CN110749614B - Method for rapidly and quantitatively detecting organic phosphorus in soil - Google Patents

Method for rapidly and quantitatively detecting organic phosphorus in soil Download PDF

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CN110749614B
CN110749614B CN201911095589.7A CN201911095589A CN110749614B CN 110749614 B CN110749614 B CN 110749614B CN 201911095589 A CN201911095589 A CN 201911095589A CN 110749614 B CN110749614 B CN 110749614B
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李伟
姜允斌
张奉民
任超
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Nanjing University
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Abstract

The invention relates to a method for rapidly and quantitatively detecting organic phosphorus in soil, which is characterized in that a soil sample is added into 0.25M NaOH and 0.05M Na 2 Extracting with EDTA under shaking in dark, centrifuging, collecting supernatant, filtering, collecting supernatant, and coolingFreezing to obtain freeze-dried powder; dissolving 50mg of freeze-dried powder in 2mL of paramagnetic ion solution, swirling, and standing to obtain liquid 31 P NMR samples, detected using a Bruker 600MHz liquid NMR spectrometer, were passed through the spectrometer 31 The chemical shift value of the P signal can determine the organic phosphorus form corresponding to the signal, and the relative abundance of the corresponding organic phosphorus or the organic phosphorus can be determined according to the relative proportion of the signal peak intensity, so that the content of the organic phosphorus can be calculated. With the usual liquids 31 Compared with the P NMR method, the invention shortens the detection time of the NMR experiment and improves the efficiency of the quantitative analysis of the organic phosphorus in the soil.

Description

一种快速定量检测土壤中有机磷的方法A Rapid Quantitative Method for Detecting Organic Phosphorus in Soil

技术领域technical field

本发明涉及一种快速定量检测土壤中有机磷的方法,属于化学检测技术领域。The invention relates to a method for rapidly and quantitatively detecting organic phosphorus in soil, belonging to the technical field of chemical detection.

背景技术Background technique

土壤中含有无机磷和有机磷,其中有机磷占土壤总磷的35-65%,了解土壤有机磷的变化动态对深入理解土壤磷的生物地球化学循环过程,以及建立高效的可持续农业管理措施具有重要意义。Soil contains inorganic phosphorus and organic phosphorus, of which organic phosphorus accounts for 35-65% of the total soil phosphorus. Understanding the dynamics of soil organic phosphorus is essential for in-depth understanding of the biogeochemical cycle of soil phosphorus and the establishment of efficient sustainable agricultural management measures is of great significance.

土壤中的无机磷主要以正磷酸盐为主,其含量可以通过分光光度法和ICP-OES法进行测定,土壤中有机磷的含量可通过酸提取的无机磷与消解后提取的总磷含量进行差减估算,同时,也可针对特定土壤有机磷形态进行提取,采用色谱法进行分析,例如使用氯仿、甲醇和水或二氯甲烷和甲醇提磷脂,随后进行色谱分离和含量测定,但是,这种方法不能确定有机磷形态,只能确定某种特定形态有机磷的含量。土壤中有机磷分子形态种类繁多,在分子水平上分析土壤有机磷的形态及其组成,需要建立先进的分析方法。The inorganic phosphorus in the soil is mainly orthophosphate, and its content can be determined by spectrophotometry and ICP-OES. The content of organic phosphorus in the soil can be determined by acid extraction of inorganic phosphorus and total phosphorus extracted after digestion. At the same time, specific soil organic phosphorus forms can also be extracted and analyzed by chromatography, such as using chloroform, methanol and water or dichloromethane and methanol to extract phospholipids, followed by chromatographic separation and content determination, but this This method cannot determine the form of organic phosphorus, but can only determine the content of a specific form of organic phosphorus. There are various molecular forms of organic phosphorus in soil, and it is necessary to establish advanced analytical methods to analyze the form and composition of organic phosphorus in soil at the molecular level.

液体31P核磁共振(NMR)光谱法是定量检测土壤有机磷形态的首选方法。Liquid 31 P nuclear magnetic resonance (NMR) spectroscopy is the preferred method for the quantitative detection of soil organic phosphorus species.

