CHAPTER III

DRY-FARM AREAS--RAINFALL

The annual precipitation of rain and snow determines primarily the

location of dry-farm areas. As the rainfall varies, the methods of

dry-farming must be varied accordingly. Rainfall, alone, does not,

however, furnish a complete index of the crop-producing

possibilities of a country.

The distribution of the rainfall, the amount of snow, the

water-holding power of the soil, and the various

moisture-dissipating causes, such as winds, high temperature,

abundant sunshine, and low humidity frequently combine to offset the

benefits of a large annual precipitation. Nevertheless, no one

climatic feature represents, on the average, so correctly

dry-farming possibilities as does the annual rainfall. Experience

has already demonstrated that wherever the annual precipitation is

above 15 inches, there is no need of crop failures, if the soils are

suitable and the methods of dry-farming are correctly employed. With

an annual precipitation of 10 to 15 inches, there need be very few

failures, if proper cultural precautions are taken. With our present

methods, the areas that receive less than 10 inches of atmospheric

precipitation per year are not safe for dry-farm purposes. What the

future will show in the reclamation of these deserts, without

irrigation, is yet conjectural.

Arid, semiarid, and sub-humid

Before proceeding to an examination of the areas in the United

States subject to the methods of dry-farming it may be well to

define somewhat more clearly the terms ordinarily used in the

description of the great territory involved in the discussion.

The states lying west of the 100th meridian are loosely spoken of as

arid, semiarid, or sub-humid states. For commercial purposes no

state wants to be classed as arid and to suffer under the handicap

of advertised aridity. The annual rainfall of these states ranges

from about 3 to over 30 inches.

In order to arrive at greater definiteness, it may be well to assign

definite rainfall values to the ordinarily used descriptive terms of

the region in question. It is proposed, therefore, that districts

receiving less than 10 inches of atmospheric precipitation annually,

be designated arid; those receiving between 10 and 20 inches,

semiarid; those receiving between 20 and 30 inches, sub-humid, and

those receiving over 30 inches, humid. It is admitted that even such

a classification is arbitrary, since aridity does not alone depend

upon the rainfall, and even under such a classification there is an

unavoidable overlapping. However, no one factor so fully represents

varying degrees of aridity as the annual precipitation, and there is

a great need for concise definitions of the terms used in describing

the parts of the country that come under dry-farming discussions. In

this volume, the terms "arid," "semiarid," "sub-humid" and "humid"

are used as above defined.

Precipitation over the dry-farm territory

Nearly one half of the United States receives 20 inches or less

rainfall annually; and that when the strip receiving between 20 and

30 inches is added, the whole area directly subject to reclamation

by irrigation or dry-farming is considerably more than one half (63

per cent) of the whole area of the United States.

Eighteen states are included in this area of low rainfall. The areas

of these, as given by the Census of 1900, grouped according to the

annual precipitation received, are shown below:--

Arid to Semi-arid Group

Total Area Land Surface (Sq. Miles)

Arizona 112,920

California 156,172

Colorado 103,645

Idaho 84,290

Nevada 109,740

Utah 82,190

Wyoming 97,545

TOTAL 746,532

Semiarid to Sub-Humid Group

Montana 145,310

Nebraska 76,840

New Mexico 112,460

North Dakota 70,195

Oregon 94,560

South Dakota 76,850

Washington 66,880

TOTAL 653,095

Sub-Humid to Humid Group

Kansas 81,700

Minnesota 79,205

Oklahoma 38,830

Texas 262,290

TOTAL 462,025

GRAND TOTAL 1,861,652

The territory directly interested in the development of the methods

of dry-farming forms 63 per cent of the whole of the continental

United States, not including Alaska, and covers an area of 1,861,652

square miles, or 1,191,457,280 acres. If any excuse were needed for

the lively interest taken in the subject of dry-farming, it is amply

furnished by these figures showing the vast extent of the country

interested in the reclamation of land by the methods of dry-farming.

As will be shown below, nearly every other large country possesses

similar immense areas under limited rainfall.

Of the one billion, one hundred and ninety-one million, four hundred

and fifty-seven thousand, two hundred and eighty acres

(1,191,457,280) representing the dry-farm territory of the United

States, about 22 per cent, or a little more than one fifth, is

sub-humid and receives between 20 and 30 inches of rainfall,

annually; 61 per cent, or a little more than three fifths, is

semiarid and receives between 10 and 20 inches, annually, and about

17 per cent, or a little less than one fifth, is arid and receives

less than 10 inches of rainfall, annually.

