1982
DOI: 10.1016/0004-6981(82)90265-7
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Smick—A scavenging model incorporating chemical kinetics

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Cited by 8 publications
(3 citation statements)
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“…The small increase in NH4 + concentration observed in the target area could be associated with a liquid-phase SO2-SO4--oxidation mechanism involving NH3, such as that proposed by Scott and Hobbs [1967]. Test calculations using SMICK [Drewes and Hales, 1982] have shown that if fully effective and acting alone this mechanism would result in unreasonably high NH4 + concentrations and pH values and comparatively small SO4--concentrations. It is possible, however, that this mechanism or a similar one may be potentially effective in increasing NH4 + concentrations in the target area while not observably affecting sulfate or hydrogen ion.…”
Section: Plume-related Deposition Of Sulfur Within the First 15 Km Rementioning
confidence: 85%
“…The small increase in NH4 + concentration observed in the target area could be associated with a liquid-phase SO2-SO4--oxidation mechanism involving NH3, such as that proposed by Scott and Hobbs [1967]. Test calculations using SMICK [Drewes and Hales, 1982] have shown that if fully effective and acting alone this mechanism would result in unreasonably high NH4 + concentrations and pH values and comparatively small SO4--concentrations. It is possible, however, that this mechanism or a similar one may be potentially effective in increasing NH4 + concentrations in the target area while not observably affecting sulfate or hydrogen ion.…”
Section: Plume-related Deposition Of Sulfur Within the First 15 Km Rementioning
confidence: 85%
“…The other component, the grid vertical velocity, is determined by the shape of the hypothetical orographic barrier shown in Figure 5 Subroutine HENRY (Table 5-13) computes the effective solubility parameter for S02' as described in Equations (68)-(71). The subroutine was borrowed directly from a previous code (Drewes and Hales;. FUNCTION SSAT (Table 5-14) computes the saturation vapor density with respect to ice, "and is needed to calculate the depositional growth rate for snow.…”
Section: Class I Subroutine Descriptionsmentioning
confidence: 99%
“…GR 10/ N,DZ ,DT,OZl,DZN,EF (50) ,EFSQ 50 Class III subroutine HENRY is presented in Table 31. This subroutine was borrowed directly from a previous code [Drewes and Hales (1977)], and computes a solubility coefficient HPRIME for S02 in water, which is defined by the equation y = HPRIME c Here y denotes the mole fraction of S02 in the gas phase, and c is its equilibrium concentration (moles/cm 3 ) in water. Arguments in the call sequence are as follows: c mole fraction S02 in gas phase or concentration S02 (moles total dissolved s02/cm3) in water HEX acidity of water in moles/liter T temperature, oK P pressure, atmospheres…”
Section: H Class III Subroutinesmentioning
confidence: 99%