由于液体NMR谱图中31P的各向同性核磁信号具有很好的分辨度,并且能够反映特定有机磷化合物的结构信息,因此土壤中有机磷通常经过溶液提取后采用一维液体31P NMR进行分析,鉴定有机磷的种类并对其进行定量比较。尽管31P NMR在土壤科学方面取得了巨大的成功,但某些因素阻碍了其在该领域更广泛的应用。由于土壤中磷含量相对较低,31PNMR测试通常需要较长的扫描时间(一个样品约16~20h),针对土壤有机磷提取液的液体31PNMR定量分析通常需要数千次脉冲扫描(即重复的31P激发-驰豫循环),来获得足够的信号以产生高质量的图谱,这使得测定土壤有机磷的31P NMR实验机时紧张,并且费用过高。Since the isotropic NMR signal of 31 P in the liquid NMR spectrum has good resolution and can reflect the structural information of specific organophosphorus compounds, organic phosphorus in soil is usually extracted by solution and then analyzed by one-dimensional liquid 31 P NMR. Analyze, identify and compare quantitatively the species of organophosphorus. Despite the great success of 31 P NMR in soil science, certain factors have hindered its wider application in this field. Due to the relatively low phosphorus content in the soil, 31 PNMR tests usually require a long scan time (about 16-20 h for a sample), and liquid 31 PNMR quantitative analysis of soil organic phosphorus extracts usually requires thousands of pulse scans (that is, repeated 31 P excitation-relaxation cycle) to obtain enough signal to produce high-quality spectra, which makes the 31 P NMR laboratory equipment for the determination of soil organic phosphorus strained and expensive.

发明内容Contents of the invention

本发明的目的在于解决上述现有技术的不足,提供一种快速定量检测土壤中有机磷的方法,该方法能有效缩短检测时间,提高了土壤中有机磷定量分析的效率。The object of the present invention is to solve the deficiencies of the above prior art, and provide a method for rapid quantitative detection of organic phosphorus in soil, which can effectively shorten the detection time and improve the efficiency of quantitative analysis of organic phosphorus in soil.

技术方案Technical solutions

针对土壤有机磷提取液的液体31P NMR定量分析通常需要数千次脉冲扫描,来获得足够的信号以产生高质量的图谱,并且脉冲循环间的间隔时间需要设置得足够长使得所有的31P核从激发状态完全恢复到平衡状态,否则核磁共振信号强度将不能定量地反映所有有机磷形态的信息。因此脉冲间隔时间从很大程度上也决定了液体31P NMR测量的实验时长。溶液中被激发的31P核恢复至平衡状态的过程主要受其自旋晶格弛豫(T1)的控制,不同种类磷化合物的T1时间也存在着显著差异。因此本发明人通过缩短脉冲间隔,来缩短检测时间,进而提高土壤有机磷定量分析的效率。具体方案如下:Liquid 31 P NMR quantitative analysis of soil organic phosphorus extracts usually requires thousands of pulse scans to obtain enough signal to generate high-quality spectra, and the interval between pulse cycles needs to be set long enough to allow all 31 P The nuclei are fully restored from the excited state to the equilibrium state, otherwise the NMR signal intensity will not be able to quantitatively reflect the information of all organophosphorus species. Therefore, the pulse interval also determines the experimental duration of the liquid 31 P NMR measurement to a large extent. The recovery process of excited 31 P nuclei in solution is mainly controlled by their spin-lattice relaxation (T 1 ), and there are significant differences in the T 1 time of different phosphorus compounds. Therefore, the inventor shortens the detection time by shortening the pulse interval, thereby improving the efficiency of quantitative analysis of soil organic phosphorus. The specific plan is as follows:

一种快速定量检测土壤中有机磷的方法,包括如下步骤:A method for rapid quantitative detection of organic phosphorus in soil, comprising the steps of:

(1)称取4g(干土重)土壤样品,加入60mL NaOH和Na2EDTA的混合溶液,混合溶液中,NaOH浓度为0.25M,Na2EDTA浓度为0.05M;避光振荡提取16h后,离心,收集上清液通过0.45μm滤膜过滤,收集过滤后的上清液,冷冻后得到冻干粉;(1) Weigh 4g (dry soil weight) soil sample, add 60mL NaOH and Na 2 EDTA mixed solution, in the mixed solution, the concentration of NaOH is 0.25M, and the concentration of Na 2 EDTA is 0.05M; Centrifuge, collect the supernatant and filter it through a 0.45 μm filter membrane, collect the filtered supernatant, and freeze to obtain a lyophilized powder;

(2)取50mg冻干粉,溶于2mL顺磁离子溶液中,涡旋30s静置2min,得到液体31P NMR样品;(2) Take 50 mg of freeze-dried powder, dissolve in 2 mL of paramagnetic ion solution, vortex for 30 s and let stand for 2 min to obtain a liquid 31 P NMR sample;

所述顺磁离子溶液配方:20-100mg/L Fe3+、0.25M NaOH、0.05M Na2EDTA、10%(v/v)D2O;The paramagnetic ion solution formula: 20-100mg/L Fe 3+ , 0.25M NaOH, 0.05M Na 2 EDTA, 10% (v/v) D 2 O;

(3)将液体31P NMR样品加入5mm NMR样品管中,使用Bruker 600MHz液体核磁共振波谱仪进行检测,得到图谱,通过图谱中31P信号的化学位移值,可确定该信号对应的有机磷形态,根据信号峰强度(面积)的相对比例,可确定对应某种或某类有机磷的相对丰度,从而计算其含量。(3) Add the liquid 31 P NMR sample into a 5mm NMR sample tube, use a Bruker 600MHz liquid nuclear magnetic resonance spectrometer to detect, and obtain a spectrum. The chemical shift value of the 31 P signal in the spectrum can determine the form of organophosphorus corresponding to the signal , according to the relative proportion of the signal peak intensity (area), the relative abundance corresponding to a certain or a certain type of organic phosphorus can be determined, thereby calculating its content.

进一步,步骤(1)中,离心的转速为10000rpm,时间为10min。Further, in step (1), the centrifugation speed is 10000rpm, and the time is 10min.

进一步,步骤(2)中,所述顺磁离子溶液配方:50mg/L Fe3+、0.25M NaOH、0.05MNa2EDTA、10%(v/v)D2O。Further, in step (2), the formula of the paramagnetic ion solution: 50mg/L Fe 3+ , 0.25M NaOH, 0.05M Na 2 EDTA, 10% (v/v) D 2 O.

进一步,步骤(3)中,Bruker 600MHz液体核磁共振波谱仪的设置参数为:31P的检测频率为242.98MHz,检测温度为25℃,脉冲程序为90°脉冲,信号采集时间为0.845s,脉冲间隔时间为0.1s。Further, in step (3), the setting parameters of the Bruker 600MHz liquid nuclear magnetic resonance spectrometer are: the detection frequency of 31 P is 242.98MHz, the detection temperature is 25°C, the pulse program is 90° pulse, the signal acquisition time is 0.845s, and the pulse The interval time is 0.1s.

本发明的有益效果:本发明提供了一种快速定量检测土壤中有机磷的方法,该方法在液体31P NMR定量分析的基础上,通过在31P NMR样品中添加顺磁离子缩短脉冲间隔,进而缩短NMR实验检测时间。与常用液体31P NMR方法相比,可大幅度提高土壤有机磷定量分析的效率。Beneficial effect of the present invention: the present invention provides a kind of method for rapid quantitative detection of organic phosphorus in soil, this method shortens pulse interval by adding paramagnetic ion in 31 P NMR sample on the basis of liquid 31 P NMR quantitative analysis, This shortens the detection time of NMR experiments. Compared with the commonly used liquid 31 P NMR method, the efficiency of quantitative analysis of soil organic phosphorus can be greatly improved.