These calculations are based upon the published average rainfall

maps of the United States Weather Bureau. In the far West, and

especially over the so-called "desert" regions, with their sparse

population, meteorological stations are not numerous, nor is it easy

to secure accurate data from them. It is strongly probable that as

more stations are established, it will be found that the area

receiving less than 10 inches of rainfall annually is considerably

smaller than above estimated. In fact, the United States Reclamation

Service states that there are only 70,000,000 acres of desert-like

land; that is, land which does not naturally support plants suitable

for forage. This area is about one third of the lands which, so far

as known, at present receive less than 10 inches of rainfall, or

only about 6 per cent of the total dry-farming territory.

In any case, the semiarid area is at present most vitally interested

in dry-farming. The sub-humid area need seldom suffer from drouth,

if ordinary well-known methods are employed; the arid area,

receiving less than 10 inches of rainfall, in all probability, can

be reclaimed without irrigation only by the development of more

suitable. methods than are known to-day. The semiarid area, which is

the special consideration of present-day dry-farming represents an

area of over 725,000,000 acres of land. Moreover, it must be

remarked that the full certainty of crops in the sub-humid regions

will come only with the adoption of dry-farming methods; and that

results already obtained on the edge of the "deserts" lead to the

belief that a large portion of the area receiving less than 10

inches of rainfall, annually, will ultimately be reclaimed without

irrigation.

Naturally, not the whole of the vast area just discussed could be

brought under cultivation, even under the most favorable conditions

of rainfall. A very large portion of the territory in question is

mountainous and often of so rugged a nature that to farm it would be

an impossibility. It must not be forgotten, however, that some of

the best dry-farm lands of the West are found in the small mountain

valleys, which usually are pockets of most fertile soil, under a

good supply of rainfall. The foothills of the mountains are almost

invariably excellent dry-farm lands. Newell estimates that

195,000,000 acres of land in the arid to sub-humid sections are

covered with a more or less dense growth of timber. This timbered

area roughly represents the mountainous and therefore the nonarable

portions of land. The same authority estimates that the desert-like

lands cover an area of 70,000,000 acres. Making the most liberal

estimates for mountainous and desert-like lands, at least one half

of the whole area, or about 600,000,000 acres, is arable land which

by proper methods may be reclaimed for agricultural purposes.

Irrigation when fully developed may reclaim not to exceed 5 per cent

of this area. From any point of view, therefore, the possibilities

involved in dry-farming in the United States are immense.

Dry-farm area of the world

Dry-farming is a world problem. Aridity is a condition met and to be

overcome upon every continent. McColl estimates that in Australia,

which is somewhat larger than the continental United States of

America, only one third of the whole surface receives above 20

inches of rainfall annually; one third receives from 10 to 20

inches, and one third receives less than lO inches. That is, about

1,267,000,000 acres in Australia are subject to reclamation by

dry-farming methods. This condition is not far from that which

prevails in the United States, and is representative of every

continent of the world. The following table gives the proportions of

the earth's land surface under various degrees of annual

precipitations:--

Annual Precipitation Proportion of Earth's Land Surface

Under 10 inches 25.0 per cent

From 10 to 20 inches 30.0 per cent

From 20 to 40 inches 20.0 per cent

From 40 to 60 inches 11.0 per cent

From 60 to 80 inches 9.0 per cent

From 100 to 120 inches 4.0 per cent

From 120 to 160 inches 0.5 per cent

Above 160 inches 0.5 per cent

Total 100 per cent

Fifty-five per cent, or more than one half of the total land surface

of the earth, receives an annual precipitation of less than 20

inches, and must be reclaimed, if at all, by dry-farming. At least

10 per cent more receives from 20 to 30 inches under conditions that

make dry-farming methods necessary. A total of about 65 per cent of

the earth's land surface is, therefore, directly interested in

dry-farming. With the future perfected development of irrigation

systems and practices, not more than 10 per cent will be reclaimed

by irrigation. Dry-farming is truly a problem to challenge the

attention of the race.

Dry-Farming : A System of Agriculture for Countries under a Low Rainfall · 第 3 / 11 章