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Agricultural Sensors
The soil heat flux sensor measures temperature gradients using a thermopile consisting of two different metallic materials. Thermopile detectors receive thermal radiation, which can generate a thermoelectric potential between junctions of two dissimilar materials.
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The NiuBoL NBL-S-HF Soil Heat Flux Sensor, also known as a soil heat flux plate or heat flow sensor, is designed to measure the rate of heat transfer through soil, building surfaces and other materials.
The sensing element uses a thermopile structure. A temperature difference across the sensor produces a thermoelectric voltage proportional to the heat flux passing through the plate. Depending on the selected configuration, the measurement can be provided through RS485, 4–20 mA or 0–2 V output.
The NBL-S-HF is suitable for soil energy-balance studies, agricultural meteorology, evapotranspiration research, environmental monitoring, forestry and building heat-transfer measurements.

| Model | NBL-S-HF |
| Product Name | Soil Heat Flux Sensor / Heat Flux Plate |
| Measured Parameter | Heat Flux |
| Measurement Range | -200 to 200 W/m² |
| Measurement Accuracy | Within ±5% |
| Supply Voltage | DC 5 V or DC 12–24 V depending on configuration |
| Output Options | RS485 / 4–20 mA / 0–2 V depending on configuration |
| Internal Resistance | <300 Ω |
| Working Current | Approx. 26 mA at 12 V for transmitter configuration |
| Working Temperature | -40 to 50°C |
| Working Humidity | 0–100%RH |
| Standard Cable Length | 5 m for current catalog configuration |
| Typical Soil Installation Depth | 3–10 cm below the natural soil surface |
The NBL-S-HF uses a thermopile consisting of junctions formed by different metallic materials. When heat flows through the sensor, a temperature difference develops across the plate and produces a thermoelectric voltage.
The generated signal is proportional to the heat flux passing through the sensor. In the basic sensing principle:
Heat Flux (W/m²) = Calibration Coefficient × Sensor Output
Transmitter versions convert the sensor signal into standard analog or digital outputs such as 4–20 mA, 0–2 V or RS485 for easier integration with monitoring systems.
Soil heat flux describes the rate at which thermal energy moves through a unit area of soil. It is normally expressed in watts per square metre (W/m²).
| Condition | Interpretation |
|---|---|
| Positive Heat Flux | Heat is moving in the positive direction defined by the sensor orientation and system convention. |
| Negative Heat Flux | Heat is moving in the opposite direction. |
| Near Zero | Relatively little net heat transfer is occurring through the measurement plane. |
The sign of the heat-flux value depends on sensor orientation and the sign convention used by the monitoring system. It should not automatically be interpreted as “summer positive” or “winter negative” without considering installation direction and local conditions.
Soil heat flux is an important component of the surface energy balance. In agricultural meteorology and evapotranspiration research, it is commonly evaluated together with net radiation, sensible heat flux and latent heat flux.
| Parameter | Role |
|---|---|
| Net Radiation | Net incoming and outgoing radiation energy at the surface. |
| Soil Heat Flux | Energy transferred between the land surface and soil. |
| Sensible Heat Flux | Energy transferred between the surface and atmosphere as sensible heat. |
| Latent Heat Flux | Energy associated with evaporation and evapotranspiration. |
The NBL-S-HF directly measures heat flux. Thermal conductivity is a material property describing how easily heat passes through soil or another material.
Thermal conductivity can be studied by combining measured heat flux with an appropriate temperature gradient and experimental method. Therefore, the heat flux plate can be part of a thermal-conductivity measurement system, but it should not be described as directly measuring soil thermal conductivity by itself.
| Bidirectional Measurement | Measures heat flow in either direction within the specified -200 to 200 W/m² range. |
| Thermopile Principle | Converts the temperature difference across the plate into an electrical signal proportional to heat flux. |
| Compact Plate Design | Suitable for installation within soil layers while minimizing disturbance to the monitored area. |
| Multiple Outputs | Available with RS485, 4–20 mA or voltage output depending on the ordered version. |
| Low Power Consumption | Suitable for long-term field monitoring and remote environmental monitoring systems. |
| Soil and Surface Measurement | Can be used for soil heat-flow measurement and suitable wall or surface heat-transfer studies. |
For soil measurement, the heat flux plate should be installed horizontally so that its surface is approximately perpendicular to the primary direction of vertical heat flow.