附图说明Description of drawings

图1为采用实施例1方法测得的土壤样品的31P NMR图谱;Fig. 1 is the 31 P NMR spectrum of the soil sample that adopts embodiment 1 method to measure;

图2为采用对比例1方法测得的土壤样品的31P NMR图谱。FIG. 2 is the 31 P NMR spectrum of the soil sample measured by the method of Comparative Example 1.

具体实施方式detailed description

下面结合附图和具体实施方式对本发明作进一步说明。The present invention will be further described below in conjunction with the accompanying drawings and specific embodiments.

实施例1Example 1

取不同的Fe3浓度,制备三种顺磁离子溶液:(20、50、100)mg/L Fe3+、0.25M NaOH、0.05M Na2EDTA、10%(v/v)D2O。然后将磷酸钠、焦磷酸钠、植酸(25mM P)和DNA(1mg/mL)分别溶于顺磁离子溶液,加入5mm NMR样品管使用Bruker 600MHz液体NMR(242.98MHz,25℃)以反转恢复法(脉冲程序t1irpg)对磷化合物的T1时间进行测定(设置10个脉冲间隔时间,各间隔时间脉冲循环均为32,信号采集时间为0.845s,驰豫间隔时间为50s),测试结果见表1:Three paramagnetic ion solutions were prepared with different Fe 3 concentrations: (20, 50, 100) mg/L Fe 3+ , 0.25M NaOH, 0.05M Na 2 EDTA, 10% (v/v) D 2 O. Then sodium phosphate, sodium pyrophosphate, phytic acid (25mM P) and DNA (1mg/mL) were dissolved in the paramagnetic ion solution, respectively, and added to a 5mm NMR sample tube using a Bruker 600MHz liquid NMR (242.98MHz, 25°C) to invert The recovery method (pulse program t1irpg) measures the T1 time of phosphorus compounds (set 10 pulse intervals, each interval pulse cycle is 32, the signal acquisition time is 0.845s, and the relaxation interval is 50s), the test results See Table 1:

表1不同顺磁离子浓度下磷化合物的自旋晶格驰豫(T1)时间Table 1 Spin-lattice relaxation (T 1 ) times of phosphorus compounds at different concentrations of paramagnetic ions

Figure BDA0002268248150000031
Figure BDA0002268248150000031

由表1可以看出,综合考虑,顺磁离子Fe3浓度为50mg/L时,磷化合物的自旋晶格驰豫(T1)时间更短。因此选用50mg/L的顺磁离子Fe3浓度进行实验。It can be seen from Table 1 that when the concentration of paramagnetic ions Fe 3 is 50 mg/L, the spin-lattice relaxation (T 1 ) time of phosphorus compounds is shorter. Therefore, a paramagnetic ion Fe3 concentration of 50mg/L was selected for the experiment.

供试土样为黑龙江省双鸭山市(N46°48′20.3″,E134°01′13.9″)一农田黑粘土,种植作物为大豆。基本理化性质:pH 6.90、C 56g kg–1、N 13g kg–1、P 1.8g kg–1The soil sample for testing is a farmland black clay in Shuangyashan City, Heilongjiang Province (N46°48′20.3″, E134°01′13.9″), and the crop is soybean. Basic physical and chemical properties: pH 6.90, C 56g kg –1 , N 13g kg –1 , P 1.8g kg –1 .

一种快速定量检测土壤中有机磷的方法,包括如下步骤:A method for rapid quantitative detection of organic phosphorus in soil, comprising the steps of:

(1)称取4g(干土重)土壤样品,加入60mL NaOH和Na2EDTA的混合溶液中,NaOH浓度为0.25M,Na2EDTA浓度为0.05M;避光振荡提取16h后,离心(转速为10000rpm,时间为10min),收集上清液通过0.45μm滤膜过滤,收集过滤后的上清液,冷冻后得到冻干粉;(1) Weigh 4g (dry soil weight) soil sample, add 60mL NaOH and Na 2 EDTA mixed solution, the concentration of NaOH is 0.25M, the concentration of Na 2 EDTA is 0.05M; after shaking and extracting in the dark for 16h, centrifuge (speed is 10000rpm, and the time is 10min), the collected supernatant is filtered through a 0.45 μm filter membrane, the filtered supernatant is collected, and freeze-dried powder is obtained after freezing;

