THE 15N NATURAL ABUNDANCE AND NITROGEN FORMS IN ULTISOL CULTIVATED WITH EUCALYPTUS AND ACACIA

Authors

  • Rodinei Facco Pegoraro
  • Ivo Ribeiro da Silva
  • Roberto Ferreira de Novais
  • Nairam Felix de Barros
  • Reinaldo Bertola Cantarutti
  • Sebastião Fonseca

DOI:

https://doi.org/10.5902/1980509821121

Keywords:

acid hydrolysis, organic nitrogen, inorganic nitrogen, litter.

Abstract

http://dx.doi.org/10.5902/1980509821121

The nutrients nitrogen and one of the most demanded by plant species, and its presence in soil under organic or mineral forms available to plants is linked to quality and quatity of plant residues added to the soil. The study aimed to evaluate the influence of cultivation of eucalyptus and acacia in the composition of organic and inorganic N forms and the natural abundance of 15N in an Ultisol. For this, we collected soil and litter samples in continuous short-rotation eucalypt (Eucalyptus urophylla x Eucalyptus grandis hybrid) (seven years) compared to a rotation system including acacia (Acacia mangium Willd.) after short-rotation eucalypt; and long-rotation eucalypt (24 years). A native vegetation (Atlantic Forest) was used as a reference for the original site condition representative for the northern coast of  Espírito Santo state. To do so, we evaluated the content of total organic C, total N, N-NH4+, N-NO3-, C/N ratio, fractionation of organic N and 15N natural abundance in soil and litter. Among the forms of organic-N hydrolyzed, the N-amino was the fraction with the highest contribution of organic N (39%), followed by the fraction of N-unidentified (27%), the fraction of N-amide (18%) and N-hexosamine (15%). The acacia plantation presented smaller natural abundance of 15N and higher levels of total N and soil organic C, and increased organic forms of N-hydrolyzed, when compared to the eucalyptus short-rotation soil. This indicates the increase of labile N-organic forms in the soil for the plants and reduction of humification of soil organic matter (SOM) of acacia. Thus, the crops rotation with acacia after eucalyptus contributed to the increase of organic forms in the soil, important for the nutrition of plants, because they are potential sources of nutrients to the plants in a short-time period.

The nutrients nitrogen and one of the most demanded by plant species, and its presence in soil under organic or mineral forms available to plants is linked to quality and quatity of plant residues added to the soil. The study aimed to evaluate the influence of cultivation of eucalyptus and acacia in the composition of organic and inorganic N forms and the natural abundance of 15N in an Ultisol. For this, we collected soil and litter samples in continuous short-rotation eucalypt (Eucalyptus urophylla x Eucalyptus grandis hybrid) (seven years) compared to a rotation system including acacia (Acacia mangium Willd.) after short-rotation eucalypt; and long-rotation eucalypt (24 years). A native vegetation (Atlantic Forest) was used as a reference for the original site condition representative for the northern coast of  Espírito Santo state. To do so, we evaluated the content of total organic C, total N, N-NH4+, N-NO3-, C/N ratio, fractionation of organic N and 15N natural abundance in soil and litter. Among the forms of organic-N hydrolyzed, the N-amino was the fraction with the highest contribution of organic N (39%), followed by the fraction of N-unidentified (27%), the fraction of N-amide (18%) and N-hexosamine (15%). The acacia plantation presented smaller natural abundance of 15N and higher levels of total N and soil organic C, and increased organic forms of N-hydrolyzed, when compared to the eucalyptus short-rotation soil. This indicates the increase of labile N-organic forms in the soil for the plants and reduction of humification of soil organic matter (SOM) of acacia. Thus, the crops rotation with acacia after eucalyptus contributed to the increase of organic forms in the soil, important for the nutrition of plants, because they are potential sources of nutrients to the plants in a short-time period.

Downloads

Download data is not yet available.

References

ABRIL, A. et al. Effect of wheat crop fertilization on nitrogen dynamics and balance in the Humid Pampas, Argentina. Agriculture, Ecosystems & Environment. v. 119, n. 1-2, p. 171-176, 2007.

BATAGLIA, O.C. et al. Métodos de análises químicas de plantas. Campinas: Instituto Agronômico, 1983. 48p. (Boletim, 78)

BALIEIRO, F.C. et al. Evaluation of the throughfall and stemflow nutrient contents in mixed and pure plantations of Acacia mangium, Pseudosamenea guachapele and Eucalyptus grandis. Revista Árvore. v.31, n.2, p.339-346, 2007.

