Seasonal dynamics in the concentrations of macronutrients and organic constituents in green and senesced leaves of three agroforestry species in southern Ethiopia

被引:5
作者
Tesfay Teklay
机构
[1] Debub University,Wondo Genet College of Forestry
[2] Swedish University of Agricultural Sciences,Department of Forest Ecology
来源
Plant and Soil | 2004年 / 267卷
关键词
shade trees; senescence; sub-humid tropical;
D O I
暂无
中图分类号
学科分类号
摘要
Foliar inputs from indigenous agroforestry trees and shrubs could provide sufficient nutrients and organic matter to sustain crop growth. However, concentrations of foliar nutrients and organic constituents show considerable seasonal, inter- and/or intra-species variations. To determine this variability, green and senesced leaves were sampled during dry and wet seasons from Cordia africana, Albizia gummifera and Milletia ferruginea trees at Wondo Genet, southern Ethiopia. Cordia is a deciduous, non-leguminous tree, while Albizia and Milletia are semi-deciduous and leguminous trees. Leaves were analyzed for concentrations of ash, N, P, K, cellulose, lignin, soluble polyphenols, and condensed tannins. Results from statistical analyses showed significant seasonal variations (P < 0.001) in concentrations of all leaf constituents, except for P and cellulose. Foliar concentrations of ash, N, soluble polyphenols, and condensed tannins were higher during the wet season while those of K and lignin were higher during the dry season. Green leaves had significantly higher (p < 0.001) N and P concentrations than senesced leaves, while senesced leaves had higher concentrations of K, cellulose, soluble polyphenols, and condensed tannins. The ‘ Relative Percentage Changes’ in concentration of N and P in senesced leaves, i.e., their enrichment or depletion with such nutrients relative to those in green leaves, were significantly higher (P < 0.001) for Cordia than Albizia and Milletia. On the other hand, there was no consistent pattern in the enrichment or depletion of senesced leaves with organic constituents, but these leaves were in most cases more enriched with organic constituents than green leaves. Over all, the percentage depletion or enrichment ranged from about 8% to 38% for N; 24% to 63% for P; −141% to 48% for K; −44% to 15% for cellulose; −44% to 51% for lignin; −203% to −61% for soluble polyphenols; and −290% to 11% for condensed tannins. It was concluded that variations in species and life-form (legume versus non-legume), season, and developmental stage of leaves could affect the quality of organic material from agroforestry species, which has important implications for management of organic residues in tropical agricultural systems.
引用
收藏
页码:297 / 307
页数:10
相关论文
共 69 条
  • [1] Aerts R(1996)Nutrient resorption from senescing leaves of perennials: are there general patterns? J. Ecol. 84 597-608
  • [2] Bell D. T.(1984)Seasonal changes in foliar macronutrients (N, P, K, Ca and Mg) in Plant Soil 81 377-388
  • [3] Ward S. C.(2000) Sm., and Plant Soil 224 185-193
  • [4] Carrera A. L.(1980) Blakely growing in rehabilitated bauxite mine soils of the Darling Range, Western Australia Annu. Rev. Ecol. Syst. 11 233-260
  • [5] Sain C. L.(1991)Patterns of nitrogen conservation in shrubs and grasses in the Patagonian Monte, Argentina Ecology 72 709-715
  • [6] Bertiller M. B.(1994)The mineral nutrition of wild plants Soil Biol. Biochem. 26 49-55
  • [7] Chapin F. S.(2001)Nutritional controls over nitrogen and phosphorus resorption from Alaskan birch leaves Can. J. For. Res. 31 333-344
  • [8] Chapin F. S.(1999)Nitrogen mineralization from leaves and litter of tropical plants: Relationship to nitrogen, lignin and soluble polyphenol concentrations New Phytol. 143 177-189
  • [9] Moilanen L(1991)Seasonal nutrient transfers by foliar resorption, leaching, and litter fall in a northern hardwood forest at Lake Clair Watershed, Quebec, Canada Oecologia 90 80-87
  • [10] Constantinides M(2001)Leaf life span and nutrient resorption as determinants of plant nutrient conservation in temperate-arctic regions Biomass & Bioenergy 21 321-334