| GMS | Can measure a large area (8 - inch diameter)
Can be used in moderately saline soils
Can be used to sense wet or dry soil moisture readings for irrigation
If soil does not dry out, little maintenance is required
Good accuracy in medium to fine soils
Data can be logged and retrieved remotely
Applicable for large soil tension range
Continuous measurement at same location
Can be permanently installed (through winter) in soil
No water refilling needed | Relatively inaccurate
Performs poorly in sandy soils due to slow reaction time (water moves fast in sandy soils)
Performs poorly in soils that shrink/swell
Susceptible to drying; must be dug out and solution reset when this occurs
Relatively slow response time to soil water changes
Sensitive to soil temperature and high salinity
Calibration in needed for each soil type
Slow reaction time
Does not work well in sandy soils | $40 - $70 per sensor\n250 for handheld metern500 -$600 for data logger |
| HDS | Sensor output is independent to electrical conductivity (EC) value.
Measurements not affected by salts in the soil
Small size
Very accurate
Soil/site calibration usually not required
Remote access of data available
Measures a wide range of matric potential
Long lasting, with no maintenance required | HDS have a larger power requirement compared to other sensor types for frequent observations
Very small area of influence
Slow reaction time
Does not work well in sandy soils | $280 - $380 per sensor\n$300 - $440 for excitation module\n$2,000 - $2,500 for data logger |