BODDEY, R.M. et al. Use of the 15N natural abundance technique to quantify biological nitrogen fixation by woody perennials. Nutrient Cycling in Agroecosystems, v.57, n.3, p.235-270, 2000.

BREMNER, J.M. Inorganic forms of nitrogen. In: BLACK, C.A.; EVANS, D.D.; ENSMINGER, L.E.; CLARK, F.E. eds. Methods of soil analysis, vol 2. Chemical and microbiological properties. ASA, Madison, Wis., 1965, p.1179-1237.

CAMARGO, F.A.C. et al. Nitrogênio orgânico do solo. In: SANTOS, G.A. et al. eds. Fundamentos da matéria orgânica do solo: Ecossistemas tropicais & subtropicais. Porto Alegre, Genesis, 2ª edição, 2008. p.87-99.

CAMARGO, O.F.A.; GIANELLO, C.; VIDOR, C. Tempo de hidrólise e concentração de ácido para fracionamento do nitrogênio orgânico do solo. Pesquisa Agropecuária Brasileira, v.32, n.2, p.221-227, 1997.

CHOI, W.J. et al. Natural 15N abundances of maize and soil amended with urea and composted pig manure. Plant and Soil, v.245, n.2, p.223-232, 2002.

CHOI, W.J. et al. Irrigation and fertilization effects on foliar and soil carbon and nitrogen isotope ratios in a loblolly pine stand. Forest Ecology and Management, v.213, n.1-3, p.90-101, 2005.

COSTA, G.S.; GAMA-RODRIGUES, A.C.; CUNHA, C.M. Decomposição e liberação de nutrientes da serapilheira foliar em povoamentos de Eucalyptus grandis no Norte Fluminense. Revista Árvore, v.29, n.4, p.563-570, 2005.

DIJKSTRA, P. et al. 13C and 15N natural abundance of the soil microbial biomass. Soil Biology and Biochemistry, v.38, n.11, p.3257-3266, 2006.

DIJKSTRA, F.A. et al. Nitrogen deposition and plant species interact to influence soil carbon stabilization. Ecology Letters, v.7, n.12, p.1192-1198, 2004.

EMPRESA BRASILEIRA DE PESQUISA AGROPECUÁRIA - EMBRAPA, Centro Nacional de Pesquisa de Solos. Manual de métodos de analise de solo. 2. ed. Rio de Janeiro, 1997. 212 p.

ESHETU, Z.; HÖGBERG, P. Effects of land use on 15N natural abundance of soils in Ethiopian highlands. Plant and Soil, v.222, n.1-2, p.109-117, 2000.

FUNDAÇÃO ARTHUR BERNARDES - FUNARBE. SAEG - Sistema para análise estatística 5.0. Viçosa, MG, 1993.

GOLCHIN, A. et al. The effects of cultivation on the composition of organic matter and structural stability of soils. Australian Journal of Soil Research, v.33, n.6, p.975-993, 1995.

HAGEDORN, F.; SPINNLER, D.; SIEGWOLF, R. Increased N deposition retards mineralization of old soil organic matter. Soil Biology and Biochemistry, v.35, n.12, p.1683-1692, 2003.

KRAMER, M.G. et al. N isotope fractionation and measures of organic matter alteration during decomposition. Ecology, v.84, n.8, p.2021-2025, 2003.

LACLAU, J.P. et al. Nutrient cycling in a clonal stand of Eucalyptus and an adjacent savanna ecossistem in Congo. 1. Chemical composition of the rainfall, througfall and the stemflow solutions. Forest Ecology and Managnement, v.176, n.1/3, p.105-119, 2003.

LEMMA, B.; OLSSON, M. Soil δ15N and nutrients under exotic tree plantations in the southwestern Ethiopian highlands. Forest Ecology and Management, v.237, n.1-3, p.127-134, 2006.

LIAO, J.D.; BOUTTON, T.W.; JASTROW, J.D. Organic matter turnover in soil physical fractions following woody plant invasion of grassland: Evidence from natural 13C and 15N. Soil Biology and Biochemistry, v.38, n.11, p.3197-3210, 2006.

MATZNER, K.M.E. Nitrogen content of forest floor Oa layers affects carbon pathways and nitrogen mineralization. Soil Biology and Biochemistry, v.34, n.11, p.1807-1813, 2002.

