Sentence examples for floor surface sample from inspiring English sources

In both the samples from floor surface (sample 5) and −20-cm level (sample 16), Fe-Ti oxide minerals are present.

It is clearly recognized that the minerals in approximately 10 nm size are abundant in the floor surface sample (sample 5) while those in approximately 1 to 10 μm size are dispersed in the −20-cm level samples.

Six successful results were obtained from the floor surface samples by the selection criteria.

The floor surface samples are all reddish (Figure 3b) whereas the −20-cm level ones are all grayish (Figure 3c).

For the floor surface samples, NRMs are probably full TRMs and the comparison seem to result in the accurate archeointensities.

The points originated from the floor surface samples (red triangles) tend to lie closer to the SD region than those from the −20-cm level samples (gray circles).

Difference in the 'baking' temperatures between the floor surface samples and the −20-cm level samples would probably also cause the differences in the rock magnetic characters.

From the view of the rock magnetic properties, the floor surface samples seem to be much more preferable for high-fidelity archeointensity researches.

The floor surface samples yielded the successful archeointensity results fairy consistent with the in situ geomagnetic field, and thus the built-in correction seemed to work well.

However, without such corrections, we obtained the archeointensity results fairy consistent with the in situ geomagnetic field from the floor surface samples.

In actual, laboratory-imparted ARMs of the −20-cm level samples resulted in the intensities one order of magnitude smaller than those of the floor surface samples (Table 1). Figure 5 Representative thermomagnetic curves.