Scientific American Supplement, No. 470, January 3, 1885Various
Science
Scientific American Supplement, No. 470, January 3, 1885
Various
Science -- Periodicals
It is difficult to conceive how the evidence for the ferment theory of
nitrification could be further strengthened; it is apparently complete in
every part. Although, however, nearly the whole of this evidence has been
before the scientific public for more than seven years, the ferment theory
of nitrification can hardly be said to have obtained any general
acceptance; it has not indeed been seriously controverted, but neither has
it been embraced. In hardly a single manual of chemistry is the production
of saltpeter attributed to the action of a living ferment existing in the
soil. Still more striking is the absence of any recognition of the
evidence just mentioned when we turn to the literature and to the public
discussions on the subjects of sewage, the pollution of river water, and
other sanitary questions. The oxidation of the nitrogenous organic matter
of river water is still spoken of by some as determined by mere contact
with atmospheric oxygen, and the agitation of the water with air as a
certain means of effecting oxidation; while by others the oxidation of
nitrogenous organic matter in a river is denied, simply because free
contact with air is not alone sufficient to produce oxidation. How much
light would immediately be thrown on such questions if it were recognized
that the oxidation of organic matter in our rivers is determined solely by
the agency of life, is strictly limited to those conditions within which
life is possible, and is most active in those circumstances in which life
is most vigorous. It is surely most important that scientific men should
make up their minds as to the real nature of those processes of oxidation
of which nitrification is an example. If the ferment theory be doubted,
let further experiments be made to test it, but let chemists no longer go
on ignoring the weighty evidence which has been laid before them. It is
partly with the view of calling the attention of English and American
chemists to the importance of a decision on this question that I have been
induced to bring this subject before them on the present occasion. I need
hardly add that such results as the nitrification of sewage by passing it
through sand, or the nitrification of dilute solutions of blood prepared
without special precaution, are no evidence whatever against the ferment
theory of nitrification. If it is to be shown that nitrification will
occur in the absence of any ferment, it is clear that all ferments must be
rigidly excluded during the experiments; the solutions must be sterilized
by heat, the apparatus purified in a similar manner, and all subsequent
access of organisms carefully guarded against. It is only experiments made
in this way that can have any weight in deciding the question.
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