The atmosphere, first subjected to analysis by Priestley and Scheele in the

latter part of the eighteenth century, consists practically of oxygen and

nitrogen in the almost constant proportion of 20.81 volumes of oxygen to

79.19 volumes of nitrogen, or, by weight, 23.01 parts of oxygen to 76.99 of

nitrogen. The gases are associated together, not as a chemical compound,

but as a mechanical mixture. Upon the oxygen present depends the power of

the atmosphere to support combustion and respiration, the nitrogen acting

as a diluent to prevent its too energetic action. It had long been known

that atmospheric nitrogen appeared to have a very slightly greater density

than nitrogen obtained from other sources. Lord Rayleigh and Sir William

Ramsay found that the fact was due to a still more inert gas which forms

nearly 1 per cent of the air, and which had not previously been separated

from nitrogen. This has been named _argon_. Besides these gases, the

atmosphere also contains aqueous vapour in variable quantity, ozone,

carbonic acid gas, traces of ammonia, nitric acid, and, in towns,

sulphuretted hydrogen and sulphurous acid gas. In addition to its gaseous

constituents the atmosphere is charged with dust, bacteria, &c. For other

gases which are present in traces, see _Neon_. See _Climate_;

_Meteorology_.--BIBLIOGRAPHY: C. Flammarion, _L'Atmosphere_; Sir Napier

Shaw, _The Weather Map_.

ATMOSPHERIC ENGINE, name given by early inventors to engines in which the

piston is restored to the bottom of its stroke by atmospheric pressure.

ATMOSPHERIC RAILWAY, so called in consequence of the motive power being

derived from the pressure of the atmosphere, or from compressed air. The

idea of thus obtaining motion was first suggested by the French engineer

Papin, about 200 years ago. In 1810, and again in 1827, Medhurst published

a scheme for 'propelling carriages through a close-fitting air-tight tunnel

by forcing in air behind them'; and in 1825 a similar project was patented

by Vallance of Brighton. About 1835 H. Pinkus, an American residing in

England, patented a pneumatic railway. The carriages were to travel on an

open line of rails, along which a cast-iron tube of between 3 and 4 feet

diameter was to be laid, having a longitudinal slit from 1 to 2 inches wide

and closed by a flexible valve along its upper side, through which a

connection could be formed between the leading carriage and a piston

working within the tube. This method was improved by Messrs. Clegg &

Samuda, who in 1840 tried some experiments on a portion of the West London

Railway with sufficient success to induce the Government to advance a loan

to the Dublin and Kingstown Railway Company, for the construction of a

pneumatic line from Kingstown to Dalkey. It was opened for passenger

traffic at the end of 1843, and was worked for many months. The London and

Croydon Company subsequently obtained powers for laying down an atmospheric

railway by the side of their other line from London to Croydon, and in

experimental trips in 1845 a speed of 30 miles an hour was obtained with

sixteen carriages, and of 70 miles with six carriages. But during the

intense heat of the summer of 1846 the iron tube frequently became so hot

as to melt the composition which sealed the valve, and the line had to be

worked by locomotives. The mechanical difficulty of commanding a sufficient

amount of rarefaction led to the abandonment of the system for railway

purposes. It has been revived, however, for the conveyance of letters and

parcels in towns by means of tubes of moderate diameter laid beneath the

streets. See _Pneumatic Dispatch_.

[Illustration: Atoll]

ATOLL', the Polynesian name for coral islands of the ringed type enclosing

a lagoon in the centre. They are found chiefly in the Pacific in

archipelagos, and occasionally are of large size. Suadiva Atoll is 44 miles

by 34; Rimsky 54 by 20. See _Coral_.

