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Major and trace elements were measured with inductively coupled plasma and mass spectrometry (ICP MS) in the filtered and acidified water samples within 2 weeks after sampling (Table 2).
Elements were measured with an integration time of 0.3 0.5 s per increment.
Finally, the insertion times (T) of the intact Wukong elements were measured with the equation T = K/2r, where r measures an average nucleotide substitution rate, which has been set to 1.3×10−8 substitutions per site per year, as proposed previously (Ma and Bennetzen 2004).
Similar(57)
The similarity of the different elements is measured, with consideration of syntactic, semantic, and structural aspects.
The leaching of Ce and Mg elements was measured with an AAnalyst atomic absorption spectrometer (PerkinElmer, USA) using a nitrous oxide/oxygen acetylene flame.
Concentrations of 20 trace elements were measured within 20%% error estimates, with respect to the reference values of GSD-1G and BHVO-2G (Fig. 4).
Between 17 and 19 elements were measured for each population, with both macro- and microelements represented.
Characteristic valences for the elements were measured in terms of the number of atoms of hydrogen with which an atom of the element can combine or that it can replace in a compound.
A total of 48 elements were measured.
Trace-element concentrations were measured with an inductively coupled plasma mass spectrometer (ICP-MS: ELAN DRC II, Perkin Elmer) after sample decomposition with HF-HNO3.
Major element concentrations were measured with an X-ray fluorescence spectrometer (XRF: MagiX PRO, Spectris) using the conventional glass bead method.
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