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施用粪肥的碱性土壤中的磷形态

Phosphorus speciation in manure-amended alkaline soils.

作者信息

Hansen Jeremy C, Cade-Menun Barbara J, Strawn Daniel G

机构信息

Department of Plant, Soil & Entomological Sciences, University of Idaho, Moscow, ID 83844-2339, USA.

出版信息

J Environ Qual. 2004 Jul-Aug;33(4):1521-7. doi: 10.2134/jeq2004.1521.

Abstract

Two common manure storage practices are stockpiles and lagoons. The manure from stockpiles is applied to soils in solid form, while lagoon manure is applied as a liquid. Soil amendment with manure in any form introduces a significant amount of phosphorus (P) that exists in both organic and inorganic forms. However, little is known about P speciation in manure stored under different conditions, or the subsequent forms when applied to soils. We used solution (31)P nuclear magnetic resonance (NMR) spectroscopy and conventional P fractionation and speciation methods to investigate P forms in dairy manure and liquid lagoon manure, and to study how long-term amendment with these manures influenced surface and subsurface soil P speciation. Our results show that the P forms in solid and lagoon manure are similar. About 30% of the total P was organic, mostly as orthophosphate monoesters. On a dry weight basis, total P was much higher in the solid manure. In the manure-amended soils the total P concentrations of the surface soils were similar, regardless of manure type. Total P in the subsurface soil was greater in the lagoon-manure-amended soil than the solid-manure-amended subsurface soil. However, the fraction of organic P was greater in the subsurface of the solid-manure-amended soil. The NMR results indicate that the majority of organic P in the soils is phytic acid, which is enriched in the surface soils compared with the subsurface soils. These results provide insight into P speciation and dynamics in manure-amended soils that will further increase our understanding on how best to manage manure disposal on soils.

摘要

两种常见的粪便储存方式是堆肥和泻湖储存。堆肥中的粪便以固体形式施用于土壤,而泻湖粪便则以液体形式施用。任何形式的粪便土壤改良都会引入大量以有机和无机形式存在的磷(P)。然而,对于在不同条件下储存的粪便中的磷形态,或者施用于土壤后的后续形态,我们了解得很少。我们使用溶液(31)P核磁共振(NMR)光谱以及传统的磷分级和形态分析方法,来研究奶牛粪便和泻湖液体粪便中的磷形态,并研究长期用这些粪便改良对表层和亚表层土壤磷形态的影响。我们的结果表明,固体粪便和泻湖粪便中的磷形态相似。总磷的约30%是有机磷,主要是正磷酸盐单酯。以干重计,固体粪便中的总磷含量要高得多。在施用粪便改良的土壤中,表层土壤的总磷浓度相似,与粪便类型无关。在亚表层土壤中,泻湖粪便改良土壤中的总磷含量高于固体粪便改良的亚表层土壤。然而,在固体粪便改良土壤的亚表层中,有机磷的比例更大。核磁共振结果表明,土壤中大部分有机磷是植酸,与亚表层土壤相比,表层土壤中植酸含量更高。这些结果为了解施用粪便改良土壤中的磷形态和动态提供了见解,这将进一步增进我们对如何最好地管理土壤粪便处置的理解。

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