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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]

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