

Multi-Collector ICP-MS Spectrometer
多接收器电感耦合等离子体质谱仪
- SKU ICM-0004
- ICP-MS
- CE (to be confirmed)
- ISO 9001 manufacturing (to be confirmed)
- Nuclear safeguards software option (to be confirmed)
Price on request — FOB / CIF quoted per order
Prices depend on configuration, quantity and destination port.
Key specifications
| Mass range | 2–260 amu |
|---|---|
| Isotope ratio precision | a few ppm or better |
| Detectors | faraday cups and ion counters |
| Analyzer | magnetic sector |
| Resolution | low to high variable |
| Plasma power | 1500–1600 W |
By Lab Manufacturers China Technical TeamLast reviewed Standards: ICH Q3D Elemental Impurities, USP <233> Elemental Impurities — Procedures, USP <730> Plasma Spectrochemistry
What is the Multi-Collector ICP-MS Spectrometer?
A multi-collector ICP-MS measures several isotopes simultaneously with dedicated detectors for high-precision ratios. It is chosen for geochronology, provenance, nuclear safeguards and precise tracer studies, where ratio precision matters more than concentration.
What is the Multi-Collector ICP-MS Spectrometer?
A multi-collector ICP-MS measures several isotopes simultaneously with dedicated detectors for high-precision ratios. It is chosen for geochronology, provenance, nuclear safeguards and precise tracer studies, where ratio precision matters more than concentration.
Overview
In this instrument a magnetic sector disperses the ion beam, and an array of faraday cups and sometimes ion counters is positioned to collect several isotopes at the same time. Simultaneous collection cancels short-term signal fluctuations, giving isotope ratio precision of a few parts per million or better, far beyond scanning instruments. A collision or reaction cell may be added to remove interferences for elements such as calcium and iron. Sample introduction can be liquid or laser ablation for spatially resolved studies. Applications include uranium-lead and rubidium-strontium geochronology, isotope fingerprints for provenance and forensics, and nuclear material accountancy. High precision demands stable plasma conditions, careful mass bias correction and matrix matching.
How does it work?
A plasma torch at atmospheric pressure ionizes the sample aerosol. Ions are extracted through a two-stage interface of sampling and skimmer cones into a vacuum region, then focused by ion optics and separated by a mass analyzer according to mass-to-charge ratio. The most common analyzer is a quadrupole, which scans rapidly across selected masses; sector field instruments provide high resolution or high sensitivity, multicollector instruments measure isotope ratios precisely, and time-of-flight analyzers record all masses simultaneously. Collision and reaction cells filled with helium, hydrogen or reactive gases suppress polyatomic interferences such as argon chloride on arsenic or argon argon on selenium. Detection uses electron multipliers with pulse counting and analog modes to cover a wide dynamic range. Calibration uses external standards, internal standards and, when needed, isotope dilution, with careful control of blanks and matrix effects.
What are the key features?
- Array of faraday cups and ion counters
- Simultaneous multi-isotope collection
- Isotope ratio precision to parts per million
- Optional collision cell for calcium and iron
- Liquid or laser ablation sample introduction
- Careful mass bias and matrix correction
What are the technical specifications?
A typical multi-collector icp-ms spectrometer configuration offers mass range of 2–260 amu, isotope ratio precision of a few ppm or better, detectors of faraday cups and ion counters, analyzer of magnetic sector, resolution of low to high variable and plasma power of 1500–1600 W. 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 Multi-Collector ICP-MS Spectrometer is used in uranium-lead and rubidium-strontium geochronology, provenance and forensic isotope fingerprints, nuclear safeguards and material accountancy and environmental and nutritional tracer studies. Across the wider ICP-MS class, laboratories also deploy it for elemental impurity testing per ICH Q3D and USP <233>, ultratrace metals in water and environmental samples and clinical and forensic trace element analysis.
Which standards and certifications apply?
Relevant standards and methods include ICH Q3D Elemental Impurities, USP <233> Elemental Impurities — Procedures, USP <730> Plasma Spectrochemistry, ISO 17294-2 Water quality — ICP-MS determination of elements, US EPA Method 200.8, US EPA Method 6020B and ISO/IEC 17025. Certification candidates for this model are CE, ISO 9001 manufacturing and Nuclear safeguards software option; each is to be confirmed for the specific configuration before shipment, and certificates are supplied only where they have been issued.
