Harvest & Post-Harvest

Drying: Temperature, RH & Airflow

Drying rate is governed by moisture gradients, surrounding vapor pressure, temperature, tissue structure, and air movement; direct high-velocity airflow can overdry surfaces while interiors remain wetter.

Key concepts

  • Water moves from wetter internal tissue toward the surface
  • Air temperature and RH determine vapor-pressure conditions around the flower
  • Air movement reduces the local boundary layer but too much direct airflow can create uneven drying
  • Dense flowers can retain internal moisture longer than their surface suggests

What to measure or observe

  • Measure room temperature and RH at representative locations
  • Check airflow distribution rather than one fan setting
  • Track mass or other consistent drying indicators over time
  • Inspect for condensation, odor changes, or mold

Common mistakes

  • Pointing strong fans directly at flowers
  • Relying on one room sensor
  • Assuming a dry-feeling exterior means moisture is uniform internally

Visuals this lesson still needs

  • Flower moisture-gradient cutaway
  • Room airflow map
  • Boundary-layer diagram
  • Surface-versus-interior drying comparison

Evidence & further reading

Sources connected to this lesson

These references support specific biological, diagnostic, environmental, or process concepts used in this lesson. They are not a substitute for crop-specific testing or local regulatory guidance.

Connected learning

Use the next piece of evidence

Move between reference material, measurement, field records, and whole-plant context instead of treating one page as the complete answer.