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The client, not completely clear about the expert s recommendation, might want to further probe the expert to consider other possibilities For example: Why not blue chip stocks Why not bonds Why not real estate The consideration of alternative recommendations arises quite naturally in a number of expert client interactions Second, rule traces are often dif cult for users to process and understand Because a rule trace is based on a display of the rules, which are reproduced directly from the knowledge base, the quality of the explanation is based on how clearly the rules are expressed Variable names that appear in the rules should be meaningful, and the logic of the rules clear, otherwise the rule trace will be dif cult to understand To improve its clarity, rules produced directly from computer code may be replaced with easy-to-understand English, also known as pseudocode.

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However, even when converted to understandable English, rules sometimes contain too much detail, which a user is simply not interested in seeing Portions of a knowledge base typically contain rules that appear only because they are intended to be implemented as an algorithm on a computer These rules are likely to be confusing to a user who does not need to understand every implementation detail A rule trace might be pitched at a higher level by rewriting the rules, or it might be cleaned up so that confusing details are left out (The disadvantage, of course, of rewriting rules in this way is that this task needs to be maintained and updated whenever there is a change in the knowledge base, whereas computer-generated rule traces require no such maintenance because they are entirely automated) Many, if not most, current.

public void gameOver( TicTacToeModel model ){ totals = null; indices = null;

ably from the present concepts of convection and ocean oor creation, Holmes laid the foundation from which modern ideas developed Between the World Wars two schools of thought developed the drifters and the nondrifters, the latter far outnumbering the former Each ridiculed the other s ideas The nondrifters emphasized the lack of a plausible mechanism, as we have already noted, both convection and Earth expansion being considered unlikely The nondrifters had dif culty in explaining the present separation of faunal provinces, for example, which could be much more readily explained if the continents were formerly together, and their attempts to explain these apparent faunal links or migrations also came in for some ridicule They had to invoke various improbable means such as island stepping-stones, isthmian links, or rafting It is interesting to note that at this time many southern hemisphere geologists, such as du Toit, Lester King, and SW.

A security policy on a database is any combination of these policies contained in an RSqlSecurityPolicy object. To create a security policy, follow these steps: 1. 2. 3. 4. 5. Declare an RSqlSecurityPolicy object. Call its Create() API. Call its SetDbPolicy() API to add the appropriate policies to that object. Use the object in an RSqlDatabase::Create() call to create a database with those policies. Call its Close() API to release its resources. The Create() API is declared as follows:

Carey, were advocates of drift, perhaps because the geologic record from the southern continents and India favors their assembly into a single supercontinent (Gondwana) prior to 200 Ma ago Very little was written about continental drift between the initial criticisms of Wegener s book and about 1960 In the 1950s, employing methodology suggested by PMS Blackett, the paleomagnetic method was developed (Section 36), and SK Runcorn and his co-workers demonstrated that relative movements had occurred between North America and Europe The work was extended by KM Creer into South America and by E Irving into Australia Paleomagnetic results became more widely accepted when the technique of magnetic cleaning was developed in which primary magnetization could be isolated.

Coupled with dating by faunal or newly developed radiometric methods, the paleomagnetic data for Mesozoic to Recent times showed that there had been signi cant differences, beyond the scope of error, in the motions between various continents An important consideration in the development of ideas relating to continental drift was that prior to World War II geologists had, necessarily, only studied the land areas Their ndings had revealed that the continental crust preserves a whole spectrum of Earth history, ranging back to nearly 4000 Ma before the present, and probably to within a few hundred million years of the age of the Earth and the solar system itself Their studies also revealed the importance of vertical movements of the continental crust in that the record was one of repeated uplift and erosion, subsidence, and.

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