Lecture 04
September 9, 2024
…all models are approximations. Essentially, all models are wrong, but some are useful. However, the approximate nature of the model must always be borne in mind….
— Box & Draper, Empirical Model Building and Response Surfaces, 1987
Text: VSRIKRISH to 22333
Eutrophication: common environmental problem in which plants and algae feed on excess nutrients and become overabundant.
Excess N and P can come from:
Excess nutrients are stored in sediment and recycled back into the lake, as well as transported by organisms/consumers.
Non-Point Source (NPS) Pollution: Intermittent, distributed waste input to surface or groundwater
It can be difficult to restore to oligotrophic state:
Restoration takes a long time and is not guaranteed (hysteresis)!
Common Approach: Mass-Balance
\[\frac{\partial\text{Mass}}{\partial t} = \text{Inputs} - \text{Outputs} - \text{Decay}\]
Assuming steady-state and decay is linear w.r.t mass:
\[\begin{align*} \frac{\partial\text{Mass}}{\partial t} &= \text{Inputs} - \text{Outputs} - \text{Decay} = 0 \\ \frac{\partial(CV)}{\partial t} &= \sum_j PS_j + \sum_i NPS_i - CQ_\text{out} - \alpha CV = 0 \end{align*}\]
\[ \begin{gather*} \sum_j PS_j + \sum_i NPS_i - CQ_\text{out} - \alpha CV = 0 \\ \Rightarrow \qquad C(Q_\text{out} + \alpha V) = \sum_j PS_j + \sum_i NPS_i \\ \Rightarrow \qquad \bbox[5pt, border: 5px solid red]{C = \frac{\sum_j PS_j + \sum_i NPS_i}{Q_\text{out} + \alpha V}} \end{gather*} \]
\[ \begin{align*} C &= \frac{\sum_i P_i/V}{Q/V + \alpha} \\[0.75em] &= \frac{\sum_i P_i/V}{\tau_w^{-1} + \alpha} \\[0.75em] &= \frac{\sum_i P_i/V}{\sum_j k_j} \end{align*} \]
What does this model assume?
What are potential impacts and acceptable levels or critical thresholds?
Generally need to limit average P concentrations to \(< 0.01-0.02\) mg/L.
\[\begin{align*} C = \frac{\sum_j PS_j + \sum_i NPS_i}{Q_\text{out} + \alpha V} &\leq \left(0.01\ \text{mg/L}\right)\left(\frac{1\ \text{mg/L}}{1000\ \text{kg/m}^3}\right) \\[0.5em] \Rightarrow \qquad \sum_j PS_j + \sum_i NPS_i &\leq \left(1 \times 10^{-5}\right) \left(Q_\text{out} + \alpha V\right) \end{align*}\]
Vollenweider model for lake P sedimentation:
\[\alpha = \frac{10}{\bar{H}} \approx \frac{10A}{V}\]
\[\begin{gather*} \Rightarrow \qquad \sum_j PS_j + \sum_i NPS_i \leq \left(1 \times 10^{-5}\right) \left(Q_\text{out} + 10A\right) \\ \Rightarrow \qquad \sum_j PS_j + \sum_i NPS_i \leq 7000\ \text{kg/yr} \\ \end{gather*}\]
Type | Area (ha) | Unit P Load (kg/ha) |
---|---|---|
Forest | 20,000 | 0.11 |
Corn | 1,000 | 2.0 |
Pasture | 3,000 | 1.0 |
Residential | 1,000 | 1.2 |
Business | 200 | 3.0 |
Unit loads taken from Osmond et al. (1997).
Type | Area (ha) | Unit P Load (kg/ha) |
---|---|---|
Forest | 20,000 | 0.11 |
Corn | 1,000 | 2.0 |
Pasture | 3,000 | 1.0 |
Residential | 1,000 | 1.2 |
Business | 200 | 3.0 |
\[\sum_i NPS_i = 9000\ \text{kg}\]
In other words, the “typical” NPS load is
\[\sum_i NPS_i = 9000\ \text{kg}.\]
This is greater than the acceptable total P load for a target concentration of 0.01 mg/L!
What can we do?
What we do next depends on whether we’re taking a prescriptive or a descriptive approach.
\[\sum_j PS_j(t) + \sum_i NPS_i(t) - C(t)Q(t) - \alpha C(t)V = F(t)\]
Wednesday: System Dynamics (Feedbacks/Bifurcations)
Next Week: Simulation Models
Homework 2: Released, due 9/19 at 9pm