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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: | ||||
The Virrib sensorSee the Environmental sensors webpage: http://www.envsens.com./virrib.html, but first read this explanation :
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 Instand 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 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: |