TY - JOUR
T1 - The rapid heating, defocused beam technique
T2 - A CO2-laser-based method for highly precise and accurate determination of δ18O values of quartz
AU - Spicuzza, M. J.
AU - Valley, J. W.
AU - Kohn, M. J.
AU - Girard, J. P.
AU - Fouillac, A. M.
PY - 1998/2/26
Y1 - 1998/2/26
N2 - We describe a laser fluorination technique specifically for quartz that allows both high-accuracy and high-precision determination of oxygen isotope ratios, regardless of grain size. The rapid heating, defocused beam technique (RHD) utilizes a defocused 32 W CO2 laser at full power which delivers 17 W (∼ 20 W/mm2) to the sample to quickly react quartz. In contrast, other recent laser fluorination studies use a tightly focused laser beam and slow heating (i.e. Sharp and Kirschner, 1995; Fouillac and Girard, 1996; Kirschner and Sharp, 1997), and find laser analysis of fine-grained quartz to be inaccurate. Three quartz standards, NBS-28, QZ-BRA, and QZ-CWRU were analyzed using the RHD technique at the University of Wisconsin to test for grain size effects. RHD analyses show no correlation between grain size and δ18O values and are in excellent agreement with δ18O values obtained using conventional fluorination techniques. Additional analyses of the same quartz standards performed at University of Wisconsin using slow heating and a focused beam yield δ18O values that are both less precise and significantly (up to 0.8‰) lower than the accepted values. Attempts to use the RHD technique with a 20 W CO2 laser which delivers 8 W (∼ 10 W/mm2) to the sample at BRGM were unsuccessful, probably due to insufficient power density of the defocused beam. We conclude that the RHD technique yields excellent accuracy and precision, but that power densities of > 15-20 W/mm2 may be necessary across a large part of the sample surface. We recommend the use of lasers with at least 30 W of power.
AB - We describe a laser fluorination technique specifically for quartz that allows both high-accuracy and high-precision determination of oxygen isotope ratios, regardless of grain size. The rapid heating, defocused beam technique (RHD) utilizes a defocused 32 W CO2 laser at full power which delivers 17 W (∼ 20 W/mm2) to the sample to quickly react quartz. In contrast, other recent laser fluorination studies use a tightly focused laser beam and slow heating (i.e. Sharp and Kirschner, 1995; Fouillac and Girard, 1996; Kirschner and Sharp, 1997), and find laser analysis of fine-grained quartz to be inaccurate. Three quartz standards, NBS-28, QZ-BRA, and QZ-CWRU were analyzed using the RHD technique at the University of Wisconsin to test for grain size effects. RHD analyses show no correlation between grain size and δ18O values and are in excellent agreement with δ18O values obtained using conventional fluorination techniques. Additional analyses of the same quartz standards performed at University of Wisconsin using slow heating and a focused beam yield δ18O values that are both less precise and significantly (up to 0.8‰) lower than the accepted values. Attempts to use the RHD technique with a 20 W CO2 laser which delivers 8 W (∼ 10 W/mm2) to the sample at BRGM were unsuccessful, probably due to insufficient power density of the defocused beam. We conclude that the RHD technique yields excellent accuracy and precision, but that power densities of > 15-20 W/mm2 may be necessary across a large part of the sample surface. We recommend the use of lasers with at least 30 W of power.
KW - Geochemistry
KW - Laser fluorination
KW - Oxygen isotopes
KW - Quartz
KW - Silicates
UR - http://www.scopus.com/inward/record.url?scp=0031822535&partnerID=8YFLogxK
U2 - 10.1016/S0009-2541(97)00131-9
DO - 10.1016/S0009-2541(97)00131-9
M3 - Article
AN - SCOPUS:0031822535
SN - 0009-2541
VL - 144
SP - 195
EP - 203
JO - Chemical Geology
JF - Chemical Geology
IS - 3-4
ER -