P-CYMENE

4-Isopropyltoluene

99-87-6

p-Isopropyltoluene

Dolcymene

Para-cymene

p-Cymol

Paracymene

Camphogen

p-Methylcumene

1-Isopropyl-4-methylbenzene

4-Cymene

2-p-Tolylpropane

Cymol

CYMENE

Benzene, 1-methyl-4-(1-methylethyl)-

p-Methylisopropylbenzene

Paracymol

1-Methyl-4-isopropylbenzene

p-Cimene

4-Isopropyl-1-methylbenzene

Cumene, p-methyl-

4-Methylisopropylbenzene

1-Methyl-4-(1-methylethyl)benzene

p-methyl cumene

p-Isopropylmethylbenzene

4-Methyl-1-isopropylbenzene

Cymene, p-

Benzene, 1-isopropyl-4-methyl-

Isopropyltoluene

1-methyl-4-(propan-2-yl)benzene

4-Isopropyltoluol

FEMA No. 2356

4-Isopropylbenzyl radical

4-methyl isopropylbenzene

4-Cymol

NSC 4162

1-methyl-4-propan-2-ylbenzene

HSDB 5128

Methyl-4-(1-methylethyl)benzene

4-methyl-1-(propan-2-yl)benzene

EINECS 202-796-7

UNII-1G1C8T1N7Q

1-isopropyl-4-methyl-Benzene

1G1C8T1N7Q

DTXSID3026645

CHEBI:28768

AI3-02272

NSC-4162

p-Mentha-1,3,5-triene

DTXCID006645

EC 202-796-7

1-Methyl-4-(1-methylethyl)-benzene

MFCD00008893

CYMENE (MART.)

CYMENE [MART.]

BENZENE,1-ISOPROPYL,4-METHYL P-CYMENE

4939-75-7

para cymene

CAS-99-87-6

isopropyltoluol

p-methyl-Cumene

4-lsopropyltoluene

MML

?4-Isopropyltoluene

p-Cymene, 99%

p-Cymene [UN2046] [Flammable liquid]

p-Cymene [UN2046] [Flammable liquid]

Carvacrol derivative, 8

p-Methylisopropyl benzene

P- Isopropylmethylbenzene

P-CYMENE [FHFI]

P-CYMENE [HSDB]

P-CYMENE [INCI]

P-CYMENE [FCC]

P-CYMENE [MI]

bmse000503

P-CYMENE [WHO-DD]

p-Cymene, analytical standard

1-Methyl-4-isopropyl benzene

p-Cymene, >=97%, FG

CHEMBL442915

NSC4162

BDBM248165

benzene, 1-methyl-4-methylethyl-

WLN: 1Y1 & R D1

1-(1-methylethyl)-4-methylbenzene

Tox21_201932

Tox21_300338

s5598

AKOS000121521

Benzene, 1-methyl-4(1-methylethyl)-

CCG-266123

LMPR0102090014

MCULE-1794861612

p-Isopropyltoluene, analytical standard

USEPA/OPP Pesticide Code: 122103

NCGC00247998-01

NCGC00247998-02

NCGC00254425-01

NCGC00259481-01

AC-34132

AS-11012

NS00005157

S0664

EN300-21455

C06575

Q284072

W-100013

p-Cymene, certified reference material, TraceCERT(R)

F8889-6466

Z104497772

InChI=1/C10H14/c1-8(2)10-6-4-9(3)5-7-10/h4-8H,1-3H

The Henry's Law constant for p-cymene is estimated as 0.011 atm-cu m/mole(SRC), derived from its vapor pressure, 1.5 mm Hg(1), and water solubility, 23.4 mg/L(2). This Henry's Law constant indicates that p-cymene is expected to volatilize rapidly from water surfaces(3). Based on this Henry's Law constant, the volatilization half-life from a model river (1 m deep, flowing 1 m/sec, wind velocity of 3 m/sec)(3) is estimated as 3.5 hours if adsorption is neglected(SRC). The volatilization half-life from a model lake (1 m deep, flowing 0.05 m/sec, wind velocity of 0.5 m/sec)(3) is estimated as 4.6 days if adsorption is neglected(SRC). The volatilization half-life from a model pond is about 30 days if adsorption is considered(4). p-Cymene's estimated Henry's Law constant indicates that volatilization from moist soil surfaces may occur(SRC). p-Cymene is expected to volatilize from dry soil surfaces based upon its vapor pressure(SRC).
Literature: (1) Daubert TE, Danner RP; Physical and Thermodynamic Properties of Pure Chemicals Data Compilation Washington, DC: Taylor and Francis (1996) (2) Banerjee S et al; Environ Sci Technol 11: 1227-29 (1980) (3) Lyman WJ et al; Handbook of Chemical Property Estimation Methods. Washington

