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In this case, water vapor concentration reaches a higher value.
Each array element displayed linear responses to the vapor concentration.
The crystal growth rate is determined by Zn and O2 vapor concentration ratio.
Ammonia (NH3) vapor concentration was varied from 25 to 1,000 ppm.
Therefore, there is a higher distribution of vapor concentration near the substrate.
Sensing properties were influenced by carboxyl content and solvent vapor concentration.
Both solution pours resulted in vapor concentration means exceeding the TLV.
The water vapor concentration uncertainty never exceeded 0.06 vol% even during times of heavy mist loading.
However, when the initial gasoline vapor concentration further increased to a higher level (higher than 2.1%), the flame brightness increased again with increasing of initial gasoline vapor concentration.
However, observations show a recent drop in the stratospheric water vapor concentration in 2001 and again in 2008 (e.g., Solomon et al. [2010a]), suggesting trends in the mesospheric water vapor concentration are far from linear.
There exists a large temperature and water vapor concentration difference between the flue gas and the desulfurization slurry.
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