Elsevier

Field Crops Research

Volume 263, 1 April 2021, 108076
Field Crops Research

Ozone flux-effect relationship for early and late sown Indian wheat cultivars: Growth, biomass, and yield

https://doi.org/10.1016/j.fcr.2021.108076Get rights and content

Highlights

  • Sensitivity of early and late sown Indian wheat cultivars to O3 were evaluated.

  • O3 flux-effect relationships were investigated for AGB and yield in wheat plants.

  • Higher accumulation of POD6SPEC was found in early sown than late sown cultivar.

  • Higher longevity, gmax and lower critical level made early sown cultivars more sensitive.

  • The grain yield loss under EO3 was 30.5 % in early and 23 % in late sown cultivars.

Abstract

Precise ozone (O3) flux models remain helpful to identify the sensitivity of crops and their cultivars under high O3 levels by assessing biomass and yield losses under natural climate and future O3 levels. In this study, we have evaluated the effects of O3 on growth, biomass, and yield of four Indian wheat cultivars by exposure-linked as well as through flux-effect relationship-based analysis using two years of empirical data. Early and late sown cultivars were exposed to ambient O3 (AO3) and elevated O3 i.e., ambient+20 ppb (EO3). The POD6SPEC (species-specific phytotoxic O3 dose above a threshold of 6 nmol m−2 PLA s-1) on flag leaves for each cultivar and treatment was derived by using DO3SE (Deposition of Ozone for Stomatal Exchange) model. Above-ground biomass was reduced more in early sown cultivars (26.1 %) than late sown (21.3 %) because of the larger negative impacts on plant growth under EO3 treatment. Loss of grain yield under EO3 exposure was high in early sown cultivars (30.5 %) compared to late sown (23 %) due to high stomatal O3 uptake during the O3 exposure period. Based on model outputs, early sown cultivars showed higher accumulated POD6SPEC (1.6–3.75 mmol O3 m−2) compared to late sown cultivar (0.65 to 1.97 mmol m−2). A negative linear relationship was obtained in above-ground biomass and grain yield concerning POD6SPEC. The relationship showed that 0.284 mmol O3 m−2 accumulated POD6SPEC is responsible for a 5% reduction of grain yield in early sown cultivars, while 0.393 mmol O3 m-2 accumulation is required for a 5% reduction in yield of late sown cultivars. The results also suggest that O3 flux-effect relationship could be a valuable tool for assessing and predicting the risk of O3 on wheat cultivars in India and for crop productivity models for predicting climate change impacts.

Introduction

Ground surface ozone (O3) is the most damaging air pollutant to horticultural and agricultural crop plants (Mills et al., 2007; Osborne et al., 2019). During the preindustrial time, the background O3 levels were 10−15 ppb. Owing to anthropogenic activity, the emissions of O3 precursors (NOx, CO, and VOCs) have been increased. The ambient O3 level has reached above the threshold of critical level over many regions of the world (Hartmann et al., 2013; Solberg et al., 2005). If current rising trends of O3 continue, the annual global concentration of O3 will reach up to 68 ppb by 2050 (Meehl et al., 2007). Air pollution and GHG emissions have risen dramatically in India over the past three decades due to tremendous growth in industrialization, urbanization, and transport. In recent decades, high O3 concentration has been detected in several regions of India (Lal et al., 2017; Sharma et al., 2019; Singh and Agrawal, 2017; Yadav et al., 2020).

Wheat is a staple crop in India and has been identified as O3 sensitive species (Feng et al., 2009; Singh et al., 2018). The deleterious effects of high O3 on wheat are described as visible leaf injury, premature leaf senescence, and reduced leaf area, plant height, and above-ground biomass, which collectively lead to a reduction in the economic yield (Liu et al., 2015; Mishra et al., 2013; Ojanpera et al., 1992; Singh et al., 2018). Long-term assessments on crop loss due to O3 have been documented since the 1980s in the USA under National Crop Loss Assessment Network (NCLAN), and in Europe under European Open-Top Chambers Programme (EOTCP) (Fuhrer, 1994; Heagle, 1989; Heck et al., 1984). Pleijel et al. (2014) have reported a 9% reduction in above-ground biomass and 14 % yield loss in wheat due to ambient O3 concentration over the Europe. However, globally O3 induced reduction in grain yield of wheat was established at 9.9 % in the northern hemisphere and 6.2 % in the southern hemisphere (Mills et al., 2018). The yield losses of 8.2–22.3 % in wheat were estimated for India because of high ambient O3 (Tang et al., 2013). India's breadbasket, the Indo-Gangetic Plain (IGP), is one of the most air-polluted regions in the country and estimated to suffer nine million tons of wheat loss annually due to high surface O3 (Lal et al., 2017).

Furthermore, the concentrations of O3 above the critical levels are known for significant impairment in plant growth and economic yield (Ainsworth et al., 2012; Feng et al., 2009; Singh et al., 2018). To derive the critical level of O3, cumulative exposure metrics such as AOT40 and cumulative stomatal flux-based metrics such as PODy have been used in many studies (Emberson et al., 2018; Mills et al., 2018). The stomatal O3 flux methods are quite useful for assessing O3 risk and provide a robust dose-response relationship between O3 uptake and yield of wheat cultivars (CLRTAP, 2017; Harmens et al., 2018; Osborne et al., 2019; Pleijel et al., 2014; Wu et al., 2016). But, this approach is more dependent on input data as compared to the exposure-based approach. In the past, various exposure-based field studies have been conducted in India to assess the yield losses of major crops under ambient and future O3 levels (Mishra et al., 2013; Mukherjee et al., 2020; Singh et al., 2018). In exposure-based metrics, we only consider the O3 concentration in the air nearby the plants to measure its impact on plants. However, many important factors such as stomatal conductance, soil moisture, weather condition, vegetation characteristics, phenology of plant are not considered, which play vital roles in stomatal O3 uptake (Feng et al., 2012; Mills et al., 2007).