(2)取50mg冻干粉,溶于2mL顺磁离子溶液中,涡旋30s静置2min,得到液体31P NMR样;(2) Take 50 mg of lyophilized powder, dissolve in 2 mL of paramagnetic ion solution, vortex for 30 s and let stand for 2 min to obtain a liquid 31 P NMR sample;

所述顺磁离子溶液配方:50mg/L Fe3+、0.25M NaOH、0.05M Na2EDTA、10%(v/v)D2O;The paramagnetic ion solution formula: 50mg/L Fe 3+ , 0.25M NaOH, 0.05M Na 2 EDTA, 10% (v/v) D 2 O;

(3)将液体31P NMR样品加入5mm NMR样品管中,使用Bruker 600MHz液体核磁共振波谱仪(31P的检测频率为242.98MHz,检测温度为25℃,脉冲程序为90°脉冲,信号采集时间为0.845s,脉冲循环数为128,脉冲间隔时间为50-0.1s)进行检测,得到图谱(图1),通过31P信号的化学位移对其形态进行鉴别,5.2ppm信号对应正磷酸盐(orthophosphate)、-4.1ppm信号对应焦磷酸盐(pyrophosphate)、5-4ppm间信号来自植酸(phytic acid)。通过BrukerTopsin软件对信号区域进行积分,计算获得这三种形态的相对丰度,结果显示:通过添加50mg/L Fe3+,将脉冲间隔时间缩短至0.1s后分析获得的三种磷形态相对丰度为50.24%、24.90%和24.87%,与使用50s的测试结果(51.52%、23.96%、24.52%)的相对偏差仍在5%范围内。脉冲间隔缩短至0.1s后,该样品液体31P NMR的测试时长为121s,与目前常用的2s脉冲间隔(时长为364s)相比,耗时约为其三分之一。(3) Add the liquid 31 P NMR sample into a 5mm NMR sample tube, use a Bruker 600MHz liquid nuclear magnetic resonance spectrometer (the detection frequency of 31 P is 242.98 MHz, the detection temperature is 25 °C, the pulse program is 90° pulse, the signal acquisition time 0.845s, the number of pulse cycles is 128, and the pulse interval time is 50-0.1s) to detect, obtain the spectrum (Fig. 1), and identify its form by the chemical shift of the 31 P signal, and the 5.2ppm signal corresponds to orthophosphate ( orthophosphate), -4.1ppm signal corresponds to pyrophosphate (pyrophosphate), and the signal between 5-4ppm comes from phytic acid (phytic acid). The signal area was integrated by BrukerTopsin software, and the relative abundance of the three forms was calculated. The results showed that the relative abundance of the three forms of phosphorus was analyzed after shortening the pulse interval time to 0.1s by adding 50 mg/L Fe 3+ . The relative deviations from the test results (51.52%, 23.96%, 24.52%) using 50s are still within 5%. After the pulse interval is shortened to 0.1s, the test time of the sample liquid 31 P NMR is 121s, which is about one-third of the time compared with the currently commonly used 2s pulse interval (364s).

对比例1Comparative example 1

土样与实施例1相同,Soil sample is identical with embodiment 1,

一种检测土壤中有机磷的方法:A method for detecting organic phosphorus in soil:

(1)将土壤样品加入含有0.25M NaOH和0.05M Na2EDTA的提取剂中(固液比1:10),避光160rpm振荡提取16h;(1) Add the soil sample to the extractant containing 0.25M NaOH and 0.05M Na 2 EDTA (solid-to-liquid ratio 1:10), and shake and extract at 160rpm in the dark for 16h;

(2)提取完成后10000rpm离心10min,收集上清液经0.45μm滤膜过滤后备用;(2) Centrifuge at 10,000 rpm for 10 min after the extraction is completed, collect the supernatant and filter it through a 0.45 μm filter membrane for later use;

