99315 Assessment of Soil Organic Carbon, Nitrogen and C/N Ratios As Key Components for Evaluating Nitrate Reduction Strategies at a Subbasin Scale.
Poster Number 463-618
See more from this Division: SSSA Division: Soil and Water Management and Conservation
See more from this Session: Soil Management Impacts on Soil Properties and Soil C and N Dynamics Poster II
Wednesday, November 9, 2016
Phoenix Convention Center North, Exhibit Hall CDE
Abstract:
In the U.S. Midwest, many states, including Iowa, Ohio, Illinois and Minnesota are developing strategies to reduce export of nitrate-N (NO3-N) from agricultural nonpoint sources to the Mississippi River. Watershed projects implemented through U.S. Department of Agriculture (USDA) assistance programs typically include a variety of in-field and edge-of-field best management practices (BMPs) to reduce NO3-N loss. Many of these conservation practices are intended, in part, to improve soil quality because of its critically important role in influencing nutrient cycling, water holding capacity and overall soil sustainability. Management of soil organic carbon (SOC) and nitrogen (N) is considered a key component to prevent N loss to groundwater and artificial drainage. Our study intensively sampled the top soil (top 20 cm) in a 780 ha subbasin of Rapid Creek watershed, Iowa to evaluate and quantify landscape-scale storage of SOC and N and to identify potential groundwater vulnerability for these soils via NO3-N leaching. Results indicated variability in N and SOC concentrations in the subbasin soils within a normal distribution and spatial analysis did not show any systematic field by field variations that would suggest potential hot spots for NO3-N loss. Significantly lower SOC concentrations were measured in shoulder landscape positions, but no other variability was detected for N or C/N ratios. We estimated the total mass of SOC and N present in the subbasin using both slope class and soil series classifications and found that both quantification methods provided similar estimates (6.22 x 103 to 5.88 x 103 Mg SOC and 5.57 x 102 to 3.71 x 102 Mg N). C/N ratios ranged from 1-37 with a mean of 18 +/-6, but consistent with SOC and N, no field-level variation in the ratios was readily apparent. Most of the soils in the subbasin had C/N ratios less than 20 which suggests potential for soil N mineralization. Without a hot-spot for soil N loss identified, we propose a basin-wide approach to reduce NO3-N export through incorporation of cover crops to reduce nitrification and increase SOC and C/N ratios.
See more from this Division: SSSA Division: Soil and Water Management and Conservation
See more from this Session: Soil Management Impacts on Soil Properties and Soil C and N Dynamics Poster II
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