“…NH 4 + accumulates in soil as a result of mineralization, N fixation (legumes), direct deposition from the atmosphere, or by application of inorganic fertilizers containing NH 4 + salts, e.g., (NH 4 ) 2 SO 4 . NH 4 + strongly sorbs to the negatively charged surfaces of soil minerals and Ch (1) MM ( [41] Ch (3) SM ( 75.5 [27,28,36,37,41,43,[45][46][47][48][49] soil organic matter (SOM) and is therefore resistant to leaching, but it may be lost by surface runoff, plant uptake, biological nitrification, or annomox reactions. NO 3 − that is produced via nitrification or directly added to soils via inorganic fertilizers, e.g., KNO 3 , is susceptible to a number of losses.…”