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was suggested (Perkin-Elmer by Schmidt and Slavin Corp.) in their compa- ny’s Chromatography 1978). Newsletter (6: 22, References I. Soldin, S. J., and Hill, J. G., Rapid micro method for measuring anticonvulsant drugs in serum by high-pressure liquid chromatography. Clin. Chem. 22,856-859 (1976). 2. Kabra, P. M., Stafford, B. E., and Marton, L. J., Simultaneous measurement of phenobarbital, phenytoin, primidone, ethosuximide, and carbamazepine by high-pressure liquid chromatography. Clin. Chem. 23, 1284-1288 (1977). 3. Fairinotti, R., Pfaff, M. C., and Mahuzier, C., Simultaneous determination of phenobarbital and valproic acid in plasma using high performance liquid chromatography. Ann. Biol. Clin. 36, 347-353 (1978). 4. Gupta, R. N., Eng, F., and Gupta, M. L., Gas-chromatographic analysis of vaiproic acid as phenacyl esters. Clin. Chem. 25, 1303-1305 (1979). 5. Borch, R. F., Separation of long chain fatty acids as phenacyl esters by high pressure liquid chromatography. Anal. Chem. 47, 2437-2439 (1975). Ram N. Gupta Paul M. Keane Mohan L. Gupta Clinical Chemistry Laboratory St. Joseph’s Hospital 50 Charlton Avenue East Hamilton, Ontario, Canada L8N 1 Y4 Simple Technique for the Camera X-Ray Powder DiffractionStudy of Urinary Calculi To the Editor: Determination of the composition of the nucleus and individual layers of a urinary calculus is of vital importance in establishing the pathogenesis of urinary stone formation. This information cannot be obtained by conventional wet chemical techniques, especially in the case of small calculi. We describe an easy, accurate method based on the classical Debye-Scherrer camera x-ray powder diffraction technique (1-4), which overcomes this problem. After being crushed slightly with a glass slide, the urinary calculus is examined in a Petri dish under a binocular stereoscopic microscope with approximately 40X magnification, to determine whether it is a simple or a mixed calculus. In the case of large or extremely hard calculi, a dental-extraction forceps or a pair of long-nosed pliers may be used to crush the calculus. Most stones are of mixed composition and consist of several concentric layers, including a nucleus, so it is desirable to separate these and examine them individually. It must be noted, however, that a difference in appearance between two consecutive layers often, but not always, means a difference in composition. In many calculi, the nucleus consists of a substance different from that of the outer shell. The carefully selected grain of microscopic size, which may weigh less than 5 g or measure less than 0.1 mm in diameter, is transferred to a clean glass slide with a thin, sharp biological dissecting needle. By means of a needle, the grain is then covered with a small drop of rubber solution (such as can be obtained in a bicycle repair kit), diluted with benzene. The grain is ground into the solution between this slide and another, without losing any material. Short strokes will prevent the powder from spreading too much. By inspection under the stereoscopic microscope, one can ascertain when the material is fine enough. The slides are separated from one another for a few seconds to allow the benzene to evaporate. Each slide will show a circular area of clear, sticky rubber, with the calculus powder confined to the center of each. The two slides are again opposed and with a circular motion the powder-rich solution is rubbed into a small ball, about 0.2 mm in diameter. This ball is mounted on the tip of a stiff hair, which has previously been wetted with rubber solution and mounted in a Debye-Scherrer x-ray powder camera, with the ball centered in the middle of the monochromatic x-ray beam. Ni-filtered Cu ka radiation, produced at 40 kV and 20 mA, and x-ray cameras of 57.3 mm diameter are used. To obtain x-ray photographs of good resolution, an exposure time of 2 h is required. Because every crystalline substance, whether organic or inorganic, has a unique and characteristic powder diffraction pattern, the x-ray diffraction spacing data obtained from the photograph of the urinary calculus can be compared with information in the J.C.P.D.S. (Joint Committee for Powder Diffraction Standards) powder data file to determine the composition of the unknown substance by means of its internal atomic arrangement. The x-ray powder patterns may also be identified by directly comparing the unknown patterns with previously prepared standard x-ray powder patterns of known substances. This physical analytical method provides a powerful tool in the routine study of calculi. Although most clinical chemistry laboratories do not have their own facilities for camera x-ray powder diffraction, such equipment is available at most universities. The technique described here is relatively simple in the hands of a skilled operator and yields much information as to the detailed structure of the calculus. References 1. Klug, H. P., and Alexander, L. E., X-Ray Diffraction Procedures. John Wiley, New York, NY, 1954, p 716. 2. Az#{225}roff, L. V., and Buerger, M. J., The Powder Method. McGraw-Hill, New York, NY, 1958, p 342. 3. Nuffield, E. W., X-Ray Diffraction Methods. John Wiley, New York, NY, 1966, p 409. 4. Flutchison, C. S., ,Laboratory Handbook of Petrographic Techniques. John Wiley, New York, NY, 1974, pp 132-179. G. J. Beukes’ A. De Waal2 Depts. of Geochemistry’ and Chemical Pathology2 University of the Orange Free State Bloemfontein, R.S.A. CLINICAL CHEMISTRY, Vol. 25, No. 11, 1979 1985