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The crystallization onset temperature of the matrix rises for about 5 °C when crystallizing from the quiescent melt.
Upon crystallizing from solution, certain compounds form cages (on the molecular scale) of definite size.
They are interpreted as crystallizing from positive δ18O magmas during protolith emplacement.
When crystallizing from the melt, the longest crystallizable propylene sequences crystallized first at any supercooling, thus controlling the segmental mobility of other segments in the distribution.
An example of fitting several empirical models of constant growth rate dispersion and of size-dependent growth rate to series of experimental data for aluminum ammonium alum crystallizing from its water solution in the MSMPRC is presented and discussed.
The development of global orientation and morphological features in linear polyethylene crystallizing from a sheared melt are studied using in-situ time-resolving wide angle X-ray scattering (WAXS) and ex-situ transmission electron microscopy.
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The rate of crystallization for samples crystallized from the glass was ~̊ 30 times greater than that for samples crystallized from the melt at identical crystallization temperatures.
The separated solid was filtered, washed with water and crystallized from dioxane, as brawn crystals; yield (75%); m.p. 280 282 °C.
The separated solid was filtered, washed with water and crystallized from ethanol to give red crystals; yield (67%). m.p. 170 172 °C.
The separated solid was filtered, washed with water and crystallized from ethanol to give white crystals; yield (88%); m.p. 111 113 °C.
The solid which separated was collected and crystallized from ethanol to give yellow crystals; yield (61%); m.p. 100 102 °C.
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