Suppression of Matrix Effects in ICP‐MS by High Power Operation of ICP: Application to Precise Determination of Rb, Sr, Y, Cs, Ba, REE, Pb, Th and U at ng g‐1 Levels in Milligram Silicate Samples

Wiley - Tập 21 Số 2 - Trang 307-319 - 1997
Akio Makishima1, Eizo Nakamura1
1The Pheasant Memorial Laboratory for Geochemistry and Cosmochemistry, Institute for Study of the Earth's Interior, Okayama University at Misasa, Misasa, Tottori‐ken 682‐01, Japan

Tóm tắt

We found that the suppression of signals for 88Sr, 140Ce and 238U in rock solution caused by rock matrix in ICP‐MS (matrix effects) was reduced at high power operation (1.7 kW) of the ICP. To make the signal suppression by the matrix negligible, minimum dilution factors (DF) of the rock solution for Sr, Ce and U were 600, 400 and 113 at 1.1, 1.4 and 1.7 kW, respectively. Based on these findings, a rapid and precise determination method for Rb, Sr, Y, Cs, Ba, REE, Pb, Th and U using FI (flow injection)‐ICP‐MS was developed. The amount of the sample solution required for FI‐ICP‐MS was 0.2 ml, so that 1.8 mg sample was sufficient for analysis with a detection limit of several ng g‐1. Using this method, we determined the trace element concentrations in the USGS rock reference materials, DTS‐1, PCC‐1, BCR‐1 and AGV‐1, and the GSJ rock reference materials, JP‐1, JB‐1, ‐2, ‐3, JA‐1, ‐2 and ‐3. The reproducibilities (RSD %) in replicate analyses (n=5) of BCR‐1, AGV‐1, JB‐1, ‐2, ‐3, JA‐1, ‐2, and ‐3 were < 6 %, and typically 2.5%. The difference between the average concentrations of this study for BCR‐1 and those of the reference values were < 2%. Therefore, it was concluded that the method can give reliable data for trace elements in silicate rocks.

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Tài liệu tham khảo

10.1016/0016-7037(89)90286-X

Ando A., 1989, 1988 values for GSJ reference samples, “Igneous rock series, Geochemistry Journal, 23, 143

10.1111/j.1751-908X.1987.tb00023.x

10.1016/0584-8547(87)80024-1

10.1016/0009-2541(92)90043-5

10.1016/S0009-2541(96)00100-3

10.1111/j.1751-908X.1993.tb00122.x

10.1021/ac00165a024

Govindaraju K., 1989, 1989 compilation of working values and sample description for 272 geostandards, Geostandards Newsletter, 13, 1, 10.1111/j.1751-908X.1989.tb00476.x

10.2343/geochemj.29.91

10.1111/j.1751-908X.1992.tb00494.x

10.5479/si.00810274.27.1

10.1016/0009-2541(90)90142-T

10.1007/978-94-011-3046-2

10.1016/0009-2541(90)90145-W

10.1029/JB095iB03p02661

10.2116/analsci.3.305

10.5702/massspec.38.241

10.1016/0009-2541(90)90143-U

10.1093/petrology/32.5.1021

RuzickaJ.andHansenE.H.(1983)Flow Injection Analysis Kagakudouzin (Kyoto) 222pp (Japanese translation).

10.1111/j.1945-5100.1995.tb01166.x

SunS.‐S.andMcDonoughW.F.(1989)Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In:SaundersA.D.andNorryM. J.(eds) Magmatism in the Ocean Basins Geological Society Special Publication No.42 313–345.

10.1039/an9871201223

10.1016/0009-2541(92)90042-4

Yoshida T., 1992, Determination of trace and ultra‐trace elements in thirty two international geostandards by ICP‐MS, Ganko, 87, 107

Yoshikawa M., 1993, Ganko, 88, 548