142-9 Modeling Solute Transport in Soil Under Conservation Agriculture Production Systems in the Philippines.

Poster Number 1625

See more from this Division: S06 Soil & Water Management & Conservation
See more from this Session: Agricultural Management Practices Impact On Soil Carbon and Nitrogen Pools and Soil Quality Dynamics: II
Monday, October 22, 2012
Duke Energy Convention Center, Exhibit Hall AB, Level 1
Share |

Paul O. Tarnate, University of the Philippines Los Banos, Los Banos, Philippines, Victor B. Ella, Land and Water Resources Division, Institute of Agricultural Engineering, University of the Philippines Los Banos, Los Banos, Philippines and Manuel R. Reyes, Natural Resources and Environmental Design, North Carolina Agricultural and Technical State University, Greensboro, NC
This study aimed to model and to compare the solute-transport behavior of soil under conservation agriculture production and plow-based systems in the Philippines. Undisturbed soil core samples were taken from both production systems from experimental sites of SANREM-CRSP in Claveria, Misamis Oriental, Philippines.  Miscible displacement and adsorption experiments were performed at the laboratory facilities of the College of Engineering and Agro-industrial Technology, University of the Philippines Los Baños.  A stochastic method, following continuous-input soil column tests, determined the dispersivity of the soil samples while a laboratory flow-through method, using pulse-input soil column tests, calculated the retardation factor.  Both the soil dispersivity and the retardation factor were optimized using the CXTFIT model to fit the observed values to the Convection-Dispersion Equation. Upper-layer plow-based soil, with a combined lowest retardation factor of 1.26 and dispersivity of 17.5 cm, had the highest peak concentration of 0.67C0 and the shortest time-to-peak of 44 s.  Soils under conservation agriculture production systems, having a high retardation factor of 6.54 in spite of the highest value of dispersivity of 27.3, exhibited the lowest peak concentration of 0.44C0 after nearly 7 min of peaking time.  These results may be indicative of higher soil organic carbon content in soils under conservation agriculture.  Model efficiencies ranging from 77% to 98% signify that the Convection-Dispersion Equation is able to adequately predict solute transport in these soils. Simulations of solute transport in response to changing soil organic carbon content for a ten-year period were performed.  Increasing the organic carbon by 30% in soils under conservation agriculture reflects a 9.6% decrease in peak concentration and a 3.1% increase in time-to-peak.  On the other hand, there are minimal changes in terms of both peak concentration and time-to-peak in soils under plow-based systems assuming 3% decrease in organic carbon. Model simulation results have practical implications on both the economics of crop production in terms of agro-chemical application and on groundwater quality protection.
See more from this Division: S06 Soil & Water Management & Conservation
See more from this Session: Agricultural Management Practices Impact On Soil Carbon and Nitrogen Pools and Soil Quality Dynamics: II