Modelling PRI for water stress detection using radiative transfer models
Introduction
The Photochemical Reflectance Index (PRI) was proposed by Gamon et al. (1992) as an indicator of the de-epoxidation state of the xanthophyll pigments related with photosynthetic processes. It is based on a normalized difference of the 530 nm band where xanthophyll pigment absorption occurs, and a reference band located at 570 nm. As the xanthophyll pigments are related to light absorption mechanisms, the PRI index has been extensively linked to light use efficiency (LUE) at the leaf scale (Guo and Trotter, 2004, Nakaji et al., 2006, Serrano and Peñuelas, 2005, Sims et al., 2006), at canopy scale using field spectrometers (Nichol et al., 2000, Nichol et al., 2002, Strachan et al., 2002, Trotter et al., 2002) and using satellite imagery such as EO-1 Hyperion (Asner et al., 2005), MODIS (Drolet et al., 2005) and AVIRIS (Fuentes et al., 2006). The estimation of LUE through the remote sensing PRI index has shown a direct link to photosynthesis rate assessment (Guo and Trotter, 2004, Nichol et al., 2000, Nichol et al., 2006, Sims et al., 2006). In addition, photosynthesis has also been related to PRI through chlorophyll fluorescence and non-photochemical quenching (Evain et al., 2004, Nichol et al., 2006).
The early detection of water stress is a key issue to avoid yield loss, which can be affected even by short-term water deficits (Hsiao et al., 1976). The pre-visual detection of water stress has been successfully achieved with remote sensing data using thermal infrared radiation since long ago (Cohen et al., 2005, Idso et al., 1978, Idso et al., 1981, Jackson et al., 1977, Jackson et al., 1981, Jackson and Pinter, 1981, Leinonen and Jones, 2004, Möller et al., 2007, Sepulcre-Cantó et al., 2006, Sepulcre-Cantó et al., 2007 Wanjura et al., 2004), and more recently being suggested the visible spectral region with the PRI index as an indicator of stress (Peguero-Pina et al., 2008; Suárez et al., 2008, Thenot et al., 2002). Alternatively, thermal imagery acquired over vegetation is sensitive to canopy transpiration because temperature is raised due to the reduction in evaporative cooling under stress conditions. Thermal remote sensing of water stress has been accomplished using spectrometers at ground level (Idso et al., 1981, Jackson et al., 1977, Jackson et al., 1981), thermal sensors at image level (Cohen et al., 2005, Leinonen and Jones, 2004, Sepulcre-Cantó et al., 2007) and using satellite thermal information (Sepulcre-Cantó et al., in press).
It is well known that severe water deficits affect many physiological processes and have a strong impact on yield (Hsiao et al., 1976). However, even moderate water deficits, which are not easy to detect, can also have important negative effects on yield (Hsiao & Bradford, 1983). It is important to be able to assess the level of stress through some pertinent indicators. This is the case of the xanthophyll cycle response to stress tracked by the PRI index, which is suggested as a pre-visual indicator of water stress and is the aim of this study. PRI has been used to assess pre-visual water stress in the work by Thenot et al. (2002) and Winkel et al. (2002) at leaf level, at canopy level (Dobrowsky et al., 2005, Evain et al., 2004, Peguero-Pina et al., 2008, Sun et al., 2008) and using airborne imaging spectroscopy (Suárez et al., 2008). Both indicators, canopy temperature and PRI, are complementary; they provide physiological information related to plant water status, transpiration and photosynthesis. High spatial resolution imagery in the visible and near infrared region is relatively easy to acquire with current airborne and satellite sensors, such as AHS, Hymap, CASI, AVIRIS, and Hyperion, among others. On the contrary, high-resolution thermal sensors are not common due to technical limitations of microbolometer technology. Moreover, high resolution thermal imagers onboard satellite platforms are restricted due to technical limitations. Current thermal medium resolution sensors on satellite platforms are limited to ASTER and LANDSAT sensors, offering spatial resolutions limited to the 60–120 m pixel-size