

Portable Soil pH Meter
便携式土壤 pH 计
- SKU SPM-0001
- Soil pH Meters
- 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
| pH range | −2 to 16 |
|---|---|
| pH resolution | 0.01 |
| pH accuracy | ±0.02 |
| Calibration points | 2 or 3 point |
| Temperature compensation | Automatic, 0–50 °C |
| Electrode type | Glass combination, refillable |
By Lab Manufacturers China Technical TeamLast reviewed Standards: ISO 10390 (soil pH), ISO 11265 (electrical conductivity), ASTM D4972 (pH of soils)
What is the Portable Soil pH Meter?
A battery-powered meter with an interchangeable electrode for soil suspensions measured in the field or greenhouse. It is the right choice for agronomists and survey teams that need reliable pH values away from the laboratory.
What is the Portable Soil pH Meter?
A battery-powered meter with an interchangeable electrode for soil suspensions measured in the field or greenhouse. It is the right choice for agronomists and survey teams that need reliable pH values away from the laboratory.
Overview
The portable soil pH meter combines a rugged, water-resistant meter body with a glass electrode that can be immersed in a soil suspension mixed in a beaker or a sample cup. It offers two or three point calibration, automatic temperature compensation and a resolution of 0.01 pH with accuracy of about 0.02 pH, which is sufficient for soil work. Field kits include a bottle of deionised water or potassium chloride solution, a measuring scoop, a mixing container and buffer sachets so that a consistent ratio can be maintained. Some models log readings and allow GPS tagging for mapping, and a backlit display helps in low light. The electrode is the critical part: a clogged junction or dried reference causes slow, drifting readings, so routine storage in a suitable solution and periodic replacement are essential for trustworthy results.
How does it work?
A soil pH meter measures the activity of hydrogen ions with a glass electrode and a reference electrode, generating a voltage that is converted to pH units. In the laboratory, the method mixes air-dried soil with water or a dilute salt solution such as potassium chloride or calcium chloride at a fixed ratio, most commonly one to five, then stirs and measures after equilibration. The salt solution gives a value closer to the field pH and reduces the effect of soluble salts, while the water method gives a higher reading. Direct-insertion meters use a sturdy electrode pushed into moist soil, which is convenient for field mapping but can be affected by contact and moisture. All electrodes must be calibrated with buffers that bracket the expected range, and temperature compensation corrects for the effect of temperature on the electrode response.
What are the key features?
- Water-resistant body suits field and greenhouse use.
- Two or three point calibration with automatic temperature compensation.
- Resolution of 0.01 pH and accuracy near 0.02 pH.
- Field kit maintains a consistent soil to solution ratio.
- Optional data logging and GPS for mapping.
- Interchangeable electrodes simplify replacement.
What are the technical specifications?
A typical portable soil ph meter configuration offers pH range of −2 to 16, pH resolution of 0.01, pH accuracy of ±0.02, calibration points of 2 or 3 point, temperature compensation of Automatic, 0–50 °C and electrode type of Glass combination, refillable. 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 pH Meter is used in field soil pH surveying, greenhouse and nursery soil testing, agronomy advisory visits and precision agriculture sampling. Across the wider Soil pH Meters class, laboratories also deploy it for lime requirement assessment, soil fertility and nutrient availability evaluation and soil survey and mapping.
Which standards and certifications apply?
Relevant standards and methods include ISO 10390 (soil pH), ISO 11265 (electrical conductivity), ASTM D4972 (pH of soils), US EPA Method 9045D and ISO 3696 (laboratory water). 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 with fresh buffers at two or three points that bracket the sample range, and record the slope, because a slow or low slope indicates an aging electrode. Keep the reference junction wet and clean, since drying and salt deposits cause drift, and store the electrode in the recommended solution rather than in water. Use air-dried soil and consistent mixing, stirring and equilibration, and measure at a controlled temperature. Rinse the electrode between samples and blot, not wipe, to avoid static charge. For direct insertion, choose moist, representative soil and average several readings, and do not rely on field values for lime recommendations without confirming against the laboratory method. Replace electrodes on schedule and maintain buffers within their shelf life.
How do I select the right Portable Soil pH Meter?
Select the portable meter for reliable pH measurements of soil suspensions away from the laboratory, and keep the field kit complete so ratios stay consistent. For very high throughput or tight tolerance work, a benchtop meter is more stable. In an RFQ, specify accuracy, electrode type, logging and kit contents.
How does it compare with other Soil pH Meters variants?
Choose the measurement approach first: laboratory suspensions for reported values and comparisons, or direct insertion for rapid field mapping. Laboratory work needs a meter with good resolution and a stable reference, plus the specified salt solution or water and a defined soil to solution ratio, because the ratio and electrolyte change the result by up to a unit. For field use, a rugged portable meter with a spear electrode is convenient, but confirm whether the reading is comparable with laboratory values or is only for relative mapping. If salinity is also of interest, a combined pH and conductivity meter saves time. Consider electrode type and replacement, temperature compensation, buffer and storage solutions, and calibration frequency. For any reported or contractual result, follow the standard method exactly, including the equilibration time.
Full specifications
| pH range | −2 to 16 |
|---|---|
| pH resolution | 0.01 |
| pH accuracy | ±0.02 |
| Calibration points | 2 or 3 point |
| Temperature compensation | Automatic, 0–50 °C |
| Electrode type | Glass combination, refillable |
| Data memory | Up to 1000 readings |
| Ingress protection | IP67 |
| Power supply | Rechargeable or AA battery |
| Operating temperature | 0–50 °C |
| Accessories | Buffers, KCl solution, cups, scoop |
Indicative values for this product class. Final specifications are confirmed on the quotation and in the calibration documents supplied with the instrument.
Applications
- Field soil pH surveying
- Greenhouse and nursery soil testing
- Agronomy advisory visits
- Precision agriculture sampling
Key features
- Water-resistant body suits field and greenhouse use.
- Two or three point calibration with automatic temperature compensation.
- Resolution of 0.01 pH and accuracy near 0.02 pH.
- Field kit maintains a consistent soil to solution ratio.
- Optional data logging and GPS for mapping.
- Interchangeable electrodes simplify replacement.
Frequently asked questions about Portable Soil pH Meter
Keep the glass bulb and reference junction moist in the storage solution recommended by the manufacturer, usually a potassium chloride solution, not deionised water, which leaches ions and slows the response. Replace the storage cap solution regularly.
Drift usually means a clogged junction, a dry or depleted reference, or an aged glass bulb. Rinse and soak the electrode, refill the reference if refillable, and recalibrate; persistent drift after these steps indicates the electrode should be replaced.
No. Automatic compensation corrects the electrode response, but the pH of the soil suspension itself changes with temperature, so samples should be measured at a consistent temperature. Compensation cannot correct that sample-related effect.
Diluting soil with more solution increases the measured pH because dilution reduces the ionic strength and releases more exchangeable hydrogen, and it also reduces the salt effect. Standards fix a ratio, so results are only comparable when the same ratio is used.
The water method gives a higher pH because it measures only the active acidity in a dilute solution. A salt solution such as potassium chloride or calcium chloride releases exchangeable acidity, giving a lower value that better reflects field conditions and is preferred for lime recommendations.
Calibrate before each measurement session and after any electrode cleaning or replacement, using fresh buffers that bracket the expected pH. Daily one-point checks during heavy use confirm stability, and slopes are recorded to detect electrode ageing.
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