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EFFECT OF THE SYSTEM OF RICE INTENSIFICATION (SRI) ON ...

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materials. These two chapters lead to chapter 4, 5 and 6 introducing <strong>SRI</strong>, Cambodian rice culture<br />

and development strategies in developing countries respectively. Chapter 7 and 8 introduce the<br />

target area in Cambodia and materials and methods applied in the field and laboratory for data<br />

collection respectively. Results are discussed and evaluated in chapter 9 and finally general<br />

conclusions are drawn in chapter 10.<br />

2. The role of Soil Organic Matter (SOM) in flooded rice soils<br />

2.1 Definition of SOM<br />

SOM can be defined as the sum of all organic matter (OM) in a soil, resulting from undecayed OM<br />

from plant tissues, soil microorganisms and animals, grasses, weeds, leaves and roots (Borggaard &<br />

Elberling, (2003). These different soil ingredients are part of different pools all responsible for the<br />

definition of SOM. The most important pools are i) the litter pool comprising e.g. crop residues, ii)<br />

light fraction - with root residues and iii) microbial biomass – the degradation of plant material<br />

(Stevenson & Cole, 1999). As all OM contains large percentages of C (Brady & Weil, 1999a) and<br />

in average SOM contains 58% C (Borggaard & Elberling, 2003). Roughly speaking can C in soils<br />

divided between two pools: Soil Organic Carbon (SOC) and Soil Inorganic Carbon (SIC) (Lal,<br />

2002). The SOC pool is composed of two very different fractions. The inert pool which does not<br />

comprise mineralization and is determined by climate, soil type and landscape position (Lal, 2006).<br />

The other pool is the labile pool which relies on management practices (Lal, 2006). The SOC pool<br />

comprising the labile factors can be influenced by management and there are direct effects on soil<br />

quality and the SOC content is linked to the labile pool (Lal, 2006). The labile pool is also<br />

interesting to focus on as it is near to the soil surface and possible GHG emissions will emit from<br />

this pool (Schlesinger & Andrews, 2000) and it has faster turnover rates of OM than the inert pool<br />

(Mandal et al., 2008). Mineralization is taking place in this pool and thereby the key to increase<br />

productivity is through SOC. This report measured the percentage of OM in the soils of Prey Veng,<br />

Cambodia. The terms, SOM, SOC, OM and C will all be used throughout this report to express the<br />

soil quality.<br />

13

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