The
Malaysian Journal of Analytical Sciences Vol 11 No 1 (2007): 29 – 35
HYDROCARBONS IN SMOKE AEROSOLS FROM CONTROLLED
BURNING OF MANGIFERA FOETIDA LITTER
FALLS
AND PANICUM
REPENS
Tay Joo Hui1, Tan Hock Seng1,
Norhayati Mohd Tahir* 1and Mhd Radzi Abas2
1Environmental Research Group (ERG), Department of
Chemical Sciences,
Faculty of
Science and Technology, Kolej Universiti Sains dan Teknologi Malaysia,
Mengabang
Telipot, 21030 Kuala Terengganu
2 Chemistry
Department, University Malaya,
50603 Kuala
Lumpur
*Corresponding
author: hayati@kustem.edu.my
Abstract
A
study has been carried out to characterize hydrocarbons emitted from the
burning of two typical garden wastes, bachang (Mangifera foetida) litter falls
and grass (panicum repens). The biomass samples were burned and their
respective smoke particulate emitted was sampled using high volume sampler
fitted with pre-cleaned glass fibre filters under smouldering and flaming
conditions. Hydrocarbons were extracted
using dichloromethane- methanol mixture
as solvent and the extracts fractionated on silica-alumina column. Detection
and quantification of aliphatic hydrocarbons and PAHs compounds were carried
out using GC-MS. For comparison,
hydrocarbons in fresh unburnt bachang litter falls and grass were also analyzed
for aliphatic and PAHs content. Result indicated that the major components in
the aliphatic fraction for all samples were n- alkane compounds which exhibited
a saw-tooth pattern that is characteristic of a biogenic origin. The major
components in this aliphatic fraction for smoke particulate matters were n-alkanes in the range of C12-C36, with an odd to even carbon predominance with
CPI values ranging from 2.89-4.32 and Cmax generally at C31;
total identified n- alkanes for these samples ranged from 221-939 µgg-1.
On the other hand, hydrocarbons present in the fresh unburnt bachang
litter falls and grass ranged from C12-C36 with C27 and C33 species
dominating and CPI value of 4.5 and 23.1, respectively; total identified n-
alkanes were significantly higher (1530-33000 µgg-1) than those
found in smoke aerosols In general, CPI
> 1 indicates n-alkanes contribution from epicuticular waxes thus it could
be concluded that, even though the overall signature of the source of n-alkanes
is maintained, burning seems to alter the distribution of aliphatic
hydrocarbon emitted accompanied with a decrease in the CPI values
and shifting in Cmax. In addition, results also indicated that
burning resulted in the formation of many PAHs compounds in all smoke aerosols
samples with total PAHs concentration ranging from 187-296 µgg-1.
Fresh unburnt bachang litter falls and grass on the other hand did not exhibit
any PAHs compound, which clearly indicated that PAHs were generally generated
from combustion process.
Keywords: smoke aerosols,
biomass, controlled burning, hydrocarbons, polycyclic aromatic hydrocarbons.
References
1. Simoneit, B.R.T. 2002. Biomass burning-
a review of organic tracers for smoke from incomplete combustion. Applied Geochemistry,
17:129-162.
2. Oros, D.R. & Simoneit, B.R.T.
2001a. Identification and emission factors of molecular tracers in organic
aerosols from biomass burning. Part 1. Temperate climate conifers. Applied
Geochemistry, 16:1513-1544.
3. Crutzen, P.J.
& Andreae, M.O.
1990. Biomass burning
in the tropics:
impacts on atmospheric
chemistry and biogeochemical
cycles. Sci. 250: 1669-1678.
4. Levine, J.S., Cofer, W.R., Cahoon, Jr.
A.R. & Winstead, E.L. 1995. Biomass burning: a driver for global change. Environ.
Sci. Technol. 29:120-125.
5. EarthTrends. (2003). Economic
Indicators-Malaysia. [online].
http://earthtrends.wri.org/pdf_library/country_profiles/eco_cou_458.pdf.
6. Abas, M.R., Oros, D.R. & Simoneit,
B.R.T. 2004b. Biomass burning as the main source of organic aerosol particulate
matter in Malaysia during haze episodes. Chemosphere, 55: 1089-1095.
7. Fang, M., Zheng, M ., Wang, F., To,
K.L., Jaafar, A.B. & Tong, S.L. 1999. The solvent -extractable organic
compounds in the Indonesia biomass burning aerosols -characterization studies.
Atmos. Environ., 33: 783-795.
8. Abas, M.R., Rahman, N.A., Omar,
N.Y.M.J., Maah, M.J., Samah, A.A., Oros, D.R., Otto, A. & Simoneit, B.R.T. 2004a.
Organic composition of aerosol particulate matter during a haze episode in
Kuala Lumpur, Malaysia. Atmos. Environ., 38: 4223-4241.
9. Oros, D.R. & Simoneit, B.R.T.
2001b. Identification and emission factors of molecular tracers in organic
aerosols from biomass burning. Part 2. Deciduous trees. Applied Geochemistry,
16:1545-1565.
10. Eglinton,
G., Hamilton, R.J. & Smith, M.M. (1962b). The alkane constituents of some
New Zealand plants and their possible taxonomic implications. Phytochem. 1:
137-145.
11. Kolattukudy,
P.E. 1970. Plant waxes. Lipids, 5:259-275.
12. Rieley,
G., Collier, R.J., Jones, D.M. & Eglinton, G. (1991). The biogeochemistry
of Ellesmere Lake, UK.-I. Source correlation of leaf wax inputs to the
sedimentary lipid records. Org. Geochem. 17:901-912.
13. Simoneit, B.R.T & Mazurek, M.A. (1982).
Organic matter of the troposphere-II. Natural background of biogenic lipid
matter in the aerosols over the rural Western United States. Atmos. Environ. 8:
251.275.
14. Eglinton,
G. and Hamilton, R.J. (1963). The distribution of alkanes. In Chemical
Plant Taxanomy, pp.187-217.Academic Press. London.
15. Pelejero,
C., 2003. Terrigenous n-alkane input in the South China Sea: high resolution
records and surface sediments. Chemical Geology, 200:89-103.