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  28/07/2002
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Phase Transmission method (virrib sensor)
how they work, some literature on them, where to get them and how much they cost:
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  photographs

Click on an image to see the manufacturer's listing further down this page.
The Virrib

This sensor seems to have vanished off the market

If you have any info, please let me know. Bruce April 2000 error-file:TidyOut.log

  basic principles

The Virrib sensor, using an RF phase detection technique samples a 15-20 liter soil sample. The sensor itself has some limitations due to its size (mainly related to installation), but the accuracy and reliability are excellent. Gabel (MoisturePoint) John Johnston

DESCRIPTION OF THE SENSOR
(Taken from
VIRRIBŪ: A SOIL MOISTURE SENSOR AND ITS APPLICATION IN AGRICULTURE)

    VIRRIBŪ is based on the principle of propagation of electromagnetic waves through the medium. The sensor consists of two stainless-steel concentric circles, connected in the body of the sensor, where the electronics proper is located. The body of the sensor is mechanically fixed with the embedding material, which also prevents water from penetrating to the electronic part. The diameter of the outer ring is 280 mm; its measurement capacity is 15-20 liters of soil. The sensor uses DC current with a voltage of from 12 to 20 volts from an external source. The output data is measured by means of a current loop, the intensity of the output current being directly proportional to the measured volume of moisture. The individual sensor measures the humidity in a space exceeding by about 60 mm the outlines of its active elements. VIRRIBŪ can measure a layer of soil that is 120 mm thick when the sensor is placed in a horizontal position; a layer 300 mm thick can be measured when the sensor is in a vertical position. Of course, the sensor cannot measure the humidity conditions above and below this layer. However, by using two sensors located above each other, the technician can obtain information on moisture conditions to a greater depth in the root zone. In cases involving a crop with a shallow root system, the second sensor may be situated deeper in the soil to determine water soaking.
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  advantages

Please submit your suggestions...
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  disadvantages

Please submit your suggestions...
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  general

Please see the correspondance below...
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  manufacturers

  • VIRRIB and is produced by firma AMET in Czech Republic. You may contact Adcon or direct the manufacturer at amet@bva.czn.cz error-file:TidyOut.log
      literature

  • VIRRIBŪ: A SOIL MOISTURE SENSOR AND ITS APPLICATION IN AGRICULTURE. TomᚠLitschmann COMMUN. IN SOIL SCI. PLANT ANAL., 22(5&6), 409-418 (1991)
  • THE CALIBRATION OF VIRRIBŪ INSTRUMENTS by: director: Dipl.Ing. Vítėzslav Hybler Prof. Dipl. Ing. Alois Prax, CSc. Department of Soil Science and Microbiology, Faculty of Agronomy, Mendel University of Agriculture and Forestry Brno, Zemėdėlská 1, 613 00 Brno, Czech Republic error-file:TidyOut.log
      details

    Dec 1998 See the www.zf.mendelu.cz site for descriptions of the following:
    Their
    SOIL MOISTURE REGULATOR (the Virrib)
    In particular there is a lot of detail in the Operating manual for irrigation management VIRRIB soil moisture sensor including

    • Fundamental characteristics
    • Technical parameters
    • The readout unit
    • Using the sensors
    • Sensor installation and operational preparation
    • Using VIRRIBŪ sensors in irrigation control
    • The calibration of moisture sensors
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      other

    Please submit your suggestions...

     

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    Relevant Links

  • Campbell Scientific
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    supports Sowacs

    MEA logo Data Logging Application and Measurement Systems Engineers

    Aquaflex
    Soil Moisture Meter

    SMEC logo
    Delta-T logo
    error-file:TidyOut.log Remote data acquisition and control systems

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    ism logo ism120x25.gif PRISM - CMP by Irrigation Scheduling Methods, Inc.

    Paltin logo
    Research, Products, Consultancy on Real-Time Water Dynamics

    Eijkelkamp.com

    The Virrib sensor

    See the Environmental sensors webpage: http://www.envsens.com./virrib.html, but first read this explanation :

    Dear soil water content buffs:
    
            At the sowacs home page 
    under the category of "other" methods the phase transmission 
    approach (the virrib sensor) is discussed with a big question mark as to how
    it works. So, here is my best hypothesis: The phase shift of a sinusoidal
    wave having traveled a fixed distance, relative to the phase at the origin,
    depends on the length of travel, the frequency, and most importantly the
    velocity. Thus for fixed frequency and travel path, a measurement of this
    phase shift will give a measure of water content.
    
