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group in AutoCAD is a named set of objects. A circle with a line through it, for instance, could become a group. Groups save time by allowing you to select several objects with just one pick. This speeds up editing operations such as moving, scaling, and erasing these objects.

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You can also specify a smart host on the Delivery tab of the Properties Sheet for an SMTP virtual server (see 23 for information on Exchange virtual servers). However, whatever setting you specify on the General tab of the SMTP connector overrides the setting for the SMTP virtual server configured as the local bridgehead server. Select the smart host option and type the IP address of Box16 in square brackets, for example, [172.16.11.16]. Then switch to the Address Space tab to specify the connector s scope and address spaces (Figure 22.7). The scope of an SMTP connector specifies what role the connector performs in routing messages. There are two possible settings:

The choice of a proper value for ). is highly problenl-specific anclis often detern.rined For a singlesolutionof a setof equations is oftenunnecessary. empirically. it However, if the system under study is to be solved repeatedly, the efficiency introdr-rced a wise by choiceof ), can be extremelyimportant.Good examples the very largesystems linear are of in algebraicequations that can occur when solvillg partialdifferentialequations a variety of engineering and scientificproblemcontexts.

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1. Let l represent the original length and w, the original width. The original area is A lw. The new length is l 4 and the new width is w 2. The new area is then l 4 w 2 . But the new area is 72 square inches smaller than the original area, so l 4 w 2 A 72 lw 72. So far, we have l 4 w 2 lw 72. The original width is three-fourths its length, so w 3 l. We will 4 3l now replace w with 3 l . 4 4 3l 3l l 4 2 l 72 4 4 ! 3l 2 3l 3l 2 3l 2 2l 4 72 on each side cancels 8 4 4 4 4 2l 3l 8 72 5l 8 72 8 8 5l 80 80 l 5 l 16 The original length was 16 inches and the original width was 3 3 4 l 4 16 12 inches.

Venus lander would have to endure pressure like a submarine, be able to fly like an airplane, take off like a rocket, and all the while endure temperatures that rise higher than the hottest day in the Caloris Basin of Mercury. On the windows you see what looks like rain. But this is no ordinary rain; it is sulfuric acid virga, liquid that precipitates from the noxious clouds and evaporates long before it can reach the ground. Highlands loom. That s the continent called Aphrodite, says the first officer. Of course, it is not a continent in the same sense as those on our home planet because there is no ocean on Venus. We just call it a continent because it is one of two large regions of high land. The other is near the pole and is known as Ishtar. Suddenly you see a bright orange glow and then what looks like a dull flash coming from a ragged, mountainous area. As you can see, that is an active volcano. We are lucky to be here while it s putting on a show. The volcanoes on Venus are something like those on the Big Island of Hawaii, with one important difference. As far as we know, the crust of Venus does not move over the volcanic hot spots the way the crust of Earth does, or if there is movement, it is much slower. The chain of the Hawaiian Islands was formed as Earth s crust moved over a hot spot welling up from Earth s mantle (Fig. 5-7A). On Venus, however, a single hot spot gets a chance to produce a volcano for a longer time (Fig. 5-7B).

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