As the sensitivity of a species to O3 mainly depends on the amount of O3 uptake and their intrinsic defense response (Dumont et al., 2013; Yadav et al., 2019), the flux-based concept is suggested to be the most preferred metrics over the exposure-based metrics (Anav et al., 2016; Pleijel et al., 2004). Over the last 20 years, many significant developments have been made in stomatal flux modelling to improve the O3 risk assessment (CLRTAP, 2017; Emberson et al., 2018, 2000; Grunhage et al., 2012; Pleijel et al., 2007). The previous studies have found a strong correlation of phytotoxic O3 dose above a flux-threshold of y (PODy) with grain yield and biomass of wheat (Grunhage et al., 2012; Harmens et al., 2018; Pleijel et al., 2014). Moreover, a significant negative flux-effect relationship has also been found, which helped in identifying the level of sensitivity of wheat cultivars under elevated O3 (Grunhage et al., 2012; Harmens et al., 2018; Pleijel et al., 2014).

In the present study, Deposition of Ozone and Stomatal Exchange (DO3SE) model was used for assessing the O3 risk and to identify the species-specific O3 sensitivity in Indian wheat cultivars. The DO3SE model estimates stomatal O3 flux of plant with a function of the O3 concentration at and the transfer of O3 across the boundary layer of leaf. Although several O3 flux-based studies have been attempted in Europe, Southeast Asia and China (Danh et al., 2016; Feng et al., 2012; Osborne et al., 2019), but this will be the first O3 flux-model based study for India to estimate stomatal O3 uptake of wheat cultivars using multiplicative algorithms. The study will be important for screening O3 tolerant Indian wheat cultivars to get the maximum yield against the future level of O3. For this purpose, early and late sown wheat cultivars were selected based on their differences in sowing time, life span, and popularity in the IGP region of India. On availability of field after rice harvest, it is a common practice to sow wheat either in early winter at the start of November using early sown cultivars (life span 5 months) or up to mid of December with late sown cultivars (life span 4 months). The aims of the present study are: (i) to determine the effects of elevated O3 on growth, biomass, and yield of early and late sown wheat cultivars; (ii) to parameterise the stomatal flux DO3SE model for Indian wheat cultivars to calculate the species-specific accumulated stomatal O3 flux (POD6SPEC); and (iii) to drive O3 flux-biomass and flux-yield relationships in early and late sown cultivars from the two years experimental data for O3 risk assessment.

Section snippets

Field location and experimental set-up

The experiments were conducted in open-top chambers (OTCs) for two consecutive years (2016−2017 and 2017−2018) from November to March. The site is located at the Botanical Garden in the campus of Banaras Hindu University (BHU), Varanasi (25°16ʹ N, 82°59ʹ E, 81 m above mean sea level) in Uttar Pradesh, India. The details of OTCs construction were described in (Dolker and Agrawal, 2019). The soil texture of the experimental site was sandy loam (coarse) and had slightly basic pH of 7.3 ± 0.1 with

Weather conditions and ozone exposure

During the two years of the experiment, the 24-h mean air temperature, VPD and daylight PAR were slightly lower in the second year (Table 1). The total rainfall was 17 and 13 mm for the first (2016−2017) and second-year (2017−2018) growing season, respectively (Table 1). The accumulated O3 over a threshold of 40 ppb (AOT40) was 11.8 and 6.8 ppm h for early sown cultivars and 8.4 and 6.2 ppm h for late sown cultivars under AO3 treatments during the first and second year of experiment,

Discussion

The ambient O3 levels are determined by existing environmental conditions; therefore, a variation can be expected between years (Hayes et al., 2019; Pleijel et al., 2007). The variations in meteorology, particularly temperature, can alter the ambient O3 concentration and thus stomatal uptake (Hayes et al., 2019). These changes are in agreement with our results, which also showed a decline of accumulated POD6SPEC due to the reduction in seasonal mean temperature and O3 concentration in the

Conclusion

The present results of both observed and modelled studies confirmed that early sown cultivars showed greater O3 induced yield losses compared to late sown cultivars. However, the magnitude of yield reduction varied under both approaches due to the uncertainty of weather conditions and some limitations in the model to accurately parameterise for specific cultivars. From the results of O3 flux-effect relationship, it was found that the critical level of POD6SPEC for 5% reduction of above-ground

CRediT authorship contribution statement

Durgesh Singh Yadav: Investigation, Methodology, Validation, Software, Data curation, Writing - original draft. S.B. Agrawal: Supervision, Formal analysis, Visualization, Project administration, Writing - review & editing. Madhoolika Agrawal: Supervision, Conceptualization, Funding acquisition, Project administration, Writing - review & editing.

Declaration of Competing Interest

Authors declare that they have no conflict of interest.

Acknowledgements

This work was carried out under Interaction of Climate Extremes, Air Pollution and Agro-ecosystems (CiXPAG) project (grant no. 244551) from Research Council of Norway, Centre for International Climate Research (CICERO), Oslo, Norway in collaboration with Dr Jana Sillmann. The authors are thankful to the Head, Department of Botany, Banaras Hindu University and coordinators, CAS in Botany and Interdisciplinary School of Life Sciences for providing the instruments and necessary facilities in order

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