            This has been known for some time, but had not evolved into
    a practical instrument. We had attempted (with very little practical success)
    to measure this phase shift for antennae transmissions through
    undisturbed soil thereby measuring a large volume of soil. The problems
    we had were with unacceptibly low power throughput, spurious pathways
    of travel, and transmission line induced phase errors. The use of 
    waveguide type transmission with the phase measuring electronics
    mounted to the waveguide and the waveguide beginning and ending
    at the electronics block could presumably solve all of those problems.
    i.e. something that looks very much like the virrib sensor.
    
            This may be the idea with the virrib phase transmission method.
    If so, it seems to me like a particularly ingenious idea. When I was
    working with this type of phase transmission, I was calling it 
    "phase domain" and would defer from calling it frequency domain
    or time domain (for fear of starting another controvercy)  and it does not
    even fit with traditional definitions of reflectometry. We at the UW
    are particularly interested in testing out any type of new inexpensive sowac
    instruments and do appreciate peoples input and ingenuity.
    
    Thanks,
    g.s.
    
    
    	************************************************
    	*   Gordon Starr                                                  *
    	*   Dissertator                                                     *
    	*   University of Wisconsin, Madison             *
    	*   Soil Science Department - Soil Physics  * 
    	*   1525 Observatory Drive                               *
    	*   Madison, WI 53716                                       *
    	*   608-262-0415                                                *
    	*   gcstarr@facstaff.wisc.edu                           *
    	*                                                                             *
    	************************************************
    
    


    And in reply to this:
    We have tested FDR, TDR and PDR (phase domain reflectometry) and really
      beleive that the latter is the best.  However, Virrib's sensor is using a
      pulse instead of a single tone signal.  Therefore, they suffer from the
      same limitation than time-domain: the pulse gets distorted when transmitted
      reducing precision. Also, Virrib's sensor is limited to 3dS/m which is too
      low to be used in south-west usa.
    
      We are willing to pre-sell samples of our new sensor to scientists only in
      May, that is 2 months earlier than official release date.  If anyone
      interested, please send your inquiry via E-mail.
    
    Romain Gagnon, Eng
      President & CEO
      Smart Rain Corporation
      1505, Place de l'Hotel-de-ville, suite 102
      St-Bruno, Quebec
      Canada, J3V 5Y6
    
      tel:   (514)441-4289
      fax:   (514)441-2147
      cell:  (514)893-6506
      E-mail:RGagnon@SmartRain.com
      WEB:   http://www.SmartRain.com
    

    but,
     The advantage found for using the cable tester for estimating the impedance
      of wave guides buried in moist soil was and continues to be the fact that
       the dielectric constant of water is nearly independent of dissolved salts in
       the 1 to 3 GHz range. Using frequencies in the more convinient (sp?) MHz
      ranges will
       create some strange dependencies between soil type, salinity, texture, and
      ogranic matter. But so does oven drying.
    
      Perhaps the use of several discrete frequencies could be used and the
      overall pattern of responses could be used to estimate texture, BD, OM,
      water, and salinity?? At one time the UofNEbraska was doing work in this
      area but I have not heard from Dr.Skopp for sometime.
    
    

    and
    Nearly is the operative word here. In agricultural settings i suppose,
      salinities are kept pretty low by irrigation and subsequent flushing out
      of collected salts. however, our work in desert soils has found many locals
      where TDR was completely inoperable, (all signal lost to the conductive 
      soil), or even worse, where the conductivity was not so high as to completely
      attenuate the signal but caused a significant over estimation of water 
      contents. Electrical insulation of the rods of the tdr probe extends the
      operation range but requires an individual calibration for each soil, which
      makes the whole technique much less friendly, not even to mention that the
      salinity level could change at a given local and invalidate the calibration.
      I have observed the same problem with salinity with the FD tool sold by
      troxler, actually even worse. I believe that soil moisture and campbell 
      scientific both no offer insulated tdr probes for just this purpose. I am
      very interested in this smart sensor, smart probe (excuse me i cant remember 
      the name of the probe) which has been discussed so much, prehaps it is the
      silver bullet for conductive soils as reported? 
      Sam Hokett
      Desert Research Inst
    
    and
    In case recent SOWACS participants missed the following posts last year,
      here they are again.  
    
