Crystal X-ray spectrometer

ID: crystal-x-ray-spectrometer

A crystal X-ray spectrometer selects a narrow wavelength interval by diffraction at known interplanar spacing and Bragg angle . For fixed diffraction order , a known lets an angular measurement determine . This reverses the crystallography problem of finding from a known wavelength.
Siegbahn's laboratory developed X-ray tubes and evacuated spectrographs for longer wavelengths. Rotating the crystal selected reflections; photographic plates recorded positions. Opposite-side exposures measured angles on both sides of the direct beam. Later tube instruments mounted a beam-defining slit opposite the plate holder. A separate double instrument compared two reflected beams with two ionization chambers. These were different instruments, not one universal assembly.[ref]
The Nobel biography describes constant-temperature spectrographs and a precision angular scale read by diametrically opposed microscopes.[ref] Temperature control matters because thermal expansion changes ; an accurately read angle cannot compensate for an unknown interplanar spacing.
Figure 1. . Original functional schematic, not a reconstruction of a particular Siegbahn instrument. Two slits illustrate collimation; the selected incident direction, rotatable crystal and movable readout define the geometry. The Bragg angle is measured from the lattice planes; the beam deflection is . The photographic plate and scanning ionization chamber are alternative readouts. Component sizes, angles and positions have no historical scale. Details.
The schematic separates preparation, selection and readout. An X-ray tube target supplies Characteristic X-rays with a possible bremsstrahlung background. A collimator limits incident directions; evacuation reduces air X-ray attenuation. Rotating the crystal brings different wavelengths into reflection. A photographic plate stores line positions over an exposure, whereas an ionization chamber can measure collected electric charge at successive angles. Neither readout alone establishes absolute wavelength: an angular zero, angular-scale calibration, diffraction order, and any required refraction correction enter the inference. Narrower slits reduce accepted angular spread but also reduce signal; a weak line can become harder to locate despite a narrower instrumental response.
A control reported in Siegbahn's lecture photographed a line system with copper-sulphate and calcium-sulphate crystals. Irregular relative shifts around copper's characteristic frequency supported anomalous dispersion; the arrangement excluded differing absorption across that frequency as the explanation.[ref] A finer angular scale alone cannot remove this physical refraction correction.

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