IUPAC Measured - University of Leeds

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Fig. 2: The HIRAC chamber equipped with recently installed temperature control system. Kinetics of Reactions of Cl atoms with C4-C5 hydrocarbons over a temperature range of 220-320 K L. N. Farrugia , F.A.W. Winiberg, D. E. Heard and P. W. Seakins School of Chemistry, University of Leeds, Leeds, LS2 9JT, UK [email protected] 1. Introduction Recent observations of high [ClNO 2 ] in inland urban areas in the USA (1) , as well as significant [Cl] in volcanic plumes, have had an impact on the importance of chlorine chemistry outside the marine environment. 2. HIRAC Highly Instrumented Reactor for Atmospheric Chemistry 3. Relative rate study of Cl + hydrocarbons 4. Temperature dependent study 5. Conclusions Good agreement with the literature for all experimental Cl+hydrcarbons rate coefficients obtained at 298 K. Excellent agreement for GC-FID and FTIR data obtained in HIRAC for n-butane, which is also a validation of the method used. First temperature dependent results for Cl + n-pentane and isopentane, with negative temperature dependence reported for isopentane reaction. Negative temperature dependence observed from isopentane+Cl. This work provides further validation of suitability of HIRAC temperature control system and relative rate method as a way of generating reliable temperature dependent rate coefficients. 7. References (1) Thornton, J. A. et al., Nature, 464, pp.271-274, 2010. (2) Glowacki, D. R. et al., Atmos. Chem. Phys., 7, pp.5371-5390, 2007. (3) Tyndall, G. S. et al., Int. Journal Chemical Kinetics., 29, 1, pp.43 55. 1996. 45.00 45.50 46.00 46.50 47.00 47.50 48.00 48.50 49.00 49.50 50.00 -60 -30 0 30 60 Temperature / o C Vertical Distance / cm (a) 47.00 47.20 47.40 47.60 47.80 48.00 48.20 48.40 48.60 48.80 49.00 -60 -30 0 30 60 Temperature / o C Horizontal Distance / cm (b) -47.00 -46.50 -46.00 -45.50 -45.00 -44.50 -44.00 -43.50 -43.00 -60.00 -30.00 0.00 30.00 60.00 Temperature / o C Vertical Distance / cm (c) -47.00 -46.50 -46.00 -45.50 -45.00 -44.50 -44.00 -60.00 -30.00 0.00 30.00 60.00 Temperature / o C Horizontal Distance / cm (d) Fig. 4: Temperature profile of HIRAC chamber at +48 o C (a + b) and -46 o C (c + d) at 1000 mbar. Fig. 6: Excellent agreement between FTIR and GC measurements in HIRAC for n- butane + ethane + Cl relative rate experiment at 298 K. Table 1: Kinetic data on reactions of Cl with propane, n-butane, isobutane, n-pentane and isopentane at 298 K. Fig. 3:(a) The photolysis lamps and (b) the FTIR Chernin cell present inside the HIRAC chamber. Fig. 1: Nighttime source of Chlorine (Thornton et al., 2010) Hydrocarbon k (Cl+hydrocarbons) / 10 -10 cm 3 molecule -1 s -1 Source propane 1.45±0.28 Wallington et al. (1988) 1.43±0.25 Tyndall et al. (1996) 1.48+0.07 This work (GC) n-butane 2.15±0.15 Tyndall et al. (1996) 2.25+0.10 Lewis et al. (1980) 2.23+0.11 This work (GC) 2.14±0.11 This work (FTIR) isobutane 1.42±0.06 Seakins et al. (1996) 1.46±0.06 Lewis et al. (1980) 1.49±0.08 This work (GC) n-pentane 2.52±0.06 Atkinson et al. (1985) 2.46±0.03 Seakins et al. (2001) 2.65±0.13 This work (GC) isopentane 2.03±0.06 Atkinson et al. (1985) 1.91±0.02 Seakins et al. (2001) 2.05±0.10 This work (GC) 6. Future Work FTIR analysis for isobutane, n-pentane and isopentane will be performed using the new FTIR data analysis techniques developed. Product analysis for the GC and FTIR data for all butanes and pentanes studied, and a look into whether there temperature effects product ratios. Further site-specific rate data and product branching fractions using deuterated compounds are planned for Cl atom reactions with other organics to obtain an insight into product ratios and mechanistic information of these reactions. 