The Chemistry of Plant LifeThatcher, Roscoe Wilfred
Science
The Chemistry of Plant Life
Thatcher, Roscoe Wilfred
Botanical chemistry
The first class includes silicon, aluminium, sodium, manganese, and certain
other rarer elements which sometimes are found in soils of some special
type, or unusual origin. These elements seem to have no rôle to play in
the nutrition of plants; although silicon is always present in plant ash
and sodium salts are found in small quantities in all parts of practically
all plants. Nearly all species of plants can be grown to full maturity in
the entire absence of these elements from their culture medium. Occasional
exceptions to this statement in the case of special types of plants are
known, and are of interest in special studies of plant adaptations, but
need not be considered here.
The second group includes iron, calcium, magnesium, and, generally, sulfur.
All of these elements are essential for plant growth, but are usually
present in the soil in ample quantities to insure a sufficient supply in
available form for all plant needs. Recent investigations have shown,
however, that there are many soils in which sulfur is present in such
limited quantities that many agricultural crops, when grown on these soils,
respond favorably to the application of sulfur-containing fertilizers. In
such cases, sulfur is a "critical" element.
The "critical" elements are those which are essential to the growth of all
plants and which are present in most soils in relatively small proportions
and any one may, therefore, be the limiting factor in plant growth so far
as plant food is concerned. These are nitrogen, phosphorus, potassium, and
(possibly) sulfur.
RÔLE OF PLANT FOOD ELEMENTS IN PLANT GROWTH
The use which a plant makes of the elements which come to it from the soil
has been studied with great persistency and care by many plant
physiologists and chemists. Many of the reactions which take place in a
plant cell are extremely complicated, and the relation of the different
chemical elements to these is not easily ascertained. It is probable that
the same element may play a somewhat different rôle in different species of
plants, in different organs of the same plant, or at different stages of
the plant's development. But the usual and most important offices of each
element are now fairly well understood, and are briefly summarized in the
following paragraphs. It should be understood that a thorough and detailed
discussion of these matters, such as would be included in an advanced study
of plant nutrition, would reveal other functions than those which are
presented here and would require a more careful and more exact method of
statement than is suitable here. However, the general principles of the
utilization of soil elements by plants for their nutrition and growth may
be fairly well understood from the following statements.
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