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The exfoliation yield was defined as α = C 1/C 0 × 100 %, where C 1 was the FL-MoS2 concentration of the upper dispersion at the ending, and C 0 was the initial concentration of natural molybdenite powders.
Moreover, because the oxygen vacancy concentration of the upper HfO2 layer (~2.3%) is lower than that of the underlying HfO2 (~6%) (Fig. 7c), the higher negative forming voltage of −11 V is needed to form filaments.
Heat transfer measurements show that the redistribution of water to form an additional lower viscosity carrier layer while increasing the solids concentration of the upper layer or layers enables the maximum drying rate, for which drying-air induced surface disturbances are acceptably small, to be increased with significant commercial benefits.
Our results show that the direct decrease in pH due to ocean warming is approximately equal to but opposite in magnitude to the indirect increase in pH associated with ocean warming (ie reduced DIC concentration of the upper ocean caused by lower solubility of CO2).
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Figure (S1) showing mean BC2.5 concentrations of the upper and lower levels of the West 4th st subway station.
At the same time (12 h pi) intracellular metabolite concentrations of the upper part of glycolysis were significantly increased.
S. pneumoniae concentration of the right upper, medium, lower lobes and the left upper and lower lobes was 4.8 ± 2.3, 4.6 ± 3.1, 3.5 ± 3.2, 3.9 ± 2.9 and 3.4 ± 3.5 CFU/gram, respectively (p = 0.848).
Subject 1 had an end-of-study concentration at the upper 95% confidence limit of the geometric mean of the 95th percentile for PFHS (10 ng/mL), and no subject was below this upper bound for PFOA (13.5 ng/mL).
Open image in new window Fig. 75 Variation curves of gas concentration at the upper corner of coalface, coalface and in return air after coal extraction.
The reductive dissolution of As-bearing Fe(III) oxides coupled to the degradation of organic matter with an estimated maximum rate of 0.22 mmol C/L/yr, mainly accounted for the depth-dependent increase of As concentration in the upper part of the shallow aquifer (<25 m deep).
At that time, the 1D model clearly showed a progressive decrease of cation concentration towards the upper surface of the sample (x = 0.5 mm) ranging from 273 mol/m at x = 0 mm height (significantly lower compared to the initial 280 mol/m imposed by the external solution at time 0 s) to 255 mol/m at x = 0.5 mm height).
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