

Portable Soil Moisture Meter
便携式土壤水分仪
- SKU SMA-0005
- Soil Moisture Analyzers
- CE (to be confirmed)
- RoHS (to be confirmed)
- ISO 9001 manufacturing (to be confirmed)
Price on request — FOB / CIF quoted per order
Prices depend on configuration, quantity and destination port.
Key specifications
| Measurement principle | Capacitance, resistance or frequency |
|---|---|
| Water content range | 0–100% (relative or calibrated) |
| Accuracy | ±3–5% with calibration |
| Probe length | 60–200 mm |
| Measurement time | 1–5 s |
| Soil type calibrations | 3–10 selectable |
By Lab Manufacturers China Technical TeamLast reviewed Standards: ISO 11465 (gravimetric water content), ISO 11274 (water retention), ASTM D5220 (neutron probe)
What is the Portable Soil Moisture Meter?
A hand-held meter with a probe that gives a quick water content reading in the field or in bags. It is the right choice for point checks, irrigation walk-throughs and rapid surveys where laboratory results are not needed.
What is the Portable Soil Moisture Meter?
A hand-held meter with a probe that gives a quick water content reading in the field or in bags. It is the right choice for point checks, irrigation walk-throughs and rapid surveys where laboratory results are not needed.
Overview
The portable soil moisture meter uses a capacitance, resistance or frequency probe inserted into the soil or a sample bag, and displays a water content value, often as a percentage or a relative index, within seconds. Simple models give a relative scale, while better ones output volumetric or gravimetric estimates calibrated for a few soil types. The meter is useful for checking irrigation uniformity, confirming that water has reached a certain depth, checking potting media before planting and carrying out rapid reconnaissance. Because the reading depends on contact, compaction, salinity and temperature, and because the measurement volume is small, results are indicative rather than reference, and several readings should be averaged. The probe is cleaned between samples, the batteries are checked, and the instrument is verified against gravimetric samples or a laboratory method periodically.
How does it work?
Soil moisture instruments use several physical principles. Dielectric sensors exploit the very high permittivity of water compared with soil minerals and air: frequency domain reflectometry measures the capacitance of the soil around a probe, while time domain reflectometry measures the travel time of a pulse along a waveguide, both giving volumetric water content after soil-specific calibration. Tensiometers measure matric potential, the suction with which soil holds water, through a water-filled tube with a porous ceramic cup and a pressure sensor, indicating how easily plants can extract water. Neutron probes emit fast neutrons that are slowed by hydrogen in water and counted to give water content over a large volume. Gravimetric sampling with oven drying remains the reference method, and portable meters give quick estimates for scheduling.
What are the key features?
- Quick water content reading within seconds.
- Insertion probe works in soil, bags and pots.
- Several soil type calibrations on better models.
- Hand-held, battery-powered and robust for field use.
- Useful for irrigation uniformity and depth checks.
- Averaging several readings improves reliability.
What are the technical specifications?
A typical portable soil moisture meter configuration offers measurement principle of Capacitance, resistance or frequency, water content range of 0–100% (relative or calibrated), accuracy of ±3–5% with calibration, probe length of 60–200 mm, measurement time of 1–5 s and soil type calibrations of 3–10 selectable. Values are indicative of the product class; the exact figures for each configuration are confirmed on the quotation and the calibration documents supplied with the instrument.
Which applications is it used for?
The Portable Soil Moisture Meter is used in irrigation walk-through and checks, potting media and greenhouse checks, rapid field reconnaissance and construction and landscaping inspections. Across the wider Soil Moisture Analyzers class, laboratories also deploy it for irrigation scheduling and control, hydrological and water balance studies and geotechnical and construction monitoring.
Which standards and certifications apply?
Relevant standards and methods include ISO 11465 (gravimetric water content), ISO 11274 (water retention), ASTM D5220 (neutron probe), ASTM D7830 (electromagnetic gauge) and FAO 56 (irrigation guidelines). Certification candidates for this model are CE, RoHS and ISO 9001 manufacturing; each is to be confirmed for the specific configuration before shipment, and certificates are supplied only where they have been issued.
