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Last modified
8/11/2009 11:32:55 AM
Creation date
8/10/2009 3:11:54 PM
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UCREFRP
UCREFRP Catalog Number
7200
Author
Odenkirchen, E. W. and R. Eisler.
Title
Chlorpyrifos Hazards to Fish, Wildlife, and Invertebrates
USFW Year
1988.
USFW - Doc Type
A Synoptic Review.
Copyright Material
NO
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<br />ENVIRONMENTAL CHEMISTRY <br /> <br />Formulations of ch1orpyrifos include emulsifiable concentrates, wettable <br />powders, granules, pellets, microencapsulates and impregnated materials. <br />Suggested di1uents for concentrates include water and petroleum distillates, <br />such as kerosene and diesel oil. Carrier compounds include synthetic clays <br />with alkyl/aryl su1fonates as wetting agents (Table 1). Little information is <br />available to assess the influence of various use formulations on toxicity, <br />dispersal, decomposition, and bioavai1abi1ity. Chemical and other properties <br />of ch10rpyrifos are summarized in Table 2. <br /> <br />The degradation half-life time (Tb1) of ch10rpyrifos is 7.1 days in <br />seawater (Schimmel et a1. 1983), and 532days in distilled water (Freed et a1. <br />1979). Degradation is usually through hydrolysis to produce <br />3,5,6-trich10ro-2-pyridino1, and phosphorthioic acid (Brust 1966; Smith 1966, <br />1968; Marshall and Roberts 1978). Temperature, ~H, radiation, and metal <br />cations all significantly affect ch10rpyrifos Tb- in water: half-life is <br />decreased with increasing water pH, temperature', su~light, and metal cation <br />concentrations (Brust 1966; Mortland and Raman 1967; Smith 1968; Schaefer and <br />Dupras 1969, 1970; Meikle and Youngson 1970). <br /> <br />In soil, Tb1 values for ch1orpyrifos range from less than 1 week to <br />more than 24 w€eks, depending on soil moisture, microbial activity, clay and <br />organic content, and temperatu~e. In t11 soils studied, increasing <br />temperature resulted in decreased Tb- values (Miles et a1. 1983). <br />Degradation was more rapid in sandy loam th&n in organic muck soils, more <br />rapid in moist than in dry soils, and more rapid in clay than in other soil <br />types (Getzin 1981; Miles et a1. 1983, 1984). The major routes of <br />ch1orpyrifos loss from soils are chemical hydrolysis in moist soils, <br />clay-catalyzed hydrolysis in dry soils, and microbial degradation and <br />volatilization (Marshall and Roberts 1978). <br /> <br />The half-life of ch10rpyrifos in sediments is comparatively long; it was <br />24 days in a sediment-water slurry (Schimmel et a1. 1983). In a pond treated <br />with ch10rpyrifos, total waterborne residues decreased by a factor of more <br />than lOX, while total sediment residues rose by about 3X (Hurlbert et a1. <br />1970). Similar results were noted in an artificial lake treated with <br />chlorpyrifos: lake water concentrations peaked 1 day after treatment at 0.9 <br />Jg/1 and plateaued near 0.2 ug/l after 3 weeks (Mu11a et a1. 1973). <br /> <br />2 <br />
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