Geoscience Reference
In-Depth Information
Ice
Ambient
water at 20
º
C
Sinking and mixing
cool dense
freshwater at 4
º
C
Air
-
∆
r
g
-
∆
r
g
F
F
Water
r
pear
/
r
air
= 654;
∆
r
= 864kgm
-3
F
B
= -8.49 10
3
N
r
pear
/
r
water
= 0.85;
∆
r
= -150kgm
-3
F
B
= 1.47 10
3
N
-80 kg m
-3
∆
r
for meltwater : ambient water
= + 1.77 kg m
-3
∆
r
for ice : ambient water
=
Fig. 3.24
Buoyant force and Archimedes principle.
Fig. 3.25
Buoyancy in the water/ice system.
Buoyant weight
per unit volume
2.6 10
4
kg
Buoyant weight
per unit volume
1.62 10
4
kg
Mineral grain
density 2,650 kgm
-3
Mineral grain
density 2,650 kgm
-3
Air
Water
Fig. 3.26
Buoyant weights of mineral grains descending along transport paths in air and water.
-ve Buoyancy
of meltwater
Midocean ridge
Ice
Ocean plate
Ocean
Continent
+ve Buoyancy
of rising magma
Asthenosphere
-ve Buoyancy
of subducting plate
Fig. 3.27
Buoyancy in oceans and ocean plates.
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