By Judy Turner
A watercolor duvet e-book that offers entire slicing and piecing directions!
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2002;201:525–40. 34. Yang Tao, Xue Zichen, et al. Oxygen and hydrogen isotopic compositions of pore water from marine sediments in the northern South China Sea. Acta Geosci Sin. 2003;24(6):511–4. 35. Gerhard B, Martae, T. Gas hydrates in marine sediments. In: Schulz HD, Zabel M, editors. Marine geochemistry. Heidelberg: Springer; 2006. pp 481–512. 1 Acoustic Detecting Technique Acoustic techniques used in laboratories are now mainly classified into two categories: ultrasonic detection and the piezoceramic bender element and resonant column test technique.
Determining S-wave travel time during bender element testing is usually completed with direct determination and calculation analysis methods. The direct method is to get the determination directly according to characteristic points of the input waveform from the transmitting bender elements and the output waveform from the receiving bender elements. The calculation analysis method is to use dynamic finite element analysis, cross-correction analysis of input signals from transmitting bender elements and output signals from receiving bender elements, phase velocity analysis, phase sensitive detection, etc.
6 ms is identical to the S-wave frequency b a 2 Development of the Experiment Detection Technique 45 46 Y. Ye Fig. 34 Spectrum analysis of the S-wave band in water-saturated loose sediment Fig. 35 Comparison of S-wave velocities measured using the FFT-WT and direct methods accurately measure the water content of a sediment specimen, but the sediment must be sampled and destroyed before measurement, so this method is not able to test the water content of a hydrate in sediment specimen. The radiometric method can accurately measure water content in sediment in situ, but the specific specimen must be independently calibrated, and the test personnel must be protected from radioactivity.