Using a structure estimation method based on molecular connectivity indices(1), the Koc of p-cymene can be estimated to be 1120(SRC). According to a classification scheme(2), this estimated Koc value suggests that p-cymene is expected to have low mobility in soil.
Literature: (1) US EPA; Estimation Program Interface (EPI) Suite. Ver. 4.11. Nov, 2012. Available from, as of July 29, 2013: http://www.epa.gov/oppt/exposure/pubs/episuitedl.htm (2) Swann RL et al; Res Rev 85: 17-28 (1983)

ANILINE

Benzenamine

Phenylamine

62-53-3

Aminobenzene

Aminophen

Arylamine

Kyanol

Anilin

Cyanol

Benzeneamine

Krystallin

Benzidam

Anyvim

Anilina

Huile D'aniline

C.I. Oxidation Base 1

Rcra waste number U012

CI Oxidation Base 1

Caswell No. 051C

Anilinum

C.I. 76000

HSDB 43

CCRIS 44

NCI-C03736

Aniline and homologues

Aniline reagent

UN 1547

CHEBI:17296

UNII-SIR7XX2F1K

SIR7XX2F1K

EINECS 200-539-3

ANILINE-N,N-D2

EPA Pesticide Chemical Code 251400

Aniline-1-13C

CI 76000

DTXSID8020090

AI3-03053

MFCD00007629

DTXCID9090

EC 200-539-3

Benzene, amino

Anilin [Czech]

ANILINE (IARC)

ANILINE [IARC]

ANILINE (MART.)

ANILINE [MART.]

ANILINE (USP-RS)

ANILINE [USP-RS]

Huile d'aniline [French]

ANILINE (USP IMPURITY)

ANILINE [USP IMPURITY]

Phenyleneamine

D'aniline

RCRA waste no. U012

Anilina [Italian, Polish]

FENTANYL IMPURITY F (EP IMPURITY)

FENTANYL IMPURITY F [EP IMPURITY]

Aniline and homologs

MESALAZINE IMPURITY K (EP IMPURITY)

MESALAZINE IMPURITY K [EP IMPURITY]

TRIMETHOPRIM IMPURITY K (EP IMPURITY)

TRIMETHOPRIM IMPURITY K [EP IMPURITY]

UN1547

benzenaminium

cyanole

BIDD:ER0581

phenyl amine

phenyl-amine

8-aniline

Benzene, amino-

Fentanyl impurity F

PhNH2

ANILINUM [HPUS]

ANILINE [HSDB]

ANILINE [INCI]

ANILINE [MI]

ANILINE [WHO-DD]

CHEMBL538

Epitope ID:117704

Aniline, analytical standard

Aniline, AR, >=99%

Aniline, LR, >=99%

C6H5NH2

Discontinued, see H924510

BDBM92572

Trimethoprim specified impurity K

Aniline, ReagentPlus(R), 99%

BENZENE,AMINO (ANILINE)

DTXSID50207744

DTXSID70178043

Aniline [UN1547] [Poison]

AMY11081

STR00216

Aniline, ACS reagent, >=99.5%

Tox21_200345

STK301792

AKOS000268796

DB06728

MCULE-9347486445

NCI 176889

Aniline, ASTM, ACS reagent, 99.5%

Aniline, SAJ first grade, >=99.0%

CAS-62-53-3

Aniline, JIS special grade, >=99.0%

Aniline, p.a., ACS reagent, 99.0%

NCGC00091297-01

NCGC00091297-02

NCGC00091297-03

NCGC00257899-01

BP-12047

Aniline, PESTANAL(R), analytical standard

DB-013441

A0463

NS00010656

EN300-33390

C00292

A833829

AMINOBENZOIC ACID IMPURITY C [EP IMPURITY]

