Propylbenzene

N-PROPYLBENZENE

103-65-1

1-Phenylpropane

Phenylpropane

Isocumene

Benzene, propyl-

1-Propylbenzene

n-Propyl benzene

Propylbenzene, n-

propyl benzene

Propyl-benzene

NSC 16941

HSDB 5353

UNII-0WR86ZHG2Z

EINECS 203-132-9

0WR86ZHG2Z

DTXSID3042219

CHEBI:42630

AI3-23862

NSC-16941

CHEMBL286062

DTXCID1022219

Propylbenzene, analytical standard

UN2364

Propylbenzene (all isomers)

benzene, propyl

3H0

Benzene, n-propyl-

PRPH

Propylbenzene, 98%

BENZENE,PROPYL

PROPYLBENZENE [MI]

PHENYLPROPANE [INCI]

WLN: 3R

N-PROPYLBENZENE [HSDB]

Propylbenzene, >=99.0% (GC)

NSC16941

Tox21_300567

BDBM50167945

MFCD00009377

AKOS000120950

MCULE-1436126757

UN 2364

NCGC00248093-01

NCGC00254532-01

CAS-103-65-1

n-Propylbenzene 100 microg/mL in Methanol

NS00006753

P0523

S0656

EN300-20607

n-Propyl benzene [UN2364] [Flammable liquid]

A800778

Q288806

J-001016

J-523764

Z104479154

InChI=1/C9H12/c1-2-6-9-7-4-3-5-8-9/h3-5,7-8H,2,6H2,1H

The Henry's Law constant for n-propylbenzene is 1.05X10-2 atm-cu m/mole(1). This Henry's Law constant indicates that n-propylbenzene 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 hour(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 days(SRC). Results of mesocosm studies simulating the Narragansett Bay indicate that volatilization is the major removal process from seawater(3); volatilization half-lives of 1.3-19 days were estimated for summer, spring and winter seasons(5). n-Propylbenzene's Henry's Law constant(1) indicates that volatilization from moist soil surfaces may occur(SRC). The potential for volatilization of n-propylbenzene from dry soil surfaces may exist(SRC) based upon it's vapor pressure of 3.42 mm Hg(4).

A Koc of 725 was measured for n-propylbenzene using a surface sediment collected from the Tamar estuary(1). A similar Koc of 676 was measured in a humic acid column via HPLC(2). Adsorption percentages ranging from 0.16 to 5.58% were measured in soil column studies using three different soil types and a sludge sample(3). Using a structure estimation method based on molecular connectivity indices(4), the Koc for n-propylbenzene can be estimated to be 955(SRC). According to a classification scheme(5), these estimated and measured Koc values suggest that n-propylbenzene is expected to have low mobility in soil.

octane

n-octane

111-65-9

Oktan

Oktanen

Ottani

n-Oktan

Oktanen [Dutch]

Oktan [Polish]

Ottani [Italian]

HSDB 108

UNII-X1RV0B2FJV

X1RV0B2FJV

NSC 9822

EINECS 203-892-1

DTXSID0026882

CHEBI:17590

AI3-28789

NSC-9822

MFCD00009556

DTXCID406882

CH3-[CH2]6-CH3

EC 203-892-1

Heptane, methyl-

Octane, all isomers

CH3-(CH2)6-CH3

octano

Normal octane

normal-Octane

octan

Octanes

Octil

MG8

OTTANE

OCTANE [INCI]

N-OCTANE [HSDB]

OCTANE [MI]

bmse000480

Octane, analytical standard

WLN: 8H

Octane, anhydrous, >=99%

Octane, reagent grade, 98%

n-C8H18

Octane, p.a., 99.0%

CHEMBL134886

NSC9822

Octane; NSC 9822; n-Octane

Tox21_202452

c0044

LMFA11000002

AKOS015904009

MCULE-3248084959

NCGC00249228-01

NCGC00260001-01

CAS-111-65-9

LS-13532

NS00006444

O0022

O0118

O0151

Octane, puriss. p.a., >=99.0% (GC)

C01387

Q150681

J-002613

F0001-0244

EEE64B73-0375-4303-AFD5-0795361807FF

InChI=1/C8H18/c1-3-5-7-8-6-4-2/h3-8H2,1-2H

Octane, electronic grade, >=99.999% metals basis, >=99% (CP)

