期刊文献+

Influence of bean rhizosphere on the biological properties and phosphorus fractionation in the calcareous soils amended with municipal sewage sludge 被引量:1

Influence of bean rhizosphere on the biological properties and phosphorus fractionation in the calcareous soils amended with municipal sewage sludge
下载PDF
导出
摘要 The biological and chemical conditions of the rhizosphere are known to considerably differ from those of the bulk soil, as a consequence of a range of processes that are induced either directly by the activity of plant roots or indirectly by the stimulation of microbial population and activity in the rhizosphere. Information about phosphorus (P) fractionation in the rhizosphere soils amended with municipal sewage sludge (MSS) is limited, were We carried out greenhouse experiments using a rhizobox in order to evaluate the effects of bean rhizosphere on the various inorganic P (Pi) fractions, organic P (Po), P in particulate fraction (PF-P), Olsen-P, dissolved organic C (DOC), microbial biomass P (MBP) and alkaline phosphatase (ALP) enzyme in 10 calcareous soils amended with MSS (10 g MSS was added to 1 kg soil). Non-occluded P, occluded P, calcium phosphate and residual P were also quantitated. The results showed that DOC, MBP and ALP activity strongly increased and PF-P and Olsen-P de- creased in the rhizosphere soils compared with in the bulk soils (P〈0.05). The contents of non-occluded P, oc- cluded P and residuaI-P fractions in the rhizosphere soils were lower than in the bulk soils, while the contents of calcium phosphate and organic P in the rhizosphere soils were higher than in the bulk soils. Simple correlation coefficients showed that P uptake had positive relationship with non-occluded P, occluded P, calcium phosphate fractions and PF-P in the rhizosphere soils. The results suggest that the short-term application of MSS to the cal- careous soils may increase Po and calcium phosphate fractions in the rhizosphere soils, and calcium phosphate fraction is potentially available to crops. The biological and chemical conditions of the rhizosphere are known to considerably differ from those of the bulk soil, as a consequence of a range of processes that are induced either directly by the activity of plant roots or indirectly by the stimulation of microbial population and activity in the rhizosphere. Information about phosphorus (P) fractionation in the rhizosphere soils amended with municipal sewage sludge (MSS) is limited, were We carried out greenhouse experiments using a rhizobox in order to evaluate the effects of bean rhizosphere on the various inorganic P (Pi) fractions, organic P (Po), P in particulate fraction (PF-P), Olsen-P, dissolved organic C (DOC), microbial biomass P (MBP) and alkaline phosphatase (ALP) enzyme in 10 calcareous soils amended with MSS (10 g MSS was added to 1 kg soil). Non-occluded P, occluded P, calcium phosphate and residual P were also quantitated. The results showed that DOC, MBP and ALP activity strongly increased and PF-P and Olsen-P de- creased in the rhizosphere soils compared with in the bulk soils (P〈0.05). The contents of non-occluded P, oc- cluded P and residuaI-P fractions in the rhizosphere soils were lower than in the bulk soils, while the contents of calcium phosphate and organic P in the rhizosphere soils were higher than in the bulk soils. Simple correlation coefficients showed that P uptake had positive relationship with non-occluded P, occluded P, calcium phosphate fractions and PF-P in the rhizosphere soils. The results suggest that the short-term application of MSS to the cal- careous soils may increase Po and calcium phosphate fractions in the rhizosphere soils, and calcium phosphate fraction is potentially available to crops.
出处 《Journal of Arid Land》 SCIE CSCD 2015年第5期644-652,共9页 干旱区科学(英文版)
基金 supported by the Shahrekord University
关键词 biological properties mineral phosphorus organic phosphorus semi-arid land biological properties mineral phosphorus organic phosphorus semi-arid land
  • 相关文献

参考文献40

  • 1Ahmad W, Rahmatullah, Gill M A, et al. 2006. Bioavailability of inor- ganic phosphorus fractions in calcareous soils estimated by neubauer technique, iron impregnated filter paper, and chemical tests. Com- munications in Soil Science and Plant Analysis, 37:1185-1193.
  • 2Anderson G. 1980. Assessing organic phosphorus in soils. In: Khasawneh F E, Sample E C, Kamprath E J. The Role of Phos- phatase in Agriculture. Madison: American Society Agronomy, 411--432.
  • 3Balik J, Pavlikov~t D, Van~k V, et al. 2007. The influence of long-term sewage sludge application on the activity of phosphatases in the rhizosphere of plants. Plant and Soil Environmental, 53: 375-381.
  • 4Brerrmer J M. 1996. Nitrogen-total. In: Sparks D L, Page A L, Helmke P A, et al. Methods of Soil Analysis: Part 3, Chemical Methods. Madison: Soil Science Society of America, 1085-1121.
  • 5Carnbardella C A, Elliott E T. 1992. Particulate organic-matter changes across a grassland cultivation sequence. Soil Science Society of America Journal, 56: 777-783.
  • 6Chang S C, Jackson M L. 1957. Fractionation of soil phosphorus. Soil Science, 84: 133-144.
  • 7Chen C R, Condron L M, Davis M R, et al. 2002. Phosphorus dynamics in the rhizosphere of perennial ryegrass (Loliumperenne L.) and ra- diata pine (Pinus radiata D. Don.). Soil Biology and Biochemistry, 34: 487-499.
  • 8Chen H. 2003. Phosphatase activity and P fractions in soils of an 18-year-old Chinese fir (Cunninghamia lanceolata) plantation. Forest Ecology and Management, 178:301-310.
  • 9Ciampitti I A, Garcia F O, Picone L I, et al. 2011. Soil carbon and phosphorus pools in field crop rotations in Pampean soil of Argentina. Soil Biology and Biochemistry, 75:616-625.
  • 10Delgado A, Ruiz J R, Del Campillo M D, et al. 2000. Calcium- and iron-related phosphorus in calcareous and calcareous marsh soils: Sequential chemical fractionation and P-31 nuclear magnetic reso- nance study. Communications in Soil Science and Plant Analysis, 31: 2483 2499.

同被引文献6

二级引证文献1

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部