Q186414

SR-01000944923

J-519591

SR-01000944923-1

Q27121173

F2190-0417

InChI=1/C6H7N/c7-6-4-2-1-3-5-6/h1-5H,7H

Aniline, United States Pharmacopeia (USP) Reference Standard

136260-71-4

The measured Henry's Law constant for aniline is 2.02X10-6 atm-cu m/mole(1). This Henry's Law constant indicates that aniline is expected to volatilize from water surfaces(2). Based on this Henry's Law constant, the volatilization half-life from a model river (1 m deep, flowing 1 m/sec, wind velocity of 3 m/sec)(2) is estimated as 12 days(SRC). The volatilization half-life from a model lake (1 m deep, flowing 0.05 m/sec, wind velocity of 0.5 m/sec)(2) is estimated as 131 days(SRC). Aniline's Henry's Law constant(1) indicates that volatilization from moist soil surfaces may occur(SRC). Aniline is not expected to volatilize from dry soil surfaces(SRC) based upon a vapor pressure of 0.67 mm Hg(3).
Literature: (1) Jayasinghe DS et al; Environ Sci Technol 26: 2275-81 (1992) (2) Lyman WJ et al; Handbook of Chemical Property Estimation Methods. Washington, DC: Amer Chem Soc pp. 15-1 to 15-29 (1990) (3) Daubert TE, Danner RP; Physical and Thermodynamic Properties of Pure Chemicals Data Compilation Washington, DC: Taylor and Francis, (2002)

Primary anilines may bind to soils due to the ability of the aromatic amino group to form covalent bonds with humic and fulvic material in soils(1). The Koc of aniline in 5 European soils was reported in the range of 43.8-497.7(2). The Koc values in 2 silt loams were 130 and 410 with the higher value occurring in the more acidic soil(3). The Koc of aniline in colloidal organic carbon from groundwater (pH 6.5) was reported as 3,870(4). The adsorption constant for adsorption to H-montmorillonite (pH 8.35) and Na-montmorillonite (pH 6.8) is 1,300 and 130(5). The Koc of aniline in 3 silt-clay loams were 269 (pH 4.4), 48 (pH 6.5) and 16 (pH 7.2)(6). A mean Koc value of 55 was determined for aniline in 4 sewage sludges(7). The Koc in five second-generation reference EUROSOILS was 8, 32, 19, 27 and 137(8). According to a classification scheme(9), this Koc data suggests that aniline may have very high to medium mobility in soil. The pKa of aniline is 4.60(10, indicating that this compound will partially exist in the protonated (cation) form; however, in the pH range between pH5 and pH9, aniline will exist primarily in the non-protonated form; in the protonated form in the environment, cations generally adsorb more strongly to soils containing organic carbon and clay than their neutral counterparts(11). In a sorption study using pond sediment from Cherokee Park pond in Athens GA, the sorption kinetics of aniline were characterized by a rapid initial loss of aniline from the aqueous phase followed by a much slower rate of disappearance. The initial sorption was a reversible cation-exchange followed by a slower covalent-binding. It was shown that at pH values greater than the pKa, sorption kinetics were slower than at pH3.75 (rate constants of 4.53-7.95/hr above versus 13.3 below)(12).
Literature: (1) Adrian P et al; Chemosphere 18: 1599-1609 (1989) (2) Gawlik BM et al; Chemosphere 36: 2903-19 (1998) (3) Pillai P et al; Chemosphere 11: 299-317 (1982) (4) Means JC; Amer Chem Soc 186th Natl Mtg 23: 250-1 (1982) (5) Bailey GW et al; Soil Sci Soc Amer Proc 32: 222-34 (1968) (6) Lee LS et al; Environ Toxicol Chem 16: 1575-82 (1997) (7) Kordel W et al; Chemosphere 35: 107-19 (1997) (8) Gawlik BM et al; Chemosphere 41: 1337-47 (2000) (9) Swann RL et al; Res Rev 85: 17-28 (1983) (10) Perrin DD; Dissociation Constants of Organic Bases in Aqueous Solution. IUPAC Chem Data Series. Suppl. London Buttersworth (1972) (11) Doucette WJ; pp. 141-188 in Handbook of Property Estimation Methods for Chemicals. Boethling RS, Mackay D, eds. Boca Raton, FL: Lewis Publ (2000) (12) Weber EJ et al; Environ Sci Technol 35: 2470-75 (2001)
Literature: #Under short-term conditions (24-hr), the sorption of aniline in a silty clay soil was not solely dependent on cation exchange and that solubility was a consideration(1); passing rainwater through a soil column had no effect on the sorption to the silty clay soil(1). Using four Indiana soils and one Iowa soil, abiotic loss of aniline from the aqueous phase to the soil phase occurred with an initial rapid loss due to reversible mass transfer processes followed by a slow loss due to irreversible reactions(2).
Literature: (1) Donaldson FP, Nyman MC; Chemosphere 65: 854-62 (2006) (2) Fabrega-Duque JR et al; Environ Sci Technol 34: 1687-93 (2000)