ATOMIC THEORY, a theory as to the existence and properties of atoms (see

_Atoms_); especially, in chemistry, the theory accounting for the fact that

in compound bodies the elements combine in certain constant proportions, by

assuming that all bodies are composed of ultimate atoms, the weight of

which is different in different kinds of matter. It is associated with the

name of Dalton, who systematized and extended the imperfect results of his

predecessors. On its practical side the atomic theory asserts three _Laws

of Combining Proportions_: (1) The Law of Constant or Definite Proportions,

teaching that in every chemical compound the nature and relative weights of

the constituent elements are definite and invariable; thus water invariably

consists of 8 parts by weight of oxygen to 1 part by weight of hydrogen;

(2) The Law of Multiple Proportions, according to which the several

proportions in which one element unites with a given weight of another

invariably bear towards each other a simple relation; thus 1 part by weight

of hydrogen unites with 8 parts by weight of oxygen to form water, and with

16 (i.e. 8x2) parts of oxygen to form peroxide of hydrogen; (3) The Law of

Combination in Reciprocal Proportions, that the proportions in which two

elements combine with a third also represent the proportions in which, or

in some simple multiple of which, they will themselves combine; thus in

olefiant gas hydrogen is present with carbon in the proportion of 1 to 6,

and in carbonic oxide, oxygen is present with carbon in the proportion of 8

to 6, 1 to 8 being also the proportions in which hydrogen and oxygen

combine with each other. The theory that these _proportional numbers_ are,

in fact, nothing else but the relative weights of atoms so far accounts for

the phenomena that the existence of these laws might have been predicted by

the aid of the atomic hypothesis long before they were actually discovered

by analysis. In themselves, however, the laws do not prove the theory of

the existence of ultimate particles of matter of a certain relative weight;

and although many chemists, even without expressly adopting the atomic

theory itself, have followed Dalton in the use of the terms _atom_ and

_atomic weight_, in preference to _proportion_, _combining weight_,

_equivalent_, and the like, yet in using the word _atom_ it should be held

in mind that it merely denotes the combining weights of the elements. These

will remain the same whether the atomic hypothesis which suggested the

employment of the term be true or false. Dalton supposed that the atoms are

spherical, and invented certain symbols to represent the mode in which he

conceived they might combine. The latest atomic hypothesis is one which

assigns an electrical structure to the atom. See _Chemistry_;

_Electricity_; _Matter_. Cf. H. E. Roscoe and A. Harden, _New View of

Dalton's Atomic Theory_; Sir J. J. Thomson, _Atomic Theory_.

ATOMIC WEIGHTS. See _Chemistry_; _Molecular Weights_.

ATOMISTS. See _Atoms_.

ATOMS, for many years regarded as the ultimate indivisible particles of the

chemical elements. The idea originated with some of the ancient

philosophers (the atomists), more especially Democritus (450 B.C.),

Epicurus, and Lucretius (99-55 B.C.), and was developed into a definite

theory by Dalton (1804). According to Dalton the atoms of any one element

are alike in all their properties, but differ from the atoms of other

elements, and when chemical combination occurs it takes place between the

atoms of the combining elements (see _Chemistry_). Various views have been

held with regard to the nature of atoms. Newton regarded them as hard,

ponderable particles, perfectly unalterable, and concluded that the

difference between substances was due to different kinds of atoms. Lord

Kelvin propounded the view that the properties of atoms might be explained

by those of vortices or vortex rings in a homogeneous frictionless fluid.

As a result of the researches of British and French physicists on radium,

the latest view is that matter and electricity are closely connected, that

atoms are not indivisible, but complex aggregates containing positive and

negative electrons, the differences between the atoms depending mainly on

the numbers of these electrons and their velocity. See _Radium_.

ATONEMENT, in Christian theology, the special work of Christ effected by

His life, sufferings, and death. The first explicit exposition of the

evangelical doctrine of the atonement is ascribed to Anselm, Archbishop of

Canterbury, in 1093.

ATRATO ([.a]-trae't[=o]), a river of S. America, in the north-west of

Colombia, emptying itself by nine mouths into the Gulf of Darien; it is

navigable by steamers of some size for 250 miles, and has long been the

subject of schemes for establishing water-communication between the

Atlantic and Pacific.

ATRAULI, a town of India, United Provinces, Aligarh district, clean, well

built, and with a good trade. Pop. 16,560.

* * * * *

Corrections made to printed original.

Article Animalcule. "but most of them are strictly microscopic.":

'miscroscopic' in original.

The New Gresham Encyclopedia. Amiel to Atrauli Vol. 1 Part 2 · 第 34 / 34 段