139-6 Sensitivity of Labile Soil Organic Carbon Pools to Short-Term Conservation Agriculture Production Systems in Cambodia.

See more from this Division: SSSA Division: Soil & Water Management & Conservation
See more from this Session: Management Impacts on Soil Properties and Soil C and N Dynamics: I
Monday, November 3, 2014: 9:45 AM
Hyatt Regency Long Beach, Shoreline A
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Lyda Hok1, Joao Carlos Moraes Sa2, Stephane Bulakia3, Manuel R. Reyes1, Vira Leng4, Rada Kong4, Florent Elie Tivet3, Clever Briedis2, Daiani da Cruz Hartman2, Lucimara Aparecida Ferreira2 and Tomas Magno2, (1)North Carolina A&T State University, Greensboro, NC
(2)Universidade Estadual de Ponta Grossa, Ponta Grossa, Brazil
(3)Centre de Coopération Internationale en Recherche Agronomique pour le Développement (CIRAD), Montpellier, France
(4)General Directorate of Agriculture, Phnom Penh, Cambodia
Conservation agriculture (CA) constitutes an effective tool to increase soil C sequestration although rigorous empirical evidence from Southeast Asia is still limited. The objective of this study was to quantify short-term impacts of CA (5 years) on labile SOC pools in a Cambodian Latosol under rice-, soybean- and cassava-based cropping systems (RCS, SCS and CCS, respectively). The field trials were initiated in 2009 and there were four treatments in each cropping system consisting of (i) conventional tillage (CT); (ii) no-till (NT) systems (one year frequency pattern of main crops); and (iii) and (iv) NT systems (bi-annual rotations of main crops with maize). The tillage and crop rotations had significant on SOC and N stocks in SCS and CCS and an increasing trend was observed in RCS. On average, NT increased SOC stocks over CT at the 0-5 cm depth by 10%, 20% and 18% and N stocks by 8%, 25% and 16% for RCS, SCS and CCS, respectively. Lower SOC stocks in the subsoil layers under NT than CT were consistently observed in the three cropping systems. Similarly, greater hot-water extractable C (HWEOC) stocks of 61%, 55% and 53%, and permanganate oxidizable C (POXC) stocks of 23%, 21% and 32% in NT than in CT soils under RCS, SCS and CCS, respectively, at 0-5 cm soil layer were apparent. When comparing to reference vegetation (RV), the order of SOC, HWEOC and POXC levels were RV > NT > CT at 0-5 cm in the three cropping systems. In conclusion, our results corroborate the concept that short-term CA impacts on SOC dynamics are detected in the topsoil layer and the potential to increase SOC in the subsoil layers when deep-rooting cover crops are included in the crop rotations. The labile SOC pools (i.e. HWEOC and POXC) could be served as sensitive indicators in short-term changes in agricultural management practices.
See more from this Division: SSSA Division: Soil & Water Management & Conservation
See more from this Session: Management Impacts on Soil Properties and Soil C and N Dynamics: I