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Investigations on the Theory of the Brownian Movement
I
On the Movement of Small Particles Suspended in a Stationary Liquid Demanded by the Kinetic Theory of Heat
(From the Annalen der Physik (4), 17, 1905, pp. 549–560)
In this paper it will be shown that according to the molecular-kinetic theory of heat, bodies of microscopically-visible size in a liquid will perform movements of such magnitude that they can be easily observed in a microscope, on account of the molecular motions of heat. It is possible that the movements to be discussed here are identical with the so-called Brownian molecular motion; however, the information available to me regarding the latter is so lacking in precision, that I can form no judgment in the matter. If the movement discussed here can actually
2 · Theory of Brownian Movement
it that one would expect to find), then classical thermodynamics can no longer be looked upon as applicable with precision to bodies even of dimensions distinguishable in a microscope: an exact determination of actual atomic dimensions is then possible. On the other hand, had the prediction of this movement proved to be incorrect, a weighty argument would be provided against the molecular-kinetic conception of heat.
§ 1. On the Osmotic Pressure to be Ascribed to the Suspended Particles
Let z gram-molecules of a non-electrolyte be dissolved in a volume V* forming part of a quantity of liquid of total volume V. If the volume V* is separated from the pure solvent by a partition permeable for the solvent but impermeable for the solute, a so-called "osmotic pressure," p, is exerted on this partition, which satisfies the equation
when V* / z is sufficiently great.
On the other hand, if small suspended particles are present in the fractional volume V* in place of the dissolved substance, which particles are also unable to pass through the partition permeable to the solvent: according to the classical theory of
Movement of Small Particles · 3
thermodynamics—at least when the force of gravity (which does not interest us here) is ignored—we would not expect to find any force acting on the partition; for according to ordinary conceptions the "free energy" of the system appears to be independent of the position of the partition and of the suspended particles, but dependent only on the total mass and qualities of the suspended material, the liquid and the partition, and on the pressure and temperature. Actually, for the calculation of the free energy the energy and entropy of the boundary-surface (surface-tension forces) should also be considered; these can be excluded if the size and condition of the surfaces of contact do not alter with the changes in position of the partition and of the suspended particles under consideration.
But a different conception is reached from the standpoint of the molecular-kinetic theory of heat. According to this theory a dissolved molecule is differentiated from a suspended body solely by its dimensions, and it is not apparent why a number of suspended particles should not produce the same osmotic pressure as the same number of molecules. We must assume that the suspended particles perform an irregular movement—even if a very slow one—in the liquid, on
4 · Theory of Brownian Movement
account of the molecular movement of the liquid; if they are prevented from leaving the volume V* by the partition, they will exert a pressure on the partition just like molecules in solution. Then, if there are n suspended particles present in the volume V*, and therefore ν in a unit of volume, and if neighbouring particles are sufficiently far separated, there will be a corresponding osmotic pressure p of magnitude given by
where N signifies the actual number of molecules contained in a gram-molecule. It will be shown in the next paragraph that the molecular-kinetic theory of heat actually leads to this wider conception of osmotic pressure.
§ 2. Osmotic Pressure from the Standpoint of the Molecular-Kinetic Theory of Heat (*)
If p1, p2, … pl are the variables of state of
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a physical system which completely define the instantaneous condition of the system (for example, the Co-ordinates and velocity components of all atoms of the system), and if the complete system of the equations of change of these variables of state is given in the form
whence
then the entropy of the system is given by the expression
where T is the absolute temperature, Ē the energy of the system, E the energy as a function of pν. The integral is extended over all possible values of pν consistent with the conditions of the problem. ϰ is connected with the constant N referred to before by the relation 2ϰN = R. We obtain hence for the free energy F,
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Now let us consider a quantity of liquid enclosed in a volume V; let there be n solute molecules (or suspended particles respectively) in the portion V* of this volume V, which are retained in the volume V* by a semi-permeable partition; the integration limits of the integral B obtained in the expressions for S and F will be affected accordingly. The combined volume of the solute molecules (or suspended particles) is taken as small compared with V*. This system will be completely defined according to the theory under discussion by the variables of condition p1…pl.
If the molecular picture were extended to deal with every single unit, the calculation of the integral B would offer such difficulties that an exact calculation of F could be scarcely contemplated. Accordingly, we need here only to know how F depends on the magnitude of the volume V*, in which all the solute molecules, or suspended bodies (hereinafter termed briefly "particles") are contained.
