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Then, given the number of times a species is sampled, it is possible to compute the expected number of singletons contributed by each species in the sample (see Material and Methods).
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For small samples it is possible to design different resonators that have much better power handling properties and higher sensitivity.
However, because of the small number of high-level samples, it is possible that differentiation was based on factors other than metal concentration.
From these samples, it is possible to classify the refractory failure into six zones by utilizing the penetration depth (calculated by area) coupled with simulations of particle trajectories.
The results indicated that, using only optical interferometer and without destroying the worn samples, it is possible to identify the wear mechanisms.
By measuring the decreased intensity through a fixed-path-length cell containing the sample, it is possible to determine the concentration of the sample.
For a random sample, it is possible to deduce the form of the function φ that describes the average contribution to the shift produced by a chain making angle θ to the axis of stress.
There are about thirty planktonic species in all, and each thrives at a different temperature, so that by counting a species' prevalence in a given sample it is possible to estimate the ocean temperatures at the time the sediment was formed.
In some samples, it is possible to use the compositions of the porphyroblasts to calculate the depth and temperature conditions at which they grew and thereby constrain the conditions at which deformation occurred.
If no surfactant is intentionally added to the sample, it is possible that the protein of interest may itself act as a surfactant.
We have successfully shown that, through several different fabrication cycles using different samples, it is possible to produce consistent values of resonance Q-factor and resonance frequency.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com