"8788","16","archive","1305",,,"disk0/00/00/87/88","2015-06-19 06:14:41","2015-06-19 06:23:53","2015-06-19 06:14:41","book_section",,,"show",,,,"","","","","","","","","","",,,,"Subba Rao","G V","","","","","","","Sahrawat","K L","","","","",,,,,"","",,,,,"","","Japan International Research Center for Agricultural Sciences (Ibaraki)","Japan","Biological nitrification inhibition (BNI) activity in sorghum: Potential role for enhancing nitrogen-use efficiency (NUE)","pub","s1.4","D4","crp1.4","public",,"paper","Sorghum; Biological Nitrification Inhibition; Nitrogen use efficiency; Ammonia",,"Proceedings of Global Consultation on Millets Promotion for Health & Nutritional Security, 18-20 December, 2013","Nitrification and denitrification are the primary drivers for generating reactive -N (NO3-, N20 and NO) the two processes of N-cycle, largely responsible for soil-N losses, resulting poor N-recovery and low-NUE in agricultural systems. Suppressing soil nitrifier activity facilitates retention of soil mineral-N as ammoninum, leads to better utilization of N in situations where 
nitrification is followed by N losses via leaching and/or denitrification. Soils in the WCS (West Central Sahelian zone of Africa) where sorghum is predominantly grown, are of light-textured sandy-loams with acidic (ph 5.0 to 6.0). Alfisols in India and Ultisols in South America are also of light-textured and acidic, where most of the sorghum grown globally. Nitrogen mineralized  from SOM (soil organic matter) or from inorganic fertilizers is quickly nutrified and lost through leaching.","2015","published",,,,,"Society for Millets Research, ICAR Indian Institute of Millets Research","Hyderabad","91-96","253",,,,,,,,,,"TRUE","8189335529",,"Millets : Promotion for Food, Feed, Fodder, Nutritional and Environment Security, Proceedings of Global Consultation on Millets Promotion for Health & Nutritional Security",,,,,"",,"","",,"","",,,,,,"",,,,,,,"",,,,,"",,,,,"","",,,,,"","",,,,,
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