31372-91-5

9065-92-3

The Henry's Law constant for n-octane is estimated as 3.2 atm-cu m/mole(SRC) derived from its vapor pressure, 14.1 mm Hg(1), and water solubility, 0.66 mg/L(2). This Henry's Law constant indicates that n-octane 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 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 4.2 days(SRC). Volatilization from water surfaces may be attenuated by adsorption to suspended solids and sediment in the water column(SRC). The estimated volatilization half-life from a model pond is 11 months if adsorption is considered(4). However, in a study using a jet fuel mixture and sterile freshwater controls from the Escambia River (Florida), a 99% loss of n-octane was attributed to evaporation at 25 deg C(5). n-Octane's estimated Henry's Law constant indicates that volatilization from moist soil surfaces may occur(SRC). The disappearance of n-octane was rapid in soil/water mixture (concentration of soil, 25 g/150 mL)(6); an initial concentration of 0.177 ug/mL n-octane disappeared completely in 5 days using a sterile sandy loam soil with an organic matter content of 5.1%(6). The potential for volatilization of n-octane from dry soil surfaces may exist(SRC) based upon its vapor pressure(1).
Literature: (1) Yaws CL; Handbook of Vapor Pressure. Houston, TX: Gulf Pub Co. 3: 78 (1994) (2) Yalkowsky SH, He Y, eds; Handbook of aqueous solubility data. Boca Raton, FL: CRC Press p. 536 (2003) (3) Lyman WJ et al; Handbook of Chemical Property Estimation Methods. Washington, DC: Amer Chem Soc pp. 15-1 to 15-29 (1990) (4) US EPA; EXAMS II Computer Simulation (1987) (5) Spain JC et al; Degrad of Jet Fuel Hydrocarbons by Aquatic Microbial Communities. Tyndall AFB, FL: Air Force Eng Serv Ctr. AFESC/ESL-TR-83-26 (NTIS AD-A139791/8) p 226 (1983) (6) Dean-Ross D; Bull Environ Contam Toxicol 51: 596-99 (1993)

The Koc of n-octane is estimated as 3.1X10+4(SRC), using a log Kow of 5.18(1) and a regression-derived equation(2). According to a classification scheme(3), this estimated Koc value suggests that n-octane is expected to be immobile in soil. Freundlich absorption coefficients of log 4.04 and log 3.49 were measured in Oberlausitz lignite (11.1% moisture content; 53.5 wt% carbon content; 0.6 wt % nitrogen content) and Pahokee peat soil (10.2% moisture content; 46.1 wt% carbon content; 3.3 wt % nitrogen content), respectively(4). Gaseous transport of volatile n-octane in unsaturated porous media was shown to be influenced by air-water interfacial adsorption and water-partitioning(5). Sorption of n-octane from air to snow was measured, resulting in a sorption coefficient of log -4.41 cu m/sq m at -6.8 deg C(6).
Literature: (1) Miller MM et al; Environ Sci Technol 19:522-9 (1985) (2) US EPA; Estimation Program Interface (EPI) Suite. Ver. 4.1. Nov, 2012. Available from, as of Oct 30, 2013: http://www.epa.gov/oppt/exposure/pubs/episuitedl.htm (3) Swann RL et al; Res Rev 85: 17-28 (1983) (4) Endo S et al; Environ Sci Technol 42): 5897-5903 (2008) (5) Kim H et al; Environ Sci Technol 35: 4457-62 (2001) (6) Roth CM et al; Environ Sci Technol 38: 4078-84 (2004)

acetic acid

ethanoic acid

64-19-7

Acetic acid glacial

Ethylic acid

Vinegar acid

Glacial acetic acid

Acetic acid, glacial

Methanecarboxylic acid

Acetasol

Essigsaeure

Acide acetique

Pyroligneous acid

Vinegar

Azijnzuur

Aceticum acidum

Acido acetico

Octowy kwas

Aci-jel

HOAc

ethoic acid

Kyselina octova

Orthoacetic acid

AcOH

Azijnzuur [Dutch]

Ethanoic acid monomer

Acetic

Essigsaeure [German]

Caswell No. 003

Otic Tridesilon

Octowy kwas [Polish]

Acetic acid (natural)

Acide acetique [French]

Acido acetico [Italian]

FEMA No. 2006

Kyselina octova [Czech]

