Abstract

Infrared canopy temperature (CT) is a well-established surrogate measure of stomatal conductance. There is ample evidence showing that genotypic variation in stomatal conductance is associated with grain yield in wheat. Our goal was to determine when CT repeatability is greatest (throughout the season and within the day) to guide CT deployment for research and wheat breeding. CT was measured continuously with ArduCrop wireless infrared thermometers from post-tillering to physiological maturity, and with airborne thermography on cloudless days from manned helicopter at multiple times before and after flowering. Our experiments in wheat, across two years contrasting for water availability, showed that repeatability for CT was greatest later in the season, during grain-filling, and usually in the afternoon. This was supported by the observation that repeatability for ArduCrop, and more so for airborne CT, was significantly associated (P < 0.0001) with calculated clear-sky solar radiation and to a lesser degree, vapor pressure deficit. Adding vapor pressure deficit to a model comprising either clear-sky solar radiation or its determinants, day-of-year and hour-of-day, made little to no improvement to the coefficient of determination. Phenotypic correlations for airborne CT afternoon sampling events were consistently high between events in the same year, more so for the year when soil water was plentiful (r = 0.7 to 0.9) than the year where soil water was limiting (r = 0.4 to 0.9). Phenotypic correlations for afternoon airborne CT were moderate between years contrasting in soil water availability (r = 0.1 to 0.5) and notably greater on two separate days following irrigation or rain in the drier year, ranging from r = 0.39 to 0.53 (P < 0.0001) for the midday events. For ArduCrop CT the pattern of phenotypic correlations, within a given year, was similar for both years: phenotypic correlations were higher during the grain-filling months of October and November and for hours-of-day from 11 onwards. The lowest correlations comprised events from hours-of-day 8 and 9 across all months. The capacity for the airborne method to instantaneously sample CT on hundreds of plots is more suited to large field experiments than the static ArduCrop sensors which measure CT continuously on a single experimental plot at any given time. Our findings provide promising support for the reliable deployment of CT phenotyping for research and wheat breeding, whereby the high repeatability and high phenotypic correlations between afternoon sampling events during grain-filling could enable reliable screening of germplasm from only one or two sampling events.

Highlights

  • Canopy temperature (CT) has been used in field phenotyping of crops since the 1960s (e.g., Fuchs and Tanner, 1966)

  • While lower CT may be linked directly to yield via greater stomatal conductance under yield potential conditions, another possibility arises under water limitation: cooler CT has been associated with increased rooting depth (Reynolds et al, 2007), and greater water use and yield (Lopes and Reynolds, 2010) when measured during grain-filling

  • ArduCrop CT and airborne CT were warmer than air temperature and airborne CT was warmer than ArduCrop CT

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Summary

Introduction

Canopy temperature (CT) has been used in field phenotyping of crops since the 1960s (e.g., Fuchs and Tanner, 1966). CT can be used as a surrogate measure of stomatal traits including stomatal conductance, stomatal aperture or leaf porosity and indirectly, photosynthetic rate (Blum et al, 1982; Smith et al, 1988; Amani et al, 1996; Fischer et al, 1998; Jones, 2004; Leinonen et al, 2006; Jones and Vaughan, 2010; Maes and Steppe, 2012). While lower CT may be linked directly to yield via greater stomatal conductance under yield potential conditions, another possibility arises under water limitation: cooler CT has been associated with increased rooting depth (Reynolds et al, 2007), and greater water use and yield (Lopes and Reynolds, 2010) when measured during grain-filling

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