Dew formation characteristics in the gravel desert ecosystem and its ecological roles on Reaumuria soongorica

As an additional source of water to plants besides rainfall, dew may have a positive impact on vegetation in the arid ecosystems. Knowledge regarding dew formation characteristics and its ecological effects on vegetation water status and photosynthetic performance in the gravel desert ecosystem is still lacking. In this study, the dew variability and formation frequency on a gravel desert were measured by microlysimeters. We quantified dew formation characteristics, investigated vegetation water response to dew events in the gravel desert ecosystem at the edge of a desert oasis, Northwestern China. The results showed water adsorption was a primary pathway of dew formation in such system, and the average daily amount of dew is 0.06 mm. Dew occurred on 36% of growing season days, the number of days with dew amounts >0.03 mm accounted for 82% of the total dew events, and the cumulative amount of dew for those days was 3.41 mm. Relative humidity, air temperature, wind speed, the difference between air temperature and soil surface temperature had significant effects on dew formation. A threshold of RH >= 30% is taken to mark possible condensation in the gravel desert ecosystem. A significant positive correlation between dew amounts and the relative moisture in the near-surface air was found when RH >= 30%. The moderate wind velocity (1-1.8 m/s) was favorable to dew formation, and when wind speed >5.47 m/s, there was no dew formation. Because of the water-absorbing scales on the leaves of Reaumuria soongorica, dew events significantly improved their relative water content, water potential, and photosynthetic performance in the early morning and ameliorating the adverse effects of plants exposed to prolonged drought. The study highlights dew is an important supplementary source of water in the gravel desert ecosystem. Although the absolute dew amounts were found not high, it can be a frequent and stable water resource. Furthermore, this study provides a comprehensive understanding of the effects of dew on plant water status in the gravel desert ecosystem.

Automated summary

This study investigates dew formation characteristics and its ecological effects on vegetation water status and photosynthetic performance in the gravel desert ecosystem at the edge of a desert oasis in Northwestern China. Water adsorption is the primary pathway of dew formation, with an average daily dew amount of 0.06 mm. Dew was found to occur on 36% of growing season days, with the cumulative amount of dew for days with dew amounts >0.03 mm accounting for 82% of the total dew events. Factors like relative humidity, air temperature, wind speed, and temperature differences significantly influence dew formation. Dew events were shown to improve the relative water content, water potential, and photosynthetic performance of Reaumuria soongorica plants, highlighting the importance of dew as a supplementary water source in the gravel desert ecosystem.