0.0030 0.0032 0.0034 0.0036 0.0038 0.0040 0.0042 0.0044 -42.0 -41.5 -41.0 -40.5 -40.0 -39.5 -39.0 -38.5 -38.0 -37.5 Measured IUPAC Herron & Huie Treacy et al. ln(k bim / molecule -1 cm 3 s -1 ) 1/(T / K) Arrhenius plot for propene ozonolysis This work: ln(k bim ) = -2282.4/T - 31.3 IUPAC: ln(k bim ) = -1880/T - 32.8 Fig. 5: Arrhenius plot for propene+O 3 reaction at 1000 mbar and over a temperature range of 233 323 K. ClNO 2 production has an impact on NO x and Cl budgets (Fig.1.). Cl:OH ratios have been monitored in various sites including the polar regions. Various studies have focused on better understanding the implications of these two cycles. 0.00 0.05 0.10 0.15 0.20 0.25 0.0 0.2 0.4 0.6 0.8 1.0 1.2 1.4 n-butane isobutane n-pentane isopentane ln [hydrocarbon] o /[hydrocarbon] t ln [ethane] o /[ethane] t A number of these studies are revealing important information on Cl atom chemistry through observing relative hydrocarbon concentrations, in most studies alkanes. Hydrogen abstraction of hydrocarbons by atomic chlorine have been of interest to kineticists for many years. Reactions involving chlorine atoms with n-butane, isobutane, n-pentane and isopentane were studied experimentally in an environmental chamber. Experiments were carried out over a temperature range of 225 325 K and at 1000 mbar. The main focus of this study was to obtain a better mechanistic understanding of these reactions and in particular the structural influence of higher hydrocarbons on hydrogen abstraction reactions. The kinetics of Cl atom hydrogen abstractions from propane, n-butane, isobutane, n-pentane and isopentane has been investigated at room temperature and 1000 mbar in the HIRAC chamber. GC-FID and FTIR techniques were used in order to analyse the rates of decay of the hydrocarbons. The relative rate technique was used to measure rate coefficients of these reactions using ethane as a reference compound. A new FTIR data analysis technique was developed and used to analyse the n-butane data obtained from this study. Lack of suitable reference spectra for other hydrocarbons inhibited analysis of other FTIR data. A comparison of the kinetic data from this study with other studies is shown in Table 1. The results obtained for experiments carried out at 298 K were all within good agreement of the literature. Fig. 7.: Relative rate plots for hydrocarbon + Cl reactions at 1000 mbar and at 298 K. Previous studies for ethane+Cl showed a positive temperature dependence, while no similar trend was found for propane and n-butane. A temperature dependent study was carried out over ~220 320 K in the HIRAC chamber using relative rate method. Results obtained for isopentane+Cl gave a negative temperature dependence (E a = -1.33 ± 0.02 kJ mol -1 ) n-pentane, isobutane and n-butane were all found to be temperature independent from this study. Fig. 8: Arrhenius plots for pentanes+Cl reaction at 1000 mbar and over a temperature range of ~ 220 320 K. Recent installation of a temperature control system has enabled studies at temperatures between ~ 223 323 K. System has been tested by conducting a temperature-dependent study for propene+O 3 (Fig.5.). An Arrhenius plot of the bimolecular rate constant for propene gave E a = 19.84 ± 0.46 kJ mol -1 . This value is within error of the IUPAC and literature data. A temperature profile of the HIRAC chamber operating at about 233 323 K to check the uniformity of the system is shown in Fig.4. The HIRAC chamber at the University of Leeds (2) allows control of the conditions of temperature, pressure and photolysis rate which are important variables affecting the rate of processes in the atmosphere. HIRAC is a 2.25 m 3 stainless steel indoor chamber equipped with a range of instruments including a GC- FID , GC-HID, FTIR, FAGE, CRDS as well as commercial NO x , O 3 and CO analysers. FTIR is coupled to HIRAC via a multipass optical arrangement on the interior of the chamber (Figure 3b). The mirror systems are robust and able to handle ranges of temperatures and pressures which the chamber is subjected to. This Chernin cell optical system is a modified multipass matrix system that features three objective mirrors with input and output apertures placed on opposite sides of the small field mirror. (a) (b)

