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This scarce antiquarian book is a selection from Kessinger
Publishing's Legacy Reprint Series. Due to its age, it may contain
imperfections such as marks, notations, marginalia and flawed
pages. Because we believe this work is culturally important, we
have made it available as part of our commitment to protecting,
preserving, and promoting the world's literature. Kessinger
Publishing is the place to find hundreds of thousands of rare and
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EXPERIMENTAL PLANT PHYSIOLOGY FOR BEGINNERS BY LUCY E. COX B. Sc.
LECTURER IN BOTANY AND NTfUKE STUDY AT QFAYSTOKE PLACE TRAINING
COLLEGE, LONDON WITH ILLUSTRATIONS LONGMANS, GREEN AND CO. 30
PATERNOSTER ROW, LONDON FOURTH AVENUE 30TH STREET, NEW YORK BOMBAY,
CALCUTTA, AND MADRAS AU rights reserved PREFACE IN this book the
main physiological facts gf plant-life ire connected together by a
series of simple experi nents, all of which can be carried out
without the use of any elaborate apparatus. As far as possible the
inferences obtained in the working of one experiment form the
starting-point for the next. The book i intended essentially as a
guide to practical work, and every experiment should therefore be
care fully worked through, not merely reaci. The best plan for a
teacher to follow, in all physiological work, is to present a
problem to the children, and encourage them to suggest the method
by which it may be solved and to draw their own conclusions from
the observations made. By a Standing Order of the London County
Council, it must be stated that the Council accepts no responsi
bility for the opinions or conclusions given in this book. L. E. C.
CONTENTS SECTION I PAGE THE FOOD OF THE PLANT . . . . . . 1 CHAPTER
1 I. THE COMPOSITION OK THE SOIL .... 1 II. THE ABSORPTION OF FOOD
FROM THE SOIL . . 2 CHAPTER II I. THE COMPOSITION OF THE AIR ....
32 II. THE ABSORPTION OF FOOD FROM THE AIR . . 43 SECTION II THE
BREATHING OF THE PLANT ..... 70 SECTION III THE GROWTH OF THE PLANT
81 INDEX 109 vii EXPERIMENTAL PLANT PHYSIOLOGY SECTION I THE FOOD
OP THE PLANT CHAPTER I T. THE COMPOSITION OF THE SOIL Introductory,
The fact that as a plant develops it increases in weight, is one
that needsno demonstration. The oak tree is obviously heavier than
the acorn from which it grows. This increase in weight must have
been caused by absorption of food-material on the part of the
plant. Now the only available sources from which a plant can absorb
food are the soil and the air. It is necessary to determine,
therefore, whether the plant takes in food from one or both of
these sources, and, further, what is the nature of the food taken
in. The Composition of the Soil. The soil is composed of grains
formed from the breaking down of rocks, to getner with a varying
amount of humus or decaying animal and vegetable matter. The
particles are loosely held together, and the spaces between are
filled with air and water. As a great many of the substances
contained in the soil are soluble in water they pass into solution
thus the water ceases to be pure and becomes a solution of various
salts. An analysis of this solution is beyond the scope of this
book, and we must be content to use the results given to us by
chemists. A 2 EXPERIMENTAL PLANT PHYSIOLOGY . The following is a
list of the more common salts dissolved in the water of the soil
made up of sodium and chlorine. calcium, sulphur, and oxygen.
magnesium, sulphur, and oxygen., , sodium, sulphur, and oxygen,
chlorine, nitrogen, oxygen, phosphorus, 1 calcium, magnesium, and
potassium. Common table salt, Gypsum Epsom salts Glaubers salts
Traces of chlorides, nitrates, and phos phates of calcium,
magnesium, and potassium From this list it appears that the
substances present called by the chemist elements are sodium,
chlorine, calcium, magnesium, sulphur, oxygen, nitro gen,
phosphorus, and potassium. It must be remembered that these are the
morecommon elements present in solution in the soil, but they are
not the only ones that may be present for instance, the important
element, carbon, is often there. It is a compound of carbon,
calcium bi-carbonate, that causes the hardness of water in
limestone districts. But, as it will be shown later, carbon
compounds in the soil are not necessary for plant-life. A plant
thrives just as well irk. a soil that contains no carbon as in one
in which this element is present. In the soil, then, certain
substances are present that are available as food...
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