

High-Resolution Sector Field ICP-MS
高分辨扇形磁场电感耦合等离子体质谱仪
- SKU IMS-0003
- ICP-MS
- CE (to be confirmed)
- ISO 9001 manufacturing (to be confirmed)
- IEC 61010-1 safety (to be confirmed)
Price on request — FOB / CIF quoted per order
Prices depend on configuration, quantity and destination port.
Key specifications
| Mass range | m/z 2–250 |
|---|---|
| Resolution settings | ~300 / 4000 / 10000 (10% valley) |
| Sensitivity (In 115, low resolution) | ≥ 1×10^9 cps/ppm |
| Sensitivity (In 115, high resolution) | ≥ 1×10^7 cps/ppm |
| Detection limit (Pb, U, low resolution) | < 0.05 ppt |
| Background | < 0.2 cps |
By Lab Manufacturers China Technical TeamLast reviewed Standards: USP <233> Elemental Impurities Procedures, ICH Q3D Elemental Impurities, EPA Method 200.8
What is the High-Resolution Sector Field ICP-MS?
A sector field ICP-MS uses a magnetic and electrostatic sector to separate analyte ions from interferences by resolving power up to 10000. It gives the lowest backgrounds and ppq-level detection limits, and is used for ultra-trace semiconductor, geochemical, nuclear and isotope ratio work.
What is the High-Resolution Sector Field ICP-MS?
A sector field ICP-MS uses a magnetic and electrostatic sector to separate analyte ions from interferences by resolving power up to 10000. It gives the lowest backgrounds and ppq-level detection limits, and is used for ultra-trace semiconductor, geochemical, nuclear and isotope ratio work.
Overview
A double-focusing sector field ICP-MS combines an electrostatic analyzer with a magnet to separate ions by mass and energy. Resolution is switched between low (R of about 300), medium (R of about 4000) and high (R of about 10000), allowing many polyatomic interferences, such as 40Ar16O on 56Fe or 40Ar35Cl on 75As, to be resolved physically rather than chemically. Because the mass filter passes ions with flat-topped peaks, isotope ratio precision reaches 0.01 to 0.05 percent RSD in some models. Detection limits reach the parts-per-quadrillion range for many elements, and background is below 0.2 cps. Sensitivity drops with higher resolution settings, with about a 100-fold loss at R of 10000. Multi-collector versions provide ultimate isotope-ratio precision for geochronology. The instruments are larger, slower at scanning, and costlier than quadrupole systems.
How does it work?
In ICP-MS, a liquid sample is nebulized into a fine aerosol, passes through a spray chamber, and is carried by argon into a plasma torch. A radio-frequency coil at 27 or 40 MHz sustains a plasma at about 6000 to 10000 K, which desolvates, atomizes and ionizes the analytes, mostly as singly charged ions. Ions are extracted through sampler and skimmer cones into a high-vacuum region, focused by ion lenses, and separated by a mass analyzer, most commonly a quadrupole. A collision or reaction cell removes polyatomic interferences such as 40Ar16O on 56Fe, using helium kinetic energy discrimination or reactive gases. An electron multiplier in pulse and analog modes counts ions across up to nine orders of magnitude.
What are the key features?
- Double-focusing magnetic and electrostatic sectors with selectable resolving power up to 10000
- Flat-topped peaks giving excellent isotope ratio precision for geochronology and tracer work
- Background below 0.2 cps enabling ppq detection limits in clean solutions
- Fast electrostatic scanning (E-scan) for quick multi-element acquisition at fixed magnet field
- Dual-mode detector with a wide dynamic range up to nine orders of magnitude
- Cleanroom-compatible sample introduction options with PFA inert kits for ultrapure acids
What are the technical specifications?
A typical high-resolution sector field icp-ms configuration offers mass range of m/z 2–250, resolution settings of ~300 / 4000 / 10000 (10% valley), sensitivity (In 115, low resolution) of ≥ 1×10^9 cps/ppm, sensitivity (In 115, high resolution) of ≥ 1×10^7 cps/ppm, detection limit (Pb, U, low resolution) of < 0.05 ppt and background of < 0.2 cps. 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 High-Resolution Sector Field ICP-MS is used in ultra-trace metals in semiconductor chemicals, isotope ratio measurement in geochemistry, nuclear material and environmental safeguards analysis, clean-room and ultrapure water monitoring and elemental analysis of high-purity reagents. Across the wider ICP-MS class, laboratories also deploy it for heavy metals in drinking water and wastewater, elemental impurities in pharmaceuticals and toxic elements in food and beverages.
Which standards and certifications apply?
