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Thus the limiting values of G E / x 1 x 2 ~ ~ are equal to the infinite-dilution limits of In yl and In y2 This result is illustrated in Fig 125(b) These results depend on Eq (127), which is valid for constant T and P Although the data of Table 122 are for constant T , but variable P , negligible error is introduced through Eq (127), because liquid-phase activity coefficients are very nearly independent of P for systems at low to moderate pressures Equation (127) has further influence on the nature of Fig 125(b) Rewritten as,

OpenSuSE distribution also has a capable GUI tool for managing disks, partitions, and the LVM Issue the command yast2 lvm_config to launch the utility, shown here:

it requires the slope of the In yl curve to be everywhere of opposite sign to the slope of the In y2 curve Furthermore, when x2 -+ 0 (and xl + I), the slope of the In yl curve is zero Similarly, when xl + 0, the slope of the In y2 curve is zero Thus, each In yi (i = 1 , 2 ) curve terminates at zero with zero slope at xi = 1

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With the volumes created, you need to put file systems on them (If you re accustomed to Microsoft Windows, this is akin to formatting the disk once you ve partitioned it) The type of file system that you want to create will determine the particular utility that you should use In this project, we want to create an ext3-type file system; therefore, we ll use the mkfsext3 utility Many command-line parameters are available for the mkfsext3 tool, but we ll use it in its simplest form here Following are the steps for creating a file system: 1 The only command-line parameter you ll usually have to specify is the partition (or volume) name onto which the file system should go To create a file system on /dev/VolGroup00/LogVol04, you would issue the following command:

Of the sets of points shown in Fig 125(b), those for G E / x l x 2 Rmost closely conform to a ~ simple mathematical relation Thus a straight line provides a reasonable approximation to this set of points, and mathematical expression is given to this linear relation by the equation: GE = A21~1 A12~2 xlx2RT where Azl and A12are constants in any particular application Alternatively,

[root@fedora-serverA ~]# mkfsext3 /dev/VolGroup00/LogVol04 mke2fs 14* (12-Jun-2010) Filesystem label= OS type: Linux Block size=4096 (log=2) (Output truncated) This file system will be automatically checked every 37 mounts or 180 days, whichever comes first Use tune2fs -c or -i to override

(129a)

Once the preceding command runs to completion, you are done with creating the file system We will next begin the process of trying to relocate the contents of the current /var directory to its own separate file system 2 Create a temporary folder that will be used as the mount point for the new file system Create it under the root folder Type

Wired!

Expressions for In yl and In y2 are derived from Eq (129b) by application of Eq (1192) ~ Since this requires differentiation of n G E / R with respect to a mole number, Eq (129b) is

[root@fedora-serverA ~]# cp -rp /var/* /new_var/

multiplied by n and all mole fractions are converted to mole numbers Thus on the right side xl is replaced by n l / ( n l n2),and x2, by n 2 / ( n l n2)Since n nl n2, this gives:

5 In order to avoid taking down the system into single-user mode to perform the following sensitive steps, we will resort to a few old military tricks Type

Differentiating with respect to n 1 in accord with Eq ( 1 192) yields:

The preceding step is necessary because the rpc_pipefs pseudo-file system happens to be mounted under a subfolder in the /var directory

Reconversion of the ni to xi (ni = nxi) gives:

7:

leads to: Further reduction, noting that x2 = 1 - X I ,

8 Restore the security contexts for the new /var folder so that the daemons that need it can use it Type

Similarly, differentiation of Eq (129b) with respect to n2 yields: In y2 = x [ ~ 2 -t- 26412 - A211~21 1 These are the ~ a r ~ u l e s ~ e ~ u a t and they represent a commonly used empirical model of ions, solution behavior For the limiting conditions of infinite dilution, they become: In y O = A12 p

(x2 = 0 )

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