Transcript of IUPAC Measured - University of Leeds

Fig. 2: The HIRAC chamber equipped with

recently installed temperature control system.

Kinetics of Reactions of Cl atoms with C4-C5 hydrocarbons over a temperature range of 220-320 K

L. N. Farrugia , F.A.W. Winiberg, D. E. Heard and P. W. Seakins

School of Chemistry, University of Leeds, Leeds, LS2 9JT, UK [email protected]

1. Introduction

• Recent observations of high [ClNO2] in inland urban areas in the USA(1), as well as

significant [Cl] in volcanic plumes, have had an impact on the importance of chlorine

chemistry outside the marine environment.

2. HIRAC – Highly Instrumented Reactor for Atmospheric Chemistry 3. Relative rate study of Cl + hydrocarbons

4. Temperature dependent study

5. Conclusions

• Good agreement with the literature for all experimental Cl+hydrcarbons rate

coefficients obtained at 298 K.

• Excellent agreement for GC-FID and FTIR data obtained in HIRAC for n-butane,

which is also a validation of the method used.

• First temperature dependent results for Cl + n-pentane and isopentane, with

negative temperature dependence reported for isopentane reaction. Negative

temperature dependence observed from isopentane+Cl.

• This work provides further validation of suitability of HIRAC temperature control

system and relative rate method as a way of generating reliable temperature

dependent rate coefficients.

7. References

(1) Thornton, J. A. et al., Nature, 464, pp.271-274, 2010.

(2) Glowacki, D. R. et al., Atmos. Chem. Phys., 7, pp.5371-5390, 2007.

(3) Tyndall, G. S. et al., Int. Journal Chemical Kinetics., 29, 1, pp.43 – 55. 1996.

45.00

45.50

46.00

46.50

47.00

47.50

48.00

48.50

49.00

49.50

50.00

-60 -30 0 30 60

Te

mp

era

ture

/ o

C

Vertical Distance / cm

(a)

47.00

47.20

47.40

47.60

47.80

48.00

48.20

48.40

48.60

48.80

49.00

-60 -30 0 30 60

Te

mp

era

ture

/ o

C

Horizontal Distance / cm

(b)

-47.00

-46.50

-46.00

-45.50

-45.00

-44.50

-44.00

-43.50

-43.00

-60.00 -30.00 0.00 30.00 60.00

Te

mp

era

ture

/ o

C

Vertical Distance / cm

(c)

-47.00

-46.50

-46.00

-45.50

-45.00

-44.50

-44.00

-60.00 -30.00 0.00 30.00 60.00

Te

mp

era

ture

/ o

C

Horizontal Distance / cm

(d)

Fig. 4: Temperature profile of HIRAC chamber

at +48 oC (a + b) and -46 oC (c + d) at 1000

mbar.

Fig. 6: Excellent agreement between FTIR

and GC measurements in HIRAC for n-

butane + ethane + Cl relative rate experiment

at 298 K.

Table 1: Kinetic data on reactions of Cl with

propane, n-butane, isobutane, n-pentane and

isopentane at 298 K.

Fig. 3:(a) The photolysis lamps and (b) the FTIR

Chernin cell present inside the HIRAC chamber.

Fig. 1: Nighttime source of Chlorine (Thornton et

al., 2010)

Hydrocarbon k (Cl+hydrocarbons) / 10-10

cm3molecule-1s-1 Source

propane

1.45±0.28 Wallington et al. (1988)

1.43±0.25 Tyndall et al. (1996)

1.48+0.07 This work (GC)

n-butane

2.15±0.15 Tyndall et al. (1996)

2.25+0.10 Lewis et al. (1980)

2.23+0.11 This work (GC)

2.14±0.11 This work (FTIR)

isobutane

1.42±0.06 Seakins et al. (1996)

1.46±0.06 Lewis et al. (1980)

1.49±0.08 This work (GC)

n-pentane

2.52±0.06 Atkinson et al. (1985)

2.46±0.03 Seakins et al. (2001)

2.65±0.13 This work (GC)

isopentane

2.03±0.06 Atkinson et al. (1985)

1.91±0.02 Seakins et al. (2001)

2.05±0.10 This work (GC)

6. Future Work

• FTIR analysis for isobutane, n-pentane and isopentane will be performed using the

new FTIR data analysis techniques developed.

• Product analysis for the GC and FTIR data for all butanes and pentanes studied, and

a look into whether there temperature effects product ratios.

• Further site-specific rate data and product branching fractions using deuterated

compounds are planned for Cl atom reactions with other organics to obtain an

insight into product ratios and mechanistic information of these reactions.

