fT.Century2

Calculates the effects of temperature on decomposition rates according to
the CENTURY model.

Functions for modeling Soil Organic Matter decomposition
in terrestrial ecosystems with linear and nonlinear systems of differential equations.
The package implements
models according to the compartmental system representation described in
Sierra and others (2012) <doi:10.5194/gmd-5-1045-2012> and Sierra and others (2014)
<doi:10.5194/gmd-7-1919-2014>.

Carlos Sierra

SoilR

Models of Soil Organic Matter Decomposition

fT.Century2 function

<dl><dt>Temp</dt>
<dd>A scalar or vector containing values of temperature for which
the effects on decomposition rates are calculated.</dd>
<dt>Tmax</dt>
<dd>A scalar defining the maximum temperature in degrees C.</dd>
<dt>Topt</dt>
<dd>A scalar defining the optimum temperature for the decomposition
process in degrees C.</dd></dl>

Arguments

Effects of temperature on decomposition rates according the the CENTURY
model — fT.Century2

<dl>

<dt>Temp</dt>
<dd>A scalar or vector containing values of temperature for which
the effects on decomposition rates are calculated.</dd>


<dt>Tmax</dt>
<dd>A scalar defining the maximum temperature in degrees C.</dd>


<dt>Topt</dt>
<dd>A scalar defining the optimum temperature for the decomposition
process in degrees C.</dd>

</dl>

fT.Century2: Effects of temperature on decomposition rates according the the CENTURY model

Description

Usage

Value

Arguments

References