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The water sorption isotherm of the tablets was determined using a dynamic water sorption analyzer.
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In the second part of the paper, we analyze model river embankments on a foundation ground with various soil profiles, including a clayey soil layer and various ground water tables, using a dynamic liquefaction analysis method.
Lipids were separated in a T3 UPLC column 1.8 μm, 2.1 × 100 mm (Acquity Waters) at 55 °C using a dynamic gradient from 68%to3%3% mobile phase A to mobile phase B in 17 min, followed by equilibration for a total run of 20 min. Mobile phase A consisted of water and acetonitrile (40 60% V/V), supplemented with 10 m m ammonium formate.
Volumetric mass transfer coefficients (kLa) of oxygen between air and water were measured experimentally using a dynamic method.
We modeled surface wetness at high resolution, using a dynamic hydrology model, to predict flood and swamp water mosquito abundances.
Water vapour sorption was measured using a dynamic gravimetric technique at 22°C (Figure 7).
Particle sizes of SNPs in DI water and seawater conditions were measured using a dynamic light scattering (DLS) technique.
Particle size and zeta potential of the particles were respectively measured by using a dynamic light-scattering (DLS) apparatus (Zetasizer Nano ZS; Malvern) after dilution with deionized water.
We used a dynamic hydrology model to simulate water table depth (WTD) and quantify the relationship between Saint Louis encephalitis virus (SLEV) transmission and hydrologic conditions in Indian River County, Florida, from 1986 through 1991, a period with an SLEV epidemic.
Here we use a dynamic scaling approach.
The resulting surface structures were further confirmed and distinguished by data obtained using dynamic water contact angle measurements.
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