0.0030 0.0032 0.0034 0.0036 0.0038 0.0040 0.0042 0.0044

-42.0

-41.5

-41.0

-40.5

-40.0

-39.5

-39.0

-38.5

-38.0

-37.5

Measured

IUPAC

Herron & Huie

Treacy et al.

ln(k

bim

/ m

ole

cu

le-1

cm

3 s

-1)

1/(T / K)

Arrhenius plot for propene ozonolysis

This work: ln(kbim) = -2282.4/T - 31.3

IUPAC: ln(kbim) = -1880/T - 32.8

Fig. 5: Arrhenius plot for propene+O3 reaction at

1000 mbar and over a temperature range of 233

– 323 K.

• ClNO2 production has an impact on NOx

and Cl budgets (Fig.1.).

• Cl:OH ratios have been monitored in

various sites including the polar regions.

Various studies have focused on better

understanding the implications of these

two cycles.

0.00 0.05 0.10 0.15 0.20 0.250.0

0.2

0.4

0.6

0.8

1.0

1.2

1.4

n-butane

isobutane

n-pentane

isopentane

ln [

hy

dro

ca

rbo

n] o

/[h

yd

roc

arb

on

] t

ln [ethane]o/[ethane]t

• A number of these studies are revealing important information on Cl atom chemistry

through observing relative hydrocarbon concentrations, in most studies alkanes.

• Hydrogen abstraction of hydrocarbons by atomic chlorine have been of interest to

kineticists for many years.

• Reactions involving chlorine atoms with n-butane, isobutane, n-pentane and

isopentane were studied experimentally in an environmental chamber. Experiments

were carried out over a temperature range of 225 – 325 K and at 1000 mbar.

• The main focus of this study was to obtain a better mechanistic understanding of

these reactions and in particular the structural influence of higher hydrocarbons on

hydrogen abstraction reactions.

• The kinetics of Cl atom hydrogen

abstractions from propane, n-butane,

isobutane, n-pentane and isopentane

has been investigated at room

temperature and 1000 mbar in the

HIRAC chamber.

• GC-FID and FTIR techniques were

used in order to analyse the rates of

decay of the hydrocarbons.

• The relative rate technique was used

to measure rate coefficients of these

reactions using ethane as a reference

compound.

• A new FTIR data analysis technique

was developed and used to analyse

the n-butane data obtained from this

study. Lack of suitable reference

spectra for other hydrocarbons

inhibited analysis of other FTIR data.

• A comparison of the kinetic data from

this study with other studies is shown

in Table 1.

• The results obtained for experiments

carried out at 298 K were all within

good agreement of the literature.

Fig. 7.: Relative rate plots for hydrocarbon + Cl

reactions at 1000 mbar and at 298 K.

• Previous studies for ethane+Cl showed a

positive temperature dependence, while

no similar trend was found for propane

and n-butane.

• A temperature dependent study was

carried out over ~220 – 320 K in the

HIRAC chamber using relative rate

method.

• Results obtained for isopentane+Cl gave

a negative temperature dependence (Ea =

-1.33 ± 0.02 kJ mol-1)

• n-pentane, isobutane and n-butane were

all found to be temperature independent

from this study.

Fig. 8: Arrhenius plots for

pentanes+Cl reaction at 1000 mbar

and over a temperature range of ~

220 – 320 K.

• Recent installation of a temperature

control system has enabled studies at

temperatures between ~ 223 – 323 K.

• System has been tested by

conducting a temperature-dependent

study for propene+O3 (Fig.5.).

• An Arrhenius plot of the bimolecular

rate constant for propene gave Ea =

19.84 ± 0.46 kJ mol-1. This value is

within error of the IUPAC and

literature data.

• A temperature profile of the HIRAC

chamber operating at about 233 –

323 K to check the uniformity of the

system is shown in Fig.4.

• The HIRAC chamber at the University

of Leeds(2) allows control of the

conditions of temperature, pressure

and photolysis rate which are

important variables affecting the rate

of processes in the atmosphere.

• HIRAC is a 2.25 m3 stainless steel

indoor chamber equipped with a

range of instruments including a GC-

FID , GC-HID, FTIR, FAGE, CRDS as

well as commercial NOx, O3 and CO

analysers.

• FTIR is coupled to HIRAC via a

multipass optical arrangement on the

interior of the chamber (Figure 3b).

• The mirror systems are robust and

able to handle ranges of temperatures

and pressures which the chamber is

subjected to.

• This Chernin cell optical system is a

modified multipass matrix system that

features three objective mirrors with

input and output apertures placed on

opposite sides of the small field mirror.

(a) (b)