Exact(24)
If we apply this notion to receptive profiles (1), we obtain the following.
Reconstruction profiles 1 show that MRI-IR improves edges visible in the MRI but degrades the tumours.
Section profiles 1 and 2 are based on lines labeled "profile 1" and "profile 2" in the two upper images.
Due to the spatially variable overlap width, the length of the transition zone differs for each profile (3.6 meters and 4.8 meters for profiles 1 and 2 respectively).
Hence, the contamination inferred within these zones along profiles 1 and 3 might be the result of percolating leachate from the topsoil.
For profiles 1 and 2, which describe achievement below the PIRLS/TIMSS Low International Benchmarks, a relative strength in mathematics is observable.
Similar(36)
Fig. 9 Temperature-dependent thermal conductivity models for profiles 1 12.
Profiles 1 6 have the most complex geometry with one additional 'Greta' coal layer overlain by the Permian coal layer.
The profiling was run from northwest to southeast, with length of survey line being 98, 36 and 145 m for profiles 1 3.
Here, we introduce an implementation of interaction profiles [1] based on Structural Interaction Fingerprints (SIFt) [2], which allow precise and rapid binding site description.
White dashed lines refer to local geothermal gradients showcased in Fig. 11 Fig. 10 Non-temperature-dependent (constant) thermal conductivity models for profiles 1 12.
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