3. Evaporation from Different Surfaces
The chapter discusses the dynamics of mass transfer in aquatic systems, focusing on the mechanisms of evaporation from water surfaces and the application of various mass transfer coefficients. It highlights the input of parameters such as wind speed and sediment characteristics, illustrating these concepts through case studies of spills in river systems. The importance of empirical correlations for predicting mass transfer rates in environmental quality monitoring is emphasized.
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What we have learnt
- Mass transfer in aquatic systems involves complex interactions between water, air, and sediments.
- Specific mass transfer coefficients are critical for accurate predictions of chemical behavior in water bodies.
- Empirical correlations must be applied carefully due to variations in physical parameters like wind speed and chemical properties.
Key Concepts
- -- Mass Transfer
- The movement of substances from one phase to another or within a phase, influenced by gradients in concentration and other physical conditions.
- -- DNAPL
- Dense Nonaqueous Phase Liquid, a type of pollutant with a density greater than that of water, which sinks and poses a significant risk to groundwater.
- -- Mass Transfer Coefficient
- A proportionality factor that quantifies the mass transfer rate of a substance across a defined area per unit concentration gradient.
- -- Empirical Correlation
- A relationship derived from experimental data that relates various parameters, often used when theoretical models are complex or unavailable.
- -- Schmidt Number
- A dimensionless number that characterizes mass transfer relative to momentum transfer in fluids.
- -- Sherwood Number
- A dimensionless number that represents the ratio of convective mass transfer to mass diffusion.
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