Calibrate dielectric sensors for the actual soil, because factory calibrations are general and can be wrong by several percent volumetric water content in clay, saline or organic soils. Install sensors with good soil contact and in a representative location, avoiding stones, roots and preferential flow paths, and disturb the soil as little as possible. For tensiometers, fill and de-air the tube, keep the ceramic cup in contact with soil and protect the unit from freezing and from drying out, which breaks the water column. Neutron probes need licensed operation, a reference count, and an access tube installed to the required depth. Gravimetric checks should be carried out periodically to confirm all methods. Record calibration, installation depth and maintenance events with the data.
How do I select the right Portable Soil Moisture Meter?
Select the portable meter for quick point checks and relative comparisons where speed matters more than reference accuracy. For continuous monitoring or reported data, use installed sensors or gravimetric sampling. In an RFQ, specify range, accuracy, soil calibrations and probe length.
How does it compare with other Soil Moisture Analyzers variants?
Decide whether water content or water potential is the useful variable: content tells how much water is present, while potential tells how available it is, so both may be needed. For irrigation scheduling, dielectric sensors give continuous volumetric content and are easy to automate, but they need soil-specific calibration because texture, salinity and organic matter change the reading. Tensiometers are preferred when the plant-available water range and the refill point matter, and they respond rapidly near field capacity, although they need maintenance and are limited in dry soil. Neutron probes are accurate over large volumes and depths but require licensing and radiation safety, so they suit research and deep profiling. Portable meters are useful for spot checks. Consider depth of measurement, logging and telemetry, installation disturbance and the salinity range expected.
Full specifications
| Measurement principle | Capacitance, resistance or frequency |
|---|---|
| Water content range | 0–100% (relative or calibrated) |
| Accuracy | ±3–5% with calibration |
| Probe length | 60–200 mm |
| Measurement time | 1–5 s |
| Soil type calibrations | 3–10 selectable |
| Display | LCD, optional backlight |
| Ingress protection | IP54 or better |
| Power supply | Battery, 9 V or AA |
| Operating temperature | 0–50 °C |
| Weight | 0.3–1 kg |
Indicative values for this product class. Final specifications are confirmed on the quotation and in the calibration documents supplied with the instrument.
Applications
- Irrigation walk-through and checks
- Potting media and greenhouse checks
- Rapid field reconnaissance
- Construction and landscaping inspections
Key features
- Quick water content reading within seconds.
- Insertion probe works in soil, bags and pots.
- Several soil type calibrations on better models.
- Hand-held, battery-powered and robust for field use.
- Useful for irrigation uniformity and depth checks.
- Averaging several readings improves reliability.
Frequently asked questions about Portable Soil Moisture Meter
Soil water content varies over short distances, and the meter measures only a small volume around the probe, so stones, roots, cracks and compaction create scatter. Taking several readings and averaging them gives a more stable estimate.
If the meter offers soil type settings, choose the closest to the soil at hand, and verify against gravimetric samples. Without a match, use the relative mode for comparisons rather than treating the value as absolute water content.
Push the probe fully into firm, undisturbed soil with good contact along its length, avoiding stones and cracks. Partial insertion measures only part of the sensing length and biases the reading, so insert to the marked depth.
Water content states how much water the soil holds, typically as a volumetric or gravimetric percentage. Water potential states how strongly the soil holds it, so it indicates availability to plants. Two soils can have the same content but very different availability.
The relationship between permittivity and water content depends on texture, bulk density, salinity, temperature and organic matter. A factory equation can be off by several percent in heavy clay or saline soil, so a local calibration against gravimetric samples improves accuracy.
A tensiometer is better when the question is how hard plants must work to extract water, such as triggering irrigation at a set suction, because it measures potential directly and responds quickly near field capacity. It is less useful in very dry soil where the water column breaks.
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