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in Figure 1-9, C1 being a non-polarized type, and C2 a polarized type Although there are always exceptions to the rules, generally the disk-style capacitors are non-polarized, and the larger canstyle electrolytic types are polarized An obvious indicator of a polarized capacitor is the negative markings on the can, which can be clearly seen in the larger capacitor shown at the top of Figure 1-8 Another thing that capacitors have in common with batteries is that polarity is very important when inserting polarized capacitors into a circuit If you install an electrolytic capacitor in reverse and attempt to charge it, the part will most likely heat up and release the oil contained inside the case causing a circuit malfunction or dead short In the past, electrolytic capacitors did not have a pressure release system, and would explode like firecrackers when overcharged or installed in reverse, leaving behind a huge mess of oily paper and a smell that was tough to forget On many capacitors, especially the larger can style, the voltage rating and capacitance value is simply stamped on the case A capacitor is rated in voltage and in farads, which defines the capacitance of a dielectric for which a potential difference of one volt results in a static charge of one coulomb This may not make a lot of sense until you start messing around with electronics, but you will soon understand that typically, the larger the capacitor, the larger the farad rating will be, thus the more energy it can store Since a farad is quite a large value, most capacitors are rated in microfarads ( F), such as the typical value of 4700 F for a large electrolytic filter capacitor, and 01 F for a small ceramic disk capacitor Picofarads (pF) are also used to indicate very small values such as those found in many ceramic capacitors or adjustable capacitors used in radiofrequency.

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give or take about a day; the other occurs on September 22, give or take about a day At the equinoxes, the Sun is exactly at the celestial equator; it rises exactly in the east and sets exactly in the west, assuming that the observer is not at either of the geographic poles The names vernal and autumnal, as used in the northern hemisphere, are not really correct in the southern hemisphere because the seasons are reversed compared with those in the north Thus it is best to speak of the March equinox and the September equinox The crude celestial maps of Fig 3-2 show the situation at either equinox That is, the date is on or around March 21 or September 22 You can deduce this because the Sun rises exactly in the east and sets exactly in the west, so it must be at the celestial equator At the latitude of Sydney, the Sun is 35 degrees away from the zenith (55 degrees above the northern horizon) at high noon on either of these days The south celestial pole, which unfortunately has no well-defined sentinel star, as is the case for the northern hemisphere, is 35 degrees above the southern horizon all the time The heavens seem to rotate clockwise around the south celestial pole In the drawing at A, imagine yourself lying flat on your back, with your head fac-

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Use C# or Visual Basic .NET source code below for PDF conversion . renderer.RenderPageRangeToMultipageTIFFFile (0, renderer.GetPageCount()-1, TIFFCompression.LZW, "multipage. tiff " ); // Open the first output file in default image viewer.
Use C# or Visual Basic .NET source code below for PDF conversion . renderer.RenderPageRangeToMultipageTIFFFile (0, renderer.GetPageCount()-1, TIFFCompression.LZW, "multipage. tiff " ); // Open the first output file in default image viewer.

North Figure 3-2 Az/el sky maps for midafternoon at 35 degrees south latitude on or around the March

Here, we are requesting the Sales by Territory report located in the AWReporter folder. As we mentioned in section 10.2.1, you can also optionally pass other arguments to control the report processing (see table 10.2). One of the most common uses of the URL arguments is to pass parameter values when requesting parameterized reports. Passing report parameters To request a report that takes parameters, you append them to the URL string in the form of query parameters. For example, the URL string to request the Sales by Territory Interactive report for the year 2004 and Northwest is:

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ing north and your feet facing south In the drawing at B, imagine yourself rotated 180 degrees, that is, with your head facing south and your feet facing north Either orientation is valid astronomically, and you will find star maps that use either scheme Every day the Sun moves slightly toward the east with respect to the background of stars At the March equinox, the Sun is at the celestial equator and is located in a certain position with respect to the stars This represents the reference point for right ascension (RA) and declination (dec) As time passes, the Sun rises about 4 minutes later each day relative to the background of stars The sidereal (star-based) day is about 23 hours and 56 minutes long; the synodic (sun-based) day is precisely 24 hours long In the southern hemisphere, the Sun s motion relative to the stars is from left to right In the drawings of Fig 3-2, the Sun is at dec = 0 degrees Suppose that these drawings represent the situation at the March equinox This point among the stars is the zero point for right ascension (RA = 0 h) As autumn passes and the Sun follows a lower and lower course across the sky, the declination and right ascension both increase for a while Remember that right ascension is measured in hours, not in degrees There are 24 hours of h right ascension in a circle, so 1 hour (written 1 h or 1 ) of RA is equal to 15 degrees

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