methanethiol

METHYL MERCAPTAN

Methylmercaptan

Mercaptomethane

74-93-1

Methyl sulfhydrate

Thiomethanol

Methanthiol

Thiomethyl alcohol

Metilmercaptano

Methvtiolo

Methylmercaptaan

Mercaptan methylique

Methaanthiol

Thiomethane

RCRA waste number U153

FEMA No. 2716

Methanethiole

CH3SH

methyl-mercaptan

Methyl thioalcohol

MeSH

UN 1064

2X8406WW9I

Methaanthiol [Dutch]

Methanthiol [German]

Methvtiolo [Italian]

Methylmercaptaan [Dutch]

Metilmercaptano [Italian]

Metilmercaptano [Spanish]

SCH 54292

Methyl mercaptan (natural)

Mercaptan methylique [French]

HSDB 813

EINECS 200-822-1

UN1064

RCRA waste no. U153

BRN 1696840

methylsulfanyl

methane thiol

methyl sulfides

methyl thiol

methyl-thiol

UNII-2X8406WW9I

(methyl)sulfane

Methylthioalcohol

a methyl thioether

sulfonium methylide

Methanethiol, purum

Methanethiol, 98.0%

METHANETHIOL [MI]

EC 200-822-1

Methanethiol, >=98.0%

4-01-00-01273 (Beilstein Handbook Reference)

METHYL MERCAPTAN [FHFI]

METHYL MERCAPTAN [HSDB]

DTXSID5026382

CHEBI:16007

CHEBI:86315

DTXSID10168842

DTXSID60992376

InChI=1/CH4S/c1-2/h2H,1H

NSC229573

AKOS009157032

NSC-229573

Methyl mercaptan [UN1064] [Poison gas]

NS00020025

C00409

Q409309

17719-48-1

Z22

The Henry's Law constant for methyl mercaptan is estimated as 0.0031 atm-cu m/mole(SRC) derived from its vapor pressure, 1,510 mm Hg(1), and water solubility, 15,400 mg/L(2). This Henry's Law constant indicates that methyl mercaptan is expected to volatilize rapidly from water surfaces(3). Based on this Henry's Law constant, the volatilization half-life from a model river (1 m deep, flowing 1 m/sec, wind velocity of 3 m/sec)(3) is estimated as 0.8 hours(SRC). The volatilization half-life from a model lake (1 m deep, flowing 0.05 m/sec, wind velocity of 0.5 m/sec)(3) is estimated as 2.8 days(SRC). Methyl mercaptan's Henry's Law constant indicates that volatilization from moist soil surfaces is expected to occur(SRC). Methyl mercaptan is expected to volatilize rapidly from dry soil surfaces based upon its vapor pressure and because it is a gas a temperatures above 6 deg C(SRC). However, gaseous methyl mercaptan gas has been found to strongly adsorb to moist and dry soil surfaces suggesting that adsorption might be an environmental sink for methyl mercaptan(4). Therefore, the importance of volatilization from soil surfaces may be attenuated by adsorption(SRC).
Literature: (1) Daubert TE, Danner RP; Physical and Thermodynamic Properties of Pure Chemicals Data Compilation. Washington, DC: Taylor and Francis (1989) (2) Hine J, Mookerjee PK; J Org Chem 40: 292-8 (1975) (3) Lyman WJ et al; Handbook of Chemical Property Estimation Methods. Washington, DC: Amer Chem Soc pp. 15-1 to 15-29 (1990) (4) Smith KA et al; Soil Sci 116: 313-9 (1973)

Using a structure estimation method based on molecular connectivity indices(1), the Koc of methyl mercaptan can be estimated to be 13(SRC). According to a classification scheme(2), this estimated Koc value suggests that methyl mercaptan is expected to have very high mobility in soil. Gaseous methyl mercaptan has been observed to partition to soils(3). For example, when gaseous methyl mercaptan was passed over six air-dried and moist (50% field capacity) soils, 2.4-32.1 mg/g and 2.2-21.4 mg/g of methyl mercaptan rapidly adsorbed to the dry and moist soils, respectively(3). Neither the capacity or rate of sorption was correlated to soil pH, organic matter content, or clay content; sterile controls ruled out the involvement of microorganisms(3); it was suggested that adsorption to soil surfaces might be an environmental sink for gaseous methyl mercaptan(3).
Literature: (1) US EPA; Estimation Program Interface (EPI) Suite. Ver. 4.1. Jan, 2011. Available from, as of July 19, 2012: http://www.epa.gov/oppt/exposure/pubs/episuitedl.htm (2) Swann RL et al; Res Rev 85: 17-28 (1983) (3) Smith KA et al; Soil Sci 116: 313-9 (1973)

