

Benchtop Soil pH Meter
台式土壤 pH 计
- SKU SPM-0002
- 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 20 |
|---|---|
| pH resolution | 0.001 |
| pH accuracy | ±0.01 |
| Calibration points | Up to 5 point |
| Temperature compensation | Automatic or manual |
| Stirrer | Integrated magnetic stirrer |
By Lab Manufacturers China Technical TeamLast reviewed Standards: ISO 10390 (soil pH), ISO 11265 (electrical conductivity), ASTM D4972 (pH of soils)
What is the Benchtop Soil pH Meter?
A mains-powered laboratory meter with high stability and precision for measuring pH in soil suspensions. It is the right choice for busy soil testing laboratories that report values against a defined standard method.
What is the Benchtop Soil pH Meter?
A mains-powered laboratory meter with high stability and precision for measuring pH in soil suspensions. It is the right choice for busy soil testing laboratories that report values against a defined standard method.
Overview
The benchtop soil pH meter provides a stable platform for the electrode, often with a stirrer, an electrode arm and a sample holder that keep the measurement consistent. Resolution of 0.01 pH or finer with accuracy near 0.01 pH, an auto-stability function and automatic temperature compensation suit the precision needed for standard methods. The meter supports multiple buffer sets, records calibration slopes and may include data management for laboratory records. Because soil pH depends strongly on the ratio and electrolyte, the laboratory controls these by using a calibrated scoop or balance, deionised water or a salt solution, and a fixed stirring and equilibration time, often one hour for the water method. Reference values and duplicate samples verify each batch, and the instrument is calibrated at the start of each session and checked during long runs.
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?
- Stable platform with stirrer and electrode arm.
- Resolution of 0.01 pH with accuracy near 0.01 pH.
- Auto-stability function confirms a valid reading.
- Stores calibration slopes and multiple buffer sets.
- Data export supports laboratory records.
- Designed for standardized suspension methods.
What are the technical specifications?
A typical benchtop soil ph meter configuration offers pH range of −2 to 20, pH resolution of 0.001, pH accuracy of ±0.01, calibration points of Up to 5 point, temperature compensation of Automatic or manual and stirrer of Integrated magnetic stirrer. 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 Benchtop Soil pH Meter is used in soil testing laboratory pH analysis, lime requirement determination, long-term soil monitoring programmes and research and reference testing. 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 Benchtop Soil pH Meter?
Select the benchtop meter for laboratory work that reports pH by a standard method and requires maximum stability and reproducibility. For rapid field mapping, a portable meter is more practical. In an RFQ, specify resolution, accuracy, stirrer and data management features.
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 20 |
|---|---|
| pH resolution | 0.001 |
| pH accuracy | ±0.01 |
| Calibration points | Up to 5 point |
| Temperature compensation | Automatic or manual |
| Stirrer | Integrated magnetic stirrer |
| Electrode type | Glass combination with ATC |
| Data memory | Up to 1000 records |
| Outputs | USB, RS-232, printer |
| Power supply | 220 VAC, 50 Hz |
| Operating temperature | 10–35 °C |
Indicative values for this product class. Final specifications are confirmed on the quotation and in the calibration documents supplied with the instrument.
Applications
- Soil testing laboratory pH analysis
- Lime requirement determination
- Long-term soil monitoring programmes
- Research and reference testing
Key features
- Stable platform with stirrer and electrode arm.
- Resolution of 0.01 pH with accuracy near 0.01 pH.
- Auto-stability function confirms a valid reading.
- Stores calibration slopes and multiple buffer sets.
- Data export supports laboratory records.
- Designed for standardized suspension methods.
Frequently asked questions about Benchtop Soil pH Meter
The standard method sets the time, commonly one hour for the water method and a shorter period for salt solutions, sometimes thirty minutes. Stirring improves contact, and measuring too early gives unstable readings, so the specified time must be followed.
Changing the soil to solution ratio changes the measured pH because dilution alters ionic strength and exchangeable acidity. Using a calibrated scoop or a balance with a fixed volume keeps the ratio constant, so results are comparable between samples and batches.
Each batch should include a duplicate and a reference soil with a known pH, and calibration slopes should be recorded. These checks detect electrode drift, buffer errors and preparation mistakes before results are released.
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.
Related models