      This discussion led to the formation of HydroTek and development of the
      WAVE-1 sensor.  See WWW.HYDROTEK.COM for further information.
    
      >
      >Posted 03/12/96
      >
      >To: IRRIGATION-L@LISTSERV.GMD.DE (AND OTHERS)
      >From: ges@oneworld.owt.com (Marty Grogan)
      >Subject: Do-It-Yourself TDR, Really Cheap!
      >
      >Use a square pulse generator, a length of 300 ohm TV (flat
      >twin lead) antenna wire and an oscilloscope.  Connect the
      >oscillator to the TV wire, a length of which is buried in
      >the ground to be measured.  The longer the buried wire, the
      >more sensitive the measurement will be.  Measure the time
      >delay along the wire using the oscilloscope by comparing an
      >entering pulse with an exiting pulse.  Be sure to match the
      >impedance at both ends of the TV wire to 300 ohms.  The TV
      >wire will perform as a variable time delay line providing an
      >indication of the dielectric changes in the surrounding dirt
      >due to changes in moisture.  The measurement will represent
      >an average over the length of wire buried.  An interval
      >measuring counter can be used instead of the oscilloscope.
      >Experiment with the pulse repetition rate and pulse width
      >until you get the best results.  Calibrate this system as
      >you would any other.  Higher rates and shorter pulses will
      >probably work best.  Both ends of the TV wire must be
      >accessible, so the wire should be buried in a circular
      >pattern.
      >
      >Integrated circuits are available to construct this setup
      >for less than twenty dollars.  A simple voltmeter could be
      >used for the indicator.
      >
      >Posted:  3/16/96
      >
      >From: ges@oneworld.owt.com (Marty Grogan)
      >To: Multiple recipients of list 
      >  (and others)
      >Subject: Re:  Really Cheap TDR
      >X-Listprocessor-Version: 6.0c -- ListProcessor by Anastasios Kotsikonas
      >X-Comment:  Precision Agriculture Mailing list
      >
      >Because of the apparent interest in transmission line TDR, I will build
      some experimental devices.  If you are interested, send EMAIL describing any
      special geometry requirements (circumference, length), dynamic response
      needed, mechanical issues, soil depth, sensitivity (relative H2O by volume),
      quantity needed, sample 
      >spacing, number of samples, etc.
      >
      >I expect to provide 4-20 ma, line powered devices at about one-third the
      regular TDR probe cost.
      >
      >If production units result, the experimental units will be replaced with
      new units in return for information about successful use.  (Postable, of
      course.)
      >
      >I am also interested in any problems you may be having using available
      equipment to see if I might be able to address solutions with the
      experimental units.
      >
      >Experimental units will include complete drawings, electrical schematics
      and a liscense to make all of the units you want for your own use.
      >
      >Some price and delivery advantage will be available for quantity orders and
      prepayment.
    
      I have completed a short run of experimental devices which are being
      evaluated by several individuals.  Full scale production will begin very soon.
    
      Although the present single unit price is around US$300, volume production
      and purchasing can easily cut production costs and prices in half.
    
      Any opinions participants would care to offer concerning decision-price
      points are quite welcome.
    
      There have been many requests for a low-power, voltage output device.  This
      type of device has been designed and will soon become available at a
      slightly lower cost than the industrial device.
    
      Marty Grogan, BSAE, MSEE
      Owner, Grogan Engineering Services
      President, HydroTek, Inc.
      1328 Rathwood Ave.
      Richland, WA  99352
      (509)627-3083 (voice and FAX)
      ges@oneworld.owt.com
    
      Specializing in Systems Integration Services for Agriculture:  Automation,
      Telemetry, Programming, Maintenance, Remote Sensing and Project Delivery.
    
                   GES--The technology buckstopper.
    

    Finally!
    I think we have established that the CS615 is TRUE TDR, but not FULL BLOWN
      TDR.  Each technology has its limitations and--fortunately--overlaps others.
      With the application of Network Analyzers, the final chapter obviously has
      not been written on SoWaCS.  Just add money--a lot in the case of "FULL
      BLOWN TDR" (Tek 1502C) or Network Analyzers. And calibrate often.
    
      Thanks for everyone's contributions while I watched SoWaCS for Bruce
      Metelerkamp until Mark Summerton comes on board as of next week.  If you
      have had any problems, email me here at:  I will try
      to take care of them so they won't be a burden to Mark.
    
    
      Dave Barnett
      UMass CEE Dept