MeCOOH

Acetic acid-17O2

Otic Domeboro

Acidum aceticum glaciale

Acidum aceticum

CH3-COOH

acetic acid-

CH3CO2H

UN2789

UN2790

EPA Pesticide Chemical Code 044001

NSC 132953

NSC-132953

NSC-406306

BRN 0506007

Acetic acid, diluted

INS NO.260

Acetic acid [JAN]

DTXSID5024394

MeCO2H

CHEBI:15366

AI3-02394

CH3COOH

INS-260

Q40Q9N063P

E-260

10.Methanecarboxylic acid

CHEMBL539

NSC-111201

NSC-112209

NSC-115870

NSC-127175

Acetic acid-2-13C,d4

INS No. 260

DTXCID304394

E 260

Acetic-13C2 acid (8CI,9CI)

Ethanoat

Shotgun

MFCD00036152

Acetic acid, of a concentration of more than 10 per cent, by weight, of acetic acid

285977-76-6

68475-71-8

C2:0

acetyl alcohol

Orlex

Vosol

ACETIC-1-13C-2-D3 ACID-1 H (D)

WLN: QV1

ACETIC ACID (MART.)

ACETIC ACID [MART.]

Acetic acid, >=99.7%

57745-60-5

63459-47-2

FEMA Number 2006

ACETIC-13C2-2-D3 ACID, 97 ATOM % 13C, 97 ATOM % D

Acetic acid, ACS reagent, >=99.7%

ACY

HSDB 40

CCRIS 5952

79562-15-5

methane carboxylic acid

EINECS 200-580-7

Acetic acid 0.25% in plastic container

Essigsaure

Ethylate

acetic aicd

acetic-acid

Glacial acetate

acetic cid

actic acid

UNII-Q40Q9N063P

acetic -acid

Distilled vinegar

Methanecarboxylate

Acetic acid, glacial [USP:JAN]

Acetasol (TN)

Acetic acid,glacial

Carboxymethyl radical

for LC-MS

Vinegar (Salt/Mix)

HOOCCH3

546-67-8

Acetic acid LC/MS Grade

ACETIC ACID [II]

ACETIC ACID [MI]

Acetic acid, ACS reagent

bmse000191

bmse000817

bmse000857

Otic Domeboro (Salt/Mix)

EC 200-580-7

Acetic acid (JP17/NF)

ACETIC ACID [FHFI]

ACETIC ACID [INCI]

Acetic Acid [for LC-MS]

ACETIC ACID [VANDF]

NCIOpen2_000659

NCIOpen2_000682

Acetic acid, glacial (USP)

4-02-00-00094 (Beilstein Handbook Reference)

77671-22-8

Glacial acetic acid (JP17)

UN 2790 (Salt/Mix)

ACETIC ACID [WHO-DD]

ACETIC ACID [WHO-IP]

ACETICUM ACIDUM [HPUS]

GTPL1058

Acetic Acid Glacial HPLC Grade

Acetic acid, analytical standard

Acetic acid, Glacial USP grade

Acetic acid, puriss., >=80%

Acetic acid, 99.8%, anhydrous

Acetic acid, AR, >=99.8%

Acetic acid, LR, >=99.5%

DTXSID001043500

Acetic acid, extra pure, 99.8%

Acetic acid, 99.5-100.0%

Acetic acid, Glacial, ACS Reagent

STR00276

Acetic acid, puriss., 99-100%

Tox21_301453

Acetic acid, glacial, >=99.85%

BDBM50074329

FA 2:0

LMFA01010002

NSC132953

NSC406306

STL264240

Acetic acid, for HPLC, >=99.8%

AKOS000268789

ACIDUM ACETICUM [WHO-IP LATIN]

