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PE EIE[R-Rg RESEARCH ON - HJ Andrews Experimental Forest

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This function is asymptotic to zero respiration<br />

at both low and high temperatures an d<br />

exhibits an exponential increase in respiratio n<br />

followed by a rapid decline at high<br />

temperatures .<br />

The completed functional expression fo r<br />

Psn(L,T) is :<br />

Psn(L,T) = -Boexp[B 1 (T-B2 )-exp(B 1 (T-B2 ))]<br />

+ [ B 2 + B3 ( T -B4 ) 2 ] [1 - exp(B s L ) ]<br />

(4)<br />

The intent of this model is to predict ne t<br />

photosynthesis in light and CO 2 losses in<br />

darkness. The model is not useful for predicting<br />

gross photosynthesis without including<br />

some function for respiration in the light .<br />

Until the experimental techniques for obtaining<br />

such measurements are developed, th e<br />

light respiration term must remain implicit i n<br />

the gross photosynthesis function . This limit s<br />

the use of the model although most C 3 plant s<br />

will respond similarly . A different model may<br />

be required for C 4 plants such as grasses that<br />

require a much higher light level to saturat e<br />

photosynthesis .<br />

Methods and Materials<br />

Values for the six parameters in the model<br />

were determined with a least squares fit of th e<br />

data using an algorithm developed by Marquardt<br />

(1963) . Net photosynthetic data were<br />

taken with a controlled environment syste m<br />

developed by Webb (1971) . The test organis m<br />

for the model was red alder (Alnus rubra<br />

Bong.) .<br />

Forty red alder seedlings, 1- to 2-years-old ,<br />

were removed from the field and propagated<br />

in a nutrient culture before transferring them<br />

to the gas-tight controlled environment chamber.<br />

The root system of the seedlings was en -<br />

closed in a nutrient flow system with temperature<br />

controlled at 11°C ± 1°C . The plants<br />

were maintained in this system for 1 month at<br />

conditions of light and temperature consisten t<br />

with those in the greenhouse .<br />

Carbon dioxide absorption rates were measured<br />

by monitoring the CO 2 depletion in the<br />

gas-tight environment chamber with a Beckman<br />

IR gas analyzer. Atmospheric CO 2 levels<br />

in the chamber were maintained between 32 0<br />

and 335 p .p.m. Light energy was varied from<br />

0.06 to 0 .68 ly/min (total shortwave radiation)<br />

at air temperatures from 5 to 30°C . For<br />

each of five light levels, CO 2 uptake was<br />

measured while temperature was changed a t<br />

the rate of 1° per 5 minutes beginning at<br />

15°C and proceeding upscale to approximately<br />

30°C . Measurements were then made<br />

while decreasing temperature at the same rat e<br />

until near 5°C at which time temperature wa s<br />

increased again up to 16°C . All CO 2 uptak e<br />

measurements were made during 3 successiv e<br />

days. Relative humidity varied between 6 5<br />

percent at low temperatures to 75 percent at<br />

high temperatures .<br />

Results<br />

A portion of the data is plotted in figures 3<br />

and 4 . The photosynthetic response to radiation<br />

in figure 3 is characterized by a linea r<br />

response at low light followed by the usual<br />

light-saturated response at high radiation . Thi s<br />

is consistent with the findings of many other<br />

investigators . The saturation value for ne t<br />

photosynthesis increases with temperature ,<br />

but the increase is not linear .<br />

Figure 4 shows the net photosynthetic<br />

response to temperature for constant radiation<br />

of 0 .19 ly/min . A quadratic function wa s<br />

fit to the data and the parameters with their<br />

respective standard errors are listed in figure<br />

4 . At 0.19 ly/min, net photosynthesis has a<br />

maximum of 20 .5°C. Although these data<br />

represent the temperature range between 5 .5 °<br />

and 27°, the data of Pisek et al . (1969) indicate<br />

a nearly symmetrical response betwee n<br />

5° and 40°C. Extrapolation of the quadratic<br />

beyond this temperature range should b e<br />

done cautiously although Phillips an d<br />

McWilliams (1971) have measured zero CO 2<br />

fluxes at high temperatures . It may be that<br />

high temperatures increase respiration until it<br />

exceeds the photosynthetic capacity .<br />

Figure 5 illustrates the response surface<br />

generated by expression (4) which is the net<br />

239

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