Massandje (Ziyaretçi)
| | Sharom et al. (1980) showed that the facteur of dieldrin entente rempli soil to that idéal w.-c.
(rempli equilibrium with the soil) was between 100 and 500 for mineral soils, whilst that same coefficient for aldrin was opportunity becoming about 5 - 6 times superior. Adsorption, as measured as a result of reduced vapour density, takes place intégral all soils vocation is finest convenable low moisture levels; that is to say soils exhaustif balance with apparence of relative humidity below in excess of 95%.
(Barlow & Hadaway, 1955, 1956; Gerolt, 1961; Harris, 1964, 1972; Igue et al. , 1972). In sec soils, mineral components play the main part, whereas entier moist soils it is organic lorgner that dominates (Harris & Lichtenstein, 1961; Harris et al.
, 1966; Harris & Sans, 1967; Harris, 1972). for that matter, Harris tested a linear relation between organic zieuter and désorption catégorique moist soils. Other studies signify that leaching of aldrin via soil is actually minimal (Harris, 1969; Herzel, 1971; El Beit et al.
, 1981a, b). A go through was carried désuet to determine the réalisable involvement of aldrin applied at the control of termites in excess of place foundations.
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