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FOULING, SCALING, AND CORROSION Fouling reduces water flow and heat transfer It can be caused by the collection of loose debris over pumpsuction screens in sumps, growth of algae in sunlit areas, and slime in shade or dark sections of water systems Material can clog pipes or other parts of a system after it has broken loose and been carried into the system by the water stream Scaling also reduces water flow and heat transfer The depositing of dissolved minerals on equipment surfaces causes scaling This is particularly so in hot areas, where heat transfer is most important Corrosion is caused by impurities in the water In addition to reducing water flow and heat transfer it also damages equipment Eventually, corrosion will reduce operational efficiency It may lead to expensive repairs or even equipment replacement Impurities have at least five confirmed sources One is the earth s atmosphere Water falling through the air, whether it be natural precipitation or water showering through a cooling tower, picks up dust as well as oxygen and carbon dioxide Similarly, synthetic atmospheric gases and dust affect the purity of water Heavily industrialized areas are susceptible to such impurities being introduced into their water systems Decaying plant life is a source of water impurity Decaying plants produce carbon dioxide Other products of vegetable decay cause bad odor and taste The byproducts of plant decay provide a nutrient for slime growth These three sources of impurities contaminate water with material that makes it possible for it to pick up more impurities from a fourth source, minerals Minerals found in the soil beneath the earth s surface are probably the major source of impurities in water Many minerals are present in subsurface soil They are more soluble in the presence of the impurities from the first three sources, mentioned above Industrial and municipal wastes are a fifth major source of water impurities Municipal waste affects bacterial count Therefore, it is of interest to health officials but is not of primary concern from a scale or corrosion standpoint Industrial waste, however, can add greatly to the corrosive nature of water It can indirectly cause a higher than normal mineral content The correction or generation of finely divided material that has the appearance of mud or silt causes fouling This sludge is normally composed of dirt and trash from the air Silt is introduced with makeup water Leaves and dust are blown in by wind and washed from the air by rain This debris settles in sumps or other parts of cooling systems Plant growth also causes fouling Bacteria or algae in water will result in the formation of large masses of algae and slime These may clog system water pipes and filters Paper, bottles, and other trash also cause fouling.

The result, shown in Figure 3-25, displays both curves on the same plot You can use the same options that we described earlier, such as choosing the color or line style of each curve if it s necessary

Place preloaded hosts at the bottom of the file because they are read and loaded only when the TCP/IP service is initialized They shouldn t ever be loaded again, so they can be loaded last Another extension tag can be used to associate a given name/address with a domain For example, to log server1 as part of the mcslpcom domain:

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There are three ways to prevent scaling The first is to eliminate or reduce hardness minerals from the feed water Control of factors that cause hardness salts to become less soluble is important Hardness minerals are defined as water-soluble compounds of calcium and magnesium Most calcium and magnesium compounds are much less soluble than are corresponding sodium compounds By replacing the calcium and magnesium portion of these minerals with sodium, solubility of the sulfates and carbonates is improved to such a degree that scaling no longer is a problem This is the function of a water softener The second method of preventing scale is by controlling water conditions that affect the solubility of scaleforming minerals The five factors that affect the rate of scale formation are: Temperature TDS (total dissolved solids) Hardness Alkalinity pH

If you ve taken calculus then no doubt you re familiar with polar and logarithmic plots Back in my day we had to generate these manually wouldn t it be nice to have a computer program do that for you or at least check your answers Thankfully MATLAB comes to the rescue Let s start by looking at polar plots, which plot the radius r as a function of polar angle q For our first example let s generate a spiral The so-called spiral of Archimedes is defined by the simple relationship: r = aq where a is some constant Let s generate a polar plot of this function for the case where a = 2 and 0 q 2p The first statement we ll use defines the constant:

The Lmhosts file is still an effective way of distributing NetBIOS lookup information, especially for static addresses like your primary servers If you use NetBIOS heavily, we recommend you supply a copy of the Lmhosts file to your clients to act as a final backup in case either the WINS servers or the broadcast service fail to operate The easiest way to do this and keep it manageable is to use the #INCLUDE directive in the local Lmhosts file to refer to an Lmhosts on a UNC share For example, you could distribute the following file,

>> a = 2;

.

The registration and resolution of WINS information within a NetBIOS environment depends on the node type of the machine you are using There are four different node types, and these use four corresponding modes to resolve the information These node types and the resolving mechanisms they use are summarized in Table 32

Well that was simple enough Now let s define the function r(q) This is done in two steps, first we have to treat q the same way we would the independent variable x in our previous plots, so we define the label name, the range over which it is valid, and the increment we want to use Next we define r:

B-node (broadcast node) P-node (peer node)

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