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
The table below shows the elements of these series both as regards
current-velocities and maximum quartz-grain diameters carried off by
each. In a great many cases, however, it is altogether unnecessary to
go into such detail, and a subdivision into six or seven divisions
is quite sufficient. Such a subdivision, based upon the doubling of
grain-sizes instead of current-velocities, has been adopted by Prof.
Milton Whitney, of the U. S. Department of Agriculture, and others.
TABLE OF DIAMETERS AND HYDRAULIC VALUES OF SEDIMENTS.
===============================================================
|Velocity per second,|Maximum diameter
Designation of materials.| or hydraulic | of quartz
| value. | grains.
-------------------------+--------------------+----------------
| _Mm._ | _Mm._
| |
Grit | (?) | 1-3
{ | (?) | .5-1
{ | 32-64 | .50
Sand { | 16-32 | .30
{ | 8-16 | .16
{ | 4- 8 | .12
{ | 2- 4 | .072
{ | 1.0- 2 | .047
Silt { | .5- 1 | .036
{ | .25-0.5 | .025
{ | 0.25 | .016
{ | < 0.25 | .010
| |
Clay | < 0.0023 |
-------------------------+--------------------+----------------
_Results of such analyses._—A tabular presentation of the results of
analyses made in accordance with the above plan will give a good idea
of the differences between the various grades of soils recognized
in farm practice, to any one accustomed to the study of figures.
But a much more satisfactory showing is made by placing the several
grain-sizes segregated, into small vials or tubes of identical diameter
and placing them in parallel series alongside of each other.[26] The
curves formed by the surfaces of the several sediment-columns in each
series show to the eye very strikingly the relations of the several
grades of soils to each other, and suggest at once that while gentle
slopes or gently undulating curves belong to soils of intermediate,
loamy character, steep grades and zigzags show soils of extreme types.
This is exemplified in the subjoined Figures:
[26] Convenient stands for this purpose, used by the writer since 1872,
may be cut from L-shaped moldings of wood, such as can be readily
ordered from any planing mill. The vials can be cemented, wired or
tied.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account