Sentence examples for mercury core from inspiring English sources

Recent laboratory measurements for iron suggested a thermal conductivity of 113 125 W m−1 K−1 for Mercury core pressure and temperature conditions and a heat flow along the adiabat of 45 100 mW m−2 (Deng et al. 2013).

Inject mercury into the core at an initial pressure of 0.3 MPa.

Team members on the MESSENGER mission orbiting Mercury with some help from Earth-based radar scientists—are reporting that Mercury's iron core is even larger than had been previously thought.

Table 2 No. of core in mercury-injection experiment Different stages during water flooding No. of core in Well LN103 No. of core in Well GJ315-7 Non-water flooding L1-1 G2-1 Water cut of 60%L1-2L1-2G2-2G2-2 cut of 80% L1-3 G2-3 Water cut of 90%L1-4L1-4G2-4G2-4

Spatial heterogeneity in peat surface characteristics (0 34 cm) was identified by measuring total mercury in eight peat cores (57 ± 8 ng g−1, average ± SE), vascular plant coverage (32 52%), water table level (4.5 14.1 cm) and dissolved gaseous elemental mercury concentrations (28 51 pg L−1) in the peat water.

Although, our technique already considered the conformance correction as suggested by previous authors (e.g. Comisky et al. 2007); it is clear that additional work is required in characterising and improving the precision of methods for estimating permeability of tight cores using mercury injection tests.

It is generally accepted that Mercury has an iron-rich core.

Samples were taken from core supplied by Mercury NZ Limited and Tauhara North No. 2 Trust.

Open image in new window Fig. 6 Plots of capillary pressure versus mercury saturation for the carbonate core samples 1 and 2. The red and blue colours represent vertically and horizontally obtained samples, respectively.

The dash and thick lines represent the uncorrected and conformance corrected data, respectively Open image in new window Fig. 9 Normalised pore-size distribution (PSD) for samples 3 and 4 Open image in new window Fig. 10 Plots of capillary pressure versus mercury saturation for the carbonate core samples 6 and 7.

We analyzed the capillary pressure under the conditions of different injection velocities by conventional mercury injection tests with four cores of similar physical properties as the previous waterflooding tests.