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Examination of DSDP/IPOD samples represents a major commitment to oceanic crustal studies.
The "well graded" curve (INL soil samples) represents a non-uniform soil with a wide range of particle sizes that are evenly distributed (Figure 5).
On the other hand, the upper boundary of 200 samples represents a very lenient scheme for compressive sampling since it represents approximately 78% of the original samples.
The neon isotopic content of these mantle-derived samples represents a non-atmospheric source of neon.
Further, pooling of the RNA samples represents a cost effective transcriptomic approach to build an EST database for closely related species of a non-model organism.
In the equine setting, the accumulation of large numbers of samples represents a significant challenge.
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Sample grain is 20 m × 20 m, and the extent of 106 samples represents an area of 400 km2.
All of the samples represented a preferred Au (1 1 1) orientation.
The samples represented a combination of depth-based sampling (0 5 cm) and horizon-based sampling (O, A and C horizons) with 123 different depths identified.
These samples represent a composite of sites (Table S1) from the region where the δ13C signal remains consistently sensitive to sunlight intensity during the summer (June August) growing season27.
The clay and SOM prediction equation was validated against a combined data set with 227 soil samples representing A, B, and C horizons from temperate North America and Europe.
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