Dimethyl disulfide

624-92-0

METHYL DISULFIDE

Dimethyldisulfide

Dimethyl disulphide

DMDS

Disulfide, dimethyl

2,3-Dithiabutane

(Methyldisulfanyl)methane

Methyldisulfide

Methyldithiomethane

(Methyldithio)methane

Sulfa-hitech

dimethyldisulphide

FEMA No. 3536

NSC 9370

1,2-Dimethyldisulfane

CCRIS 2939

HSDB 6400

EINECS 210-871-0

UNII-3P8D642K5E

CHEBI:4608

Dimethyl-d6 disulfide

AI3-25305

3P8D642K5E

NSC-9370

MFCD00008561

DTXSID4025117

(CH3S)2

EC 210-871-0

Paladin

UN2381

dimethydisulfide

methyl disulphide

Dimethyl disulfane

Disulfide dimethyl

MeS-SMe

Disulfide, dimethyl-

methyldisulfanyl methane

Dimethyl disulfide, 98%

Dimethyl disulfide, 99%

(Methyldisulfanyl)methane #

Dimethyl disulfide, >=99%

WLN: 1SS1

DTXCID805117

METHYL DISULFIDE [HSDB]

CHEMBL1347061

Dimethyl disulfide, >=99.0%

DIMETHYL DISULFIDE [FHFI]

NSC9370

BDBM233038

Dimethyl disulfide, >=98%, FG

AMY39506

EINECS 272-923-9

Tox21_201525

AKOS009157459

Dimethyl disulfide, analytical standard

MCULE-7451882535

UN 2381

NCGC00091798-01

NCGC00091798-02

NCGC00259075-01

CAS-624-92-0

Dimethyl disulfide, natural, >=98%, FG

D0714

Dimethyl disulfide, purum, >=98.0% (GC)

NS00001484

EN300-36043

InChI=1/C2H6S2/c1-3-4-2/h1-2H

C08371

E78981

A833808

Dimethyl disulfide [UN2381] [Flammable liquid]

Q419800

Q-100719

F0001-1676

The Henry's Law constant for dimethyl disulfide is reported as 1.21X10-3 atm-cu m/mole(1). This Henry's Law constant indicates that dimethyl disulfide is expected to volatilize rapidly from water surfaces(2). Based on this Henry's Law constant, the volatilization half-life from a model river (1 m deep, flowing 1 m/sec, wind velocity of 3 m/sec)(2) is estimated as 3.5 hours(SRC). The volatilization half-life from a model lake (1 m deep, flowing 0.05 m/sec, wind velocity of 0.5 m/sec)(2) is estimated as 4.1 days(SRC). Dimethyl disulfide's Henry's Law constant indicates that volatilization from moist soil surfaces may occur(SRC). In a laboratory study, the volatilization rate of dimethyl disulfide from a tidal marsh soil (at field capacity or 1.5 field capacity) ranged from 0.1 to 0.4 ng (sulfur basis)/min(3). Dimethyl disulfide is expected to volatilize from dry soil surfaces(SRC) based upon a vapor pressure of 28.7 mm Hg(4).
Literature: (1) Vitenberg AG et al; J Chromatography 112: 319-27 (1975) (2) Lyman WJ et al; Handbook of Chemical Property Estimation Methods. Washington, DC: Amer Chem Soc pp. 15-1 to 15-29 (1990) (3) Farwell SO et al; Soil Biol Biochem 11: 411-5 (1979) (4) Daubert TE, Danner RP; Physical & Thermodynamic Properties of Pure Chemicals: Data Compilation. New York, NY: Hemisphere Pub Corp (1989)

