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2. Ask each attendee to send the producer/moderator at least three ideas, using the chat feature. Give participants two minutes to respond. 3. Work with the producer/moderator to select what you feel are the 20 most valuable suggestions. 4. Conduct a poll to allow the group to select its favorite three suggestions. Hide the results until the end of the poll. 5. Display the results of the poll. Thank attendees for their help. Indicate that you will be sharing these suggestions with management. Nice Idea Use a burning match simulation to illustrate how much time attendees have left to respond to the poll. You can nd such a simulation at http://www.swishzone.com/index.php area=resources&tab=movies &do=page&action=detailed&link id=497. Approximate Time 15 to 20 minutes.

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requirements and a common destination, and potentially can be used for header compression within the network. The advantage of using MPLS may derive more from lower infrastructure costs and improved QoS characteristics than from bandwidth efficiency. Table 5-3 depicts some of the issues and potential solutions that affect the transport side of a VoMPLS solution. Hopefully, VoMPLS will build on the experience of VoIP in terms of issues such as echo, prioritization/queue management, and so on. The following lists some typical service-related capabilities that are required beyond transport, just to come out with a voice service that is on the par with existing services. As indicated elsewhere, a VoP needs compelling new services to promote its deployment:

Certain RF dynamics such as split cells (a cell split into two or.

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2. Natural and industrial emission inventories contain (A) geographical data (B) the time period when emissions were generated (C) types of activities causing emissions (D) the chemical and physical identity of pollutants (E) All the above 3. Greenhouse gases include all the following, except (A) (B) (C) (D) (E) water vapor nitrous oxide carbon dioxide methane butyric acid

through temperature effects occurred over geologic time (millennia) and shortening the time to laboratory time and increasing the temperature to above and beyond the cracking temperature (at which the chemistry changes) does not offer conclusive proof of high temperatures (Speight, 2007a) Nevertheless, at some point during or after the maturation process, the gas and crude oil migrate from the source rock either upward or sideways or in both directions (subject to the structure of the accompanying and overlying geological formations) Eventually, the gas and crude oil became trapped in reservoirs that may be many miles from the source rock It is rare that the source rock and the reservoir were one and the same Thus, a natural gas field may have a series of layers of crude oil/gas and gas reservoirs in the subsurface.

Since you ve seen my curriculum vitae, you know that I have been an educator for over 17 years. Since we ve met several times, you know that I still retain the drive, energy, and commitment it takes to excite students in a subject they find dull, at best irrelevant, at worst. Since we ve discussed my fortune in receiving the State of Connecticut s Outstanding Educator Award for the past three years, you know that my abilities are well recognized, for which I am grateful. So, if there is any uncertainty at all, please be assured beyond a shadow of a doubt that I am extremely eager to bring my talents and experience to bear on behalf of the students, families, faculty, and administration of my new home in South Helena. Thank you once again, Maurice, for your time and candor. Most sincerely,

In some instances, the natural gas and crude oil parted company leading to the occurrence of reservoirs containing only gas (nonassociated gas) Reservoirs generally comprise a geologic formation that is made up of layers of porous, sedimentary rock, such as sandstone, in which the gas can collect However, for retention of the gas each trap must have an impermeable base rock and an impermeable cap rock to prevent further movement of the gas Such formations, known as reservoirs or traps (ie, naturally occurring storage areas) vary in size and can retain varying amounts of gas There are a number of different types of these formations, but the most common is, characteristically, a folded rock formation such as an anticline as occurs in many petroleum reservoirs (Fig 21), that traps and holds natural gas.

On the other hand, a reservoir may be formed by a geologic fault that occurs when the normal sedimentary layers sort of split vertically, so that impermeable rock shifts down to trap natural gas in the more permeable limestone or sandstone layers Essentially, the geologic formation which layers impermeable rock over more porous, oil and gas rich sediment has the potential to form a reservoir..

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