ginner (like me), a very good
review for practical as well as theoretical issues is "Analysis of soils and
minerals using X ray absorption spectroscopy" (Kelly et al. 2008).
Good luck,
Hana
*
> Thank you very much.
&g
when sum of components is
different
than one in these heterogeneous soil samples (with unknown composition and
probably high effect of disorder)?
2. Any reason not to constrain all fractions to be positive?
Thanks,
Hana
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>
>
Why don't you ask Sam Webb at SSRL about it? Sixpack is his 'baby':
samw...@slac.stanford.edu
Best,
Hana
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h the same steps size, and a calibration standard was used)?
2. For harder situation; when different steps were used - I found that sixpack
(according to its manual) interpolating all spectra to the same energy grid -
does this solve the problem?
I will be happy to be advised. Thanks,
Dear list experts,
Here is another challenging question for me; can someone help?
I have soil samples, trying to fit the first shell, I have 3 different optional
bond lengths, which might give a lot of information. Now I have two questions:
1. If I do not know of specific structure (XRD implies a
OK, so I lost my freedom, but got some wisdom... in case of a mix of complex
unknown material, it might be fatal I guess.
Thanks Scott!
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Scott Calvin writes:
>
> Hi Hana,
> > On Jun 27, 2011, at 2:04 PM, Hana wrote:
> > > I guess my question is obvious to most of you, but after some
> > practice and reading, the following is still unclear to me
> > (hopefully some other beginner
I guess my question is obvious to most of you, but after some practice and
reading, the following is still unclear to me (hopefully some other beginners
will benefit): Normally I have calibrated my spectra using a calibration foil –
so energy shift was done according to that companion standard.
to my understanding?
specifically, I am trying to compare my measurements(collected at 10K) to
literature data of these metals adsorbed on iron oxides (collected at room
temperature).
I would appreciate any advise,
Hana
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If