I wonder if you've asked yourself the most basic questions
Well to be fair whitehare already provided the critical info: he wants to bury 30 of these with no intention of ever digging them up again. Sounds sensible to me. And it seems neither gypsum nor resistive techniques are applicable in that case.
I'd be curious to know which approach Tom has taken with his moisture sensors.
I currently use Watermark sensors which, as far as I've seen, haven't been discussed in this thread. These are not gypsum blocks, at least not entirely. According to the mfr, "The sensor consists of a pair of highly corrosion resistant electrodes that are imbedded within a granular matrix. A current is applied to the WATERMARK to obtain a resistance value. The WATERMARK Meter or Monitor correlates the resistance to centibars (cb) or kilopascals (kPa) of soil water tension.
The WATERMARK is designed to be a permanent sensor, placed in the soil to be monitored and “read†as often as necessary with a portable or stationary device. Internally installed gypsum provides some buffering for the effect of salinity levels normally found in irrigated agricultural crops and landscapes."
I have used these for years and have had them buried in the yard for years with the only maintenance required when they are mechanically disturbed (like a person or mole digging around it). I have cabled these as far as twenty feet from my telemetry equipment and couple a temperature sensor to the Watermark probe to handle temperature compensation in the telemetry equipment.
Are they accurate? Who knows? I've never calibrated them to a kPa device. However, I can look at the lawn and correlate a dry lawn with a 'dry' reading and vice versa. As long as they are repeatable, then I'm happy. Which brings us to:
Of course a threshold is what you're after. But that threshold needs to work regardless of ongoing changes in the environment.
Exactly so. Just how precise a reading do you need? You want to know if the root system is getting 'enough' water. To my mind, any precision beyond this is a pointless fallacy. How many kPa do you need? I suppose a farmer investing in hundreds of acres of a crop that has a specific target specified would care - I don't have that kind of information for any of the plants I'm trying to keep alive.
Irrigation itself for example is known to change salt levels over time. If one could assume constant salinity over the lifetime of the sensor things would obviously be simpler. Just not sure if that assumption is reasonable.
From what I've read, the main variant to salinity levels would be due to fertilizer and you can make adjustments during the brief period that those are permeating the soil. In theory I should have data that shows this behavior, but I don't recall specifically noticing the effect (maybe I didn't fertilize enough
Finally, I've seen reference to 'Irrometers' as 'gypsum blocks'. Not so. An 'Irrometer' is a brand of tensiometer that actually measures the 'pull' of water into the soil. They are very accurate, expensive (by residential standards), and need to be removed before soil reaches freezing conditions. Watermark probes can tolerate frozen soil.
Tom