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The first INSERT statement (for Detroit this time) will still fail, because the new row refers to employee number 115 as the office manager, and Ben Adams is not yet in the database! To prevent this insertion deadlock, at least one of the foreign keys in a referential cycle must permit NULL values. In the actual definition of the sample database, the MGR column does not permit NULLs, but the REP_OFFICE does. The two-row insertion can then be accomplished with two INSERTs and an UPDATE, as shown here:

However, slip occurs in iron crystals with shear stresses of only 4 to 5 kpsi, which is more than two orders of magnitude smaller The theoretical shear strength of the other pure metals is also 400 to 500 times larger than the actual shear strength The commonly accepted explanation of why the actual shear stress is so much lower than the theoretical value is that slip does not occur by the simultaneous movement of all the atoms along the slip plane; rather, it occurs by the movement of individual rows (the dislocation row or plane) of atoms Thus it is the movement of dislocations along the slip plane to the grain boundary that causes the actual shear stress for plastic deformation to be so low Figure 3211c, d, and e illustrates the movement of a dislocation that results in slip.

MPEG-4 s language for describing and dynamically changing the scene is named the Binary Format for Scenes (BIFS). BIFS commands are available not only to add or delete objects from the scene, but also to change

INSERT INTO SALESREPS (EMPL_NUM, NAME, REP_OFFICE, HIRE_DATE, SALES) VALUES (115,'Ben Adams', NULL, '2008-04-01', 0.00); INSERT INTO OFFICES (OFFICE, CITY, REGION, MGR, TARGET, SALES) VALUES (14,'Detroit', 'Eastern', 115, 0.00, 0.00); UPDATE SALESREPS SET REP_OFFICE = 14 WHERE EMPL_NUM = 115;

In real crystals of metals, slip terminates at the grain boundaries or the freesurface faces and causes substantial jogs or steps, much larger than shown in Fig 3211 Experimental study of the spacings of the slip planes and the sizes of the jog have been made on some of the common metals The spacing of the parallel planes along which slip occurs varies randomly, with an average distance between slip planes of about 2000 atom diameters The length of the step or jog at the surface of the grain is approximately 200 to 700 atom diameters The atomic displacements associated with slip, unlike those of the initial movements of dislocations, are irreversible in that the slip jog remains when the shear stresses are removed That is, slip causes a permanent change in shape, or plastic deformation, as it is called.

Part III:

The evidence of slip is seen on metallurgically prepared samples as slip lines when examined under a microscope The slip lines are the intersection of the crystallographic planes along which slip occurred with the etched surface of the specimen Slip results in a narrow band on either side of the slip plane within which the lattice structure is severely distorted These slip lines do not appear on the face of a specimen that is metallurgically polished after slip occurs; they appear only after etching with a suitable chemical reagent that dissolves the metal being studied The slip lines become visible for the same reason that grain boundaries are visible after etching: The internal energy of the material within the distorted area is considerably higher than that of the material within the rest of the crystal.