HI John-- We've run polyethylene foil (PEF-1, <100ug) then biotite (NBS-30, ~2mg) for D/H, and saw ca. -103 and -69 respectively (sorry, no statistics on hand right now, but std dev < 3 per mil if I recall correctly). In both cases, we got clean peaks 3 to 6 V on mass 2 (1 to 2 V on mass 3)--run a DeltaPlus XP. Newly packed reactor w/ crucible run at ~1450, with 8 min run times to let the CO peak level out (sample drop ~70 sec, switch to CO at ~170 just to follow it, not for isotopes). take care gerry John Dilles wrote: > Hi all > > We have been restandardizing for D/H mineral analyses on our TCEA unit > (running at 1450°C) connected to a CF mass spec in Alan Mix's lab. In > parallel the U of Oregon lab has been doing the same. We have run into > a problem in that biotite standards are yielding different D/H ratios > compared to one muscovite standard. We are using NBS-30 biotite > (nominal values something between -65 and -67 ”) and as a primary > standard, and Misasa sericite/muscovite (Kusakabe, person commun. > 2007; -59.1 ± 0.3 (2 std error of mean) as a secondary standard. > > Both the OSU and U of O labs have gotten results for H2 gases derived > from Misasa sericite that are isotopically lighter than the gases > derived from NBS-30 biotite. > > For example, in a 2005 run, using NBS -30 as a nominal standard, we got: > > NBS-30 Biot Misasa Sericite > accepted value (~-66”) (-59”) > measured -67.3±2.9 -73.6±1.4 > analyses n=4 n=5 > > I am puzzled because the Misasa sericite is a well-behaved standard > according to Dr. Kusakabe, and in our experience running it for > several years as a secondary standard in our conventional D/H lab > (using a 1400°C resistance furnace, and U reduction of water to H2). > > So far, our working hypothesis is that in the TCEA, the H2 gas > liberated from biotite at 1450°C has a significantly different offset > (fractionation?) from original biotite, compared to H2 gas liberated > from muscovite. Maybe this has something to do with Fe-bearing minerals? > > Anyone else seen this, or have any suggestions for an explanation? > > Cheers, > > JOHN Dilles >