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Gem Swap 2. You'll Also Like 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:.
The sensor geometry with respect to the earth is shown in Figure 6. We note that the ppm unit defined by Eq.
GEM-2 can be configured to a vertical coplanar mode or horizontal dipole mode by simply turning it 90 degrees about the ski axis Figure 7.
The mutual coupling ratio for is given in equation 4 as: 4 where J1 is the first-order Bessel function. The integrals in Eqs. We notice from the above equations that conductivity and frequency appear as a single product.
For multifrequency data, therefore, Eqs. Figures 8 and 9 bleow illustrate the computed in-phase and quadrature responses over half-space for the GEM-2 horizontal and vertical coplanar coils.
We assume for this example the sensor height at 1 meter, typically waist level for a surveyor. In essence, the observed ppm value y-axis determines the conductivity-frequency product x-axis , which is then divided by the transmitter frequency to obtain the half-space conductivity.
Materials, including radioactive waste, were "systematically" buried in many parallel trenches. Magnetic anomalies are inherently dipolar in nature and, thus, a target is commonly located at the slope, rather than the peak, of an anomaly.
This problem of target location renders the magnetic anomaly hard to interpret, particularly for a target made of many individual items such as drums and cans buried in these trenches.
In contrast, it can be shown theoretically by forward modeling that a GEM-2 anomaly is almost monopolar centered directly above the target and, consequently, is easier to interpret than dipolar magnetic anomalies.
Figure 10g is from an old facility engineering drawing that supposedly shows the trench locations. We do not know whether this old drawing was intended to show the design plan before, or the "as-built" map after, the trench construction.A new generation jewel match 3 game now available on Google Store. More levels, more puzzles and move fun! All levels free try it now! This is the most puzzle. Kongregate free online game Gem Swap II - In this game there will be a number of gems arranged in a particular pattern. You need to swap. Finden Sie Top-Angebote für Bejeweled 2 PC-Spiel Puzzle Logik Gem Swap bei eBay. Kostenlose Lieferung für viele Artikel! Gem Valley - Match 3 Game: halsansmaland.se: Appstore for Android. Reviewed in the United Kingdom on 2 October Verified Purchase. Alright game. CLASSIC GEM-MATCHING Play the most popular puzzle game of the century with powerful new gems. You'll find cascades of fun as you test your.