Sentence examples for dryness coefficient from inspiring English sources

By contrast, Es4 gas is dry with an average dryness coefficient of 0.970 and displays the typical characteristics of coal-type gas from Carboniferous-Permian coal measures.

In contrast to the thermogenic gas model, the gas shows a negative relationship of δ13C2 to both the δ13C1 and the dryness coefficient.

In this type of gas mixture, the dryness coefficient floats around 0.95, the n-heptane content varies from 50%to70%0%, the methylcyclohexane content varies from 30%to50%0%, and the δ13C2 values vary from −26‰ to −28‰.

The results show that the dryness coefficient of the natural gas ranges between 0.71 ∼ 0.93, δ13C values range between −45.3 ∼ −38.0‰ in methane, −32.0 ∼ −25.6‰ in ethane and −30.0 ∼ −25.3‰ in propane.

The hypothesis is supported by (1) roughly a positive correlation between the gas dryness coefficient and methane δ13C1 value, (2) significantly heavier δ13C1 values in the eastern part of the study area than in the west, and (3) significantly heavier δ13C1 values than anticipated for unaltered gas co-generated with C2 C4.

Most of the gases in the middle and eastern part of the No. 1 fault-slope zone are characterized by high gas dryness coefficients and have methane δ13C1 values heavier than primary gas.

The results indicate that Es3M gas is predominantly oil-type gas and that Es3L gas is mainly mixed gases dominated by coal-type gas, with average dryness coefficients (C1/C1 5) of 0.877 and 0.920, respectively.

The charge and mixing of the dry gas into the Ordovician pools may have resulted in increase in wax contents of the oils, gas/oil ratios, gas dryness coefficients and methane δ13C values, leading to a positive correlation between gas/oil ratio and paraffin wax content as a result of continuous fractionation and removal of light components of an oil with progressive gas influx and thus gas washing.

The combined analysis of these curves yields the pressure dependencies of local cake dryness, specific cake resistance, and consolidation coefficient in the wide range of solid pressure (5×103 5×105 Pa).

Similarly, variation of dryness fraction, local boiling two phase flow coefficient, and total pressure drop can be predicted for two phase region.

A significant correlation coefficient between the prevalence of antibodies to toxoplasma and dryness during late summer was reported.