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Book Chapter

Gas Exchange and Atmospheric Properties of Flooded Soils

  • Stepniewski W
  • Glinski J
Springer US, (1988), 269-278
DOI: 10.1007/978-1-4684-8378-9_23
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Abstract

Downward transport of oxygen in flooded soils is extremely difficult due to saturation of the soil with water. Compared to well-drained soils, there is a great difference in the depth of oxygenation and the consequences are of great practical importance.

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Stepniewski, W., & Glinski, J. (1988). Gas Exchange and Atmospheric Properties of Flooded Soils. In The Ecology and Management of Wetlands (pp. 269–278). Springer US. https://doi.org/10.1007/978-1-4684-8378-9_23

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