Abstract:
Organic carbon accumulation in paddy ecosystems is faster and more pronounced than in other
arable ecosystems. The carbon and nitrogen are stored predominately as organic forms in the
soil, so mineralization affects both. Soil Nitrogen (SN) can be considered as an essential
component of soil carbon sequestration. The combined effect of fresh organic C inputs with low
soil N availability leading to a higher SOM mineralization rate and a lower Soil Carbon (SC)
storage potential. Hence, soil C responses to N enrichment might play a key role in detecting
potential atmospheric CO2 concentration trajectories. Therefore, the current study was
conducted to detect the relationships among soil C, N, and other influential chemical properties
associated with C sequestration capacity in paddy soils of Sri Lanka. Conditional Latin
Hypercube Sampling design (CLHs) was employed for the study covering all major paddy
growing areas (wet, intermediate, and dry zones). One thousand pooled soil samples were
collected throughout the country. Soil C and N contents were estimated by using CHN elemental
analyzer. Soil pH and Electrical Conductivity (EC) were measured using standard protocols.
Statistical analyses were performed using R statistical software. The current study reported the
zonal average values of soil C and N contents under wet, intermediate, and dry climatic
conditions. The average SC% for the wet zone (n=146) was 5.32 ± 2.82. Meanwhile, the average
SC% for the intermediate zone (n= 179) and dry zone (n= 675) were 2.24 ± 0.75 and 1.91 ± 0.82.
The average SN% for the wet, intermediate and dry zones were 0.51 ± 0.31, 0.22 ± 0.12 and 0.22
± 0.17. Specifically, a highly significant, positive linear relationship was found between SC and
SN contents (r=0.73, p<2.2 e-16). Furthermore, significant negative relationships were recorded
between SC and pH (r= -0.38, p<2.2e-16) as well as SN and pH (r=-0.30, p= 2.2e-16). The study
confirms that the increased level of soil N and low pH conditions enhanced the soil C storage
potential in paddy soil. Thus, the modest increases in SC resulting from N fertilizer applications
up to sensible agronomic rates would be useful in enhancing C sequestration capacity in paddy
soils of Sri Lanka.
