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Denitrification Denitrification Is a Natural Soil Microbial - Process Where Nitrate (NO3 ) Is Converted to Nitrogen (N) Gases That Are Lost to the Atmosphere

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Denitrification Denitrification Is a Natural Soil Microbial - Process Where Nitrate (NO3 ) Is Converted to Nitrogen (N) Gases That Are Lost to the Atmosphere Nitrogen NUMBER 5 NOTES Denitrification Denitrification is a natural soil microbial - process where nitrate (NO3 ) is converted to nitrogen (N) gases that are lost to the atmosphere. Denitrification occurs when soil bacteria use nitrate for their respira- tion in the place of oxygen in the air. This process occurs most rapidly in warm, wet soils with an abundance of nitrate. What is it? tion losses of added N fertilizer may exceed 50%. oil microbes are capable of converting nitrate into vari- Why Does It Occur? ous gases under certain conditions. This loss of nitrate When the oxygen (O ) supply in soil becomes limited, a by denitrification has negative economic consequences 2 variety of bacteria use the oxygen in nitrate for respiration. Sfor crop production since valuable N fertilizer is lost to the Denitrification most commonly occurs in wet or waterlogged air. However in many aquatic systems and for wastewater soils where the oxygen supply for respiration is restricted. Some treatment, denitrification has a positive benefit of lowering the fungi can denitrify, but they are not considered significant. nitrate concentration in water. Denitrification can be viewed as either desirable or detrimental depending on the objectives. When Does It Occur? Denitrification results in the reduction of nitrate to a variety Denitrification proceeds rapidly when water-filled pore of gases (including NO, N2O, or N2). One of these gases is space in soils exceeds 60%. The end-product gas depends nitrous oxide (N2O), a potent greenhouse gas that can remain on the soil conditions and the microbial community. As the in the air for over 100 years. Nitrous oxide has also been linked oxygen deficit increases, microbes tend to convert more of the with depleting stratospheric ozone. Although losses from the nitrate to N2 gas. For the purposes of nutrient management, process may have global implications, the total losses from denitrification results in a loss of valuable N, but the impact denitrification are generally less than 1% of total fertilizer N in the atmosphere will vary. applied to agricultural soils. In unusual conditions, denitrifica- Nitrogen Notes is a series of bulletins written by scientific staff of the International Plant Nutrition Institute (IPNI). This series was supported by a grant from the California Department of Food & Agriculture and through a partnership with the Western Plant Health Association. This series is available as PDF files at www.ipni.net/publications. Nitrogen NOTES their energy from soluble organic carbon. Therefore denitrifica- tion is enhanced in soils with a ready supply of organic carbon, such as manure, compost, cover crops, or crop residues. Soluble carbon also influences the end product of denitrification. Pro- duction of N2 commonly dominates with an adequate supply NO N2 - NO of soluble carbon, while N2O and NO production is more 3 likely if soluble carbon limits microbial growth. There have been experimental attempts to stimulate deni- trification in the field to remove nitrate from water by adding NO - N O 2 2 soluble carbon (such as edible oil, molasses, and other rap- idly degraded carbon sources) as energy sources for microbes. Denitrification Reaction Sequence Similarly, passing nitrate-rich surface water through a reactor - - - - - - - - - - - - - - gaseous - - - - - - - - - - - - - - NO - NO - NO N O N or through a constructed wetland to stimulate denitrification 3 2 2 2 is a common technique for water treatment. Nitrate Nitrite Nitric Oxide Nitrous Oxide Nitrogen Gas Soils that go through a prolonged dry period followed by rainfall or irrigation typically have a burst of soluble carbon Figure 1. Nitrate must be present in the soil for denitrification to that can support a spike in denitrification. Waterlogging also occur. The most common end products of denitrification are stimulates the release of soluble carbon into the soil that may N O and N gases that return to the atmosphere. 