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201Chapter 12 Chromatography and Electrophoresis Chapter 12 1. (a) To calculate the number of theoretical plates we use equation 12.15; thus N w t 16 16 0.15 min 8.04 min 46000 plates 2 A A r,A 2 # #= = =` aj k .N w t 16 16 858 26 0.15 min min 4 00 plates 2 B r,B 2 B # #= = =` aj k .N w t 16 16 6 8 43 44 0.1 min min 4 00 plates 2 C r,C 2 C # #= = =` aj k he average number of theoretical plates is 46 300. (b) he height of a theoretical plate, H, is equal to L/N where L is the length of the column and N is the number of theoretical plates. Using the average number of theoretical plates from part (a) gives the average height as H 46300 plates 20 m m 1000 mm 0.43 mm/plate # = = (c) heoretical plates do not really exist; they are, instead, an artiicial construct that is useful for modeling the variables that afect the width of a solute’s peak and its resolution relative to other solutes. As we see from equation 12.15, the number of theoretical plates for a solute is deined in terms of its retention time and its peak width. Two solutes may have identical retention times but diferent peak widths because retention time is a function of the equilibrium between the concen- tration of solute in the mobile phase and the concentration of solute in the stationary phase, but peak width is a function, in part, of the kinetic efects that control how quickly the solute moves within the stationary phase and within the mobile phase. 2. Using equation 12.1, the resolution between solutes A and B is ( ) . . ( . . ) . .min min min min R w w t t2 0 15 0 15 2 8 26 8 04 1 47 1 5AB A B r,B r,A .= + - = + - = and the resolution between solutes B and C is ( ) . . ( . . ) . . min min min min R w w t t2 0 15 0 1 2 8 43 8 1 1 6 26 10 1BC r, B C C r,B .= + - = + - = To calculate selectivity factors or to calculate resolution using equa- tion 12.19, we irst must calculate each solute’s retention factor using equation 12.8; thus . . . . .min min mink t t t 1 19 8 04 1 19 5 756 5 76A m r,A m .= - = - = . . . . .min min mink t t t 1 19 8 1 19 5 5 9426 941 m m B r,B .= - = - =