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Partition coefficients between fluids and melts of element i ( D i fluid / melt ) were calculated using PyMCA software (Solé et al. 2007).
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The enthalpy of melting was calculated as the area defined by the heat flow curve and base line between the points of onset and end of the endothermic effect on the heat flow curve.
The H2O content of the melt was calculated by mass balance calculation of all phases assuming that water was concentrated in only the melt.
Glacial melt is calculated in "mass balance," a measure of how much ice has been gained or lost.
Daily melt was calculated by the positive degree day algorithm66 using degree day factors for Satujökull, Iceland67, 5.6 mm d−1 °C−1 for snow and 7.7 mm d−1 °C−1 for ice.
For the fast and slow recombination reaction rates an acidic and basic melt was calculated respectively in the cathode in an operating MCFC.
During the isothermal crystallization, relative crystallinity increased with crystallization time, following an Avrami equation with exponent n ≈ 2. The fold surface free energy for the copolymer crystallized from the melt was calculated to be 73 erg cm−2, about 24 erg cm−2 higher than that of pure PEEK.
Assuming magmatic temperatures of 925°C, the viscosity of the melt is calculated to be 103.3−3.
Partition coefficients between the aqueous fluids and melts were calculated for Pb, Rb, and Sr ( D Pb, Rb, Sr fluid / melt ).
Surface tensions of melts are calculated as a function of x from the P-V-T data for the liquid state using the theory of Prigogine and Patterson.
For the second inclusion, the volume fraction of aqueous fluid at final clathrate melting was calculated to vary between 85 and 81%.
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