High-sensitivity and high-precision (2 SD ≤ 0.06‰)
measurement of chromium (Cr) isotopes at the 10 ng level was successfully
carried out using double spike multiple-collector inductively couple
plasma mass spectrometry (MC-ICP-MS). To enhance the signal sensitivity
and stability, the Aridus II desolvating nebulizer system was improved
by placing its waste gas trap bottle in an ice chamber (5 °C
cold trap). This setup, beyond Cr isotope analysis, can be applied
to most heavy metal isotope measurements. The sensitivity of the 52Cr signal is ≥300 V mg–1 L (with
a 1011Ω amplifier and a 110 μL min–1 uptake rate), an enhancement of ≥1.5 times compared to the
Aridus II without the cold trap. In addition, the relative standard
deviation of the 52Cr signal varied ≤4% over 8 h,
demonstrating high stability. The δ53Cr values of
common geological reference materials determined using 10 ng of Cr
are in excellent agreement with results measured at 25 ng and 50 ng
and are consistent with previous determinations, validating the accurate
and precise Cr isotope ratio measurements. An empirical method is
proposed to correct for the residual (after subtraction) effect of
Fe interference on δ53Cr determination. This method
relies on a linear relationship between the [Fe]/[Cr] and δ53Cr shift within one analytical session. Finally, we report
the δ53Cr values of 19 new reference materials, ranging
from −0.44‰ to 0.49‰. Among them, GSS-7 (−0.44
± 0.02‰, 2 SD, n = 5), GSS-4 (0.48 ±
0.02‰, 2 SD, n = 5), and GSD-10 (0.49 ±
0.05‰, 2 SD, n = 5) can be used as candidate
reference materials for interlaboratory comparisons to complement
existing ones that are mostly isotopically unfractionated from the
bulk silicate earth.