| Installation Item | Recommendation |
|---|---|
| Location | Choose a representative measurement location within the study area. |
| Typical Depth | Install approximately 3–10 cm below the natural soil surface according to the measurement objective. |
| Orientation | Place the plate horizontally with the correct sensor face oriented according to the installation instructions. |
| Soil Contact | Ensure both surfaces of the plate maintain close contact with the surrounding soil. |
| Cable Routing | Keep a short section of the cable buried before routing it toward the soil surface to reduce heat conduction along the cable. |
| Backfilling | Restore the excavated soil as close as practical to its original position and density after installation. |
Direct surface installation is generally avoided because natural soil surfaces are uneven and exposed directly to solar radiation, wind and air-temperature changes. These conditions can make measurements less representative of actual soil heat transfer.
Installing the plate below the surface provides better contact with the soil and reduces direct radiative effects. The appropriate installation depth should still be selected according to the research method and project requirements.
The NBL-S-HF can also be used for suitable wall or building-surface heat-transfer measurements. The sensor should maintain close thermal contact with the measured surface.

For temporary surface measurement, a suitable thermal-contact material can be applied between the sensor and the measured surface to reduce air gaps. The sensor should be allowed to reach thermal equilibrium before measurements are evaluated.
| Interface | RS485 |
| Protocol | Modbus RTU |
| Default Baud Rate | 9600 bps |
| Optional Baud Rates | 4800 / 2400 bps when specified during ordering |
| Data Format | 8 data bits, no parity, 1 stop bit |
| Read Function | Function Code 03 |
| Write Function | Function Code 06 |
| Heat Flux Register | 0x002A |
| Device Address Range | 1–127 |
| Wire Color | Function |
|---|---|
| Red | Power + |
| Black | Power - / GND |
| Yellow | RS485 A+ |
| Blue | RS485 B- |
Wiring note: Output configuration varies between RS485, 4–20 mA and voltage versions. Always confirm the ordered model and wiring identification before connection.
| Soil Energy Balance | Agricultural Meteorology | Evapotranspiration Research |
| Greenhouse Research | Forestry | Environmental Monitoring |
| Surface Energy Studies | Building Heat Transfer | Scientific Research |
For agricultural research and evapotranspiration studies, the NBL-S-HF Soil Heat Flux Sensor can be combined with other meteorological and soil sensors.
| Sensor | Measurement |
|---|---|
| NBL-S-HF Soil Heat Flux Sensor | Soil heat flux in W/m² |
| Net Radiometer / Pyranometer | Radiation energy at the surface |
| Soil Temperature Sensor | Soil temperature and temperature gradient |
| Soil Moisture Sensor | Soil water conditions influencing thermal properties |
| Air Temperature & Humidity Sensor | Atmospheric conditions |
| Data Logger | Synchronizes and records all measurement channels |
| Error | Possible Effect |
|---|---|
| Poor Soil Contact | Air gaps can disturb the heat-transfer path and reduce measurement representativeness. |
| Installing Directly on Surface | Can introduce radiation, wind and uneven-surface effects. |
| Incorrect Orientation | Can reverse the sign of the reported heat-flux direction. |
| Cable Routed Directly Upward | Can introduce unwanted heat conduction along the cable. |
| Highly Disturbed Soil | Different density and structure around the sensor may affect heat transfer compared with undisturbed soil. |
A1. It measures the rate of heat transfer through soil or another measured surface, expressed in W/m².
A2. The current NBL-S-HF configuration has a measurement range of -200 to 200 W/m².
A3. A negative value indicates that heat is moving in the direction opposite to the sensor's defined positive direction. Interpretation depends on sensor orientation and system sign convention.
A4. No. It directly measures heat flux. Thermal conductivity can be evaluated when heat-flux data is combined with temperature-gradient measurements and an appropriate calculation method.
A5. The instruction manual recommends a typical soil installation depth of approximately 3–10 cm. The exact depth should match the research method and monitoring objective.
A6. Yes. The sensor can be used for suitable wall or surface heat-transfer measurements when close thermal contact is maintained.
A7. Depending on the selected configuration, RS485, 4–20 mA and voltage output versions are available.
A8. Yes. The RS485 version can connect to a compatible data logger, PLC or IoT gateway for local recording or remote transmission.
NBL-S-HF-Soil-Heat-Flux-Sensor.pdf
The NBL-S-HF Soil Heat Flux Sensor provides heat-flow measurements for agricultural meteorology, environmental research, soil energy-balance studies and building heat-transfer monitoring. RS485 and analog output options allow the sensor to be integrated with both scientific data-acquisition equipment and IoT monitoring systems.
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