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Effects of Agricultural Management Practices On Carbon Sequestration in Soils From a Tropical Agroecosystem: Understanding the Contribution of Geochemical Controls of Soil Carbon Sequestration.

Poster Number 1919

Tuesday, November 5, 2013
Tampa Convention Center, East Hall, Third Floor

Pavithra Sajeewani Pitumpe Arachchige1, Ganga Hettiarachchi1, Leila Maurmann2, Dorothy M Menefee1, Charles W. Rice1 and Telmo Jorge Amado3, (1)Department of Agronomy, Kansas State University, Manhattan, KS
(2)Department of Chemistry, Kansas State University, Manhattan, KS
(3)Federal University of Santa Mari, Rio Grande do Sul, Brazil
Soil carbon (C) sequestration has been identified as one of the effective potential mitigation option for increasing atmospheric carbon dioxide concentration. Climate, mineralogy and agricultural management practices affect soil organic C (SOC) content, chemistry as well as SOC stabilization mechanisms. This research is focused on understanding the SOC sequestration based on agricultural management practices and aggregate size fractions by determining chemistry of SOC, SOC and mineral associations and interactions. 

Oxisols were collected from 0-5, 5-15 and 15-30 cm depths from the Center of Experimentation and Research Fundacep in Cruz Alta-RS, Brazil which had been under same agricultural management practices since 1985. Main plots were tillage operated plots (no till/conventional till), whereas sub plots were different crop rotations. Four aggregate size fractions were separated by wet aggregate sieving method. Humic acid was extracted from each aggregate size fraction according to IHSS method and analyzed by FTIR,13C NMR and HPLC. Iron (Fe) mineralogy, total OC, amorphous and total Fe/Al oxides are determined. Results will be integrated to further our understanding on how agricultural management practices affecting geochemical mechanisms controlling C sequestration in tropical soils.

See more from this Division: SSSA Division: Soil Chemistry
See more from this Session: Towards a Conceptual Model of Soil Carbon Cycling Across Scales: III

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