Abstract
Nitrogen uptake from non-exchangeable NH +4 byLolium multiflorum and availability of fertilizer NH +4 and fertilizer NO -3 were studied in pot experiments with three different soil types. The luvisol derived from loess released considerable amounts of non-exchangeable NH +4 when cropped. In this soil fertilizer NH +4 was only weakly fixed and was as available to the crop as fertilizer NO -3 . The recovery of fertilizer NH +4 was even higher than the recovery of fertilizer NO -3 . In the fluvisol (alluvial soil) and in the cambisol (brown earth from basalt) N recovery was higher from NO -3 fertilizer than from NH +4 fertilizer. In these soils NH +4 fertilizer was strongly fixed by 2:1 clay minerals and thus less available to the grass. Particularly in the basaltic soil the content of non-exchangeable NH +4 was low and so was the release of nonexchangeable NH +4 . At the same time this soil showed the strongest fixation of fertilizer NH +4 . Release and refixation of fertilizer NH +4 in the loess soil appears to be an important feature of this soil type with a beneficial effect on soil nitrogen turnover and availability.
Similar content being viewed by others
References
Bajwa MI (1984) Effect of soil clay mineralogy on the efficiency of ammonium sulfate in flooded rice. Fert Res 5, 281–284
Guo PC, Bohring J and Scherer HW (1983) Verhalten von Dünger-NH +4 in Böden unterschiedlicher tonmineralischer Zusammensetzung. Z Pflanzenernähr Bodenk 146, 752–759
Keerthisinghe G, Mengel K and DeDatta SK (1984) The release of nonexchangeable ammonium (15N labelled) in wetland rice soils. Soil Sci Soc Am J 48, 291–294
Kowalenko GG and Ross GJ (1980) Studies on the dynamics of ‘recently’ clayfixed NH +4 using15N. Can J Soil Sci 60, 61–70
Martin AE, Gilkes RJ and Skjemstad JO (1970) Fixed ammonium in soils developed on some Queensland phyllites and its relation to weathering. Aust J Soil Res 8, 71–80
McBeth IG (1917) Fixation of ammonium by soils. J Agric Res 9, 141–155
Mengel K and Scherer HW (1981) Release of nonexchangeable (fixed) ammonium under field conditions during the growing season. Soil Sci 131, 226–232
Praag HJ van, Fischer V and Riga A (1980) Fate of fertilizer nitrogen applied to winter wheat as Na15NO3 and (15NH4)2SO4 studied in microplots through a four-course rotation: 2. Fixed ammonium turnover and nitrogen reversion. Soil Sci 130, 100–105
Rolston DE, Fried M and Goldhamer DA (1976) Denitrification measured directly from nitrogen and nitrous oxide gas fluxes. Soil Sci Soc Am J 40, 259–266
Scharpf HC (1977) Der Mineralstickstoffgehalt des Bodens als Maßstab für den Stickstoffdüngerbedarf. Diss Fak Gartenbau und Landeskultur TH Hannover
Scherer HW (1984) Beziehung zwischen dem Stickstoff-Entzug der Pflanzen und der Abnahme von spezifisch gebundenem NH4-N im Boden. Z. Pflanzenernähr Bodenk 147, 29–36
Scherer HW and Mengel K (1979) Der Gehalt an fixiertem Ammoniumstickstoff auf einigen repräsentativen hessischen Standorten. Landw Forsch 32, 416–424
Scott AD and Smith SJ (1966) Susceptibility of interlayer potassium in micas to exchange with sodium. Clays and Clay Min Proc 14th Nat Conf, 69–81
Silva, JA and Bremner JM (1966) Determination and isotope — ratio analysis of different forms of nitrogen in soils: 5. Fixed ammonium. Soil Sci Soc Am Proc 30, 587–594
Walsh, LM and Murdock JT (1963) Recovery of fixed ammonium by corn in greenhouse studies. Soil Sci Soc Am Proc 27, 200–204
Webster CP and Dowdell RJ (1982) Nitrous oxide emission from permanent grass swards. J Sci Food Agric 33, 227–230
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Scherer, H., Mengel, K. Importance of soil type on the release of nonexchangeable NH +4 and availability of fertilizer NH +4 and fertilizer NO -3 . Fertilizer Research 8, 249–258 (1986). https://doi.org/10.1007/BF01048626
Accepted:
Issue Date:
DOI: https://doi.org/10.1007/BF01048626