We will call x1, y1, z1 the rectangular Co-ordinates of the centre of gravity of the first particle, x2, y2, z2 those of the second, etc., xn, yn, zn those of the last particle, and allocate for the centres of gravity of the particles the indefinitely small domains of parallelepiped form dx1, dy1, dz1; dx2
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dy2, dz2, … , dxn, dyn, dzn, lying wholly within V*. The value of the integral appearing in the expression for F will be sought, with the limitation that the centres of gravity of the particles lie within a domain defined in this manner. The integral can then be brought into the form
where J is independent of dx1, dy1 etc., as well as of V*, i.e. of the position of the semi-permeable partition. But J is also independent of any special choice of the position of the domains of the centres of gravity and of the magnitude of V*, as will be shown immediately. For if a second system were given, of indefinitely small domains of the centres of gravity of the particles, and the latter designated dx′1dy′1dz′1; dx′2dy′2dz′2 … dx′ndy′ndz′n, which domains differ from those originally given in their position but not in their magnitude, and are similarly all contained in V*, an analogous expression holds:
Whence
Therefore
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But from the molecular theory of Heat given in the paper quoted, (*) it is easily deduced that dB / B (or dB′ / B respectively) is equal to the probability that at any arbitrary moment of time the centres of gravity of the particles are included in the domains (dx1…dxn) or (dx′1…dx′n) respectively. Now, if the movements of single particles are independent of one another to a sufficient degree of approximation, if the liquid is homogeneous and exerts no force on the particles, then for equal size of domains the probability of each of the two systems will be equal, so that the following holds:
But from this and the last equation obtained it follows that
We have thus proved that J is independent both of V* and of x1, y1, … , zn. By integration we obtain
and thence
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It has been shown by this analysis that the existence of an osmotic pressure can be deduced from the molecular-kinetic theory of Heat; and that as far as osmotic pressure is concerned, solute molecules and suspended particles are, according to this theory, identical in their behaviour at great dilution.
§ 3. Theory of the Diffusion of Small Spheres in Suspension
Suppose there be suspended particles irregularly dispersed in a liquid. We will consider their state of dynamic equilibrium, on the assumption that a force K acts on the single particles, which force depends on the position, but not on the time. It will be assumed for the sake of simplicity that the force is exerted everywhere in the direction of the x axis.
Let ν be the number of suspended particles per unit volume; then in the condition of dynamic equilibrium ν is such a function of x that the variation of the free energy vanishes for an arbitrary virtual displacement δx of the suspended substance. We have, therefore,
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It will be assumed that the liquid has unit area of cross-section perpendicular to the x axis and is bounded by the planes x = 0 and x = l. We have, then,
and
Therefore
for any value of δx, but since this must hold
and, assuming the validity of the law of osmotic pressure (van 't Hoff),
The required condition of equilibrium is therefore
or
The last equation states that equilibrium with the force K is brought about by osmotic pressure forces.
Equation (1) can be used to find the coefficient of diffusion of the suspended substance. We can look upon the dynamic equilibrium condition considered here as a superposition of two processes proceeding in opposite directions, namely:
I. A movement of the suspended substance under the influence of the force K acting on each single suspended particle.
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2. A process of diffusion, which is to be looked upon as a result of the irregular movement of the particles produced by the thermal molecular movement.
If the suspended particles have spherical form (radius of the sphere = P), and if the liquid has a coefficient of viscosity k, then the force K imparts to the single particles a velocity (*)
and there will pass a unit area per unit of time
particles.
If, further, D signifies the coefficient of diffusion of the suspended substance, and μ the mass of a particle, as the result of diffusion there will pass across unit area in a unit of time,
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Since there must be dynamic equilibrium, we must have
We can calculate the coefficient of diffusion from the two conditions (1) and (2) found for the dynamic equilibrium. We get
The coefficient of diffusion of the suspended substance therefore depends (except for universal constants and the absolute temperature) only on the coefficient of viscosity of the liquid and on the size of the suspended particles.
§ 4. On the Irregular Movement of Particles Suspended in a Liquid and the Relation of this to Diffusion
We will turn now to a closer consideration of the irregular movements which arise from thermal molecular movement, and give rise to the diffusion investigated in the last paragraph.
Evidently it must be assumed that each single particle executes a movement which is independent of the movement of all other particles; the movements of one and the same particle after
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different intervals of time must be considered as mutually independent processes, so long as we think of these intervals of time as being chosen not too small.
We will introduce a time-interval τ in our discussion, which is to be very small compared with the observed interval of time, but, nevertheless, of such a magnitude that the movements executed by a particle in two consecutive intervals of time τ are to be considered as mutually independent phenomena.
