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�-" <br /> Al. <br /> Mnv'�' ; - -, 11- 1 <br /> ' To 4 M <br /> 4MM001 <br /> V- 0.M <br /> r, <br /> �iLS G6-2 <br /> • wysicai State (at 20'C): liq=c (60) i <br /> • color: colorless to brou-n (6G) <br /> v Odor: characteristic kerosene 1ika (60) <br /> • Odor 'threshold: ,o data E i <br /> • Liouid Densis (g/ml at 20'C' :fuel oil ^os. Z. <br /> 2-D - .87-.95• fuel ail nos. <br /> 1-D (at 15'C) - .81-.936 (60) <br /> Freezing/Melsing ?oint CC)" -48-13 (60) <br /> • 5oili=g Point ('C)• 131- >SSE (60) <br /> • rlasa Point ('C): =antes =-om 38-74 for various <br /> grades a= !�.el oil -no. I to 69-169 for grades 394,SQ6, <br /> Of fuel oil ao. 3 207) <br /> • Flammablo -J, in Ai`, lk by Vol=m: 0.6-1.3% (51.60 i <br /> to 5-0-7.5% for fuel•oil nos. 1 - 3 5:6,507) <br /> ?HYSIGQ- • Autoigoition Temper:xzvro ('C): 177-329 (51,60,506.1 <br /> r:MUCAL dapandiu; on grade for fael oil nos. 1 - 3 507,513) <br /> DATA • Vapor Pressure (= Hg a= 21'C)• 2..12-26.4 (60) ; <br /> ■ Saturated Concentration im Air <br /> (09/=3 at 20-C): not available ) j <br /> • Solubility in Slater (mg/L at 20'C): _ (27,97) <br /> • Viscosity: fuel oil nos. 1. 2 <br /> 1-D. 2-D (cp at 21-C) - 1.152-1.965: ::uel I <br /> oil row. 4, 5, 6 (ep at 3S-C) - 14.5-493.5 (60) <br /> • Suriaca Tension (dyne/cm ac 201C): 21-32 (60) <br /> • Log (Octaaol-Water Partition Coefficiene), <br /> In R : 3.3-7.06 (TMi <br /> a Soil A.orptioa Coefficient. 'K : 962- I <br /> 5.5 x 104 <br /> oc #� <br /> E <br /> o Henry's Law Constant (ata-m3/mol at 20'C): { <br /> 5.9 x 10-5 - 7.4 (�) <br /> •' 3ioco:neentration Faccor: hot available ( ) — <br /> Dicsal oil hyr3roc2sbons are e__caected to have moderate <br /> mobility and moderate persistence in most susiace soils; <br /> pgrsisteree in deep soils and ground Waver hay be nighrx. <br /> Volatilization, sorption, phot aoxid.aci.on. and i <br /> biodegradation are all potential `ate processes. Surface. i <br /> Spills may be weathered to i limited exr.cnt by evaporation; <br /> FEi5ISTE•10E downward mi�racion of wearhered surface spills and <br /> IN Tri£ SOIL- sub-surface discharges represent a potential threaz to i <br /> VATZR SYSTES inderlying ground water. Biodegradation or fuel oil i <br /> hydrocarbons is exvected to occur under envi;or=encai <br /> conditions favorable to microbial oxidation: r-arurally- <br /> Occurring, `►ydracarbon-degradin, mi.croorgarisys have been <br /> isolated __om u:olluzed soils and, to a lesser extent. non- <br /> polluted soils. The hydroc=bons of residual f"I oils are � <br /> expected to be less mobile ilos:er aaLeous solubility. zi.gher <br /> sorption and lower volacili--T) and more persistent (slower <br /> biodegradation) than Che z_gncor diesel oil 4yarocarbons, f <br /> Range of values for representative hydrocarbons from ma-lor co=uorenc <br /> tlasses (see Table 66-3). <br /> a/n7 <br />