Abstract

In Mediterranean Europe, winter cereals can experience soil waterlogging starting from crop establishment up to stem elongation and, in late sowings, this stress is combined with temperatures favorable to plant metabolism. Oats response to waterlogging has been rarely investigated, but these species seems to recover better than other cereals. In a 2-year experiment, Avena sativa and Avena byzantina were sown at the end of winter in pots placed outdoors. At the two-tiller stage, plants were exposed to waterlogging for periods ranging from 0 to 35 days. The dry weight and the N-concentration of shoots and roots were determined on waterlogged plants and drained controls at the start and the end of each waterlogging period, and at maturity. At maturity, the grain yield and its components were determined. To relate oat response to its specific morphological and developmental traits, results were compared to the published results in wheat and barley. Both oat species suffered severe damage during waterlogging: the uptake of nitrogen and the N-concentration of shoots were reduced after 7 days, tiller initiation and root growth after 14 days, and shoot growth after 21 days. All plants survived waterlogging, and the relative growth rates of roots and shoots and the net uptake rate of nitrogen were resumed during recovery. Nevertheless, at maturity, the straw and root biomass were markedly lower with all waterlogging durations, and grain yield decreased by 42% up to approximately 81% following an asymptotic equation. The most affected yield components were the number of panicles per plant and the number of kernels per panicle, but their relative sensitivity changed according to waterlogging duration. The slight increase in tiller fertility in response to short waterlogging and the small and irregular decrease in the number of kernels per spikelet suggest that the two oats could recover the initiation and size of inflorescences better than other winter cereals. Despite this, waterlogging in spring was highly detrimental to these oats because of severe damage under waterlogging and because of the inability to initiate new tillers and adequately resume root growth during recovery, once plants had achieved the phase of stem elongation.

Highlights

  • Soil is considered waterlogged when excess water saturates the soil pores, with either no layer or a very fine layer of water on the soil surface, so that the gas exchange of roots with the atmosphere is inhibited (Sasidharan et al, 2017)

  • Aiming to fill the lack of knowledge about the response of oats to waterlogging, and to give insight into both the direct effects of waterlogging on plant growth parameters and the ability to resume them during recovery, we exposed plants of A. sativa and A. byzantina sown at the end of winter to different waterlogging durations

  • We argue that the more advanced growth stage at the end of waterlogging was an important reason for the scarce recovery observed in A. sativa and A. byzantina sown at the end of winter, and our hypothesis is in agreement with de San Celedonio et al (2014), who found that delayed sowings increased the negative response of wheat to waterlogging

Read more

Summary

Introduction

Soil is considered waterlogged when excess water saturates the soil pores, with either no layer or a very fine layer of water on the soil surface, so that the gas exchange of roots with the atmosphere is inhibited (Sasidharan et al, 2017). Crop losses due to waterlogging are expected to increase as a consequence of increased extreme precipitation events associated with climate change (Herzog et al, 2016). Waterlogging is a compound stress that severely changes the soil environment, first by reducing oxygen availability. Additional negative conditions caused by waterlogging in soil are the accumulation of CO2, ethylene, and biochemically reduced compounds in the root environment, generally combined with nutrient deficiency (Pang et al, 2007; Herzog et al, 2016). Lower soil nitrogen has been reported as a consequence of denitrification and N leaching (Bronson and Fillery, 1998; Nguyen et al, 2018)

Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call