Suppr超能文献

长期耕种下稀树草原土壤中某些微量元素的状况与动态

The status and dynamics of some trace elements in a savanna soil under long-term cultivation.

作者信息

Agbenin J O, Felix-Henningsen P

机构信息

Department of Soil Science, Ahmadu Bello University, Zaria, Nigeria.

出版信息

Sci Total Environ. 2001 Sep 28;277(1-3):57-68. doi: 10.1016/s0048-9697(00)00859-7.

Abstract

A recent study in the savanna suggested that the surface soils might be contaminated with Ti, V, U and Th because of increasing phosphate fertilizer applications. In this study, we determined the dynamics of Ga, V, U, Nb, Y, La, Ce and Nd in a savanna soil that has received NPK fertilizers, farmyard manure (FYM) and FYM + NPK for 50 years using an adjacent uncultivated or native site as a reference. The concentrations of the elements in the soils were determined by X-ray fluorescence. Mass balance calculations indicated that Nb, U, Y, La, Ce and Nd increased by between 8 and 61% in the cultivated soil compared with the uncultivated natural site. Long-term application of FYM increased the masses of Nb (16%), Th (40%), La (26%), Ce (44%) and Nd (54%). There were no discernible changes in the masses of the trace elements that could be unambiguously associated with phosphate fertilizer applications. It was, thus, concluded that physical accumulation as leaching losses and crop removal depleted soluble ions, stabilization by organo-mineral complexes and aeolian deposition are the probable soil enrichment mechanisms of these trace elements during cultivation.

摘要

最近在热带稀树草原进行的一项研究表明,由于磷肥施用量的增加,表层土壤可能受到钛、钒、铀和钍的污染。在本研究中,我们以相邻的未开垦或原生地块为参照,测定了一块连续50年施用氮磷钾化肥、农家肥以及农家肥与氮磷钾化肥混合肥料的热带稀树草原土壤中镓、钒、铀、铌、钇、镧、铈和钕的动态变化。土壤中这些元素的浓度通过X射线荧光法测定。质量平衡计算表明,与未开垦的天然地块相比,耕种土壤中的铌、铀、钇、镧、铈和钕增加了8%至61%。长期施用农家肥使铌(16%)、钍(40%)、镧(26%)、铈(44%)和钕(54%)的质量增加。与磷肥施用明确相关的微量元素质量没有明显变化。因此,得出的结论是,淋溶损失和作物吸收导致可溶离子耗尽后的物理积累、有机-矿物复合体的稳定作用以及风沙沉积是这些微量元素在耕种过程中可能的土壤富集机制。

文献AI研究员

20分钟写一篇综述,助力文献阅读效率提升50倍。

立即体验

用中文搜PubMed

大模型驱动的PubMed中文搜索引擎

马上搜索

文档翻译

学术文献翻译模型,支持多种主流文档格式。

立即体验