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

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where T = leaf temperature, ° K<br />

S = solar radiation, gcal cm-2 min<br />

Pn = net photosynthesis rate ,<br />

mg CO 2 (g dry wt)-1 hr 1<br />

(3i = parameters to be estimate d<br />

Equation 7 was derived from equation 8 and<br />

equation 9 :<br />

P(L)=a+b 1nS (8)<br />

which had been used to fit photosynthesis dat a<br />

from several herbaceous species (Blackman an d<br />

Rutter 1946, Blackman and Wilson 1951) .<br />

Equation 8 was coupled with equation 9 suggested<br />

by data of Pisek and Winkler (1958) ,<br />

Krueger and Ferrell (1965), and others :<br />

G(T) = a + bT + cT2 (9 )<br />

Data from two species of oak were obtained<br />

from infrared gas analysis and wer e<br />

used to estimate the parameters of equation 7<br />

by stepwise multiple regression analysis . Som e<br />

of the terms of equation 7 were nonsignificant,<br />

and were thus discarded . The final<br />

model was :<br />

Pn =Qo +(3 1 T+(3 2 In S+(3 5 T In S (10 )<br />

Having estimated the parameters of equation<br />

10, the model was used to predict photo -<br />

synthesis of oak in the field . Their model gav e<br />

fair to good agreement with subsequentl y<br />

measured net photosynthesis .<br />

In terms of the criteria discussed above ,<br />

equation 10 is generally inadequate . It doe s<br />

allow for interaction between two variables but<br />

fails to take into consideration other factor s<br />

that affect photosynthetic rate (stomatal behavior,<br />

micrometeorological conditions, plan t<br />

nutrition) . The model does satisfy the requirement<br />

that the Pn model be solved as a functio n<br />

of systems variables, that is, Pn = f [S, T] .<br />

In terms of the other criteria, the model fall s<br />

short of having a great deal of theoretica l<br />

validity in that the function is one of convenience<br />

rather than having general physicalchemical<br />

meaning . It is unnecessary to discuss<br />

in detail Botkin's model with respect to the<br />

other criteria . Like most photosynthesis models,<br />

it is specified at the leaf level, where th e<br />

inputs to the leaf are measured, and the<br />

relations between the leaf subsystems are<br />

inferred .<br />

While his model has many failings, it doe s<br />

have one virtue. If one were interested in<br />

comparing Pn = f[T,L] in two species under<br />

identical conditions, this model may be adequate,<br />

given that some other factor, e .g . ,<br />

stomatal resistance, is not limiting . The fact<br />

that the parameters of the model were estimated<br />

by least-squares allows the use o f<br />

statistical tests useful in comparing such data .<br />

Energy Budget Mode l<br />

Idso and Baker (1968) based their model of<br />

photosynthesis and their earlier model (Ids o<br />

and Baker 1967) on that of Gates (1965 )<br />

which is an energy budget model where precis e<br />

measurement of incoming radiant energy is<br />

equated with outgoing energy . Thus, at equilibrium,<br />

the amount of energy leaving a leaf i s<br />

equal to that coming in . Gates ' (1965) leaf<br />

energy budget model is :<br />

where<br />

(1 +r) (S + s) (<strong>Rg</strong>' +R a)<br />

as 2 +a t 2 (11 )<br />

-e taTZ ± C±LE= 0<br />

a s = mean total absorbance of plant to<br />

sunlight and skyligh t<br />

r = reflectance of underlying ground<br />

or plane surface to sunlight and<br />

skylight, S and s<br />

at = absorbance of plant to thermal<br />

radiation, <strong>Rg</strong> and Ra<br />

e t = emissivity of plant to thermal<br />

radiatio n<br />

Tl = leaf temperature ° K<br />

C = energy gained or lost by convection<br />

cal cm-2 min- 1<br />

L = latent heat of evaporation ca l<br />

cm-2 miri- l<br />

E = transpiration rate of leaf gm cal - 2<br />

min- 1<br />

S, s, <strong>Rg</strong>, Ra = various short and lon g<br />

wave radiation inputs ca l<br />

cm-2 min 1<br />

232

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