Dry-Farming : A System of Agriculture for Countries under a Low RainfallWidtsoe, John Andreas
Science
Dry-Farming : A System of Agriculture for Countries under a Low Rainfall
Widtsoe, John Andreas
Dry farming
All plants when carefully burned leave a portion of ash, ranging
widely in quantity, averaging about 5 per cent, and often exceeding
10 per cent of the dry weight of the plant. This plant ash
represents inorganic substances taken from the soil by the roots. In
addition, the nitrogen of plants, averaging about 2 per cent and
often amounting to 4 per cent, which, in burning, passes off in
gaseous form, is also usually taken from the soil by the plant
roots. A comparatively large quantity of the plant is, therefore,
drawn directly from the soil. Among the ash ingredients are many
which are taken up by the plant simply because they are present in
the soil; others, on the other hand, as has been shown by numerous
classical investigations, are indispensable to plant growth. If any
one of these indispensable ash ingredients be absent, it is
impossible for a plant to mature on such a soil. In fact, it is
pretty well established that, providing the physical conditions and
the water supply are satisfactory, the fertility of a soil depends
largely upon the amount of available ash ingredients, or plant-food.
A clear distinction must be made between the_ total _and _available
_plant-food. The essential plant-foods often occur in insoluble
combinations, valueless to plants; only the plant-foods that are
soluble in the soil-water or in the juices of plant roots are of
value to plants. It is true that practically all soils contain all
the indispensable plant-foods; it is also true, however, that in
most soils they are present, as available plant-foods, in
comparatively small quantities. When crops are removed from the land
year after year, without any return being made, it naturally follows
that under ordinary conditions the amount of available plant-food is
diminished, with a strong probability of a corresponding diminution
in crop-producing power. In fact, the soils of many of the older
countries have been permanently injured by continuous cropping, with
nothing returned, practiced through centuries. Even in many of the
younger states, continuous cropping to wheat or other crops for a
generation or less has resulted in a large decrease in the crop
yield.
Practice and experiment have shown that such diminishing fertility
may be retarded or wholly avoided, first, by so working or
cultivating the soil as to set free much of the insoluble plant-food
and, secondly, by returning to the soil all or part of the
plant-food taken away. The recent development of the commercial
fertilizer industry is a response to this truth. It may be said
that, so far as the agricultural soils of the world are now known,
only three of the essential plant-foods are likely to be absent,
namely, potash, phosphoric acid, and nitrogen; of these, by far the
most important is nitrogen. The whole question of maintaining the
supply of plant-foods in the soil concerns itself in the main with
the supply of these three substances.
The persistent fertility of dry-farms
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