Photosynthesis and Photorespiration in Whole ... - Plant Physiology
Photosynthesis and Photorespiration in Whole ... - Plant Physiology
Photosynthesis and Photorespiration in Whole ... - Plant Physiology
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736<br />
[180<br />
V. d[ 180 = [180 . dv - 2 u. dt<br />
2 2 [16Q is<br />
I 02] + I 0 ]<br />
dl[ 180 -dv u.dt/V<br />
[180] V 1[1602] + [180 ]<br />
By subtract<strong>in</strong>g equation I from equation 3:<br />
GERBAUD AND ANDRE <strong>Plant</strong> Physiol. Vol. 64, 1979<br />
The comparison of the P, derived from this formula with the value<br />
(2) already known is a test of the validity of our measures.<br />
PHYSIOLOGICAL VALUE OF THE MEASUREMENTS<br />
The measure of the true rate of 02 uptake can be biased by two<br />
(3) causes. (a) If the 02 from photosynthesis is taken up as well as the<br />
external 02 <strong>in</strong> the process of photorespiration, then our measurement<br />
will be less than the true rate. This sort of recycl<strong>in</strong>g seems to<br />
be neligible, due to the high relative pressure of the outer 02 (22).<br />
d[ 80 1 d[Ne] - u.dt/V<br />
1 2] [Ne] 160 ] + [ 180<br />
Dur<strong>in</strong>g the course of the day, the total 02 concentration [02] stays<br />
<strong>in</strong> the range 21 to 22%, so that we may consider it as a constant <strong>in</strong><br />
the <strong>in</strong>tegration of equation 4:<br />
(4)<br />
z<br />
0<br />
z<br />
8<br />
Trd[Ne] d[ 1802 2<br />
1 T<br />
=Fu.dt<br />
INe 118 O<br />
Jo [Ne] [ °2]- [02].V 0<br />
Hence:<br />
[02] *V I[0210 [Ne]1<br />
U = <strong>in</strong> TJ<br />
[[118021 [NeIT<br />
(5)<br />
(6)<br />
The net 02 evolution P0 was calculated from the <strong>in</strong>crease of 02<br />
concentration <strong>in</strong> the chamber. In the unit time the plant assimilates<br />
a volume Pc of CO2, (k+ 1) Pc of the mixture (CO2 + kN2) is<br />
<strong>in</strong>jected <strong>in</strong>to the chamber <strong>and</strong> the plant produced P0 of 02;<br />
therefore the follow<strong>in</strong>g volume must be expelled from the chamber:<br />
Lv<br />
=<br />
(k+1)Pc<br />
+<br />
P0 - Pc<br />
or<br />
Av<br />
=<br />
k.P c<br />
+P<br />
(7)<br />
conta<strong>in</strong><strong>in</strong>g an amount 11602] Av of 1602.<br />
The plant produces only 1602, <strong>and</strong> <strong>in</strong> our case 1802 is about 50<br />
times less concentrated <strong>in</strong> the cell than 1602, so that we shall<br />
equate here the uptake of 1602 with the total 02 uptake U. Hence<br />
the <strong>in</strong>crease of 1602 <strong>in</strong> the chamber is:<br />
V A[ 16 ] 1<br />
T<br />
0 2<br />
1 [ + k p [16<br />
T<br />
1160<br />
L<br />
2<br />
'r 64<br />
(8) .f<br />
-E<br />
z<br />
(9) o<br />
w<br />
A<br />
HOURS<br />
C02<br />
0 x<br />
D<br />
a<br />
a<br />
k.<br />
- 2C<br />
From P. we calculate the photosynthetic ratio po/PC. The gross 02<br />
evolution E was calculated from the net evolution plus the uptake:<br />
E = PO + U.<br />
Test of <strong>Photosynthesis</strong>. There is another way of measur<strong>in</strong>g<br />
photosynthesis than count<strong>in</strong>g the pulses of <strong>in</strong>jected CO2: the<br />
decrease of neon concentration is related to volume dv, (eq. 1),<br />
which is proportional to the photosynthesis, because AV = k<br />
Pc+P0 <strong>in</strong> equation 7 can be replaced with<strong>in</strong> a good approximation<br />
by (k+ 1) Pc, that is, set <strong>in</strong> the differential form: dv = (k+ 1) Pcdt,<br />
hence:<br />
d[Ne] / [Ne] = - (k+1) pC.dt / V (10)<br />
1 T dN 1 [me]0<br />
= 1T kV1 d{Ne] = 1 V n (11)<br />
P =<br />
_ln ---<br />
c T k+1 o [Ne] T k+1 [HeiT<br />
0<br />
-<br />
y 2( to -10DO<br />
Y.<br />
R<br />
I-<br />
- T<br />
n n n<br />
of I I 1- 1 a I I I I I I 0<br />
Q, I - - - - - "<br />
2 4 6 8 10 12 1x 16 18 20 22 24<br />
HOURS<br />
FIG. 1. Recorded data dur<strong>in</strong>g a typical day of a 46-day-old plant of<br />
wheat (day/night temperature 20.3 C/18.4 C, PAR irradiance 175 w m-2,<br />
02= 21%, CO2 = 335 ,l/1). The two parts show <strong>in</strong> parallel the time course<br />
of the gas exchanges (A), <strong>and</strong> the isotopic concentrations (B). PR: net<br />
photosynthesis (C02); R: night respiration; T: transpiration. The decrease<br />
of 1802 traces the 02 traces the 02 uptake by the plant, us<strong>in</strong>g Ne as an<br />
<strong>in</strong>ternal st<strong>and</strong>ard. The slight variations of 1602 correspond to the photosynthesis<br />
or respiration. Initial concentrations were [18021 = 2970,l/1, [Ne]<br />
= 3,160 ul/l; isotopes were added before the beg<strong>in</strong>n<strong>in</strong>g of the light periods<br />
when their concentrations went under 0.5%.<br />
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Copyright © 1979 American Society of <strong>Plant</strong> Biologists. All rights reserved.