GPR reflection and dispersion analysis methods for water content: Multi-year study of GPR estimates and soil core measurements of water content

Author(s):  
Robert W Jacob ◽  
John F Hermance ◽  
Jan van der Kruk
Geophysics ◽  
2018 ◽  
Vol 83 (4) ◽  
pp. D127-D150 ◽  
Author(s):  
Fuqiang Zeng ◽  
Wenzheng Yue ◽  
Chao Li

Dispersion analysis of waves can reveal important mechanical properties of the formation around the borehole. The traditional dispersion analysis methods are affected by wave modes and aliasing. A new method is developed to perform dispersion analysis of borehole array acoustic logging, which combines the semblance of time-slowness coherence based on differential phase (STC-DP) processing and band-pass filters. Unlike the classic STC method, STC-DP is not sensitive to the window length. Two kinds of band-pass filters, the multiple filter technique and the finite-impulse response filter, are used. The band-pass filters can decompose the waveform signal into a series of waveforms in the frequency-time domain. In contrast to traditional dispersion analysis methods, there is no knowledge of wave modes. The new method can extract multimode dispersion curves, especially for the weak wave mode. For most dispersion analysis methods, the aliasing will appear in the high-frequency band when the scanning range of slowness is large enough. The aliased modes might interfere with other true modes, but the aliased modes are quite different from other true modes in the time-slowness grid. Therefore, aliased modes can be removed in the time-slowness grid based on the modal dispersion curves. Synthetic and field examples are used to verify the advantages of the proposed method over traditional dispersion analysis methods.


1990 ◽  
Vol 70 (2) ◽  
pp. 255-258 ◽  
Author(s):  
J. A. STONE ◽  
K. C. WIRES

Soil core volumes, from a long-term fertility experiment on Brookston clay loam, were adjusted for soil water content at sampling to explain large year-to-year fluctuations in bulk density and porosity. Adjusting the long-term soil core data decreased values of bulk density, total porosity, and air-filled porosity and reduced the variation between years. However, the year-to-year variation remained highly significant. Year-to-year fluctuations in bulk density and porosity on Brookston clay loam soil do not appear to be solely the result of changes in soil volume due to differences in soil water content at the time of sampling. Key words: Shrinkage, bulk density, porosity


2021 ◽  
Vol 329 ◽  
pp. 01028
Author(s):  
Ziwei Li

In this paper, based on the application of water-flooded layer interpretation plate, multi-well comparison, and the combination of dynamic and static analysis methods to optimize the well selection of fill hole wells, and through the analysis of the production of fill hole wells in **block in recent years, we summarize the relationship between fill hole effect and fill hole well injection and extraction well spacing, connection relationship, water content before the measure, and the relationship between fill opening thickness of the patch opening, so as to provide reference for the next step to continue to carry out fill hole work and find fill hole potential.


2016 ◽  
Vol 13 (2) ◽  
pp. 1468-1474 ◽  
Author(s):  
Bo Wang ◽  
Shengdong Liu ◽  
Fubao Zhou ◽  
Zean Hu ◽  
Lanying Huang ◽  
...  

Author(s):  
Songquan Sun ◽  
Richard D. Leapman

Analyses of ultrathin cryosections are generally performed after freeze-drying because the presence of water renders the specimens highly susceptible to radiation damage. The water content of a subcellular compartment is an important quantity that must be known, for example, to convert the dry weight concentrations of ions to the physiologically more relevant molar concentrations. Water content can be determined indirectly from dark-field mass measurements provided that there is no differential shrinkage between compartments and that there exists a suitable internal standard. The potential advantage of a more direct method for measuring water has led us to explore the use of electron energy loss spectroscopy (EELS) for characterizing biological specimens in their frozen hydrated state.We have obtained preliminary EELS measurements from pure amorphous ice and from cryosectioned frozen protein solutions. The specimens were cryotransfered into a VG-HB501 field-emission STEM equipped with a 666 Gatan parallel-detection spectrometer and analyzed at approximately −160 C.


Author(s):  
R.D. Leapman ◽  
S.Q. Sun ◽  
S-L. Shi ◽  
R.A. Buchanan ◽  
S.B. Andrews

Recent advances in rapid-freezing and cryosectioning techniques coupled with use of the quantitative signals available in the scanning transmission electron microscope (STEM) can provide us with new methods for determining the water distributions of subcellular compartments. The water content is an important physiological quantity that reflects how fluid and electrolytes are regulated in the cell; it is also required to convert dry weight concentrations of ions obtained from x-ray microanalysis into the more relevant molar ionic concentrations. Here we compare the information about water concentrations from both elastic (annular dark-field) and inelastic (electron energy loss) scattering measurements.In order to utilize the elastic signal it is first necessary to increase contrast by removing the water from the cryosection. After dehydration the tissue can be digitally imaged under low-dose conditions, in the same way that STEM mass mapping of macromolecules is performed. The resulting pixel intensities are then converted into dry mass fractions by using an internal standard, e.g., the mean intensity of the whole image may be taken as representative of the bulk water content of the tissue.


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