Gem 2 Game

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Gem 2 Game

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Oops, something went wrong. Try again! The idea of using multiple frequencies stems from the skin-depth effect, which is inversely proportional to frequency: a low-frequency signal travels far through a conductive earth and, thus, "sees" deep structures, while a high-frequency signal can travel only a short distance and thus, "sees" only shallow structures.

Therefore, scanning through a frequency window is related to depth sounding. Figure 2 shows a nomogram from which one may determine the skin depth for a given frequency Won, Using the main software called WinGEM2 in a Windows environment, a PC connected to the GEM-2 can upload the operating parameters to the GEM-2, then download the data after the survey.

Depth sounding by changing the transmitter frequency is called "frequency sounding," which measures the target response at many frequencies in order to image the subsurface structure.

Because the method involves a fixed transmitter-receiver geometry, the sensor can be built into a single piece of hardware, such as GEM-2; as a result, it produces extremely precise, sensitive, and thermally stable measurements.

In contrast, depth sounding by changing the separation between the transmitter and receiver is called "geometrical sounding," which usually requires multiple operators tending separate coils connected by wires and measuring consoles.

Maintaining a precise coil separation is difficult and, therefore, some measurements e. For shallow surveys, the frequency sounding method offers high spatial resolution, survey speed, light logistics, and data precision.

Figure 3 shows the electronic block diagram of the GEM The sensor contains a transmitter coil and a receiver coil separated by about 1.

Such geometry is called "bistatic" configuration. It also contains a third "bucking coil" that removes or bucks the primary field from the receiver coil.

All coils are molded into a single board dubbed "ski" in a fixed geometry, rendering a light and portable package. Attached to the ski is a removable signal-processing console.

For frequency-domain operation, the program prompts for a set of desired transmitter frequencies. Built-in software converts these frequencies into a digital bit-stream which is used to construct the desired transmitter waveform for a particular survey.

This bit-stream controls the H-bridge transmitter driving the transmitter coil to generate a complex waveform that contains all frequencies specified by the operator.

Any integral number of the base period may be used for a consecutive transmission in order to enhance the signal-to-noise ratio.

In Figure 4a, we show an example transmitter current waveform, generated by a bit-stream designed to transmit three frequencies, 90Hz, 4,Hz, and 23,Hz.

Figure 4b depicts the waveform details for the first 33 bits, showing the current flow in the transmitter coil. Figure 4c shows the amplitude spectrum of the transmitter current waveform of Figure 4a.

The maximum current peak to peak for the present transmitter is close to 10 amperes, corresponding to a dipole moment of about 3 A-m2.

Note that the transmitter current decreases logarithmically with frequency. The GEM-2 has two recording channels: one from the bucking coil called the reference channel and the other from the bucked receiver coil called the signal channel.

Both channels are digitized at a rate of , Hz and bit resolution. This produces a 6,long time-series per channel during a base period. In order to extract the inphase and quadrature components, we then convolve i.

This convolution renders an extremely narrow-band, match-filter-type, signal detection technique. A single computer in a DSP chip coordinates all controls and computations for both transmitter and receiver circuits.

GEM-2 may also be used to measure the background environmental noise spectrum. This is obtained from the signal-channel time-series at a typical location within a specified survey area, then computing its entire Fourier spectrum at an interval of the base frequency 30 Hz.

Using the environmental noise spectrum, the operator can safely avoid locally-noisy frequency bands. The in-phase and quadrature data derived thrpugh the convolution are converted into parts-per-million, or ppm, units defined in equation 1 as:.

These ppm values are the raw data logged by the GEM It is obvious that the ppm unit defined above is sensor-specific and has little physical meaning.

All parameters required for the ppm computation, such as the sensor output in free-space simulated by hanging GEM-2 from the top of a tall tree , amplifier characteristics of the two receiving channels, and the coil geometry, are stored in GEM-2 for real-time use.

In most shallow geophysical surveys, the ppm data generated by GEM-2, often plotted on a contour map for each frequency, are sufficient to locate buried objects without going through elaborate processing or interpretation.

One can also estimate the target depth from the data obtained at multiple frequencies. This mode of operation, called a "bump finder" survey, is appropriate and productive where there are numerous shallow, small, nondescript targets and the survey objective is to find as many targets as possible.

The goal is not to determine a detailed geometry for each object, given typical time constraints and the large quantities of objects to be detected.

In such a survey, the in-phase and quadrature ppm data are sufficient to indicate the location, size, and depth of a "bump" without converting the data into any other more physically meaningful quantities.

Figure 5 is shown as an example; we look for a buried pipe and our main interest in this case is its location.

This figure shows the GEM-2 in-phase response at 7, Hz over a known stainless-steel pipe of inch diameter, buried at a depth of approximately 30 feet.

A magnetic survey failed to detect the pipe, presumably because it is made of stainless steel, a non-ferrous metal.

In this example, the plot showing the ppm response is sufficient to locate the pipe. The survey over this pipe included seven frequencies, and the response was highly dependent on frequency.

For example, the pipe was not recognizable at around 2 kHz or 12 kHz. Since the in-phase and quadrature ppm data contain all information on the measurement geometry, they can be the raw input for any inversion software.

Traditionally, however, EM data are displayed in "apparent conductivity" by imagining that the earth below the sensor is represented by a homogeneous and isotropic half-space.

While the earth is heterogeneous with regard to geologic variations, it can be represented by an equivalent homogeneous half-space that would result in the same observed data.

GEM-2 measures the secondary field from the earth and buried objects therein at frequencies specified by the operator.

When the field is normalized against the primary field at the receiver coil, it is called the mutual coupling ratio Q , which, for horizontal coplanar mode or vertical dipole mode , can be written in equation 2 as:.

Next in GEM-2 is only the beginning of a new generation of many broadband EM Emser Depesche Vergleich. Its built-in operating software allows a surveyor to cover about one acre Swiss Limousine hour at line spacing of five feet. When all pieces in the block are destroyed, you can proceed Xl Spiele the next level. Exit Full Screen. When the field is normalized against the primary field at the receiver coil, Book Of Ra 2 Deluxe Download Free is called the mutual coupling ratio Qwhich, for horizontal coplanar mode or vertical dipole modecan be written in equation 2 as:.

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