Chemical Fact Sheet

Chemical Abstract Number (CAS #) 309002
CASRN 309-00-2
1,4:5,8-Dimethanonaphthalene, 1,2,3,4,10,10-hexachloro-, 1,4,4a,5,8,8a-hexahydro-, endo,exo-
Analytical Methods EPA Method 505
EPA Method 508
EPA Method 525.2
EPA Method 608
EPA Method 617
EPA Method 625
EPA Method 8081
EPA Method 8270
Molecular FormulaC12H8Cl6

Link to the National Library of Medicine's Hazardous Substances
Database for more details on this compound.

Use INSECTICIDE (ESP AGAINST TERMITES); INSECTICIDE AGAINST SOIL & COTTON INSECTS, TURF PESTS, WHITE GRUBS & CORN ROOTWORMS. SRP: FORMER USE INSECTICIDE HIGHLY EFFECTIVE AGAINST A RANGE OF SOIL-DWELLING PESTS AT 0.5 TO 5.0 KG/HECTARE. SRP: FORMER USE Aldrin has been used mainly against insects, primarily soil insects, which attack field, forage, vegetable, and fruit crops. Effective against termites, used for wood preservation and to combat ant infestations.
Apparent Color COLORLESS CRYSTALLINE SOLID ; White crystalline substance. ; Colorless needles ; Brown to white, crystalline solid ; Tan to dark brown solid
Odor Mild chemical odor
Boiling Point 145 deg C at 2 mm Hg
Melting Point 104 DEG C
Molecular Weight 364.93
Density 1.6 at 20 deg C/4 deg C (solid)
Environmental Impact Aldrin is no longer produced or used in the United States and any past releases have probably been converted to dieldrin. Aldrin residues in soil and plants will volatilize from soil surfaces or be slowly transformed to dieldrin in soil. Biodegradation is expected to be slow and aldrin is not expected to leach. Aldrin was classified as moderately persistent meaning its half-life in soil ranged from 20-100 days. Aldrin residues in water will volatilize from the water surface and photooxidization is expected to be significant. Photolysis has been observed in water, although the absorption characteristics of aldrin indicate it should not extensively directly photolyze in the environment. Bioconcentration will be significant. Adsorption to sediments is expected and biodegradation is expected to be slow. Vapor phase xpected to be slow. Vapor phase aldrin residues in the atmosphere are expected to react with photochemically erated hydroxyl radicals with an estimated half-life of 35.46 min. Aldrin in s expected to be adsorbed to particulate matter and no rate can ed for the reaction of adsorbed aldrin with hydroxyl radicals. Direct lysis may also occur, in spite of the low absorption of aldrin at >290 nm. r, is expected to be a slow process relative to reaction with icals. Due to the cessation of aldrin manufacture and use in the posure of humans in the USA to the chemical is expected to be low.
Environmental Fate TERRESTRIAL FATE: APPLICATION OF ALDRIN AT 3, 9, & 15 KG AI/HA IN CLAY LOAM & SANDY LOAM SOIL EVERY YEAR FROM 1972-1974 SHOWED RESIDUES REMAINED LONGER IN CLAY LOAM THAN IN SANDY LOAM SOIL. RATE OF CONVERSION TO DIELDRIN WAS HIGHER IN SANDY LOAM THAN IN CLAY LOAM SOIL. ALDRIN RESIDUES LEACHED INTO SOIL WITH RAIN WATER. NEITHER ALDRIN NOR DIELDRIN TRANSLOCATED IN MAIZE, PEARL MILLET PLANTS & GRAINS. UNDER MOST ENVIRONMENTAL CONDITIONS ALDRIN IS GRADUALLY CONVERTED TO DIELDRIN. AFTER ADDITION OF ALDRIN TO SOIL SAMPLES, WATER SOLUBLE DICARBOXYLIC ACID WAS ISOLATED. AFTER PREPARATIVE ISOLATION & METHYLATION, GC, MS SHOWED MATERIAL TO BE IDENTICAL WITH AUTHENTIC DIHYDROCHLORDENDICARBOXYLIC ACID DIMETHYL ESTER . TERRESTRIAL FATE: Aldrin was applied at 1.5 kg ai/ha to flooded soil. After 30, 90, 120, 240, and 270 days, 44.2%, 55.4%, 74.13%, 88.07%, and 100% of the aldrin had dissipated from the soil . Aldrin applied at 20 lb/6 "in" acre to muck and loam had respective half-lives of 3.75 and 2.40 months for the first half-year and 13.0 and 9.7 months for the following three years . Three and one-half years following the application to a Miami silt loam of 20 and 200 lb aldrin/6 in acre, 1.12% and 2.55%, respectively, of the calculated initial amount of aldrin remained . Aldrin was applied 20 lb/6 "in" acre to Miami silt loam and at 100 lb/6 in acre to Plainfield sand . After incubation for 56 days at 6, 26, and 46 deg C, 83.8%, 55.7% and 13.7% of the initial amount of recoverable aldrin remained on the Miami silt loam and 63%, 38%, and 10.2% remained on the Plainfield sand, respectively . After 2 months incubation at 30 deg C, 44%, 58%, and 33% of about 15 ppm of aldrin applied remained in the Maahas, Louisiana, and Casiguran soils under upland (80% water saturated), respectively, and under flooded conditions, 65%, 81%, 74%, and 64% remained in the Pila, Maahas< uisiana and Casiguran soils, respectively . Soils were treated with aldrin at 5 lb/acre from 1958-62 . Dieldrin was formed from aldrin in the soil and constituted 50 and 90% of the aldrin plus dieldrin residues recovered in 1959 and 1963, respectively . Soils from AR, FL, HI, MD, MT, OR, and SC were treated with 10 ml of 0.5% aqueous aldrin emulsion/10 g soil . The preparations were placed randomly around a test site in the Harrison Experimental Forest in southern Mississippi. In all preparations except the Hawaiian soil, the percent degradation in the upper 0.5 inch layer (36-72%) was greater than in the lower layer (unspecified depth) (11-33%). In the Hawaiian soil samples, degradation in the lower layer was 63% and in the upper layer was 49% . Aldrin was converted into dieldrin in these studies . When aldrin was applied to agricultural soils in Germany, Spain, England and the United States, significant amounts of dieldrin derived from the applied aldrin were detected in the soils within 6 months of aldrin application(6). Aldrin was classified as moderately persistent meaning its half-life in soil ranged from 20-100 days(7). AQUATIC FATE: A river die away test was conducted in capped bottles with aldrin in raw water from the Little Miami River in Ohio. The river receives domestic and industrial wastes and farm runoff. After 2, 4, and 8 weeks, 20, 60, and 80% of the initial amount of aldrin had degraded . Volatilization from water is also expected to be significant and will occur at a rate directly proportional to the rapidity of wind and current velocity and inversely proportional to the depth of the water body. Bioconcentration and adsorption to sediments are expected to be significant. Photooxidation is expected to be significant. Biodegradation is expected to be slow. ATMOSPHERIC FATE: The half-life for the reaction of vapor phase aldrin with photochemically generated hydroxyl radicals in the atmosphere was estimated to be 35 min . Slow photolysis of aldrin vapor (60% in one week vs 16% in a dark control) was observed . This is expected due to the weak absorption of aldrin above 290 nm . Direct photolysis, therefore, is not expected to be significant compared to reaction with hydroxyl radicals.
Drinking Water Impact SURFACE WATER: Major USA rivers - 100 sites, maximum residue 0.085 ug/l . Niagara-on-the-Lake, 1980-82, 75 samples, 1% pos, <0.1 ng/l avg . New Jersey - 604 samples,

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