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The preceding XML states the following about the application This Web application may have zero or more security constraints Each security constraint contains zero or more collections of pages, and access to any of the pages is predicated on the user being a member of the specified role A user s membership in a role is determined using some form of authentication method The previous webxml excerpt says, Users that try to access any page inside of the top-level trainer directory must be authenticated using form-based authentication, with the authentication database being provided by the container-specific file realm Once authenticated, they must be a member of the trainer group in order to be allowed to see the page Each of the elements related to authorization in <securityconstraint> is described in Table 14-2 You may ask, if the only interesting element inside of <auth-constraint> is <role-name>, why do we need the <auth-constraint> element This is to distinguish the role from the <user-data-constraint> element, which dictates which transport-level security is to be used to protect the resources in the collection More on <user-data-constraint> in the next section

K / K ' the ratio of the forward and reverse adsorption rate constants, is the conven, where K tional adsorption equilibrium constant The second equality in this equation is equivalent to Eq (14106), and indicates that the adsorption equilibrium constant is equal to Henry's constant divided by m, ie, K = klm Since the assumptions upon which it is based are fulfilled at low surface coverage, the Langmuir isotherm is always valid as 0 -+ 0 and as n -+ 0 Even though these assumptions become unrealistic at higher surface coverage, the Langmuir isotherm may provide an approximate overall fit to n vs P data; however, it does not lead to reasonable values form Substituting a = A / n in Eq (14103) gives:

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try { String query = new String ("UPDATE Customers " + "SET Discount = 25 " + "WHERE Discount IN (12,15)"); DataRequest = DatabasecreateStatement(); DataRequestexecuteUpdate (query); DataRequestclose(); }

The last aspect of Web application security is Data Security Generally, this aspect builds on top of authentication and authorization, but this need not necessarily be the case For example, any user may view the Web page for Sun s Mojarra on javanet at https://javaserverfacesdev javanet/, but in order to file issues in the issue tracker, or take any other actions, the user must have the appropriate authentication and authorization As with all aspects of containermanaged security, data security is configured using the webxml file Let s complete our example from the trainer by stating that all trainer pages be transmitted between server and client using data security

n = 0) to P = P and Il = Il yields:

<web-app> <!-- intervening elements omitted --> <security-constraint> <web-resource-collection> <web-resource-name>trainer modules</web-resource-name> <url-pattern>/trainer/*</url-pattern> </web-resource-collection>

The IS NULL test evaluates the value of a column designated in the test to determine whether the column is NULL that is, the column is empty of any value If so, the IS NULL test returns a true, and the UPDATE statement updates the column specified in the SET clause Listing 11-45 illustrates how to use the IS NULL test in the UPDATE statement In this example, the IS NULL test determines whether the LastName column is NULL If so, a zero is placed in the Discount column If not, the value of the Discount column remains unchanged

14:

This equation provides the only means for evaluation of spreading pressure The integration may be carried out numerically or graphically with experimental data, or the data may be fit to an equation for an isotherm For example, if the integrand n / P is given by Eq (14107), the Langmuir isotherm, then:

try { String query = new String ("UPDATE Customers " + "SET Discount = 0 " + "WHERE LastName IS NULL "); DataRequest = DatabasecreateStatement(); DataRequestexecuteUpdate (query); DataRequestclose(); }

<auth-constraint> <role-name>trainer</role-name> </auth-constraint> <user-data-constraint> <transport-guarantee>CONFIDENTIAL</transport-guarantee> </user-data-constraint> </security-constraint> <login-config> <auth-method>BASIC</auth-method> <realm-name>form</realm-name> </login-config> <!-- intervening elements omitted --> </web-app>

an equation valid for n -+ 0 No equation of state is known that leads to an adsorption isotherm which in general fits experimental data over the entire range of n from zero to full monolayer coverage Isotherms that find practical use are often 3-parameter empirical extensions of the Langmuir isotherm An example is the Toth equation:24

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