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15.1.4.4 Destination JMS Destination objects are represented by the javax.jms.Destination Java interface. Each JMS messaging domain has two Java interfaces that inherit from this independent interface (one for a temporary destination and one for a nontemporary destination). A temporary destination only exists for the lifetime of the session that creates it. Therefore, this package contains four names, representing the four possible subtypes: Queue, TemporaryQueue, Topic, and TemporaryTopic. Even though there are several methods for obtaining a Destination object, we will only consider how we would lookup a nontemporary Destination in Figure 15.9. This can essentially be done in the same way that we obtained the Connection Factory object, except that in this code, we would specify the destination (Topic or Queue) name using the proprietary JMS Provider de ned syntax. The generic-example code to create a Destination object is shown in Figure 15.9. Note that this is not the proprietary mechanism for actually de ning and creating a destination within the JMS Provider instance. Instead, this is the mechanism we use to specify the details for the administered object, so that we can create Message Producer objects and Message Consumer objects that connect to the destination within the JMS Provider instance.

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The main thing to remember about a custom function written in VBA is that a value is always assigned to its name a minimum of one time, generally when it has completed execution. To create a custom function, start by inserting a VBA module. (Or you can use an existing module.) Enter the keyword Function, followed by the function s name and a list of its arguments (if any) in parentheses. You can also declare the data type of the return value by using the As keyword (this is optional, but recommended). Insert the VBA code that performs the work, and make sure that the appropriate value is assigned to the term corresponding to the function s name at least once within the body of the Function procedure. End the function with an End Function statement. Function names must adhere to the same rules for variable names. If you plan to use your custom function in a worksheet formula, make sure the name is not in the form of a cell address (for example, a function named J21 won t work in a formula). And, avoid using function names that correspond to Excel s built-in function names. If there is a function name conflict, Excel will always use its built-in function.

Function Reverse(InString) As String Returns its argument, reversed Dim i as Integer, StringLength as Integer Reverse = StringLength = Len(InString) For i = StringLength To 1 Step -1 Reverse = Reverse & Mid(InString, i, 1) Next i End Function

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The Developers Edition of Microsoft Office includes a Setup Wizard that helps you prepare your applications for distribution.

The granular nature of the aquifer, and the lack of gradients steep enough to provoke turbulent ows The aquifer is underlain by dense mudstones of Tertiary age, which also outcrop in the valley anks where the sands and gravels feather-edge; the river partially penetrates the aquifer and can only interact with the aquifer via its bed sediment Pumping tests show high values of S consistent with uncon ned conditions; piezometry beneath the alluvium indicates local con nement, in that head in wells piercing the gravels rises above the elevation of the base of the alluvium Although the aquifer is composed of interleaving lenses of sand and gravel, the variations in K associated with these occur over distances of only a few meters, with repetition of patterns on scales of tens of meters; strati cation of the sands and gravels implies K vertical < K horizontal Sampling of streambed sediment revealed it all to be of ne silt/mud grade (hence low K ); there is no evidence that it varies dramatically from place to place; as the streambed is always fully saturated, it can only have con ned -type storativity (i.e. very low values for S) Because the alluvium forms the banks of the river in almost all places, and the aquifer is much more permeable than either the alluvium or the streambed sediment, and because the channel gradient is very gentle, the law of groundwater refraction suggests that ow in the streambed sediment will be predominantly vertical almost everywhere