sively WicA to qupiuli thii<t. and are commonly called soda waters. The <arli(Piiio acid used in making the common artificial ai'ratcd waters is prepared by trcatinj: a mineral carbonate, as chalk or liine-stonc, with dilute snli)luiric acid. The gas thus obtained is forced into bottles or siphons containini; water. yicldin<r a brisk, sparkling liciuid with a pungent but pleasant acidulous taste. Artificial waters, similar to seltzers, vichy, and other well known mineral waters, are produced by dissolving the known ingredients of the mineral water in distilled water and then im])rcgnating them with carbon dioxide gas. The carbonic acid water mixed with fruit syrups is the ordinary soda water of the pharmacy. Formerly carbonic acid water was made on a small scale in an apparatus called a gazogene or seltzogene {see accompanying figure), in which sodium bicarbonate was decom- posed by tartaric acid in the presence of water. A recent invention is the use of capsules contain- ing liquefied carbon dioxide. The liquid which it is desired to impregnate with the gas is placed in a specially constructed bottle, the top of which is provided w-ith a receptacle for the capsule containing the liquefied gas: the covering of the capsule is then ruptured, setting free the acid, which is absorbed by the liquid in the bottle. Aerated waters may also be said to occur natu- rally, for water taken from a spring contains gases, such as oxygen, nitrogen, and carbon diox- ide, dissolved in it. Similarly, running waters, such as rivers and rain waters, absorb gases from the atmosphere, which may be expelled by boiling. See A Treatise on Bereruf/es, by C. H. Sulz, and the articles, Carboxateu or Acid- irLOu.s Wateks, and JIineral Waters.
A'ËRA'TION (Lat. aer, air). In botany,
the cxcliaiigc of gases between living plant tissue
and the surrounding medium. This exchange is
manifested by two processes. In one of these,
viz., the manufacture of certain foods (see
PliOTOSY.NTiiEsls) , carbon dioxide is required by
the plant and oxygen must be eliminated. On
the contrary, in the other process, viz., respira-
tion (q.v.), oxygen is necessary and carbon diox-
ide must be eliminated. The former process is
confined to giecn jplants: the latter is essential
to all excc]>t a few of the lowest and simplest
type (anaerobic bacteria). Among the smaller
plants, and those whose bodies are made ip of
interwoven filaments (Fungi), the gaseous ex-
changes can take place directly, since almost
every part of the body is in contact with the air
or with water. In the former case, the outside
gases dissolve in the constituent water of the
cell-wall and are then free to enter; or, arising
within the cell, and being already dissolved,
they pass ofl' into the air. In water plants
the free inward or outward migration of dis-
solved gases depends on the relative amounts
inside and outside the body. (See Absorption.)
In the larger land plants the greater number
of cells and the more compact structure make
it impossible for the cells more distant from the
surface to conduct the necessary changes at an
adequate rate. Such plants have therefore devel-
oped an extensive aerating system (fig. 1), con-
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Diagraninintic cross-section of a leaf, showing the intercellnlar spaces in the interior, i, and in the epi- dermis t= gtomata), a.
sisting of irregular passages, i, between the inte- rior cells, which communicate with the outer air through microscopic openings, ,«, between the sur- face cells ( see Stomata ), or through larger breaks in the coiky layers of tissue on the surface of the stems. { See Lenticels. ) The intercellular pas-
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Pan of a cross-section of the root of Jnssia?a. show- ing acrcncliyma, witll cllornious inliTcellLilar spaces, the cells hi'ing a mere scutToUling between the surface (not shown) and the central cylinder (at the lower margin).
sages and stomata are formed by the partial separation of the cells as they mature. In land