
By Ryan Bent · 8 August 2026
Watering choices are still made by feel on most farms, and feel is costly. A soil moisture meter replaces that guess with a number you can act on.
The trouble is that a soil moisture meter can be any of six different tools.
Some read how much water the soil holds. Others read how hard a root must work to pull that water out. They are not the same, and buying the wrong one can waste a whole season.
This guide sets out what each soil moisture meter measures, where to put it, and how to read it. Every figure below traces to published field research rather than to product packaging.
A soil moisture meter belongs to one of two families. One family reports water content, and the other reports soil water tension.
Both are valid, and they answer different questions.
Water content is the volume of water held in a given volume of soil. It is usually given as a percent.
A reading of 25 percent means a quarter of that soil volume is water. To make the number useful, multiply it by the depth of the root zone. That turns a percent into a depth of water the crop can draw on.
Soil water tension is the energy a root must spend to pull water off soil particles. Wet soil sits near zero, and tension climbs as the profile dries.
| Technology | Reads | Site calibration | Main weakness |
|---|---|---|---|
| Capacitance / FDR | Water content | Preferred | Salinity, clay, temperature |
| Time domain reflectometry | Water content | Rarely needed | Small sensing volume |
| Neutron probe | Water content | Usually required | Licensing and shallow depths |
| Oven drying | Water content | Not applicable | Takes 24 hours |
| Tensiometer | Tension | Not needed | Narrow working range |
| Granular matrix sensor | Tension | Per soil type | Slow response in sand |
These sensors read the electric behaviour of the soil around a pair of rods. Water has a far higher dielectric constant than soil or air, so the reading tracks water content closely.
They respond almost at once and cost less than the others. Their working frequency sits below 100 MHz, which is why a soil-specific calibration is advised.
A TDR soil moisture meter times a voltage pulse travelling along steel rods buried in the soil.
Because it works at much higher frequencies, its reading leans far less on texture, salt and heat. Site calibration is rarely needed, which is why researchers reach for it first. The trade-off is a small sensing volume and a higher price.
The neutron probe is the most exact indirect method, and also the least handy. It uses a radioactive source, so operators need training and a licence, and it reads poorly in the top few inches.
Oven drying is the yardstick every other method is measured against. A sample is weighed wet, dried at 105 degrees Celsius for 24 hours, then weighed again.
Collect samples with a proper soil auger or core sampling kit rather than a spade. A disturbed sample gives a false bulk density, and that error carries straight through the sum.
A tensiometer is a water-filled tube with a porous ceramic tip and a vacuum gauge on top.
These sensors measure electric resistance inside a porous block that balances with the soil around it. Handheld meters read from 0 to 199 centibars, and loggers stretch that range further.
Gypsum blocks work the same way but use a much finer matrix. That matrix melts away in salty or always wet soil, and readings drift from block to block over time. Extension guidance is blunt: they are not advised for irrigation scheduling.
The useful range of a gypsum block sits in dry soil, above roughly 50 centibars. Even in good ground a block lasts only a couple of seasons.
Where you put a soil moisture meter decides whether the data means anything. The guidance is to set sensors in pairs, at roughly one-third and two-thirds of the crop root-zone depth.
Deep-rooted crops such as maize and alfalfa justify a third depth.
Pick a spot with typical soil rather than a handy one. Field edges, high points, hollows and slopes all read differently from the block they sit in.
Where a field holds two clear soil types, track each one on its own. Averaging a sand and a clay gives a number that fits neither. Split the field into zones instead.
A factory calibration is made in a lab soil that is almost certainly not yours.
Capacitance readings shift with salt, clay, bulk density and soil heat. Any one of those can move a reading enough to trigger the wrong watering call.
Granular matrix sensors carry a heat assumption too. They are factory set to a default soil temperature, so readings from a cold spring profile need a small correction.
An oversized hole is the fastest way to ruin a good soil moisture meter. Gaps leave air against the probe, and air reads as bone-dry soil. Push the sensor into a snug hole and keep soil disturbance low.
Simple and cheap beats exact and fragile at this scale.
Here the soil moisture meter must survive a season outdoors and feed a schedule. A logged granular matrix or capacitance array at two or three depths is the workhorse choice.
Numbers that will be challenged need a method that holds up.
They give a rough hint at best. Treat one as a prompt to go and check rather than as a number you would water on.
Set the shallow sensor at about one-third of the root-zone depth and the deeper one at two-thirds.
Every two to three days suits most irrigated crops. Reading more often rarely changes the call, and it burns logger memory.
It affects most of them. Capacitance and resistance sensors are worst hit, while a TDR probe holds up better in salty ground.
Not safely, unless the whole farm shares one soil type and one crop.
Choosing a soil moisture meter is really a choice about what question you need answered.
If you are watering a known soil, a tension sensor at two depths will tell you when to start the pump. If you must budget water across a profile or report to a third party, a content sensor backed by oven drying is the stronger case.
Whatever you buy, fit it properly and check it against a dried sample once a season. An unchecked soil moisture meter is just a confident guess. Browse the grain and soil moisture testers and matching soil core sampling kits before you commit.