Measuring carbon stock in peat soils - Balai Penelitian Tanah
Measuring carbon stock in peat soils - Balai Penelitian Tanah
Measuring carbon stock in peat soils - Balai Penelitian Tanah
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46<br />
Agus et al. (2011)<br />
Analyzer (IRGA) or Gas Chromatography (GC)<br />
o By us<strong>in</strong>g IRGA the gas from a closed chamber flows <strong>in</strong>to the IRGA<br />
(Figure 18) by us<strong>in</strong>g a pressure pump and CO concentration is<br />
2<br />
directly read by the IRGA every second for approximately 2.5<br />
m<strong>in</strong>utes. A l<strong>in</strong>ear relationship between time of observations with<br />
the concentration of CO gas is used to calculate the CO flux to<br />
2 2<br />
the ground surface.<br />
o If us<strong>in</strong>g a GC, the gas samples are collected from closed<br />
chambers us<strong>in</strong>g syr<strong>in</strong>ges (Figure 19) and then the gas<br />
concentration is measured by a GC (Hue et al. 2000).<br />
Closed chamber<br />
PC or data logger<br />
Unit IRGA<br />
Figure 18. Infra-Red Gas Analyzer (IRGA) and the closed chamber for measur<strong>in</strong>g CO 2<br />
gas flux emitted from the soil<br />
Empirical relationship of land management and emissions<br />
From a review of publications based on research <strong>in</strong> Sarawak, Malaysia, and<br />
(ma<strong>in</strong>ly) Kalimantan, Indonesia, Hooijer et al. (2006, 2010) developed a l<strong>in</strong>ear<br />
relationship between the depth of dra<strong>in</strong>age, DD, and CO emissions:<br />
2<br />
E bo (t CO 2 /ha/yr) = 0,91 DD (cm) [11]