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A total 600 consecutive sweeps each lasting 200 ms were collected and sampled at 4,000 Hz.
A total of 600 consecutive sweeps (sweep duration, 200 ms) were collected and sampled at 4000 Hz.
A total of 600 consecutive sweeps each lasting 200 ms were collected and sampled at 4,000 Hz.
Additionally, 3D 1H-15N and 1H-13C NOESY-HSQC spectra with mixing times of 120 ms were collected to generate distance restraints.
For each of the three stimulation paradigms a total of 600 consecutive sweeps of 240 ms were collected and sampled at 512 Hz.
During continuous median-nerve stimulation at the wrist, 500 sweeps (sweep duration, 50 ms) were collected and sampled at 5000 Hz.
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A high-resolution 3D MPRAGE dataset (1 mm isotropic resolution, linear phase encoding order, TE/TR 3.7/8.13 ms, FA = 8°, TI = 960 ms) was collected at 3T.
Continuous core samples from three vertical sites located over a maximum spatial distance of 65 m were collected and analyzed for particle size distribution, porosity, and water content.
A series of short cores (ca. 0.5 m) were collected from the intertidal zone and reclaimed lowlands of Greatham Creek in the Tees estuary.
Soil cores (as deep as 13 25 m) were collected at each of the four landscape positions along the two transects for the determination of soil water contents, root distributions, and soil tritium contents.
To close this knowledge gap, non-salt-affected and salt-affected soils (0 0.30 m) were collected from two agricultural regions: in India (irrigation induced salinity) and in Australia (salinity associated with ground water or non-ground water associated salinity).
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