An Inter-comparison of Three Commercial Porometers L. Bissey 1 , D. Cobos 2 , C. Campbell 2 1. School of Earth and Environmental Science, Washington State University, 2. Decagon Devices, Inc. 962, 673, 410. 1053, 964, 356. 678, 674, 362. 753, 573, 322. 701, 560, 383.
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L. Bissey1, D. Cobos2, C. Campbell2
1. School of Earth and Environmental Science, Washington State University, 2. Decagon Devices, Inc.
962, 673, 410
1053, 964, 356
678, 674, 362
753, 573, 322
701, 560, 383
690, 918, 425
Stomatal conductance regulates the rates of several necessary processes in plants including transpiration, carbon dioxide assimilation, and respiration. Both steady state and dynamic porometers are currently used to measure stomatal conductance. However, few tests or measurements have been performed to compare the results obtained with the various porometers. It is important for scientists to understand the performance of each porometer in order to compare stomatal conductance data gathered from various models. In this study, we focused on three commercially available porometers: the AP-4 (Delta-T Devices, Cambridge, UK), the SC-1 (Decagon Devices, Pullman, WA), and the LI-1600 (Li-Cor, Lincoln, NE). The objective of this study was to understand the relationship between the stomatal conductance data gathered with the different instruments
We tested our first assumption by measuring spatial variability of stomatal conductance on a leaf using all three instruments. For large leaves, stomatal conductance was measured at six points on the leaf surface.
The second assumption is certainly not completely valid. Not only do the effects of previous porometer measurements likely affect stomatal conductance, the environmental conditions controlling stomatal conductance often change minute-by-minute.
Stomatal conductance data were normalized using natural-log transformation. A paired t-test was used to determine the confidence intervals of the difference between instruments.
Stomatal conductance measurements at different locations on single, fully sunlit leaves show that significant spatial variability is present over the leaf surface (Figure 2).
Figure 2. Example data showing leaf-level stomatal conductance variability. Numbers in black, blue, and purple are conductance data obtained using the AP-4, SC-1, and LI-1600 respectively. Data from different instruments were collected at different times and should not be compared among porometers.
Figure 1 shows the agreement of stomatal conductance values obtained from the AP-4, the LI-1600, and the SC-1 as well as the differences between each mean pair. After normalizing all of the data using log transformation, a regression of SC-1 verses the AP-4 (Fig 1-c) reveals that the SC-1 generally measures slightly lower conductance readings than the AP-4 (slope of 0.9701 and an R2 of 0.62 (n=235). A regression of the formerly mentioned instruments against the LI-1600 suggests that both the AP-4 (Fig 1-b) and the SC-1 (Fig 1-a) give conductance readings above that of the LI-1600 with slopes of 1.0202 and 1.1182, respectively and R2 of 0.45 (n=155) and 0.52 (n=129), respectively. Mean difference graphs (Figure 1 d - f) show the trends in instrument differences from low to high conductivity values. These data suggest that high conductance values may incorporate more measurement error that low conductance values. However, not enough high conductance values are available to make any specific conclusions.
Fig. 1. Correlation plots containing one-to-one lines of the regression of the natural log of the stomatal conductance data obtained from each instrument are shown on the left while corresponding plots showing matched pair stomatal conductance means and matched pair stomatal conductance differences for each instrument are shown on the right. Plots a and d compare the LI-1600 and the SC-1, plots b and e compare the LI-1600 with the AP-4, and plots c and f compare the AP-4 with the SC-1.
We measured stomatal conductance of approximately 200 leaves of various species with an AP-4, SC-1, and LI-1600 under field conditions. Changes in environmental conditions were minimized by taking measurements with the three porometers on similar locations of each leaf in rapid succession. On each leaf, stomatal conductance measurements with the three porometers were conducted in random order to prevent systematic bias from previous porometer measurements. Each porometer was factory calibrated within 60 days of the beginning of measurements.
This methodology assumes that: 1) stomatal conductance was measured on the exact same footprint on each leaf, and 2) environmental factors (radiation, temperature) didn’t change over the 1-2 minute timescale needed to make the three measurements on each leaf.
Table 1. Results from paired t-test (H0: µD=0, α=0.05) showing the agreement between the natural log transformed stomatal conductance data obtained by the LI-1600, the SC-1, and the AP-4. Data were obtained in field conditions with paired samples having identical environmental conditions. Statistics on the non log transformed data are also included.
* Values are descriptive statistics only.
Delta T devices. Draft Leaf Porometer (SC-1) Evaluation. Unpublished manuscript. October 2006.
Doug Cobos, Decagon Devices