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The greater the electron electron repulsion, the larger the species becomes, and vice versa The ionization energy (IE) is the energy needed to completely remove an electron from an atom It may be expressed in terms of 1 atom or a mole of atoms Energy is required in this process in order to overcome the attraction of the nucleus for the electrons There are two factors affecting the magnitude of the ionization energy One is the size of the atom The closer the electrons are to the nucleus, the more energy is needed to overcome the effective nuclear charge Therefore, ionization energy tends to decrease from top to bottom within a group, since the valence electrons (the first ones to be lost) are farther away from the nucleus The other factor is the magnitude of the effective nuclear charge.

The greater the effective nuclear charge, the more energy is required to remove the electron Since the effective nuclear charge increases from left to right within a period, the ionization energies will also increase from left to right The increased effective nuclear charge results in the atom becoming slightly smaller, which also leads to a greater nuclear attraction for the electrons The ionization energy for the removal of a second electron is greater in all cases than the first, because the electron is being pulled away from a positively charged ion and the attraction is greater than from a neutral atom..

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In this section, we discuss how architectures that contain instantiated components can be configured. Architectures that contain other components are called structural architectures. These components are configured through component configuration statements. Let s first look at some very simple examples of component configurations, and then at some progressively more complex examples. The first example is a simple 2 to 4 decoder device. Figure 7-1 shows the symbol for the decoder, and Figure 7-2 shows the schematic. The components used in the design are defined using the VHDL description shown here:

There s one final change to be made. In 4, you created a displayAction() that would accept an item ID and retrieve the corresponding record from the database using a Doctrine query. However, that query did not take account of the item s current display status. Since there now exists a mechanism for administrators to adjust an item s visibility status, it s a good idea to update this displayAction() to also take this status into account and display only those items which are set as publicly visible. To do this, update the ItemController::displayAction, located at $APP_DIR/ application/modules/catalog/controllers/ItemController.php, such that it incorporates the visibility-adjusting condition in the Doctrine query:

URL url = null;

Analyzing the preceding PathPing report, the link between 172.16.87.218 (hop 1) and 192.168.52.1 (hop 2) has a 13 percent drop-packet rate. Dropped packets represent data that needs to be retransmitted, which adversely affects data throughput. All other links appear to be functioning normally with 0 percent packet-loss rates. Packet loss between the first and second hops could indicate heavy network traffic, congested routers, or slow links. For information about PathPing (as well as the related Ping and Trace Route tools), see Configuring TCP/IP on the companion CD and 24, Configuring IP Addressing and Name Resolution, in this book, and Windows XP Professional Help and Support Center. Also, see the TCP/IP Core Networking Guide of the Microsoft Windows 2000 Server Resource Kit.

| Name/* case and space normalized */

Geological time includes the history of the Earth from the first hints of its formation until today. It is measured mathematically, chemically, and through observation. Figure 5.1 shows a geological time clock with one second roughly equal to one million years. In 1785, Scottish scientist James Hutton, often called the father of modern geology, tried to figure out the Earth s age. He studied and tested local rock layers in an attempt to calculate time with respect to erosion, weathering, and sedimentation. Hutton knew that over a few years, only a light dusting of sediments are deposited in an undisturbed area. He figured out that sedimentary rock must have been compressed, tighter and tighter, from the weight of upper rock layers over many ages. He also thought that changes in a sedimentary rock layer, through uplifting and fracturing of weathering and erosion, could only have taken place over a very long period of time. Hutton was one of the first scientists to suggest that the Earth is extremely ancient compared to the few thousand years that earlier theories suggested. He thought the formation of different rock layers, the building of towering mountains, and the widening of the oceans must have taken place over millions of years. Hutton wrote the principle of uniformitarianism suggesting that changes in the Earth s surface happened slowly instead of all at once. His early work paved the way for other geologists to realize the Earth was not in its final form, but still changing. Gradual shifting and compression changes occurred across different continental land forms.

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