DB03166

MCULE-8295936189

UN 2789

Acetic acid, >=99.5%, FCC, FG

Acetic acid, natural, >=99.5%, FG

Acetic acid, ReagentPlus(R), >=99%

CAS-64-19-7

USEPA/OPP Pesticide Code: 044001

Acetic acid, USP, 99.5-100.5%

NCGC00255303-01

Acetic acid 1000 microg/mL in Methanol

Acetic acid, SAJ first grade, >=99.0%

DB-085748

Acetic acid 1000 microg/mL in Acetonitrile

Acetic acid, >=99.99% trace metals basis

Acetic acid, JIS special grade, >=99.7%

Acetic acid, purified by double-distillation

NS00002089

Acetic acid, UV HPLC spectroscopic, 99.9%

EN300-18074

Acetic acid, Vetec(TM) reagent grade, >=99%

Bifido Selective Supplement B, for microbiology

C00033

D00010

ORLEX HC COMPONENT ACETIC ACID, GLACIAL

Q47512

VOSOL HC COMPONENT ACETIC ACID, GLACIAL

Acetic acid, glacial, electronic grade, 99.7%

TRIDESILON COMPONENT ACETIC ACID, GLACIAL

A834671

ACETASOL HC COMPONENT ACETIC ACID, GLACIAL

Acetic acid, >=99.7%, SAJ super special grade

ACETIC ACID, GLACIAL COMPONENT OF BOROFAIR

ACETIC ACID, GLACIAL COMPONENT OF ORLEX HC

ACETIC ACID, GLACIAL COMPONENT OF VOSOL HC

SR-01000944354

ACETIC ACID, GLACIAL COMPONENT OF TRIDESILON

SR-01000944354-1

ACETIC ACID, GLACIAL COMPONENT OF ACETASOL HC

Glacial acetic acid, meets USP testing specifications

InChI=1/C2H4O2/c1-2(3)4/h1H3,(H,3,4

Acetic acid, >=99.7%, suitable for amino acid analysis

Acetic acid, >=99.7%, for titration in non-aqueous medium

Acetic acid, for luminescence, BioUltra, >=99.5% (GC)

Acetic acid, p.a., ACS reagent, reag. ISO, reag. Ph. Eur., 99.8%

Acetic acid, semiconductor grade MOS PURANAL(TM) (Honeywell 17926)

Glacial acetic acid, United States Pharmacopeia (USP) Reference Standard

Acetic acid, puriss. p.a., ACS reagent, reag. ISO, reag. Ph. Eur., >=99.8%

Glacial Acetic Acid, Pharmaceutical Secondary Standard; Certified Reference Material

158461-04-2

2887-46-9

Acetic acid, puriss., meets analytical specification of Ph. Eur., BP, USP, FCC, 99.8-100.5%

The Henry's Law constant for acetic acid has been experimentally determined to be 1.43X10-7 atm-cu m/mole at 25 deg C(1). This Henry's Law constant indicates that acetic acid is expected to be essentially nonvolatile from water surfaces(2). Acetic acid's Henry's Law constant indicates that volatilization from moist soil surfaces is not expected to be an important fate process(SRC). Acetic acid is expected to volatilize from dry soil surfaces(SRC) based upon a vapor pressure of 15.7 mm Hg at 25 deg C(3).
Literature: (1) Johnson BJ et al; J Atmos Chem 24: 113-119 (1996) (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. Design Inst Phys Prop Data, Amer Inst Chem Eng. New York, NY: Hemisphere Pub Corp (1989)

A log Koc of 0.00 (Koc = 1), which was derived from experimental measurements, has been reported for acetic acid(1,2). According to a classification scheme(3), this Koc value suggests that acetic acid is expected to have very high mobility in soil. No detectable sorption was measured for acetic acid using the OECD Guideline 106 method employing an acidic forest soil, pH 2.8, an agricultural soil, pH 6.7, and a lake sediment, pH 7.1(4). Adsorption of acetic acid to 3 nearshore marine sediments collected from three different locations resulted in Kd values of 0.65 (Koc = 228), 0.085 (Koc = 6.5) and 0.046 (Koc = 27) using clastic mud (3.5% organic carbon, pH 7.0), muddy sand (1.3% organic carbon, pH 7.7), and carbonate sand (0.17% organic carbon, pH 8.1), respectively(5). The pKa of acetic acid is 4.76(6), indicating that this compound will exist partially in anion form in the environment and anions generally do not adsorb more strongly to soils containing organic carbon and clay than their neutral counterparts(7).
Literature: (1) Schuurmann G et al; Environ Sci Technol 40: 7005-7011 (Supplemental material) (2006) (2) Meylan WM et al; Environ Sci Technol 26: 1560-7 (1992) (3) Swann RL et al; Res Rev 85: 17-28 (1983) (4) Von Oepen B et al; Chemosphere 22: 285-304 (1991) (5) Sansone JF et al; Geochimica et Cosmochimica Acta 51: 1889-1896 (1987) (6) Serjeant EP, Dempsey B; Ionisation Constants of Organic Acids in Aqueous Solution. IUPAC Chemical Data Series No. 23. New York, NY: Pergamon Press, p. 989 (1979) (7) Doucette WJ; pp. 141-188 in Handbook of Property Estimation Methods for Chemicals. Boethling RS, Mackay D, eds. Boca Raton, FL: Lewis Publ (2000)
Literature: #In 24 hr aqueous adsorption studies using montmorillonite and kaolinite clay adsorbents, 2.4-30.4% of added acetic acid was observed to be in the adsorbed phase(1). In adsorption studies using the adsorbent hydroxyapatite (a mineral which occurs in the environment as a result of the diagenesis of skeletal apatite), only 5% of added acetic acid (in aqueous solution, pH 8.0) became adsorbed to the hydroxyapatite(2). Acetic acid has been noted to leach from biological disposal areas(3).
Literature: (1) Hemphill L, Swanson WS; Proc of the 18th Industrial Waste Conf, Eng Bull Purdue Univ, Lafayette IN 18: 204-17 (1964) (2) Gordon AS, Millero FJ; Microb Ecol 11: 289-98 (1985) (3) Abrams EF et al; Identification of Organic Compounds in Effluents from Industrial Sources. USEPA-560/3-75-002 p. 3 (1975)

