Monitoring soil moisture helps to:
- time irrigation to avoid over- or under-watering
- match stocking rates to pasture availability
- plan fertiliser application and pasture renovation
- avoid waterlogging and improve drainage outcomes
- respond to seasonal shifts and forecasted rainfall.
How to monitor soil moisture
There are several practical methods available:
- Soil moisture probes. Installed in paddocks to measure moisture at multiple depths (typically up to 1 metre). These provide real-time data and are used across NSW in networks like the Hunter Soil Moisture Project and the Murray Valley representative sites. Probes can also measure soil temperature, rainfall and wind speed.
- Manual observation. Digging up soil and feeling for moisture remains a reliable method. Pulling plants and inspecting root zones can help assess whether irrigation is needed.
- Weather-based scheduling. Uses evapotranspiration data and crop factors to estimate how quickly soil moisture is being depleted. This method is especially useful for irrigators managing high-value crops.
- Remote sensing and plant-based sensors. These technologies measure canopy temperature, sap flow and stem growth to assess plant water stress. While more advanced, they can support strategic irrigation decisions.
Farming forecaster
What Does Farming Forecaster Measure?
Read transcriptThe Farming Forecaster probes and platform provides free, easy to access regional weather data for farmers and their advisors.
Monitoring sites vary from full weather stations to individual monitoring systems for:
- rainfall
- air and soil moisture
- temperature
- wind speed and direction.
It does not contain information on solar radiation.
Farming Forecaster:
- shows how widespread rain has been
- shows how much rain has fallen in the different locations
- shows how soil moisture is declining or rising
- predicts pasture growth for the next 3 months
- provides ground cover and plant-available water estimates
- allows comparison of current soil moisture data to that of previous 2 seasons.
The amount of stored soil moisture reflects rainfall infiltration and water holding capacity. This gives landholders an indication of how long good plant growth can be expected into spring.
Farming Forecaster
Start using Farming Forecaster.
Moisture monitoring advice for irrigators
If you’re irrigating, especially with flood systems, timing is critical. Delaying the first spring irrigation often leads to poor water-use efficiency and reduced yields. The key to get the timing right is to monitor soil moisture levels in the active root zone and irrigate before stress occurs. To do this you can:
- use probe data or manual checks to assess moisture at 30 cm depth
- use a matric potential reading of –60 kPa at 30 cm is a common trigger to irrigate
- prioritise paddocks with lighter soils, good crop potential or fast drainage
- be ready to order water and ensure channels and outlets are clear
- consider strategic irrigation if water is limited by focusing on critical growth stages like flowering and pod fill in canola, or head emergence in cereals.
If you’re using centre pivot or drip systems, small, frequent irrigations can be applied with minimal risk of waterlogging. These systems are especially valuable in seasons with limited water availability.
Irrigation
Learn more about irrigation planning in NSW.
How to read soil moisture probe data
Soil moisture probes can help landholders understand how much water is available in the soil profile and how crops or pastures are using it over time.
Probe graphs are most useful when they are used to identify patterns, rather than focusing only on the numbers. Look at how each sensor line changes after rainfall or irrigation, and how it trends while plants are actively growing.
Each line on a graph usually represents a sensor at a different depth. Comparing the lines can show how far water has moved through the profile and where plant roots are drawing moisture from.
What to look for in the graph
- Sharp rises or spikes: these usually show water moving into the soil after rainfall or irrigation. A spike in deeper sensor lines can show that water has moved further down the profile.
- Small daily rises and falls: these ripples can show plant roots taking up moisture during the day, followed by small overnight changes when plant water use slows.
- Downward trends: these show moisture being drawn down as plants use water. The depth of the drawdown can indicate how deep roots are actively accessing moisture.
- Flat lines: these can show that moisture at that depth is not changing. This may mean roots are not using water from that part of the profile, or that the soil is already dry or too wet to show much movement.
This example graph below shows 8 lines for an 80 cm probe, with each sensor 10 cm apart starting just below the soil surface.
- The spike indicates a rainfall event that increased soil moisture to 70 cm.
- Ripples show small changes daily fluctuations.
- The downward trend shows draw down in the first 40 cm of the soil, however the 50 cm sensor line remains flat. This means the plant roots aren’t accessing this moisture.

Over time, these patterns show where moisture is available and how deep roots are drawing water from. In wetter conditions, roots will likely use water closer to the surface before drawing from deeper layers as the upper soil dries.
If roots appear to stop drawing water at the same depth each season, there may be a physical or chemical constraint limiting root growth. Further investigation, such as soil testing or advice from an agronomist, may help identify the cause.
Getting started
If you’re not confident in interpreting soil moisture data, consider working with an agronomist or Local Land Services officer to help apply it to your irrigation decisions.
Contact Local Land Services NSW
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