2 2 support rapid denitrification. Controlling Factors Where Does It Occur? Presence of Nitrate: Denitrification only occurs when Denitrification potential is greatest in the topsoil where nitrate is present (Figure 1). One method for minimizing microbial activity is highest. The topsoil contains the highest denitrification is to maintain a minimum concentration of concentration of carbon, the microbial energy source. Nitrate nitrate needed to support healthy plant growth. This can be moving below the topsoil is increasingly less likely to be deni- accomplished through techniques such as split fertilizer appli- trified with depth, as microbial activity generally drops rapidly cations, fertigation, or the use of controlled-release fertilizers. beneath the root zone. One study reported that 68% of the Another approach is the use of a nitrification inhibitor denitrification potential occurred in the top ½ inch of the soil. added to N fertilizer. Nitrification inhibitors temporarily A shortage of appropriate bacteria does not limit denitrification restrict Nitrosomonas bacteria from converting ammonium to in most agricultural soils. nitrite. Slowing this process reduces the rapid appearance of Plant roots have a variable impact on denitrification. Roots nitrate that commonly follows fertilization with ammonium- release significant amounts of soluble carbon and sloughed root based fertilizer, or manure. cells. Oxygen in the soil is consumed during root respiration. Temperature: Most soil microbial processes are strongly Conversely, plant roots dry the soil as they draw moisture for influenced by temperature. Studies show that denitrification is most rapid at temperatures between 80°F and 100°F, which is warmer than most soils, even during summer. Nitrification N2 The relatively mild winter temperatures and rainfall pat- s terns in California agricultural regions permit denitrification Denitrification to continue year-round (although slower in the winter). N2O Soil wetness: The presence or absence of oxygen is one of the largest factors determining the extent and duration of NO denitrification. Denitrification can occur in aerobic (adequate ux of nitrogen gase oxygen) conditions, but to a relatively insignificant degree. fl Wet soils are generally the trigger for denitrification to oc- cur. Nitrogen gases can begin to appear as soon as 15 minutes Net after saturation if conditions are favorable. At higher soil mois- ture, N tends to become the major product of denitrification, 2 25 50 75 100 compared with N2O (Figure 2). In flooded rice production, there are usually very low con- Water-filled pore space, % centrations of nitrate that can be denitrified because of careful Figure 2. Nitrous oxide is produced through denitrification when the fertilizer management. However during in-season draining soil becomes wet and water-filled pore space begins to events, nitrate may be produced which can be denitrified dur- exceed 60%. In very wet soils, N2 becomes more prevalent ing subsequent flooding events. from denitrification. Adapted from: A.F. Bouwman, Nature Presence of dissolved carbon: Denitrifying bacteria obtain 392, 866-867 (30 April, 1998). Nitrogen Notes 2 Nitrogen NOTES evapotranspiration and they deplete soil nitrate as the plant Crop and Soil Management Practices for Controlling Denitrification grows. 1. Minimize fertilizer and manure N applications in excess of the crop The process of denitrification ranges widely across a field. requirement to avoid surplus nitrate in the soil. Many conditions, such as the random placement of crop 2. Time N fertilizer application for when plants are rapidly growing and residues, soil macropores and aggregation, and small-scale have a requirement for the applied N. variations in soil organic matter and fertilizer distribution 3. Apply irrigation water to properly meet crop needs. Avoid overwatering will all influence denitrification rates on a micro-scale. This and waterlogging as much as possible. Non-uniform irrigation can result variation makes accurate field measurements of denitrification in saturated zones in the field. 4. Use appropriate N sources, including controlled-release fertilizers, nitrifi- challenging. cation inhibitors, or urease inhibitors when they fit within the manage- Denitrification Hotspots: Considerable confusion about ment plan. denitrification results from the complexity of the process 5. Avoid soil compaction that can impede water flow and result in ponding through the year, and variability across fields (Figure 3). Small and waterlogging; improve drainage in fields with excessive wetness. areas (hotspots) and brief denitrification bursts often contribute 6. Use urea or ammonium-based fertilizers where denitrification is antici- pated. most of the annual N2O emissions from a field. For example, one study showed that more than 80% of denitrification 7. Plant cover crops to reduce the concentration of residual nitrate in soil between cultivated crops. from a soil core occurred in and around a single decomposing 8. Mow or kill cover crops as close to the time of planting the next crop as leaf, which comprised less than 1% of the soil core volume. possible to minimize nitrate accumulation during decomposition. Variations in soil texture and water holding capacity across the 9. Time applications of animal manure and compost to avoid wet soils. landscape will also influence denitrification losses. Manure provides a source of carbon and nitrogen that can stimulate Management factors such as fertilizer source, rate, timing, denitrification. and placement as
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