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To carry out client-side programming in e-commerce applications, there are several different ways, which include using HTML, JavaScript, Java Applets, and ActiveX controls. Furthermore, one could also use plugins, which are applications of different sorts that are embedded in a web page for performing special functions (e.g. showing animations). In this chapter, we will focus on HTML because it forms the basis of nearly all the client-side programming techniques. Furthermore, we will give an overview of JavaScript towards the end of this chapter. It enhances the functions of HTML and makes a web page more interactive and dynamic. While there are many client-side programming techniques available, HTML and JavaScript are currently the most commonly used programming techniques for building the user interface at the client side. A very important factor in client side programming for e-commerce applications is downloading time. This is the time required to download a web page and its associated elements from the server side to the client side over the internet. This depends on many factors, including the quality of the network and the type of connection to the network. For B2C applications, many clients are likely to access the internet using dial-up modems, working at 56.6 Kbps or below. In B2B applications,

So, what country is home to Apple Computers Frankly, who cares What difference would it make Of course, you know Apple is the quintessential American company. It encompasses much of what the world loves about the United States, and the truth is, I don t think anybody else could have created anything so cool and, well, American as Apple. I mean, think of it: the Big Apple, apple pie, baseball, Chevrolet c mon, you know the drill. And there s no U.S.-based company that is truly bene ting from a world without economic

The Entry widget is used to accept single-line text strings from a user. Let s now look at the syntax to display an Entry widget in an application:

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The toolbar appears across the top of the Document window, whether in Design or Code view. On the toolbar you ll find some of the most frequently used commands that affect the entire document. The toolbar itself is toggled by choosing View Toolbar or by choosing Ctrl+Shift+T (Command+Shift+T). One of the best features of the toolbar is its quick and easy access to changing your Web page s title, as shown in Figure 3-5.

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<form name=''search"action="/servlet/vbs.mall.searchengine. SearchEngine" method="get > " <div align="center"><center><table border="l" cellpadding=" 'I cellspacing='I 0'I 5 bgcolor="#FFCC99 bordercolor="black"> <tr> <td align="center"colspan="3"><b>AdvancedSearch:<b></td> </tr>

SECTION 2.4. Modeling: Free Oscillations (Mass Spring System), page 61 Purpose. To present a main application of second-order constant-coefficient ODEs my cy ky 0

so Xn-k+i - bi(x) is a multiple of g(x) and must be a codeword. Using these codewords for i = 0, 1, . . . , k - 1 to form the rows of the generator matrix, we obtain

By including a textual justi cation, a rule trace could display not only the rule itself but also an English explanation. The causal diagram, together with these explanatory textual fragments, would offer even more system transparency than either one alone could.

by a mechanism by which oceanic lithosphere also was destroyed at high rates. An important aspect of the origin of TTG suites is the type of source material that melted to produce the magma. Early petrologic studies suggested that these magmas could result from the partial melting of subducted oceanic crust in the presence of water (Martin, 1986). However, more recent work has emphasized other sources, including the lower crust of arcs and the base of thick oceanic plateaux (Smithies, 2000; Condie, 2005a). The importance of the source material is illustrated by a two-stage model proposed by Foley et al. (2003). This model envisages that during the Early Archean, oceanic crust was too thick to be subducted as a unit, and so its lowermost parts delaminated and melted (Fig. 11.7a). These lower roots are inferred to have been pyroxenites that were produced by the metamorphism of ultrama c cumulate layers. The melting of the pyroxenite did not favor the generation of TTG

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