Sains Malaysiana 49(8)(2020): 1809-1817
http://dx.doi.org/10.17576/jsm-2020-4908-05
Tracing
the Carbon Flow in Tropical Watershed using Stable Isotope Technique
(Mengesan
Aliran Karbon di dalam Legeh Sungai Tropika Menggunakan Teknik Isotop Stabil)
MOHAMAD SHAIFUL MD YUSUFF1, MUHAMMAD
IZZUDDIN SYAKIR1,2* & WIDAD FADHULLAH1
1Environmental
Technology Division, School of Industrial Technology, Universiti Sains Malaysia,
11800 Minden, USM Pulau Pinang, Malaysia
2Centre for Global Sustainability Studies,
Universiti Sains Malaysia,
11800 Minden, USM Pulau Pinang, Malaysia
Diserahkan:
17 Mac 2019/Diterima: 25 Mac 2020
ABSTRACT
Research on catchment area have
traditionally involved concentration and flux measurement to better understand
weathering, transport and cycling of materials from land to sea. Potentially,
modification of terrestrial environment can alter the carbon flow in a
catchment. This research is to characterize dissolved inorganic carbon (DIC) in
Sungai Kurau and Tasik Bukit Merah. A progressive depletion of (δ¹³C–DIC:
-14.20 ± 0.47‰) towards downstream (δ¹³C–DIC: -24.44 ± 0.59‰) is observed.
The trend indicates photosynthesis activity at the upper stream system where
microbial respiration process is observed to occur at the Tasik Bukit Merah
located at downstream area. The dynamic of carbon pathway is highly affected by
allochthonous input and autochthonous process in the catchment system. Land use
activities within the catchment can disturb the balance between biological and
geological processes which control the carbon pool in Kurau catchment.
Keywords: Carbon-13; carbon cycle;
photosynthesis; respiration; Tasik Bukit Merah
ABSTRAK
Penyelidikan di kawasan tadahan secara
tradisinya melibatkan kepekatan dan pengukuran fluks untuk lebih memahami
luluhawa, pengangkutan dan kitaran bahan dari darat ke laut. Berpotensi,
pengubahsuaian persekitaran daratan dapat mengubah aliran karbon dalam kawasan
tadahan. Kajian ini adalah untuk mengenal pasti karbon bukan organik yang
dilarutkan (DIC) di Sungai Kurau dan Tasik Bukit Merah. Pengurangan progresif
(δ¹³C-DIC: -14.20 ± 0.47‰) ke arah hiliran (δ¹³C-DIC: -24.44 ± 0.59‰)
diperhatikan. Petunjuk ini menunjukkan aktiviti fotosintesis pada sistem hulu
sungai dengan proses respirasi mikrob diperhatikan berlaku di Tasik Bukit Merah
yang terletak di kawasan hilir sungai. Dinamik laluan karbon amat dipengaruhi
oleh input dan proses autoktonus dalam sistem kawasan tadahan. Aktiviti
penggunaan tanah dalam kawasan tadahan boleh mengganggu keseimbangan antara
proses biologi dan geologi yang mengawal kelompok karbon di kawasan tadahan
Kurau.
Kata kunci: Fotosintesis; karbon-13; kitaran karbon; respirasi; Tasik Bukit
Merah
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*Pengarang
untuk surat-menyurat; email: misyakir@usm.my
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