The next point to consider is the measurement of the
flour. To be in thoroughly good condition, flour should be
BREAD.
i)
three months old (it may be used at the end of a fortnight
or three weeks, but never produces such good results), must be
stored in a perfectly dry place, and kept as much as possible
from contact with the air, as the least suspicion of damp
will be enough to give it a musty, unpleasant flavour, which
nothing can either eradicate or hide. The following scale
of weights for flour is well worth mastering :
One pint of flour weighs 14oz.
One quart (two pints, or half a quartern) weighs ljlb.,
and will make a loaf weighing not quite 2Bb.
One quartern (two quarts, or half a gallon, or a quarter
cf a stone) weighs 3ilb., and makes a loaf weighing 4lb. 6oz.
the statutory quartern.
One gallon (half a stone or two quarterns) weighs 71b.,
and produces 8 Jib. of bread.
One stone (or two gallons or a peck) weighs 14lb., and
makes 17^1b. of bread.
Two pecks (or two stones) weigh 281b., and equal half a
bushel.
One bushel (four pecks) weighs 56lb., and makes 701b. of
bread.
One sack of flour weighs 2801b., and equals five bushels.
One pound ahead of bread is the usual daily average of
home-made bread, but, like all averages, this varies some-
what, one person almost living on bread, whilst another
barely touches it. But a little practice soon enables one
to judge.
Next to be considered are the different kinds of ferment
used to “ raise ” or lighten bread, of which there are several
varieties. Of these the original one, brewer’s yeast or
“barm,” as it was called (and, indeed, still is in out of the
way parts), was for long enough the only ferment used. The
objection to it was that its quality was never quite to be
relied on, and the least carelessness in the manufacture or the
storing of it was sufficient to render it practically unusable —
a point certainly not improved in these modern times, when
10
BREAD, CAKES, AND BISCUITS.
a good deal more than hops and grain are used in brewing.
The next ferment taken up was ammonia, a volatile salt
chemically prepared from the ammoniacal products of the
gas works, ivory black, animal charcoal, and other manu-
factures. This sesqui-carbonate of ammonia, to give it its
technical name, has long been used, in trade recipes
especially, under the various names of sal. vol., voil, and
saleratus. It is to be had in lumps, which should be
pounded fine as wanted, and in its rock state should be
stored in a tightly-stoppered bottle, as it soon loses its
strength. The objection to this form of leaven is that,
unless very carefully and exactly used, it gives a pronounced
and anything but pleasant “hartshorn” flavour, frequently
noticeable in inferior cakes and pastry. Next came baking
powders of various more or less excellent kinds. These,
however, though certainly labour-savers and very con-
venient, possess a failing common to ammonia, that, namely,
of producing, by chemical action, a practically indissoluble
residuum in the articles with which they are incorporated.
Of course, the same thing, to some extent, happens with
yeast, but the original constituents of yeast being practi-
cally the same as the material it is mixed with, this
residuum is not more unwholesome than the flour and
moisture that nourish it.
Page 6
Presented as published in 1902. Historical recipes may not meet modern food-safety standards. Cook from the modern interpretation, not the original instructions.
AI-modernized reading of the original text
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The next point to consider is the measurement of the
flour. To be in thoroughly good condition, flour should be
BREAD.
i)
three months old (it may be used at the end of a fortnight
or three weeks, but never produces such good results), must be
stored in a perfectly dry place, and kept as much as possible
from contact with the air, as the least suspicion of damp
will be enough to give it a musty, unpleasant flavour, which
nothing can either eradicate or hide. The following scale
of weights for flour is well worth mastering :
One pint of flour weighs 14oz.
One quart (two pints, or half a quartern) weighs ljlb.,
and will make a loaf weighing not quite 2Bb.
One quartern (two quarts, or half a gallon, or a quarter
cf a stone) weighs 3ilb., and makes a loaf weighing 4lb. 6oz.
the statutory quartern.
One gallon (half a stone or two quarterns) weighs 71b.,
and produces 8 Jib. of bread.
One stone (or two gallons or a peck) weighs 14lb., and
makes 17^1b. of bread.
Two pecks (or two stones) weigh 281b., and equal half a
bushel.
One bushel (four pecks) weighs 56lb., and makes 701b. of
bread.
One sack of flour weighs 2801b., and equals five bushels.
One pound ahead of bread is the usual daily average of
home-made bread, but, like all averages, this varies some-
what, one person almost living on bread, whilst another
barely touches it. But a little practice soon enables one
to judge.
Next to be considered are the different kinds of ferment
used to “ raise ” or lighten bread, of which there are several
varieties. Of these the original one, brewer’s yeast or
“barm,” as it was called (and, indeed, still is in out of the
way parts), was for long enough the only ferment used. The
objection to it was that its quality was never quite to be
relied on, and the least carelessness in the manufacture or the
storing of it was sufficient to render it practically unusable —
a point certainly not improved in these modern times, when
10
BREAD, CAKES, AND BISCUITS.
a good deal more than hops and grain are used in brewing.
The next ferment taken up was ammonia, a volatile salt
chemically prepared from the ammoniacal products of the
gas works, ivory black, animal charcoal, and other manu-
factures. This sesqui-carbonate of ammonia, to give it its
technical name, has long been used, in trade recipes
especially, under the various names of sal. vol., voil, and
saleratus. It is to be had in lumps, which should be
pounded fine as wanted, and in its rock state should be
stored in a tightly-stoppered bottle, as it soon loses its
strength. The objection to this form of leaven is that,
unless very carefully and exactly used, it gives a pronounced
and anything but pleasant “hartshorn” flavour, frequently
noticeable in inferior cakes and pastry. Next came baking
powders of various more or less excellent kinds. These,
however, though certainly labour-savers and very con-
venient, possess a failing common to ammonia, that, namely,
of producing, by chemical action, a practically indissoluble
residuum in the articles with which they are incorporated.
Of course, the same thing, to some extent, happens with
yeast, but the original constituents of yeast being practi-
cally the same as the material it is mixed with, this
residuum is not more unwholesome than the flour and
moisture that nourish it.