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Micro-X-ray computed tomography (μ-CT) showed that porosity generally increased in the sample from bottom to top, the pore size fractions shifted toward larger pores in elevated sample levels, and horizontal homogeneity was found throughout each sample with minor deviations in the bottom region.
By convention, positive scores are given when targets for a miRNA family display downregulation, indicating that the biological activity of the cognate miRNAs is increased in the sample, while negative values are obtained for upregulation of targets, suggesting a decreased activity.
Positive values are obtained when targets for a given miR-seed display more downregulation than the reference, indicating that the activity of this miR-seed is increased in the sample, while negative values are obtained for upregulation of targets, suggesting a decreased activity.
Heterogeneity decreased in the NRCT subgroup, while heterogeneity increased in the sample size and RCT subgroups, compared with overall heterogeneity.
This suggests that progressively increasing amount of ODN was retained by MCH in the wells as the proportion of MCH to ODN increased in the sample.
Interestingly, expression levels of LOXL1 increased in the sample homozygous for the protective haplotype (26%) with respect to the samples harbouring neutral haplotypes.
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After 12 h, TRF1 mRNA levels increased in the samples in which a G2/M-phase arrest became more pronounced (Figure 4a, compare also Figure 1b).
The dielectric loss in the frequency range 1 MHz to 1.3 GHz remained almost constant as the Cr content was increased in the samples.
However, as the milling time increased, the intensity of the cerium hydride peak increased in the samples.
Strikingly, the amount of iRBC adhering to the placenta sections was four-fold increased in the samples from recrudescent primiparous females (Figure 4A).
The fluorescence intensity dramatically increased in the samples treated by the increasing amount of myoinositol.
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CEO of Professional Science Editing for Scientists @ prosciediting.com