Using a structure estimation method based on molecular connectivity indices(1), the Koc of dimethyl disulfide can be estimated to be 40(SRC). According to a classification scheme(2), this estimated Koc value suggests that dimethyl disulfide is expected to have very high mobility in soil. Gas chromatographic studies with various air-dry and moist soils have shown that soil can sorb atmospheric, gas phase dimethyl disulfide(3). In one closed-system test, 17-94% of input dimethyl disulfide was sorbed by the soil in 10 min(3); in a 15-day test, dimethyl disulfide sorption was 101-306 ug sorbed/g soil(3). Soil microbes were found to be important for the gas phase sorption of dimethyl disulfide as 15-day sorption in sterilized soil was only 9-98 ug sorbed/g soil(3).
Literature: (1) US EPA; Estimation Program Interface (EPI) Suite. Ver. 4.1. Jan, 2011. Available from, as of Nov 7, 2013: http://www.epa.gov/oppt/exposure/pubs/episuitedl.htm (2) Swann RL et al; Res Rev 85: 17-28 (1983) (3) Bremner JM, Banwart WL; Soil Biol Biochem 8: 79-83 (1976)

4,7-Dimethylundecane

Undecane, 4,7-dimethyl-

17301-32-5

4,7-dimethy-lundecane

4,7-Dimethylundecane #

Undecane,4,7-dimethyl-

DTXSID50333996

CHEBI:140568

LMFA11000693

NS00096003

1-UNDECENE

821-95-4

Undec-1-ene

n-1-Undecene

1-Hendecene

Undecene

alpha-Undecene

alpha-Undecylene

alpha-Nonylethylene

Undecene-1

CCRIS 5720

HSDB 1090

.alpha.-Undecene

EINECS 212-483-7

NSC 73983

UNII-1446756A8F

NSC-73983

1446756A8F

DTXSID5061168

CHEBI:77444

MFCD00008956

Hendecene

68526-57-8

1-Undecene, 97%

N-NONYLETHYLENE

?1-UNDECENE

.ALPHA.-UNDECYLENE

1-UNDECENE [HSDB]

3,4-dichlorophenethylalcohol

.ALPHA.-NONYLETHYLENE

DTXCID0048268

NSC73983

EINECS 271-214-1

LMFA11000332

STL453737

AKOS009156849

MCULE-8437878932

LS-14020

DB-056580

NS00038169

U0025

U0052

D92764

EC 271-214-1

Q14745306

The Henry's Law constant for 1-undecene is estimated as 1.48 atm-cu m/mole(SRC) using a fragment constant estimation method(1). This Henry's Law constant indicates that 1-undecene is expected to volatilize rapidly from water surfaces(2). Based on this Henry's Law constant, the volatilization half-life from a model river (1 m deep, flowing 1 m/sec, wind velocity of 3 m/sec)(2) is estimated as 1 hr(SRC). The volatilization half-life from a model lake (1 m deep, flowing 0.05 m/sec, wind velocity of 0.5 m/sec)(2) is estimated as 5 days(SRC). However, the volatilization half-life does not take into account the effects of adsorption. This is apparent from the results of two EXAMS model runs, one in which the effect of adsorption was considered, yielding an estimated half-life of 21 days in a model pond 2 m deep, and one in which the effect of adsorption was ignored, yielding an estimated half-life of 42 hrs in a model pond 2 m deep(3). 1-Undecene's Henry's Law constant(1) indicates that volatilization from moist soil surfaces may occur(SRC). 1-Undecene is not expected to volatilize from dry soil surfaces(SRC) based upon a vapor pressure of 0.493 mm Hg(4).
Literature: (1) Meylan WM, Howard PH; Environ Toxicol Chem 10: 1283-93 (1991) (2) Lyman WJ et al; Handbook of Chemical Property Estimation Methods. Washington, DC: Amer Chem Soc pp. 15-1 to 15-29 (1990) (3) USEPA; EXAMS II Computer Simulation (1987) (4) Daubert TE, Danner RP; Physical and Thermodynamic Properties of Pure Chemicals: Data Compilation. Design Inst Phys Prop Data, Amer Inst Chem Eng NY, NY: Hemisphere Pub Corp 5 Vol (1989)

Sol in ether, chloroform, ligroin; insol in water
Literature: Lide, D.R. (ed.). CRC Handbook of Chemistry and Physics. 79th ed. Boca Raton, FL: CRC Press Inc., 1998-1999., p. 3-327

Using a structure estimation method based on molecular connectivity indices(1), the Koc for 1-undecene can be estimated to be about 3180(SRC). According to a classification scheme(2), this estimated Koc value suggests that 1-undecene is expected to have slight mobility in soil.
Literature: (1) Meylan WM et al; Environ Sci Technol 26: 1560-67 (1992) (2) Swann RL et al; Res Rev 85: 17-28 (1983)