range. These current technical limitations for acquiring high-spatial resolution thermal imagery emphasize the need for developing pre-visual water stress indicators in the VIS/NIR region for agricultural and precision farming methods. Technically, CMOS and CCD VIS/NIR imaging sensors based on silicon detectors provide very high spatial resolution with pixel sizes at the centimetre level and cost-effective for precision agriculture imagers and future satellite platforms. Thus, attention must be placed on VIS/NIR narrow-band indicators of pre-visual stress, such as PRI, as well as chlorophyll fluorescence for stress-detection methods (Dobrowsky et al., 2005, Pérez-Priego et al., 2005, Suárez et al., 2008, Thenot et al., 2002). Nevertheless, the PRI index cannot be readily used to map vegetation stress without considering leaf and canopy structural effects on the index. PRI bands at 531 and 570 nm are affected by both leaf and canopy parameters such as chlorophyll content (Cab), dry matter (Cm), leaf thickness, leaf area index (LAI), and leaf angle distribution function (LADF), among others (Barton and North, 2001, Suárez et al., 2008). Thus, PRI maps obtained over canopies with variable LAI mask the sensitivity of the index to stress, mostly tracking the spatial variation of the canopy leaf area density and structure (Barton and North, 2001, Suárez et al., 2008). Consequently, modelling work at leaf and canopy scale is needed to enable an operational application of PRI to map water stress in non-homogeneous canopies where structural changes play the main role in the reflectance signature.
A new modelling method is presented in this paper based on radiative transfer simulation to estimate a theoretical PRI baseline for non-stress conditions for two tree species, olive and peach, and for an herbaceous continuous canopy of maize. The method compares imaged PRI with theoretical non-stress PRI obtained through model inversion for existing structural and background conditions, defining a within field threshold to detect stressed vegetation.
Section snippets
Study sites
The three main study sites used for field and airborne data collection are located in Córdoba, southern Spain (37.8°N, 4.8°W), on soils classified as Typic Xerofluvents. The climate is Mediterranean with an annual rainfall of 650 mm concentrated between autumn and spring. The first study site corresponds to a 4 ha irrigated-olive orchard (Olea europaea L. cv. “Arbequino”) established in 1997 in a 3.5 × 7 m grid. The tree lines follow a north–south direction and the trees were planted on ridges to
PRI measurements at the leaf level
Leaf level measurements on olive and peach tree leaves showed differences in the leaf spectra between the full-irrigated (FI) and the regulated deficit irrigation (RDI) treatments. Fig. 6a shows the mean leaf spectra corresponding to both irrigation treatments. In the near infra-red part of the spectrum, differences can be detected due to leaf structural changes in response to water stress. Differences in the green region (Fig. 6b) are due to confounding effects of both chlorophyll content and
Conclusions
This study presents a methodology for water stress detection in annual and perennial irrigated crops using remotely sensed PRI index and radiative transfer modelling. The method accounts for leaf and canopy inputs N, Cab and LAI to simulate the PRI values to identify crop crowns/blocks under stress. The methodology presented was successfully tested on two tree orchards (olive and peach trees) and a closed canopy of an annual crop (maize). The PRI index tracked water stress levels in crops under
Acknowledgments
Financial support from the Spanish Ministry of Science and Innovation (MCI) for the projects AGL2005-04049, EXPLORA-INGENIO AGL2006-26038-E/AGR, CONSOLIDER CSD2006-67, and AGL2003-01468 is gratefully acknowledged, and in-kind support provided by Bioiberica through the project PETRI PET2005-0616. Technical support from UAV Navigation and Tetracam Inc. is also acknowledged. M. Morales, C. Ruz, G. Sepulcre-Cantó, D. Notario, M. Guillén, C. Trapero, I. Calatrava, A. Vera and M. Ruiz Bernier are
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