Pesticide is removed from the reach segment in outflow. The amount of dissolved and particulate pesticide removed from the reach segment in outflow is:
pstsol,oβ=QβVFdββpstrchwtrββ 7:4.1.13
pstsorb,oβ=QβVFpββpstrchwtrββ 7:4.1.14
where pstsol,oβ is the amount of dissolved pesticide removed via outflow (mg pst), pstsorb,oβ is the amount of particulate pesticide removed via outflow (mg pst), Q is the rate of outflow from the reach segment (m3 H2βO/day), Fdβ is the fraction of total pesticide in the dissolved phase, Fpβ is the fraction of total pesticide in the particulate phase, pstrchwtrβ is the amount of pesticide in the water (mg pst), and V is the volume of water in the reach segment (m3 HO).
Table 7:4-1: SWAT+ input variables that pesticide partitioning.
: Pesticide settling velocity (m/day)
.swq
CHPST_KOC
Kdβ: Pesticide partition coefficient (m3/g)
.swq
CHPST_REA
kp,aqβ: Rate constant for degradation or removal of pesticide in the water (1/day)
.swq
CHPST_VOL
vvβ: Volatilization mass-transfer coefficient (m/day)
.swq
CHPST_STL
Pesticides will partition into particulate and dissolved forms. The fraction of pesticide in each phase is a function of the pesticideβs partition coefficient and the reach segmentβs suspended solid concentration:
Fdβ=1+Kdββconcsedβ1β 7:4.1.1
Fpβ=1+KdββconcsedβKdββconcsedββ=1βFdβ 7:4.1.2
where Fdβ is the fraction of total pesticide in the dissolved phase, Fpβ is the fraction of total pesticide in the particulate phase, Kdβ is the pesticide partition coefficient (m3/g), and concsedβ is the concentration of suspended solids in the water (g/m3).
The pesticide partition coefficient can be estimated from the octanol-water partition coefficient (Chapra, 1997):
7:4.1.3
where is the pesticide partition coefficient (m/g) and is the pesticideβs octanol-water partition coefficient (mg m(mg m)). Values for the octanol-water partition coefficient have been published for many chemicals. If a published value cannot be found, it can be estimated from solubility (Chapra, 1997):
7:4.1.4
where is the pesticide solubility (moles/L). The solubility in these units is calculated:
7:4.1.5
where is the pesticide solubility (moles/L), is the pesticide solubility (mg/L) and is the molecular weight (g/mole).
Pesticide in the particulate phase may be removed from the water layer by settling. Settling transfers pesticide from the water to the sediment layer. The amount of pesticide that is removed from the water via settling is:
pststl,wtrβ=depthvsβββFpββpstrchwtrββTT 7:4.1.12
where pststl,wtrβ is the amount of pesticide removed from the water due to settling (mg pst), vsβ is the settling velocity (m/day), depth is the flow depth (m), Fpβ is the fraction of total pesticide in the particulate phase, pstrchwtrβ is the amount of pesticide in the water (mg pst), and TT is the flow travel time (days).
Pesticides in both the particulate and dissolved forms are subject to degradation. The amount of pesticide that is removed from the water via degradation is:
pstdeg,wtrβ=kp,aqββpstrchwtrββTT 7:4.1.6
where pstdeg,wtrβ is the amount of pesticide removed from the water via degradation (mg pst), kp,aqβ is the rate constant for degradation or removal of pesticide in the water (1/day), pstrchwtrβ is the amount of pesticide in the water at the beginning of the day (mg pst), and TT is the flow travel time (days). The rate constant is related to the aqueous half-life:
kp,aqβ=t1/2,aqβ0.693β 7:4.1.7
where kp,aqβ is the rate constant for degradation or removal of pesticide in the water (1/day), and is the aqueous half-life for the pesticide (days).
Pesticide in the dissolved phase is available for volatilization. The amount of pesticide removed from the water via volatilization is:
pstvol,wtrβ=depthvvβββFdββpstrchwtrββTT 7:4.1.8
where pstvol,wtrβ is the amount of pesticide removed via volatilization (mg pst), vvβ is the volatilization mass-transfer coefficient (m/day), depth is the flow depth (m), Fdβ is the fraction of total pesticide in the dissolved phase, pstrchwtrβ is the amount of pesticide in the water (mg pst), and TT is the flow travel time (days).
The volatilization mass-transfer coefficient can be calculated based on Whitmanβs two-film or two-resistance theory (Whitman, 1923; Lewis and Whitman, 1924 as described in Chapra, 1997). While the main body of the gas and liquid phases are assumed to be well-mixed and homogenous, the two-film theory assumes that a substance moving between the two phases encounters maximum resistance in two laminar boundary layers where transfer is a function of molecular diffusion. In this type of system the transfer coefficient or velocity is:
7:4.1.9
where is the volatilization mass-transfer coefficient (m/day), is the mass-transfer velocity in the liquid laminar layer (m/day), is the mass-transfer velocity in the gaseous laminar layer (m/day), is Henryβs constant (atm m mole), is the universal gas constant ( atm m (K mole)), and is the temperature (K).
For rivers where liquid flow is turbulent, the transfer coefficients are estimated using the surface renewal theory (Higbie, 1935; Danckwerts, 1951; as described by Chapra, 1997). The surface renewal model visualizes the system as consisting of parcels of water that are brought to the surface for a period of time. The fluid elements are assumed to reach and leave the air/water interface randomly, i.e. the exposure of the fluid elements to air is described by a statistical distribution. The transfer velocities for the liquid and gaseous phases are calculated:
7:4.1.10
where is the mass-transfer velocity in the liquid laminar layer (m/day), is the mass-transfer velocity in the gaseous laminar layer (m/day), is the liquid molecular diffusion coefficient (m/day), is the gas molecular diffusion coefficient (m/day), is the liquid surface renewal rate (1/day), and is the gaseous surface renewal rate (1/day).
OβConnor and Dobbins (1958) defined the surface renewal rate as the ratio of the average stream velocity to depth.
7:4.1.11
where is the liquid surface renewal rate (1/day), is the average stream velocity (m/s) and is the depth of flow (m).
Pesticide in a reach segment is increased through addition of mass in inflow as well as resuspension and diffusion of pesticide from the sediment layer. The amount of pesticide in a reach segment is reduced through removal in outflow as well as degradation, volatilization, settling and diffusion into the underlying sediment.