c3_temperature_param_sharkey | R Documentation |
Parameters describing the temperature response of important C3 photosynthetic
parameters, intended to be passed to the
calculate_temperature_response
function.
c3_temperature_param_sharkey
List with 11 named elements that each represent a variable whose temperature-dependent value can be calculated using an Arrhenius equation or a polynomial equation:
Gamma_star_at_25
: The value of chloroplastic CO2 concentration
at which CO2 gains from Rubisco carboxylation are exactly balanced by
CO2 losses from Rubisco oxygenation (Gamma_star
) at 25
degrees C.
Gamma_star_norm
: Gamma_star
normalized to its value at
25 degrees C.
gmc_norm
: The mesophyll conductance to CO2 diffusion
(gmc
) normalized to its value at 25 degrees C.
J_norm
: The electron transport rate (J
) normalized to
its value at 25 degrees C.
Kc_at_25
: The Michaelis-Menten constant for rubisco
carboxylation (Kc
) at 25 degrees C.
Kc_norm
: Kc
normalized to its value at 25 degrees C.
Ko_at_25
: The Michaelis-Menten constant for rubisco oxygenation
(Ko
) at 25 degrees C.
Ko_norm
: Ko
normalized to its value at 25 degrees C.
RL_norm
: The rate of non-photorespiratory CO2 release in the
light (RL
) normalized to its value at 25 degrees C.
Tp_norm
: The maximum rate of triose phosphate utilization
(Tp
) normalized to its value at 25 degrees C.
Vcmax_norm
: The maximum rate of rubisco carboxylation
(Vcmax
) normalized to its value at 25 degrees C.
In turn, each of these elements is a list with at least 2 named elements:
type
: the type of temperature response
units
: the units of the corresponding variable.
Many of these parameters are normalized to their values at 25 degrees C. These
variables include _norm
in their names to indicate this.
Response parameters were obtained from Sharkey et al. (2007). In this
publication, gas concentrations are expressed as partial pressures (in
Pa
or kPa
) rather than mole fractions (micromol / mol
or
mmol / mol
). However, for consistency with
c3_temperature_param_bernacchi
, here we prefer to use mole
fractions.
To convert a concentration expressed as a partial pressure (P
; in
Pa
) to a concentration expressed as a mole fraction (C
; in
micromol / mol
), we need a value for atmospheric pressure; we will use
the typical value of 101325 Pa
. Then C = P / 101325 * 1e6
or
C = P * cf
, where cf = 1e6 / 101325
is a conversion factor. The
same correction can be used to convert kPa
to mmol / mol
. The
value of cf
can be accessed using PhotoGEA:::c_pa_to_ppm
.
References:
Sharkey, T. D., Bernacchi, C. J., Farquhar, G. D. & Singsaas, E. L. "Fitting photosynthetic carbon dioxide response curves for C3 leaves" Plant, Cell & Environment 30, 1035–1040 (2007) [\Sexpr[results=rd]{tools:::Rd_expr_doi("10.1111/j.1365-3040.2007.01710.x")}].
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