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dlebauerAlomir
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update tillage specification (#138)
* update tillage specification * clarified language 🤞 * Update docs/parameters.md --------- Co-authored-by: Mike Longfritz <[email protected]>
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docs/model-structure.md

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@@ -245,9 +245,8 @@ Total heterotrophic respiration is the sum of respiration from soil and litter p
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$$
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R_{H} = f_{R_H} \cdot
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\left(\sum_j K_j \cdot C_j
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\mathfrak{\cdot D_{\text{tillage,}j}}
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\right) \cdot
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D_{\text{temp}} \cdot D_{\text{water,}R_H} \cdot D_{CN}
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D_{\text{temp}} \cdot D_{\text{water,}R_H} \cdot D_{CN} \mathfrak{\cdot D_{\text{tillage}}}
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\tag{7}\label{eq:rh}
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$$
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@@ -613,24 +612,22 @@ urease inhibitors (Gurung et al 2021) that slow down the rate.
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### $\frak{Tillage}$
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To represent tillage, we define two new adjustment factors that modify the decomposition rates
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of litter $K_{\text{litter}}$ and soil organic matter $K_{\text{som}}$:
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To represent the effect of tillage on decomposition rate, we define the tillage dependency function $D_{\textrm{till}}$, which is a function of a tillage effect $f_{\textrm{till}}$:
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Event parameters from the `events.in` file:
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$$
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D_{\textrm{till}}(t) = 1 + f_{\textrm{till}}\cdot e^{-t/30} \tag{25}\label{eq:till}
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$$
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$f_{\textrm{till}}$ is specified in the `events.in` file, and $D_{\textrm{till}}(t)$ is multiplied by the $KC$ term in the calculation of $R_H$ (Eq. \eqref{eq:rh}).
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* SOM decomposition modifier $D_{K\text{,tillage,litter}}$
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* Litter decomposition modifier $D_{K\text{,tillage,som}}$
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A value of $f_{\textrm{till}}=0.2$ represents an initial 20% increase that will exponentially decay. The rate of exponential decay is 1/30 days. This rate was chosen such that $D_{\textrm{till}}$ integrates to 30, which is equivalent to DayCent’s 30‑day step function.
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These values specified as fractions (e.g. 0.2 for 20% increase in decomposition rate). They are set to 0 by default and are expected to be >0. They are set in the `events.in`, and are effective for one month after the tillage event.
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If multiple tillage events at times $t_z$ occur with effects $f_{\textrm{till,}z}$, they add linearly thus:
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$$
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K^{\prime}_{\text{i}} = K_{\text{i}} \cdot (1+D_{K\text{,tillage,}i})
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D_{\textrm{till}}(t) = 1 + \sum_{z} f_{\textrm{till,}z}\, e^{-(t-t_{z})/30},\quad t\ge t_{z}.
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$$
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Where $i$ is either litter or soil organic matter pool, and $K^{\prime}$ is the transiently adjusted decomposition rate.
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The choice of one month adjustment period is based on DayCent (Parton et al 2001).
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### $\frak{Planting \ and \ Emergence}$
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A planting event is defined by its emergence date and directly specifies the amount of carbon added to each of four plant carbon pools: leaf, wood, fine root, and coarse root. On the emergence date, the model initializes the plant pools with the amounts of carbon specified in the events file.
@@ -646,7 +643,12 @@ Because a harvest event only specifies the fraction of above and belowground car
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The removed fraction is calculated as follows:
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$$
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F^C_{\text{harvest,removed}} = f_{\text{remove,above}} \cdot C_{\text{above}} + f_{\text{remove,below}} \cdot C_{\text{below}}
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% these next two eqns can prob. be simplified
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% noting that f_removed + f_transfer = 1
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% and using i \in \{\text{above}, \text{below}\}
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% and j in removed, litter
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F^C_{\text{harvest,removed}} = f_{\text{remove,above}} \cdot C_{\text{above}} + f_{\text{remove,below}} \cdot C_{\text{root}}
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\tag{27}\label{eq:harvest_removed}
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$$
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The fraction transferred to litter is calculated as follows:

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