Title of document: Dynamics of Soil Carbon, Nitrogen and Soil Respiration in Famer’s Field with Conservation
Agriculture, Siem Reap, Cambodia
Authors: Don Immanuel A. Edralin, Gilbert C. Sigua and Manuel R. Reyes
Journal’s name if any: International Journal of Plant & Soil Science
Ministry/Government Agency/Organisation: North Carolina Agricultural and Technical State University, Greensboro, NC, USA; United States Department of Agriculture, Agricultural Research Service, Coastal Plains Soil, Water, and Plant Research Center, Florence, SC, USA.
Year of publication: 2016
Geographic focus: National level
Main issues / topics addressed (for example: No tillage; conventional tillage; soil organic carbon; soil quality index; cover crops.…)
School of agroecology (if any):
Web address to original document (if any):
The years of intensive tillage in many countries, including Cambodia have caused significant decline in agriculture’s natural resources that could threaten the future of agricultural production and sustainability worldwide. Long-term tillage system and site-specific crop management can affect changes in soil properties and processes, so there is a critical need for a better and comprehensive process-level understanding of differential effects of tillage systems and crop management on the direction and magnitude of changes in soil carbon storage and other soil properties. A study was conducted in farmer’s field to evaluate the effect of conservation agriculture
(CA) and conventional tillage (CT) on soil carbon, nitrogen and soil respiration in three villages of Siem Reap, Cambodia. Soil organic carbon (p≤0.01), soil total nitrogen (p≤0.01) and soil respiration (p≤0.10) for at least in two villages were significantly affected by tillage management. The soil quality was improved in villages with CA compared with villages with CT by increasing soil organic carbon (10.2 to 13.3 Mg ha-1) and soil nitrogen (0.87 to 1.11 Mg ha-1) because of much higher soil moisture (15.7±8.6 to 20.0±11.9%) retained in CA and with reduced soil temperature (30.4±2.0 to 32.4±2.3°C) during the dry period. Additionally, field soil respiration was higher in CA (55.9±4.8 kg CO2-C ha-1 day-1) than in CT (36.2±13.5 kg CO2-C ha-1 day-1), which indicates more microbial activity and increased mineralization of soil organic carbon for nutrient release. The soil’s functions of supporting plant growth and sink of carbon and recycler of nutrients was likely improved in agroecosystem with CA than in system with CT. Our results have suggested that CA may have had enhanced soils’ carbon and nitrogen contents, nutrient supplying capacity and microclimate for soil microorganisms in three villages with vegetable production.