Abstract
Field implantable and laboratory sensors for the measurement of moisture in soil based on the increase of soil dielectric permittivity with volume fraction of water were developed. A typical sensor consists of a case containing a high-frequency (31-MHz) oscillator whose frequency determining resonance LC network is coupled to the built-in electrode via a capacitor T network. Increases in moisture cause a shift in the resonance frequency, which is detected by an external differential frequency counter or readout. The T network and electrode electronic switches reduce the undesirable influence of soil conductivity on the frequency shift. Although the sensor contains active elements, it acts as a passive transducer since power is supplied to the sensor from the readout unit through the two-conductor cable which transmits the RF.
| Original language | English |
|---|---|
| Pages (from-to) | 112-118 |
| Number of pages | 7 |
| Journal | IEEE Transactions on Geoscience Electronics |
| Volume | 16 |
| Issue number | 2 |
| DOIs | |
| State | Published - Apr 1978 |
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