Principles of operation of optical methods

Optical methods allow the detection of density variations that occur in a fluid due to changes in temperature and/or speed and/or composition. The principle on which these methods are based is that the variation of density, p, produces a variation of the refractive index, n, of the fluid which in turn influences the trajectory (refraction) and the phase of the light rays that pass through the fluid. Appropriate optical devices convert the resulting effect in changes of light intensity on a screen or on a photograph.

Подпись: n1 -1 ІП + 2 Подпись: pR(X) Подпись: (6.1)

The index of refraction, n, of a transparent medium, which is the ratio between the speed of light in vacuum and the speed of light in the substance, is related to the density by the Lorenz-Lorentz equation:

where R (l) is, for each substance, a function of the wavelength, l of the light.

When the index of refraction n = 1, as in the case of gases (see Table 6.1), Equation (6.1) can be expanded in series and, stopping the

Substance

Index of Refraction, n [-] (Sodium D line)

Quartz

1.45843

Gelatin

1.516-1.534

Canada balsam

1.53

Crown Glass

1.517

Flint Glass

1.575-1.89

Water (15°C)

1.33377

Air (0°C, 760 mm Hg)

1.0002926

Carbon dioxide

1.000448-1.000454

Helium

1.00036-1.00036

Nitrogen

1.000296-1.000298

Water vapor

1.00249

Table 6.1

Refractive index of some substances

series at the first two terms, the simpler Gladstone-Dale equation is obtained:

n = 1 + K(X) p = 1 + ^( ) p (6.2)

Ps

where K(l) = 1.5 R(l) and ps is the density at standard conditions (T = 0°C, p = 760 mmHg).

The values of P for some gases are reported in Table 6.2.

Changes in the Gladstone-Dale constant with the wavelength are limited to a few percentages (see Table 6.3).

Gas

P.104

Air

2.92

Carbon dioxide

4.51

Nitrogen

2.97

Helium

0.36

Oxygen

2.71

Water vapor

2:54

Table 6.2

Values of constant P for l = 589.3 nm

Wavelength l nm

Gladstone-Dale constant K.103 m3kg_1

262.0

0.2426

296.0

0.2380

334.0

0.2348

436.0

0.2297

470.0

0.2287

479.8

0.2284

489.0

0.2281

505.0

0.2276

510.0

0.2276

521.0

0.2272

546.0

0.2269

578.0

0.2265

579.0

0.2263

614.7

0.2261

644.0

0.2258

Table 6.3

Gladstone-Dale constant for air

Подпись: Figure 6.14

Effects of a change of refractive index on a light ray

Assume that the fluid is confined in a region of space and that the region is crossed by a beam of parallel rays of monochromatic light that propagate along the axis z. A generic ray (Figure 6.14), in the absence of disturbance, i. e. the properties of the fluid are uniform in the region, reaches the screen at the point P at time t; if the fluid properties are not uniform, the trajectory of the ray deviates of an angle A© from the straight line due to the phenomenon of refraction and the ray reaches the screen at the point P’ at the time t’ Since a change in density is related to a change in refractive index, and thus to the speed of light in the medium, the various rays reach the screen at different times. Appropriate optical systems highlight separately, by variations in the brightness of the image, the displacement PP’ (shadowgraph) or the deflection A© (Schlieren method) or the phase delay At (interferometric methods).

We will show below that the shadowgraph method is sensitive to the gradients of the gradients of density, the Schlieren method and the differential interferometer visualize the values of density gradients, and the separated beam interferometer measures the difference Ap between the local density and a reference density. It is then obvious that an interferogram obtained with a separated beam interferometer lends itself to a quantitative analysis of the density field much better than a shadowgraph that requires a double integration resulting in heavy approximation errors.