ICP-MS requires high-purity argon, a vacuum system with roughing and turbomolecular pumps, stable power and a temperature-controlled room. Interface cones, torch and sample introduction parts wear and must be inspected and replaced, and cone condition affects sensitivity and stability. Contamination is critical at nanogram per litre levels, so clean sample preparation areas, ultrapure acids and dedicated labware are essential. Matrix effects require internal standards, dilution or matrix matching, and high dissolved solids need dilution or a robust interface. Daily tuning, mass calibration and performance checks with a multi-element standard maintain data quality. Add automation and audit trails for regulated environments and monitor collision gas and pump oil.
How do I select the right Multi-Collector ICP-MS Spectrometer?
Select a multi-collector instrument when precise isotope ratios, not just concentrations, are the goal, as in geochronology, provenance or nuclear work. Specify the isotope systems, precision required and whether laser ablation is needed. Confirm mass bias correction strategies and the availability of reference materials for your systems.
How does it compare with other ICP-MS variants?
Select an ICP-MS configuration by the required detection limits, the number of elements, the isotope information needed and the matrix. A single quadrupole with a collision cell handles most routine ultratrace work economically. A triple quadrupole adds reaction-cell mass selection for difficult interferences and low-level sulfur, phosphorus and halogens. High-resolution sector field instruments resolve spectral overlaps and offer higher sensitivity for semiconductor and geochemical work. Multicollector instruments provide the precision needed for isotope ratio studies. Time-of-flight instruments capture the full mass spectrum for rapid multi-element or single-particle analysis. Laser ablation adds direct solid sampling. Match the sample introduction, collision gas and software to your matrices and regulatory requirements.
Full specifications
| Mass range | 2–260 amu |
|---|---|
| Isotope ratio precision | a few ppm or better |
| Detectors | faraday cups and ion counters |
| Analyzer | magnetic sector |
| Resolution | low to high variable |
| Plasma power | 1500–1600 W |
| Argon consumption | 15–20 L/min |
| Sample introduction | liquid or laser ablation |
| Detector positions | up to 16 faraday cups |
| Interface | Ethernet |
Indicative values for this product class. Final specifications are confirmed on the quotation and in the calibration documents supplied with the instrument.
Applications
- Uranium-lead and rubidium-strontium geochronology
- Provenance and forensic isotope fingerprints
- Nuclear safeguards and material accountancy
- Environmental and nutritional tracer studies
Key features
- Array of faraday cups and ion counters
- Simultaneous multi-isotope collection
- Isotope ratio precision to parts per million
- Optional collision cell for calcium and iron
- Liquid or laser ablation sample introduction
- Careful mass bias and matrix correction
Frequently asked questions about Multi-Collector ICP-MS Spectrometer
Plasma signal fluctuates on a short timescale, and sequential measurement of isotopes would capture these fluctuations as ratio errors. Collecting all isotopes at once from the same ion beam cancels the fluctuation, giving precision that scanning instruments cannot reach.
Mass bias arises because heavier and lighter isotopes are transmitted and detected with slightly different efficiency. It is corrected using an internal isotope pair with a known ratio, by sample-standard bracketing, or by a combination. Correction method and frequency are defined in the method and validated with reference materials.
Yes, it can measure concentrations, usually by isotope dilution, which is among the most accurate calibration approaches because the isotopically enriched spike corrects for recovery and matrix effects. The instrument's strength remains high-precision ratios rather than routine multi-element concentration screening.
Plasma and matrix species form polyatomic ions that share mass with analyte ions, such as argon chloride with arsenic and argon argon with selenium. A cell filled with helium or a reactive gas removes or shifts these interferences before mass analysis, lowering background and improving accuracy at ultratrace levels.
Elements such as mercury, iodine and boron stick to tubing and cones, causing carry-over. Rinsing with dilute acid, adding complexing agents such as gold or ammonia to rinse solutions, and running blanks between samples control memory effects. Method development defines rinse time and composition for each problematic element.
Common internal standards are lithium-6, scandium, germanium, rhodium, indium, terbium, holmium and bismuth, chosen to bracket the mass range of the analytes. They correct for signal drift, matrix suppression and nebulization differences. The standard must not be present in the sample and should have similar ionization behavior.
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