Try beta.chemspider
- 4 of 5 defined stereocentres
(3aR,5R,6S,6aR)-5-[(4S)-2,2-Dimethyl-1,3-dioxolan-4-yl]-2,2-dimethyl-6-propoxytetrahydrofuro[2,3-d][1,3]dioxole
CCCO[C@@H]1[C@@H]2[C@H](O[C@@H]1C3COC(O3)(C)C)OC(O2)(C)C
InChI=1S/C15H26O6/c1-6-7-16-11-10(9-8-17-14(2,3)19-9)18-13-12(11)20-15(4,5)21-13/h9-13H,6-8H2,1-5H3/t9?,10-,11+,12-,13-/m1/s1
WHYCYJUAIQNWPT-ZLOUSURVSA-N
CSID:17462198, http://www.chemspider.com/Chemical-Structure.17462198.html (accessed 07:33, Apr 30, 2024)
Validated by Experts, Validated by Users, Non-Validated, Removed by Users
Predicted data is generated using the ACD/Labs Percepta Platform - PhysChem Module, version: 14.00
Predicted data is generated using the US Environmental Protection Agency�s EPISuite
Log Octanol-Water Partition Coef (SRC): Log Kow (KOWWIN v1.67 estimate) = 1.82 Boiling Pt, Melting Pt, Vapor Pressure Estimations (MPBPWIN v1.42): Boiling Pt (deg C): 346.62 (Adapted Stein & Brown method) Melting Pt (deg C): 119.37 (Mean or Weighted MP) VP(mm Hg,25 deg C): 3.8E-005 (Modified Grain method) Subcooled liquid VP: 0.000328 mm Hg (25 deg C, Mod-Grain method) Water Solubility Estimate from Log Kow (WSKOW v1.41): Water Solubility at 25 deg C (mg/L): 332.2 log Kow used: 1.82 (estimated) no-melting pt equation used Water Sol Estimate from Fragments: Wat Sol (v1.01 est) = 2418.3 mg/L ECOSAR Class Program (ECOSAR v0.99h): Class(es) found: Neutral Organics Henrys Law Constant (25 deg C) [HENRYWIN v3.10]: Bond Method : 9.89E-014 atm-m3/mole Group Method: Incomplete Henrys LC [VP/WSol estimate using EPI values]: 4.551E-008 atm-m3/mole Log Octanol-Air Partition Coefficient (25 deg C) [KOAWIN v1.10]: Log Kow used: 1.82 (KowWin est) Log Kaw used: -11.393 (HenryWin est) Log Koa (KOAWIN v1.10 estimate): 13.213 Log Koa (experimental database): None Probability of Rapid Biodegradation (BIOWIN v4.10): Biowin1 (Linear Model) : -1.8484 Biowin2 (Non-Linear Model) : 0.0000 Expert Survey Biodegradation Results: Biowin3 (Ultimate Survey Model): 2.0547 (months ) Biowin4 (Primary Survey Model) : 3.0462 (weeks ) MITI Biodegradation Probability: Biowin5 (MITI Linear Model) : 0.1395 Biowin6 (MITI Non-Linear Model): 0.0041 Anaerobic Biodegradation Probability: Biowin7 (Anaerobic Linear Model): -1.6445 Ready Biodegradability Prediction: NO Hydrocarbon Biodegradation (BioHCwin v1.01): Structure incompatible with current estimation method! Sorption to aerosols (25 Dec C)[AEROWIN v1.00]: Vapor pressure (liquid/subcooled): 0.0437 Pa (0.000328 mm Hg) Log Koa (Koawin est ): 13.213 Kp (particle/gas partition coef. (m3/ug)): Mackay model : 6.86E-005 Octanol/air (Koa) model: 4.01 Fraction sorbed to airborne particulates (phi): Junge-Pankow model : 0.00247 Mackay model : 0.00546 Octanol/air (Koa) model: 0.997 Atmospheric Oxidation (25 deg C) [AopWin v1.92]: Hydroxyl Radicals Reaction: OVERALL OH Rate Constant = 62.1187 E-12 cm3/molecule-sec Half-Life = 0.172 Days (12-hr day; 1.5E6 OH/cm3) Half-Life = 2.066 Hrs Ozone Reaction: No Ozone Reaction Estimation Fraction sorbed to airborne particulates (phi): 0.00396 (Junge,Mackay) Note: the sorbed fraction may be resistant to atmospheric oxidation Soil Adsorption Coefficient (PCKOCWIN v1.66): Koc : 10 Log Koc: 1.000 Aqueous Base/Acid-Catalyzed Hydrolysis (25 deg C) [HYDROWIN v1.67]: Rate constants can NOT be estimated for this structure! Bioaccumulation Estimates from Log Kow (BCFWIN v2.17): Log BCF from regression-based method = 0.701 (BCF = 5.024) log Kow used: 1.82 (estimated) Volatilization from Water: Henry LC: 9.89E-014 atm-m3/mole (estimated by Bond SAR Method) Half-Life from Model River: 1.029E+010 hours (4.289E+008 days) Half-Life from Model Lake : 1.123E+011 hours (4.679E+009 days) Removal In Wastewater Treatment: Total removal: 2.11 percent Total biodegradation: 0.09 percent Total sludge adsorption: 2.02 percent Total to Air: 0.00 percent (using 10000 hr Bio P,A,S) Level III Fugacity Model: Mass Amount Half-Life Emissions (percent) (hr) (kg/hr) Air 7.82e-007 4.13 1000 Water 27.2 1.44e+003 1000 Soil 72.7 2.88e+003 1000 Sediment 0.0887 1.3e+004 0 Persistence Time: 1.73e+003 hr
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