Sentence examples for 2 fine from inspiring English sources

Table 4 Particle-size distribution of soils collected from the O/A horizon (0 10 cm) at 3 topographic positions Topographic Particle size (μm) position Very fine (< 2) Fine (2 53) Medium (53 250) Coarse (>250) Summit 1.6 19.8 17.5 61.0 Footslope 2.1 15.1 18.2 64.5 Lakeshore 1.1 6.0 9.5 83.3 Data are percentages.

On the Guatemalan Pacific piedmont and in Tabasco, two specialized ceramic traditions (both of which began in Late Classic times) evolved: (1) plumbate (so called because of its slip, which had an unusually high iron content in the natural clay that fired to a lead-colour glaze); and (2) Fine Orange (so called because of its fine-grained, temperless paste).

Macroscopically, a well-circumscribed mass in the right lobe of the thyroid is observed (d) Fig. 2 Fine needle aspiration smears.

By checking the microstructures and distribution of elements in those conditions, the enhanced power durability can be attributed to: 1) using of Cu layer, 2) fine grain strengthening, 3) solution strengthening.

These fine particles are most likely (1) soot emitted by a denser traffic an indirect consequence of the affluence and (2) fine acidic and S-rich particles such as ammonium sulphate.

Treatments were administration of FA at the rate of 600 g/d in the form of: (1) coarse CS in the rumen; (2) fine CS in the rumen; (3) TG in the rumen; and (4) TG in the abomasum for 14 days.

The maximum hardness is observed on the sections of the HAZ 1 (coarse-grained) and 2 (fine-grained) adjacent to the weld metal, having an acicular structure.

The Permian Ripon Formation contains siltstone and three distinct sandstone lithologies: (1) very fine-grained sandstones, (2) fine-grained sandstones, and (3) medium-grained sandstones.

(2) Fine-tuning In the back-propagation, the traditional detection networks, e.g., RCNN or SPPnets, are highly inefficient because the number of RoIs is large and the entire image also is processed when each RoI needs to be retrained.

The micropores were present between (1) the micrites of carbonate lime mud (yellow arrow), (2) fine-grained calcite as the result of microborings from calcareous sponges of coarser carbonate organisms (orange arrow), and (3) neoform fine-grained calcite existing as geopetal filling in the preexisting chamber inside ooids and forams (red arrow).

Mapping was performed in three steps: (1) identification of QTL in a small F2 population, (2) fine-mapping of these QTL in a larger F2 population, and (3) verification of the QTL in a commercial line, Hy-Line.