28-10 Handbook of Dynamic System Modeling
marsh sector diagram of Figure 28.3, a line from high marsh plants goes to detritus and another line from
insects to birds is added. The line from rats and raccoons to birds is also reversed (rats and raccoons eat
birds eggs but few rats and raccoons are eaten by birds in the marsh). Finally, a missing line is added from
salt to the primary producers.
Only the low-elevation portion of the marsh sector has been translated into equations and simulated
in this chapter. The equation list for this simulation is given in Table 28.1. Equations for the high marsh
portion would differ little other than in the calibration of constants to reflect high marsh conditions.
The correspondence between equations in Table 28.1 and the symbols on the diagram (Figure 28.3)
will become apparent by cross-referencing the diagram labels with the column of Table 28.1 labeled
“Meaning.”
The 16 storages involved in the low marsh subsector are listed first in Table 28.1 (Eqs. [001]–[016]).
These are followed by the rate equations, then model inputs, model constants, and the time parameters
used in the simulation. A total of 141 entries are made in Table 28.1.
28.3.1 Equation Naming Convention Used in this Chapter
The equation list uses a naming convention for variables that helps to track the relationship among model
variables. In general, storage i is indicated by Q
i
and rates of flow from storage j to storage
k
by J
jk
. Marsh
variables are preceded by an M and estuarine water variables by a W. For example, MQ
7
represents the
marsh plants (Eq. [007]), and WQ
4
the nutrients in estuarine water (Eq. [077]). MJ
71
represents the flow
from plants to detritus (MQ
1
) in the marsh (Eq. [048]). J
W4M4
represents the two-way interaction (upper
left of the diagram in Figure 28.3) that defines exchange of nutrients between the water and the marsh.
By listing W
4
as the first subscript, the positive direction is toward the marsh for this two-way nutrient
exchange. Equally, a negative flow represents export of nutrients from the marsh.
Constants in rate equations are indicated by a K. An A denotes an auxiliary variable that must first
be calculated to assign a value to a flow rate. Constants and auxiliaries are prefixed and subscripted like
the rate to which they apply. MA
20
, for example, denotes the light available for evaporation of water
(Eq. [031]), which is used to compute evaporation (MJ
20
, Eq. [040]). The latter equation also uses the
proportionality constant denoted as MK
20
.
A subscript of 0 indicates a location outside the system boundary. A flow from a source outside the
boundary to a given storage i is labeled J
0i
. Sunlight from outside the system is assimilated by benthic
microalgae (MQ
9
), for example, so their rate of gross primary production is labeled MJ
09
(Eq. [034]).
Conversely, flows that leave the system from storage i are denoted by J
i0
. The flow MJ
a0
, for example,
identifies the metabolic heat loss from microbes (MQ
a
). The equation number for MJ
a0
is 054 in Table 28.1.
Note that the constant in the equation, MK
a0
, has the same subscript. If more than one flow from a given
source connects to the same sink, the flows are distinguished by a third character appended to the name.
Evaporation and transpiration, which are two ways in which water leaves the marsh system boundary, are
represented by MJ
20
(Eq. [040]) and MJ
207
(Eq. [041]), respectively. The added 7, in this case, indicates
plants (MQ
7
) that are involved in the rate. Additional characters are also used to distinguish the same flow
converted to different units. Burial of detritus in sediment requires energy units when subtracted from
the detritus storage as MJ
15
(Eq. [035]), but requires mass units when added to the sediment as MJ
15D
(Eq. [036]).
Likewise, if more than one auxiliary variable is calculated for the same flow rate, a third subscript is
used. To calculate gross primary production of low marsh plants (MJ
07
, Eq. [033]), for example, requires
calculation of available light (MA
07a
, Eq. [027]), and a multiplier based on other environmental conditions
(MA
07b
, Eq. [028]).
Model constants associated with a flow have the same subscript as the flow. For example, the equation
for assimilation of meiofauna by macrofauna, MJ
bc
, has a constant MK
bc
(Eq. [060]). As before, where
a given equation has more than one constant, a third character is appended to distinguish the two. The
equation for the two-way exchange of sediment between estuary and marsh (J
W6M5
, Eq. [025]) has a rate
constant K
W6M5
for restoring equilibrium, and an equilibrium constant K
W6M5n
.