
-
max. pressure: 1100 atm at 11km
-
Density:
-
mass/unit volume, max. 1g/cm3 at ~4°C
-
decreases at lower and higher temperatures
-
seawater ~1.0278g/cm3
-
Temperature effects:
-
ice (lattice structure) less dense than water, floats.
-
density increases with salinity;
-
seawater sinks as cooled.
-
small density increase as pressure increases.
-
Dissolving Ability:
-
water as solvent, separate charged ions from each other.
-
continual process of transporting salts from land to ocean by run-off,
makes seawater saline.
|
Department
of Geological Sciences,
1001
E. Tenth Street, Bloomington, IN 47405-1403
Phone:
(812) 855-5582 Last updated: 7 October 2000
Comments:
simon@indiana.edu
Copyright
2000, The Trustees of Indiana University
|