From Soil Sensors
- Stable—no sensor drift, ensuring continual accuracy.
- Patented technology that accurately measures moisture and electrical conductivity permits more accurate optimization of watering and fertilization than with just moisture.
- Depended on by the USDA, NOAA, leading irrigation companies, and many universities for over 20 years. Used by NASA for ground truthing of satellite-based soil imaging.
- Soil moisture calibration has been rigorously peer-reviewed, making it one of the most trusted soil sensors available.
- Can remain in-situ indefinitely, or relocated and redeployed without worry.
- Ideal for remote locations, harsh environments and applications where data is critical.
- Enables measurement of native (undisturbed) soil, even hard-packed clay.
- Industry-leading 5-year warranty.
- Repeatable accuracy and stability without the need for calibration in most soils.
- Digital sensor using the SDI-12 protocol—no setup, just connect to data logger. Compatible with any SDI-12 capable data logger.
- Zero maintenance required.
- Unparalleled spatial and temporal measurement consistency. No sensor-to-sensor variations across locations, seasons, soil types or moisture range.
- Instant measurement of the 3 most significant soil parameters simultaneously—moisture, salinity and temperature.
- Unlike most TDR or capacitance-based sensors, HydraProbe is less sensitive to changes in temperature, salinity, and soil mineralogy.
The HydraProbe Field Portable puts the power of HydraProbe in the palm of your hand.
Take soil measurements anywhere, without the effort or expense of setting up a permanent soil monitoring system. Your smartphone communicates wirelessly with the HydraProbe using an ad-hoc wi-fi network created by the HydraProbe Field Portable.
Simply insert the probe into the soil, and tap on the “Sample” button in the app. The location of each measurement is recorded along with the soil measurement data. All data can be saved and emailed as a .CSV for analysis in Excel.
HydraProbe is a “dielectric impedance”-based sensor developed by the physics department at Dartmouth College. Unlike capacitance or time domain based soil sensors, HydraProbe fully characterizes the dielectric spectrum using a radio frequency at 50 MHz.
Complex mathematical computations performed by an onboard microprocessor process the reflected signal measurements to accurately determine the soil’s dielectric permittivities, the key parameters behind the soil moisture and bulk EC measurement.
Low inner-sensor variability means there is no need for sensor-specific calibrations.
This method has passed the most rigorous scientific peer review from dozens of journals such as the Vadose Zone Journal, American Geophysical Union, and The Journal of Soil Science Society of America.
- The bulk EC (electrical conductivity) of the soil is correlated to the soil’s salinity because salts when mixed with water will conduct electricity. The bulk EC parameter is sometimes called “salinity”.
- Many nutrients are salts—a source of salinity. Nutrient accumulation, poor drainage and saline irrigation water can lead to the unwanted buildup of salinity in soil.
- High bulk EC can affect moisture readings and create errors with capacitance based moisture sensors. HydraProbe’s soil moisture measurement is less sensitive to salinity than other capacitance based probes.
- The soil bulk EC can change dramatically with water content and can be affected by the quality of the irrigation water, fertilization, drainage, and other natural processes.
- Compaction, clay content and organic matter, can influence moisture holding trends over time, also affecting bulk EC capacities in soil.
- The effect of bulk EC on the moisture availability to a plant’s roots is great. As salinity changes the water needs also change.
- A temperature corrected bulk EC parameter is available so the user can make comparison independent of soil temperature.
- Because HydraProbe also measures the dielectric permittivities, algorithms can be applied to approximate the EC of the soil pore water allowing for better soil salinity characterizations.
- Operating temperature range:
- In soils: freezing to +55°C
- Standard temperature probe range: -10°C to +55°C
- Extended temperature probe range: -30°C to +55°C***
- Storage temperature range: -40°C to +55°C
- Water resistance: Tolerates continuous full immersion
- Cable: 18 gauge (22 gauge for RS-485 and analog versions), UV resistant, direct burial
- Vibration and shock resistance: Excellent; potted components in PVC housing and 304 grade stainless steel tines
- Length: 4.9” (124 mm):
- Diameter: 1.6” (42 mm):
- Weight: 7 oz. (200 g):
- Cable weight: 0.86 oz/ft (80g/m):
- Sensing volume (cylindrical region): Length: 2.2” (5.7 cm) Diameter: 1.2” (3.0 cm):
- 1: Voltage 1
- 2: Voltage 2
- 3: Voltage 3
- 4: Voltage 4
- 5: Voltage 5
- 6: Soil Temperature in Celsius
- 7: Soil Temperature in Fahrenheit
- 8: Water fraction by volume
- 9: Loss Tangent
- 10: Soil Conductivity (temperature corrected) in Siemens / meter
- 11: Real dialectric permittivity
- 12: Real dielectric permittivity (temperature corrected)
- 13: Imaginary dialectric permittivity
- 13: Imaginary dialectric permittivity (temperature corrected)
- 15: Soil conductivity in Seimens / meter
- 16: Diode Temperature in Celsius
- 17: Saved for future development
- 18: ADC Reading 1
- 19: ADC Reading 2
- 20: ADC Reading 3
- 21: ADC Reading 4
- 22: ADC Reading 5
* Accuracy may vary with some soil textures.
** Extended temperature range sensor (down to -30° C) available
*** ”Extended Temperature Range” version available, which can measure down to -22°F (-30°C) for research, cold-climate, high-altitude, arctic applications or any other measurement situation where there will be significant below-freezing ground temperatures.