Relevant standards and methods include USP <233> Elemental Impurities Procedures, ICH Q3D Elemental Impurities, EPA Method 200.8, EPA Method 6020B, ISO 17294-2, ASTM D5673, EN 15763, GB 5009.268, ISO/IEC 17025 and IEC 61010-1. Certification candidates for this model are CE, ISO 9001 manufacturing and IEC 61010-1 safety; 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, typically 99.996 percent or better, with consumption around 15 to 20 L per minute, plus cooling water or a recirculating chiller, dedicated exhaust ventilation and stable power. Use trace-metal-grade acids, low-blank labware such as PFA or FEP, and ultrapure water at 18.2 MΩ·cm. Tune daily for sensitivity, oxide ratio (CeO/Ce below 2 percent) and doubly charged ratio (Ce++/Ce below 3 percent). Clean or replace cones, torch and nebulizer according to matrix load, and check the peristaltic pump tubing regularly. Use internal standards to correct drift. For pharmaceutical and regulated work, require software with audit trails and follow USP <233> and ICH Q3D method validation.
How do I select the right High-Resolution Sector Field ICP-MS?
Select a sector field ICP-MS when physical resolution of interferences, sub-ppt backgrounds or high-precision isotope ratios are required. For routine regulatory metals, a quadrupole system is more economical. In an RFQ, specify resolution settings, sensitivity at each setting, background, isotope ratio precision and cleanroom-compatible introduction kits.
How does it compare with other ICP-MS variants?
Choose the ICP-MS class by interference severity, detection limit and budget. A single quadrupole with a collision cell handles most water, food and clinical work at low cost. Triple quadrupole ICP-MS/MS adds mass-shift reaction chemistry for difficult interferences such as sulfur, phosphorus, arsenic in chloride and rare earth oxides. Sector-field instruments offer high resolution and the lowest background for semiconductor and geochemical work, and TOF systems capture the full mass spectrum for fast transient signals. Check matrix tolerance, for example total dissolved solids up to 0.2 percent or aerosol dilution options for higher levels, argon consumption, sample introduction kits, autosampler and software compliance features. Verify the detection limits and background equivalent concentrations in your own matrix rather than relying on deionized water values.
Full specifications
| Mass range | m/z 2–250 |
|---|---|
| Resolution settings | ~300 / 4000 / 10000 (10% valley) |
| Sensitivity (In 115, low resolution) | ≥ 1×10^9 cps/ppm |
| Sensitivity (In 115, high resolution) | ≥ 1×10^7 cps/ppm |
| Detection limit (Pb, U, low resolution) | < 0.05 ppt |
| Background | < 0.2 cps |
| Isotope ratio precision (107Ag/109Ag) | ≤ 0.05% RSD |
| Abundance sensitivity | < 1×10^-6 (at low resolution) |
| Detector dynamic range | ~9 orders of magnitude |
| Argon consumption | ~16–18 L/min |
Indicative values for this product class. Final specifications are confirmed on the quotation and in the calibration documents supplied with the instrument.
Applications
- Ultra-trace metals in semiconductor chemicals
- Isotope ratio measurement in geochemistry
- Nuclear material and environmental safeguards analysis
- Clean-room and ultrapure water monitoring
- Elemental analysis of high-purity reagents
Key features
- Double-focusing magnetic and electrostatic sectors with selectable resolving power up to 10000
- Flat-topped peaks giving excellent isotope ratio precision for geochronology and tracer work
- Background below 0.2 cps enabling ppq detection limits in clean solutions
- Fast electrostatic scanning (E-scan) for quick multi-element acquisition at fixed magnet field
- Dual-mode detector with a wide dynamic range up to nine orders of magnitude
- Cleanroom-compatible sample introduction options with PFA inert kits for ultrapure acids
Frequently asked questions about High-Resolution Sector Field ICP-MS
A resolving power of about 2500 separates 40Ar16O+ from 56Fe+, so medium resolution of around 4000 on a sector field instrument resolves this interference fully. Quadrupole instruments need collision or reaction cell chemistry instead.
Higher resolution uses narrower slits so fewer ions pass to the detector. Sensitivity drops by about one to two orders of magnitude at R of 10000 compared with low resolution. The gain is resolution of interferences that would otherwise raise background or bias results.
It is technically suitable but usually not economical. Its strength lies in ultra-trace and isotope work. Routine drinking water methods such as EPA 200.8 are met by quadrupole systems, which are cheaper, faster and simpler to operate and maintain.
ICP-MS typically reaches low parts-per-trillion (ng/L) detection limits for most elements in clean aqueous solutions, and sub-ppt for some heavy elements. Real-world limits are higher because of sample dilution, blank contamination and matrix effects, so they must be established by method validation.
ICP-OES measures light emitted by excited atoms and ions, reaching ppb detection limits over a wide linear range and high matrix tolerance. ICP-MS measures ions by mass, reaching ppt limits, and provides isotope information, but it tolerates fewer dissolved solids and costs more to operate.
In helium kinetic energy discrimination mode, larger polyatomic ions collide more often with helium and lose more energy than analyte ions, so a bias voltage blocks them. Reactive gases such as oxygen or ammonia can instead convert the analyte or the interference to a different mass.
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