MAY, B.M.; ATTIWILL, P.M. Nitrogen-fixation by Acacia dealbata and changes in soil properties 5 years after mechanical disturbance or slash-burning following timber harvest. Forest Ecology and Management, v.181, n.3, p.339-355, 2003.

MIKUTTA, R. et al. Mineralogical impact on organic nitrogen across a long-term soil chronosequence (0.3–4100 kyr). Geochimica Et Cosmochimica Acta, v.74, n.7, p.2142-2164, 2010.

NADELHOFFER, K.J.; FRY, B. Controls on natural nitrogen-15 and carbon-13 abundances in forest soil organic matter. Soil Science Society of America Journal, v.52, n.6, p.1633–1640, 1988.

NGUYEN, T.H.; SHINDO, H. Effects of different levels of compost application on amounts and distribution of organic nitrogen forms in soil particle size fractions subjected mainly to double cropping. Agricultural Sciences, v.2, n.3, p.213-219, 2011.

OMETTO, J.C. Bioclimatologia vegetal. São Paulo, Ceres, 1981. 425p.

PEGORARO, R.F. et al. Fenóis derivados da lignina, carboidratos e aminoaçúcares em serapilheira e solos cultivados com eucalipto e pastagem. Revista Árvore, v.35, n.2, p.359-370, 2011.

PICCOLO, M.C. et al. 15N natural abundance in forest and pasture soils of the Brazilian Amazon Basin, Plant and Soil, v.182 n.2, p.249-258, 1996.

PRIETO-FERNÁNDEZ, A.; CARBALLAS, T. Soil organic nitrogen composition in Pinus forest acid soils: variability and bioavailability. Biology and Fertility of Soils, v.32, n.3, p.177-185, 2000.

SAINJU, U.M., SINGH, B.P.; WHITEHEAD, W.F. Long-term effects of tillage, cover crops, and nitrogen fertilization on organic carbon and nitrogen concentrations in sandy loam soils in Georgia, USA. Soil & Tillage Research, v.63, n.3, p.167-179, 2002.

SCHULTEN, H.R.; SCHNITZER, M. The chemistry of soil organic nitrogen: a review. Biology and Fertility of Soils, v.26, n.1, p.1-15, 1998.

SHARPLEY, A.N.; SMITH, S.J. Nitrogen and phosphorus in soils receiving manure. Soil Science, v.159, n.4, p.253-258, 1995.

SIX, J. et al. Stabilization mechanisms of soil organic matter: implications for C-saturation of soils. Plant and Soil, v.241, n.2, p.155-176, 2002.

SJÖBERG, G. et al. Impact of long-term N fertilization on the structural composition of spruce litter and mor humus. Soil Biology and Biochemistry, v.36, n.4, p.609-618, 2004.

STEEL, R.G.D.; TORRIE, J.H.; DICKEY, D.A. Principles and procedures of statistics: a biometrical approach. New York : McGraw-Hill, 1997. 666p.

STEVENSON, F.J. Humus Chemistry: Genesis, Composition and Reactions. 2.ed. New York, Willey & Sons Inc., 1994. 496p.

TEMPLER, P.H. et al. Plant and soil natural abundance δ15N: indicators of relative rates of nitrogen cycling in temperate forest ecosystems. Oecologia, v.153, n.2, p.399-406, 2007.

XIAO-TANG, J. et al. Effect of long-term fertilization on organic nitrogen forms in a calcareous alluvial soil on the North China Plain. Pedosphere, v.16, n.2, p.224-229, 2006.

YEOMANS, J.C.; BREMNER, J.M. A rapid and precise method for routine determination of organic carbon in soil. Communications in Soil Science and Plant Analysis, v.13, n.13, p.1467-1476, 1988.

YONEBAYASHI, H.; HATTORI, T. Improvements in the method for fractional determination of soil organic nitrogen. Soil Science and Plant Nutrition, v.32, n.4, p.189-200, 1980.

Published

2016-03-31

How to Cite

Pegoraro, R. F., Silva, I. R. da, Novais, R. F. de, Barros, N. F. de, Cantarutti, R. B., & Fonseca, S. (2016). THE 15N NATURAL ABUNDANCE AND NITROGEN FORMS IN ULTISOL CULTIVATED WITH EUCALYPTUS AND ACACIA. Ciência Florestal, 26(1), 295–305. https://doi.org/10.5902/1980509821121

Issue

Section

Technical Note

Most read articles by the same author(s)

1 2 > >>