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available in a wide variety of capacities, from 256 MB up to 2 GB, with varying timing ratings, such as Column Address Select/Strobe (CAS) latency timing, that factor into part costs. Memory timings determine how quickly memory cells may be loaded with fresh information, how quickly such information is refreshed and accessed, and how quickly the module can establish a ready state for the next operation. This impacts the rest of the input/output subsystem directly, much of which relies heavily on the current contents of main memory. Standard memory timings for DDR modules usually sit somewhere around 3-5-5-8, a modest collection of values. High-performance DDR modules boast latency ratings of 2-3-2-6, and the absolute best is 2-2-2-5. DDR2 sports higher timing values, but the operation of DDR2 is entirely different from DDR. At any rate, low latency ratings for DDR2 are around 3-2-2-8, plus or minus a few points. DDR2 memory is currently used exclusively in recent Pentium 4 models, and does not affect systems with AMD processors. While there s no rule that states low-latency parts will provide substantial performance gains, they are relevant for high-definition systems where high bandwidth, heavier encoding/decoding rates, and more data to handle puts more of a premium on system speeds. Your mileage will certainly vary.

Here are a few general tips: Make sure that you declare all your variables. Use Option Explicit at the top of your modules to force yourself to do this. If you reference an Excel object more than once, create an object variable for it. Use the With-End With construct whenever possible. If your macro writes information to a worksheet, turn off screen updating by using Application.ScreenUpdating = False. If your application enters data into cells that are referenced by one or more formulas, set the calculation mode to manual to avoid unnecessary calculations.

Inventory turnover ratios are discussed in some detail in the section on cash conservation and working capital management in 11. For our purpose, only the basic turnover ratio and the subsequent ratio to determine the number of days inventory is held will be discussed at this point. The inventory turnover ratio equation is Cost of sales for the period / Average inventory during the period Inventory turnover can be determined on a monthly, quarterly, semiannual, or yearly basis. We will assume the following information regarding inventory for the Month of March is as follows: Food inventory on March 1: $ 8,434 Food inventory on March 31: $ 6,870 Cost of sales for March: $55,700 Average inventory ($8,434 $6,870) / 2 $15,304 / 2 $7,652

6.7.2 Bulk organic contributions to particulate water content in the regime subsaturated with respect to water vapour

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Conversely, we can bound the number of sequences with complexity signi cantly lower than the entropy. From the AEP, we can divide the set of sequences into the typical set and the nontypical set. There are at

in a document. DIV is called a block-level element because you use it to affect a complete block of text. It can enclose headers, paragraphs, tables and other block-level elements, and any combination of these elements. Therefore you can, for example, use the DIV element to mark up both headers and paragraphs at the same time.

Essential Windows CE Application Programming by Robert Burdick Wiley Computer Publishing, John Wiley & Sons, Inc. ISBN: 0471327476 Pub Date: 03/01/99

of permeable rocks in the subsurface (see Section 15) and have touched upon the interplay between landforms and groundwater discharge features (see Section 331) At the scale of entire catchments, the details of the interaction between geological structure and landscape critically determine patterns of groundwater discharge via springs, wetlands, and stream beds As Higgins et al (1988) have noted: The landscape consists of a series of interconnected hillslopes The variability of hillslope length, steepness and shape are re ected in variable water-table con gurations, which in turn translate into other aspects of ground-water conditions Clearly the occurrence of different types of springs (Figure 51) depends upon the manner in which hillslopes intersect sedimentary contacts, intrusive contacts, faults, and other geological features.

Similarly, where low-permeability bedrock reaches the surface in the axis of a stream valley that is elsewhere occupied by more permeable unconsolidated sediments, and the groundwater present in the latter meets the bedrock high, it will be forced to ow upwards through the stream bed (eg Malcolm et al 2005) Rather more subtly, the aspect of a slope (ie the direction in which it faces) can considerably in uence its hydrogeological behavior: In the Northern Hemisphere, southern and southwestern slopes receive greater insolation than northern and northeastern slopes This leads to differences in soils, vegetation, and water retention and in ltration rates Such factors create feedback systems that affect the amount of water that enters the ground-water zone (Higgins et al 1988) We have already seen that the dissolution of minerals naturally present in rocks accounts for much of the dissolved solids content of groundwaters.