Adani Fabrizio, Genevini Pierluigi, Tambone Fulvia, Montoneri Enzo
Dipartimento di Produzione Vegetale, Università degli Studi di Milano, Via Celoria 2, Milano, Italy.
Chemosphere. 2006 Nov;65(8):1414-8. doi: 10.1016/j.chemosphere.2006.03.070. Epub 2006 May 15.
The humic acid (HA) fraction of a food and vegetable residues compost (CM) was taken as indicator to trace the fate of CM organic matter in four years CM amended soil. (1)H and (13)C NMR spectroscopy were used to investigate the nature of the HA isolates from CM, control soil (S(4)) and amended soil. The result indicated a significant structural difference between CM HA and S(4) HA, and supported the presence of both HA fractions in soil at the end of the amendment trials. However, the nature and content of CM HA in soil did not fully explain the increase of soil cation exchange capacity (CEC) after amendment. All CM humic fractions (i.e., fulvic acid, humic acid and humin) were found to contribute to the change of the soil organic matter composition. It is concluded that although CM HA is a suitable indicator of the survival of compost organic matter in soil during amendment, all three humic fractions should be monitored and analyzed to fully understand changes in the composition and properties of amended soil.
将一种食品和蔬菜残渣堆肥(CM)中的腐殖酸(HA)组分作为指标,以追踪在连续四年用CM改良的土壤中CM有机质的去向。采用(1)H和(13)C核磁共振光谱法研究从CM、对照土壤(S(4))和改良土壤中分离出的HA的性质。结果表明,CM HA和S(4) HA之间存在显著的结构差异,并支持在改良试验结束时土壤中存在这两种HA组分。然而,土壤中CM HA的性质和含量并不能完全解释改良后土壤阳离子交换容量(CEC)的增加。发现所有CM腐殖质组分(即富里酸、腐殖酸和胡敏素)都对土壤有机质组成的变化有贡献。得出的结论是,虽然CM HA是改良期间堆肥有机质在土壤中留存情况的合适指标,但为了全面了解改良土壤的组成和性质变化,应监测和分析所有三种腐殖质组分。