Suppose there are altogether n suspended particles in a liquid. In an interval of time τ the x‑Co-ordinates of the single particles will increase by Δ, where Δ has a different value (positive or negative) for each particle. For the value of Δ a certain probability-law will hold; the number dn of the particles which experience in the time-interval τ a displacement which lies between Δ and Δ + dΔ, will be expressed by an equation of the form
where
and φ only differs from zero for very small values of Δ and fulfils the condition
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We will investigate now how the coefficient of diffusion depends on φ, confining ourselves again to the case when the number ν of the particles per unit volume is dependent only on x and t.
Putting for the number of particles per unit volume ν = f(x,t), we will calculate the distribution of the particles at a time t + τ from the distribution at the time t. From the definition of the function φ(Δ) there is easily obtained the number of the particles which are located at the time t + τ between two planes perpendicular to the x‑axis, with abscissae x and x+dx. We get
Now, since τ is very small, we can put
Further, we can expand f(x+Δ, t) in powers of Δ:
We can bring this expansion under the integral sign, since only very small values of Δ contribute anything to the latter. We obtain
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On the right-hand side the second, fourth, etc., terms vanish since φ(Δ)=φ(−Δ); whilst of the first, third, fifth, etc., terms, every succeeding term is very small compared with the preceding. Bearing in mind that
and putting
and taking into consideration only the first and third terms on the right-hand side, we get from this equation
This is the well-known differential equation for diffusion, and we recognise that D is the coefficient of diffusion.
Another important consideration can be related to this method of development. We have assumed that the single particles are all referred to the same Co-ordinate system. But this is unnecessary, since the movements of the single particles are mutually independent. We will now refer the motion of each particle to a co-ordinate
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system whose origin coincides at the time t=0 with the position of the centre of gravity of the particles in question; with this difference, that f(x,t) dx now gives the number of the particles whose x Co-ordinate has increased between the time t=0 and the time t=t by a quantity which lies between x and x+dx. In this case also the function f must satisfy, in its changes, the equation (1). Further, we must evidently have for t=0,
The problem, which accords with the problem of the diffusion outwards from a point (ignoring possibilities of exchange between the diffusing particles) is now mathematically completely defined; the solution is
The probable distribution of the resulting displacements in a given time t is therefore the same as that of fortuitous error, which was to be expected. But it is significant how the constants in the exponential term are related to the coefficient of diffusion. We will now calculate with the help
Movement of Small Particles · 17
of this equation the displacement λx in the direction of the X‑axis which a particle experiences on an average, or—more accurately expressed—the square root of the arithmetic mean of the squares of displacements in the direction of the X‑axis; it is
The mean displacement is therefore proportional to the square root of the time. It can easily be shown that the square root of the mean of the squares of the total displacements of the particles has the value λx√3. (12)
§ 5. Formula for the Mean Displacement of Suspended Particles. A New Method of Determining the Real Size of the Atom
In § 3 we found for the coefficient of diffusion D of a material suspended in a liquid in the form of small spheres of radius P
Further, we found in § 4 for the mean value of the displacement of the particles in the direction of the X‑axis in time t
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By eliminating D we obtain
This equation shows how λx depends on T, k, and P.
We will calculate how great λx is for one second, if N is taken equal to 6·10²³ in accordance with the kinetic theory of gases, water at 17°C is chosen as the liquid (k = 1·35·10−2), and the diameter of the particles 0·001 mm. We get
The mean displacement in one minute would be, therefore, about 6 μ.
On the other hand, the relation found can be used for the determination of N. We obtain
It is to be hoped that some enquirer may succeed shortly in solving the problem suggested here, which is so important in connection with the theory of Heat.
(Received, 11 May, 1905.)
II
On the Theory of the Brownian Movement
(From the Annalen der Physik (4), 19, 1906, pp. 371–381)
Soon after the appearance of my paper (*) on the movements of particles suspended in liquids demanded by the molecular theory of heat, Siedentopf (of Jena) informed me that he and other physicists—in the first instance, Prof. Gouy (of Lyons)—had been convinced by direct observation that the so-called Brownian motion is caused by the irregular thermal movements of the molecules of the liquid. (**)
Not only the qualitative properties of the Brownian motion, but also the order of magnitude of the paths described by the particles correspond completely with the results of the theory. I will not attempt here a comparison of the slender experimental material at my disposal with the
(**) Gouy, Journ. de Phys., 2e sér., 7, p. 561, 1888; Compt. rend., 109, p. 102, 1889.