- #1
AppeltjeBosheuvel
I'm reading through my soil heat flux chapter and I have two questions: it seems that
1. Cs (volumetric heat capacity) in soil increases with increasing soil moisture. I assume volumetric heat capacity is the amount of J it takes to heat up a volume with 1 degree. Does that mean that the more water is in a soil, the more J it takes to heat up a volume? Is this correct?
2. It also has a graph of conductivity over soil moisture content, here clay is less of a conductor than sand. Why is this so? Cause clay is less permeable?
I would love some help :) Thank you
1. Cs (volumetric heat capacity) in soil increases with increasing soil moisture. I assume volumetric heat capacity is the amount of J it takes to heat up a volume with 1 degree. Does that mean that the more water is in a soil, the more J it takes to heat up a volume? Is this correct?
2. It also has a graph of conductivity over soil moisture content, here clay is less of a conductor than sand. Why is this so? Cause clay is less permeable?
I would love some help :) Thank you