Solar Heat Transfer in Soil
Introduction to Solar Heat Transfer
Use of dry solar heat for heating applications
Common practice to use 100 grams as the mass of dry samples for calculations
Assignment reference to fractions in heat calculations
Heat Transfer Properties of Soil
Overview of Thermodynamic Concepts
Discussion on solar radiation, specific heat, and water content in soil
Fourier's Law of Heat Conduction
Examining how heat flows through soil:
Use of Fourier equation for heat transfer
Mathematical representation in similar form to Darcy's Law for fluid flow
Fourier equation components:
Heat flux (denoted as $q$)
Thermal conductivity denoted as $k$
Temperature gradient expressed as $ rac{ ext{d}T}{ ext{d}x}$
Units:
Heat transfer: Watts per square meter ($ ext{W/m}^2$)
Thermal conductivity: Watts per meter Kelvin ($ ext{W/(m K)}$)
Factors Influencing Thermal Conductivity
Materials and Structures
Comparison of thermal conductivity across different materials
Air (lowest thermal conductivity)
Water (moderate thermal conductivity)
Mineral soils (highest thermal conductivity)
Influence of soil structure:
Loose structures with larger pores exhibit low thermal conductivity
Dense structures with less pore space are generally better conductors of heat
Building Materials Implications
Common use of porous rocks for construction to insulate from external temperatures
Rock types:
Igneous rocks (intrusive and extrusive) hold air pockets formed during rapid cooling
Historical and geographical context of material selection for building purposes
Thermal Conductivity Variability in Soil
Variability Due to Moisture Content
Wet soils generally have higher thermal conductivity compared to dry soils
Aggregated soils have lower thermal conductivities due to larger pore spaces
Introduction of water in soil influences thermal dynamics:
Movement of water through soil can either cool it or heat it depending on the temperature differential
Temperature Changes with Soil Depth
Soil Temperature Profiles
General behavior of soil temperature with depth:
Temperature often decreases with depth due to water presence
Discussion surrounding stabilization of temperatures at a certain depth
Concept of Temperature Gradients
Temperature in soil varies daily and seasonally
Peak temperatures occur signifying daily fluctuations in temperature
Seasonal Changes in Soil Temperature
Observed differences in soil temperature across seasons, influenced by depth:
Cold months show increasing temperature with depth, while warm months show the opposite trend
Presentation of graphical data representing soil temperature profiles
Soil Temperature Management Techniques
Techniques to Manipulate Soil Temperature
Use of mulches as an insulating layer:
Dry plant residues with low thermal flux reduce temperature variations
Allow for stabilization of soil temperature across fluctuations in air temperature
Black plastic mulches used for soil solarization decrease pathogen presence
Challenges associated with synthetic mulches:
Breakdown into microplastics poses environmental risks
Effects of Mulch in Various Seasons
Observed trends between air temperature and soil temperature with mulches versus without:
Mulched soil reflects lower surface temperatures during warmer months
Discussion of potential impacts during winter months on soil conditions
Soil and Climate Interaction
Impact of Soil Moisture and Temperature on Climate
Relationship between soil moisture depletion and the atmospheric vapor pressure deficit
Thermal radiation emissions from soil contribute to climate change dynamics
Role of permafrost in carbon release and greenhouse gas effects
Conclusion
Summary of class topics leading into winter break
Encouragement and final thoughts for students regarding the learning material and upcoming breaks.