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土壤和凋落物磷-31核磁共振光谱法:萃取剂、金属与磷弛豫时间

Soil and litter phosphorus-31 nuclear magnetic resonance spectroscopy: extractants, metals, and phosphorus relaxation times.

作者信息

Cade-Menun B J, Liu C W, Nunlist R, McColl J G

机构信息

Dep. of Environmental Sciences, Policy and Management, Univ. of California at Berkeley, USA.

出版信息

J Environ Qual. 2002 Mar-Apr;31(2):457-65.

Abstract

Phosphorus-31 nuclear magnetic resonance (NMR) spectroscopy is an excellent tool with which to study soil organic P, allowing quantitative, comparative analysis of P forms. However, for 31P NMR to be tative, all peaks must be completely visible, and in their correct relative proportions. There must be no line broadening, and adequate delay times must be used to avoid saturation of peaks. The objective of this study was to examine the effects of extractants on delay times and peak saturation. Two samples (a forest litter and a mineral soil sample) and three extractants (0.25 M NaOH, NaOH plus Chelex (Bio-Rad Laboratories, Hercules, CA), and NaOH plus EDTA) were used to determine the differences in the concentration of P and cations solubilized by each extractant, and to measure spin-lattice (T1) relaxation times of P peaks in each extract. For both soil and litter, NaOH-Chelex extracted the lowest concentrations of P. For the litter sample, T1 values were short for all extractants due to the high Fe concentration remaining after extraction. For the soil sample, there were noticeable differences among the extractants. The NaOH-Chelex sample had less Fe and Mn remaining in solution after extraction than the other extractants, and the longest delay times used in the study, 6.4 s, were not long enough for quantitative analysis. Delay times of 1.5 to 2 s for the NaOH and NaOH-EDTA were adequate. Line broadening was highest in the NaOH extracts, which had the highest concentration of Fe. On the basis of these results, recommendations for future analyses of soil and litter samples by solution 31P NMR spectroscopy include: careful selection of an extractant; measurement of paramagnetic ions extracted with P; use of appropriate delay times and the minimum number of scans; and measurement of T1 values whenever possible.

摘要

磷-31核磁共振(NMR)光谱是研究土壤有机磷的一种出色工具,可对磷形态进行定量、比较分析。然而,要使³¹P NMR具有定量性,所有峰必须完全可见,且相对比例正确。不能有线宽展宽,并且必须使用足够的延迟时间以避免峰饱和。本研究的目的是研究萃取剂对延迟时间和峰饱和的影响。使用两个样品(一个森林凋落物样品和一个矿质土壤样品)和三种萃取剂(0.25 M NaOH、NaOH加螯合树脂(Bio-Rad Laboratories,Hercules,加利福尼亚州)以及NaOH加EDTA)来确定每种萃取剂溶解的磷和阳离子浓度的差异,并测量每种萃取物中磷峰的自旋晶格(T1)弛豫时间。对于土壤和凋落物,NaOH-螯合树脂萃取的磷浓度最低。对于凋落物样品,由于萃取后残留的铁浓度较高,所有萃取剂的T1值都很短。对于土壤样品,萃取剂之间存在明显差异。萃取后,NaOH-螯合树脂样品溶液中残留的铁和锰比其他萃取剂少,并且该研究中使用的最长延迟时间6.4 s对于定量分析来说不够长。NaOH和NaOH-EDTA的延迟时间为1.5至2 s就足够了。NaOH萃取物中的线宽展宽最高,其铁浓度也最高。基于这些结果,对未来通过溶液³¹P NMR光谱分析土壤和凋落物样品的建议包括:仔细选择萃取剂;测量与磷一起萃取的顺磁性离子;使用适当的延迟时间和最少的扫描次数;以及尽可能测量T1值。

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