Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regionsHilgard, Eugene W. (Eugene Woldemar)
Science
Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regions
Hilgard, Eugene W. (Eugene Woldemar)
Soils
PHYSICAL FACTORS OF WATER COMPARED WITH OTHER SUBSTANCES
(PER UNIT WEIGHT).
================================+===================================
Capillary ascent in glass tubes | Specific Heats.
of one mm. diameter. |
|
Water 14 mm.| Water 1.000
Alcohol 6 mm.| Ice .502
Olive oil 1 mm.| Steam .475
| Clay, Glass .180-.200
| Charcoal .241
HEAT RELATIONS. | Wood .032
Density. | Gold, Lead .032-.031
| Zinc .096
Water at 0° C. (freezing | Steel .119
pt.) .99988|
Water at 4° (Maximum | Heat of fusion.
density) 1.00000| Water (Ice) 80 Cal.
Water at 15° C. (ordinary | Metals 5-28 “
temperature) .990 | Salts, (incl. silicates) 40-63 “
Ice at 0° (freezing pt.) .92800|
--------------------------------+-----------------------------------
+===================================
| Heat of Evaporation.
|
| Water at 20°C. 613 Cal.
| “ “ 100°C. 637 “
| Alcohol 209 “
| Spirits of Turpentine 67 “
+-----------------------------------
Summarizing the meaning of the data given in the above table with
respect to organic life, we see, first, that water rises higher both
in the soil and in the tissues of the plant than any other liquid.
Second, that as its density decreases in cooling after a certain point
is reached, it freezes at the _surface_ instead of at the _bottom_, as
other liquids do; and as solid water (ice) is lighter than fluid water,
ice stays at the surface and is readily melted when spring comes.
Third, since its temperature changes more slowly than that of any other
liquid, it serves to prevent injuriously rapid changes of temperature
in plants and animals as well as in soils. Its high “heat of fusion”
also serves to prevent quick freezing of plant and animal tissues, so
that the brief prevalence of a low temperature may be more readily
borne. Finally, the large amount of heat absorbed in evaporation of
water serves to keep both plants and animals cool under excessive
external temperatures which would otherwise quickly destroy life.
Public-domain text, read in full here on John Shaqi.
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