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)

1-TRIDECANOL

Tridecanol

112-70-9

Tridecan-1-ol

Tridecyl alcohol

26248-42-0

n-Tridecan-1-ol

n-Tridecanol

n-Tridecyl alcohol

80206-82-2

1-Hydroxytridecane

MFCD00004756

DTXSID2021947

CHEBI:34123

NSC-5252

8I9428H868

DTXCID901947

N-TRIDECYL-D27 ALCOHOL

CAS-112-70-9

CCRIS 8591

HSDB 5574

NSC 5252

EINECS 203-998-8

BRN 1739991

AI3-35264

UNII-8I9428H868

EINECS 279-420-3

1-Tridecanol, 97%

Maybridge1_004320

SCHEMBL20879

1-TRIDECANOL [HSDB]

BIDD:ER0306

CHEMBL24832

WLN: Q13

TRIDECYL ALCOHOL [INCI]

HMS553M10

AMY5938

NSC5252

BBA24842

Tox21_202208

Tox21_300138

LMFA05000171

STL287936

AKOS005267216

CS-W004293

HY-W004293

MCULE-4385103550

NCGC00164019-01

NCGC00164019-02

NCGC00164019-03

NCGC00254162-01

NCGC00259757-01

1-Tridecanol, purum, >=98.0% (GC)

BP-28084

BS-14333

SY049489

NS00007712

T0803

H10847

EN300-1841776

A894533

Q161684

J-002821

J-016351

85AD1334-FDF8-446D-BF63-A7EE6B26FE07

F0001-0261

The Henry's Law constant for 1-tridecanol is estimated as 1.3X10-4 atm-cu m/mole(SRC) using a fragment constant estimation method(1). This Henry's Law constant indicates that 1-tridecanol 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 14 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 8.5 days(SRC).However, volatilization from water surfaces is expected to be attenuated by adsorption to suspended solids and sediment in the water column. The volatilization half-life from a model pond is about 16 years when adsorption is considered(3). 1-Tridecanol's Henry's Law constant indicates that volatilization from moist soil surfaces may occur(SRC). 1-Tridecanol is not expected to volatilize from dry soil surfaces(SRC) based upon a vapor pressure of 4.36X10-4 mm Hg(4).

The Koc of 1-tridecanol is estimated as 35,000(SRC), using a log Kow of 5.82(1) and a regression-derived equation(2). According to a classification scheme(3), this estimated Koc value suggests that 1-tridecanol is expected to be immobile in soil.

Nonan-1-ol

1-Nonanol

143-08-8

Nonanol

NONYL ALCOHOL

n-Nonyl alcohol

Pelargonic alcohol

1-Hydroxynonane

Nonalol

Octyl carbinol

n-Nonanol

n-Nonan-1-ol

Alcohol C-9

Nonylalkohol

Pelargonalkohol

Alcohol C9

FEMA No. 2789

28473-21-4

NSC 5521

MFCD00002990

NGK73Q6XMC

DTXSID6022008

CHEBI:35986

NSC-5521

C9 alcohol

HSDB 5145

EINECS 205-583-7

UNII-NGK73Q6XMC

BRN 0969213

nonanols

nonyl-alcohol

AI3-03962

N-nonyl-alcohol

EINECS 249-048-6

Nonanol-(1)

