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However, in the literature, there are numerous reports of net negative fluxes of N<jats:sub>2<\/jats:sub>O, (i.e. fluxes from the atmosphere to the soil). Such fluxes are frequent and substantial and cannot simply be dismissed as experimental noise.<\/jats:p><jats:p>Net N<jats:sub>2<\/jats:sub>O consumption has been measured under various conditions from the tropics to temperate areas, in natural and agricultural systems. Low mineral N and large moisture contents have sometimes been found to favour N<jats:sub>2<\/jats:sub>O consumption. This fits in with denitrification as the responsible process, reducing N<jats:sub>2<\/jats:sub>O to N<jats:sub>2<\/jats:sub>. However, it has also been reported that nitrifiers consume N<jats:sub>2<\/jats:sub>O in nitrifier denitrification. A contribution of various processes could explain the wide range of conditions found to allow N<jats:sub>2<\/jats:sub>O consumption, ranging from low to high temperatures, wet to dry soils, and fertilized to unfertilized plots. Generally, conditions interfering with N<jats:sub>2<\/jats:sub>O diffusion in the soil seem to enhance N<jats:sub>2<\/jats:sub>O consumption. However, the factors regulating N<jats:sub>2<\/jats:sub>O consumption are not yet well understood and merit further study.<\/jats:p><jats:p>Frequent literature reports of net N<jats:sub>2<\/jats:sub>O consumption suggest that a soil sink could help account for the current imbalance in estimated global budgets of N<jats:sub>2<\/jats:sub>O. Therefore, a systematic investigation into N<jats:sub>2<\/jats:sub>O consumption is necessary. This should concentrate on the organisms, reactions, and environmental factors involved.<\/jats:p>","DOI":"10.1111\/j.1365-2486.2006.01280.x","type":"journal-article","created":{"date-parts":[[2006,11,17]],"date-time":"2006-11-17T14:15:10Z","timestamp":1163772910000},"page":"1-17","source":"Crossref","is-referenced-by-count":857,"title":["Soils, a sink for N<sub>2<\/sub>O? 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