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ICP-MS
MC-ICP-MS
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Advantages:
- Rapid Quantitative & Semiquantitative analysis of trace
elements (6Li to 238U)
- Multi-Element Technique
- Small Samples (< 100 mg)
- High Sensitivity
- Excellent Precision & Accuracy
- Reaction Cell Option
Disadvantages
- Destructive Technique
- Sample Homogenization
- Sample Preparation
- Spectral Interferences (many circumvented with Collision
Cell)
Solution ICP-MS analysis requires the introduction of dilute solutions with total dissolved solids (TDS) less than 0.1%. All solutions must be filtered and free of particulates. Solutions should be diluted with 2-3% nitric acid. Method blanks should always be included in submitted sample set.
For plant and soil digestions and extracts in preparation for
Quadrupole ICP-MS analysis, we recommend that you contact ANR
Analytical
Laboratory (http://groups.ucanr.org/danranlab/)
located at UC Davis.
Silicate rocks are
dissolved
by acid digestion. We will dissolve small
sample batches of pre-powdered silicate rocks upon request. Please
email or call for more information.
Silicate Rock Standards:
Tables 1 and 2
show analytical results by ICP-MS 7500a for two basalts, BHVO-1 and
BCR-1, which are geochemical reference standards prepared by the U.S.
Geological
Survey.
We are available for
consultation
regarding methodology and data reduction
Laser
Ablation (LA) ICP-MS
Advantages:
- Rapid quantitative & semi-quantitative trace element
analysis
- Easy sample preparation
- Small sampling area (~100- 5 µm)
- Non-destructive
- Real-time data reduction (with Glitter software)
Disadvantages
- Spectral Interferences (many circumvented with the
collision cell)
- Standards need to be well-matched to unknowns
MC-
ICP-MS
Please contact us at icplab@ucdavis if you have any questions.
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