Parallel-plate impedance sensing of moisture content in single seeds and grain kernels

Author(s):  
S.O. Nelson ◽  
K.C. Lawrence ◽  
C.V.K. Kandala
1994 ◽  
Vol 37 (3) ◽  
pp. 887-891 ◽  
Author(s):  
S. O. Nelson ◽  
K. C. Lawrence

Author(s):  
Vanja Mandrić Radivojević ◽  
Slavko Rupčić ◽  
Mario Srnović ◽  
Goran Benšić

This article is a result of measuring the dielectric constant of a dielectric used in studying the influence of dielectrics on the antennae reflection coefficients. A paper having a density of 0.797 g/cm3, moisture content of 0% and temperature of 210C, is used as a dielectric. Although the literature provides a lot of data on the dielectric properties of wood and paper, without direct measurement of the dielectric constant it is impossible to know its amount for the dielectric used in the defined frequency range. Dielectric constant measurements are performed in the frequency range from 100 Hz to 100 kHz, while the frequency range of its impact on the aperture antenna reflection coefficients is up to 2 GHz. The frequency range from 100 KHz to 10 GHz is interpolated and fitted by using measurements and available literature data and by respecting physical influences and phenomena and functional changes of the dielectric constant of paper within the given range


Geophysics ◽  
1975 ◽  
Vol 40 (5) ◽  
pp. 865-885 ◽  
Author(s):  
John C. Cook

Laboratory measurements of RF complex permittivity have been made on a variety of “rocks” encountered in mining, tunneling, and engineering works. An RF impedance bridge and a parallel‐plate capacitance test cell were employed at frequencies of 1, 5, 25, and 100 Mhz. The results predict that low‐loss propagation will be possible in certain granites, limestones, coals, and dry concretes. Existing VHF mining radar equipment should be capable of exploring into such rocks to distances of up to hundreds of feet. Useful but shorter probing distances are predicted for other coals, gypsums, oil shales, dry sandstones, high‐grade tar sands, and schists. Radar probing distances of less than 10 ft are predicted for most shales, clays, and fine‐grained soils. Uncombined moisture content is evidently the, governing factor. Efforts were made throughout the experiments to preserve or simulate the original moisture content of the “rocks” in place.


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