WEBINAR

Soil CO2 production is the sum of respiration from heterotrophic and autotrophic organisms in the soil, and it is strongly temperature dependent. On a seasonal scale, soil CO2 production depends on soil moisture content, organic matter content, plant growth, and other factors. Because soil is resistant to gas transport, a strong CO2 concentration gradient exists across the soil profile. This gradient is a major driving force for soil CO2 flux. Two techniques are commonly used to measure soil CO2 flux: chamber-based systems (open and closed) and gradient methods. In this webinar, we discuss the requirements of chamber-based closed soil CO2 flux systems in detail.
Please fill out this form to watch this webinar:
Jason Hupp
Field Applications Scientist
Access our full collection of technical content and materials.