Search result for:  id10=WA 0821 1305 0400 Harga Pengadaan XRF Analysis Bruker Nias Sumatera Utara [[Tiga Pillar]]

SeisImager can export processing or modeling results in several different formats. Two-dimensional sections can be exported to grid data which can be imported into Surfer and one-dimensional velocity profiles, traveltime curves, dispersion curves etc. can be exported as ASCII data, easily importable into Excel or other software.

Very often I am asked what the difference is between the Lite, Std and Pro versions of the 2D Refraction software licenses. SeisImager/2D Software Packages • Standard version: for use on seismograph with mouse or PC with mouse; allows up to 16K samples per trace, 128 traces per shot, 360 traces per interpretation, and 65 shots per interpretation.• Professional version: for use on seismograph with mouse or PC with mouse; allows virtually unlimited input up to 2M samples per trace, 48K traces per shot, 48K traces per interpretation, and 48K shots per interpretation.• Lite version: included with purchase of Geometrics Windows-based seismographs. For use on seismograph with mouse or PC with mouse; allows up to 16K samples per trace, 64 traces per shot, 51 traces per interpretation, and 12 shots per interpretation.• Demonstration version: for use on PC with mouse, may be launched 15 times; same allowances as Lite version; no printing capability.Note: The number of shots per spread and spreads per interpretation are dependent on the actual trace number used. The Standard and Professional versions are also available for rent. SeisImager Software Suite* Refraction & Surface Wave Data Analysis Software 40 hr - $200 75 hr - $300 250 hr- $500. See Rentals - Geometrics : Geometrics and email rentals@geometrics.com to set up an order.

If you are doing refraction and reflection then the trigger timing accuracy is important - especially when trying to get high resolution imaging. For MASW the trigger timing accuracy is less important because the frequencies of interest are lower and the Analysis method only relies on the phase differences of the signals between geophones and not the absolute time between shot event and the signal received on the geophone. If you are acquiring individual records for each hammer blow and then inputting them into Pickwin, then a hammer trigger is not required, you can use an auto trigger method for the Geode. If you are stacking the data in the Geode, then a hammer trigger will be required.

Here are a few additional details relating to the measurement of elevation: GNSS AccuracyAccuracy depends on multiple aspects of the GNSS system: among them are clock accuracy, atmospheric effects, and satellite geometry. Satellite geometry"Satellite geometry" refers to how the currently visible satellites are distributed in the sky - close to each other or scattered around. The best satellite geometry includes satellites that are near the axes on which you hope to locate your receiver; for example, to locate your receiver on the East/West axis, it's helpful to have good reception from satellites low in the sky in the East and in the West. If you also have satellites that are low in the sky near the South and North horizons, you will have good accuracy on the horizontal (latitude/longitude) plane. It's best to have satellites scattered around the sky, overhead as well as near the horizon all around. HDOPMagArrow records HDOP, a standard measure of satellite geometry's effect on horizontal (or latitude/longitude) accuracy. A smaller number (less than 1.0 is very good) indicates that the visible satellites are in good positions to contribute to accuracy. Vertical AccuracyThe reason that GNSS systems aren't as accurate on the vertical axis as on the horizontal axes is that no satellites are visible in a full half of that axis: the half that is below the horizon. Consequently, vertical accuracy is on average about half that of horizontal accuracy; calculated offset from true elevation is on average about twice that as on the horizontal axes. While on average HDOP can therefore be used to estimate VDOP (the similar measurement of the effect of satellite geometry on the vertical axis), that estimate is only a rule of thumb; it is possible to have an excellent HDOP, reflecting very good horizontal satellite geometry, while having poor vertical satellite geometry. In those cases, good HDOP does not indicate good VDOP. Keeping in mind that possibility, a combination of good HDOP and many satellites in view usually indicates good VDOP. Practical effects Some data processing techniques (upward continuation, for example) can include elevation as an input. Customers who are considering using GNSS elevation in those techniques should conduct a careful Analysis of their data and develop test routines to verify that all their data meet the requirements of the technique and its application to a particular survey. Some customers who require very accurate elevation data incorporate LIDAR data and drone elevation data into their analyses.

Magnetic surveying as a means of estimating depth to basement requires the collection of a data set that can be processed to yield the average radial power spectra as a function of survey position. The assumption here is that the basement rocks are much more magnetic that the overlying sediment and make a much greater contribution to the observed magnetic anomalies than do the sediments at the longer spatial wavelengths. This type of power spectral Analysis relies on accurate data that are extensive in two dimensions relative to both the depth of the basement and the aerial extent of structural high that you seek. If the data are not extensive, the spatial truncation of the data set will limit power spectra to short wave lengths and this is likely to bias the spectra power average yielding a poor estimate of depth to basement. If this discussion intrigues you, contact Magnetometer Sales for a more thorough discussion.