Nonyl alcohol, 8CI

1-Nonanol, 98%

EC 205-583-7

NONYL ALCOHOL [FCC]

SCHEMBL19807

NONYL ALCOHOL [FHFI]

NONYL ALCOHOL [HSDB]

WLN: Q9

4-01-00-01798 (Beilstein Handbook Reference)

BIDD:ER0370

CHEMBL24563

N-NONYL ALCOHOL [MI]

DTXCID402008

Nonyl alcohol, >=98%, FCC

BDBM22607

FEMA 2789

NSC5521

Tox21_300869

LMFA05000092

STL283956

AKOS009031412

CS-W009532

DB03143

HY-W008816

MCULE-4020281400

1-Nonanol, purum, >=98.0% (GC)

NCGC00248194-01

NCGC00254773-01

BP-31117

BS-42231

CAS-143-08-8

SY011469

N0292

NS00002633

EN300-19921

D70513

A808013

Q161662

J-007741

F0001-0508

Z104476100

2E051A08-F94E-40C2-88CA-7030E15C76BF

InChI=1/C9H20O/c1-2-3-4-5-6-7-8-9-10/h10H,2-9H2,1H

The Henry's Law constant for 1-nonanol estimated as 3.08X10-5 atm-cu m/mol(SRC) derived from its vapor pressure, 2.27X10-2 mm Hg at 25 deg C(1), and water solubility, 140 mg/L(2). This Henry's Law constant indicates that 1-nonanol is expected to volatilize 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 1.6 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)(3) is estimated as 15 days(SRC). 1-Nonanol's Henry's Law constant indicates that volatilization from moist soil surfaces may occur(SRC). 1-Nonanol is not expected to volatilize from dry soil surfaces(SRC) based upon its vapor pressure(1).
Literature: (1) Daubert TE, Danner RP; Data Compilation Tables of Properties of Pure Compounds NY, NY: Amer Inst for Phys Prop Data (1989) (2) Barton AFM; pp. 438 in Solubility Data Series Vol 15 (1984) (3) Lyman WJ et al; Handbook of Chemical Property Estimation Methods. Washington, DC: Amer Chem Soc pp. 15-1 to 15-29 (1990)

An estimated BCF of 160 was calculated for 1-nonanol(SRC), using a log Kow of 3.77(1) and a regression-derived equation(2). According to a classification scheme(3), this BCF suggests the potential for bioconcentration in aquatic organisms is high(SRC), provided the compound is not metabolized by the organism(SRC).
Literature: (1) Barton AFM; pp. 438 in Solubility Data Series Vol 15 (1984) (2) Meylan WM et al; Environ Sci Technol 26: 1560-7 (1992) (3) Swann RL et al; Res Rev 85: 17-28 (1983) (4) Lyman WJ et al; Handbook of Chemical Property Estimation Methods, NY: McGraw-Hill Chapt 4, Eqn 4-5 (1982)

1-PENTADECANOL

pentadecan-1-ol

629-76-5

Pentadecyl alcohol

Pentadecanol

n-Pentadecanol

n-1-Pentadecanol

Neodol 5

31389-11-4

67762-25-8

MFCD00004759

333QVA4G2Q

DTXSID0027270

CHEBI:77468

NSC-66446

n-pentadecyl alcohol

DTXCID207270

CAS-629-76-5

Alfol 15

UNII-333QVA4G2Q

n-pPentadecanol

Pentadecanol-(1)

EINECS 211-107-9

NSC 66446

1-Pentadecanol, 99%

AI3-33881

SCHEMBL29548

CHEMBL26561

AMY5936

PENTADECYL ALCOHOL [INCI]

1-pentadecanol (ACD/Name 4.0)

NSC66446

EINECS 267-006-5

Tox21_201699

Tox21_300553

LMFA05000194

STL453722

AKOS009031435

CS-W004295

HY-W004295

Pentadecanol,95%; n-Pentadecyl alcohol

NCGC00164169-01

NCGC00164169-02

NCGC00164169-03

NCGC00254478-01

NCGC00259248-01

BP-30139

PD166618

SY049687

NS00013962

P0036

EN300-20042

H10901

A868289

Q27146999

F0001-1704

1991DA79-7140-48B0-9F03-1E3D88AC4F28

InChI=1/C15H32O/c1-2-3-4-5-6-7-8-9-10-11-12-13-14-15-16/h16H,2-15H2,1H