| 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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