Outlines of dairy bacteriology, 10th edition: A concise manual for the use of students in dairyingRussell, H. L. (Harry Luman)
Science
Outlines of dairy bacteriology, 10th edition: A concise manual for the use of students in dairying
Russell, H. L. (Harry Luman)
Dairy microbiology
If the substances decomposed contain but little sugar, as do animal
tissues, the conditions are favorable for the growth of the
putrefactive bacteria, and foul-smelling gases are formed. When
sugars are present, as in milk, the environmental conditions are
most favorable for the acid-forming bacteria that do not as a rule
produce offensive odors.
Many of the bacteria form substances known as enzymes which are able
to produce certain decomposition changes in the absence of the
living cells, and it is by virtue of these enzymes that the
organisms are able to break down such enormous quantities of
organic matter. Most of these enzymes react toward heat, cold,
and chemical poisons in a manner quite similar to the living
cells. In one respect, they are readily differentiated, and that
is, that practically all of them are capable of producing their
characteristic chemical transformations under conditions where the
activity of the cell is wholly suspended as in a saturated ether or
chloroform atmosphere. The production of enzymes is not confined to
bacteria, but they are found throughout the animal and plant world,
especially in those processes that are concerned in digestion.
Rennet, used in cheese making, is an example of an animal enzyme.
=Distribution of bacteria.= As bacteria possess greater powers of
resistance than almost any other form of life, they are found very
widely distributed over the surface of the earth. In soil they are
abundant, because of the fact that all of the conditions necessary
for growth are here best satisfied. They are, however, distributed
with reference to the layers of the soil; the soil proper, i.e.,
that turned over by the plow, is extremely rich in them on account
of the abundance of organic matter. But at the depth of a few feet
they decrease rapidly in numbers, and in the deeper layers, from six
to ten feet, or more, they are normally not present, because of the
lack of proper food supply and oxygen. The fertility of the soil is
closely associated with their presence.
The bacteria are found in the air because of their development in
the soil below. They are unable to grow even in a moist atmosphere,
but are so readily dislodged by wind currents from the soil that
over land areas the lower strata of the air always contain them.
They are more numerous in summer than in winter; city air contains
larger numbers than country air. Wherever dried fecal matter is
present, as in barns, the air contains many forms.
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