(3)采用冷冻干燥对样品进行富集;(3) Enrich the sample by freeze-drying;

(4)使用含10%以上D2O的NaOH溶液完全溶解量富集样品,完成制作液体31P NMR样品;(4) Enrich the sample with the complete dissolution of NaOH solution containing more than 10% D 2 O, and complete the production of liquid 31 P NMR samples;

(5)将液体31P NMR样品加入5mm NMR样品管中,使用Bruker 600MHz液体核磁共振波谱仪(脉冲循环数为25600,脉冲间隔时间为2和0.1s,其他参数及测试温度与实施例1相同),得到图谱(图2)。通过31P信号的化学位移对其形态进行鉴别,5.2ppm信号对应正磷酸盐(orthophosphate)、-4.1ppm信号对应焦磷酸盐(pyrophosphate)、5-2ppm信号对应磷酸单酯(monoesters)、19ppm信号对应膦酸酯(phosphonates)。通过Bruker Topsin软件对信号区域进行积分,计算获得这三种形态的相对丰度,结果显示:缩短脉冲间隔时间至0.1s与目前常用的2s获得的谱图存在显著差异,对于磷形态鉴别,使用0.1s的谱图没有明显膦酸酯信号。对于磷形态定量分析,使用0.1s和2s谱图间各个形态的相对丰度偏差均达到了10%以上。(5) The liquid 31 P NMR sample is added in the 5mm NMR sample tube, using Bruker 600MHz liquid nuclear magnetic resonance spectrometer (the number of pulse cycles is 25600, the pulse interval time is 2 and 0.1s, other parameters and test temperature are the same as in Example 1 ) to obtain the spectrum (Fig. 2). The morphology is identified by the chemical shift of the 31 P signal. The signal of 5.2ppm corresponds to orthophosphate, the signal of -4.1ppm corresponds to pyrophosphate, the signal of 5-2ppm corresponds to monoesters, and the signal of 19ppm Corresponds to phosphonates. The signal area is integrated by Bruker Topsin software, and the relative abundance of these three forms is calculated. The results show that there is a significant difference between the spectrum obtained by shortening the pulse interval time to 0.1s and the currently commonly used 2s. For the identification of phosphorus forms, use There is no obvious phosphonate signal in the spectrum at 0.1s. For the quantitative analysis of phosphorus species, the relative abundance deviation of each species between the 0.1s and 2s spectra has reached more than 10%.

Claims (2)

1. A method for rapidly and quantitatively detecting organic phosphorus in soil is characterized by comprising the following steps:
(1) A soil sample weighing 4g of dry soil was weighed, and 60mL of 0.25M NaOH and 0.05M Na were added 2 Performing vibration extraction on the EDTA solution for 16h in a dark place, centrifuging, collecting supernatant, filtering the supernatant through a 0.45-micron filter membrane, collecting the filtered supernatant, and freezing to obtain freeze-dried powder;
(2) Dissolving 50mg of lyophilized powder in 2mL of paramagnetic ion solution, swirling for 30s, and standing for 2min to obtain liquid 31 A P NMR sample;
the formula of the paramagnetic ion solution comprises the following components: 50mg/L Fe 3+ 、0.25 M NaOH、0.05 M Na 2 EDTA、10% (v/v) D 2 O;
(3) Mixing liquid 31 Adding a P NMR sample into a 5mm NMR sample tube, detecting by using a Bruker 600MHz liquid nuclear magnetic resonance spectrometer to obtain a spectrum, and obtaining a standard spectrum through the spectrum 31 The chemical shift value of the P signal can determine the organic phosphorus form corresponding to the signal, and the relative abundance of the corresponding organic phosphorus or the organic phosphorus can be determined according to the relative proportion of the peak intensity or the area of the signal, so that the content of the organic phosphorus can be calculated;
in the step (3), the setting parameters of the Bruker 600MHz liquid nuclear magnetic resonance spectrometer are as follows: 31 the detection frequency of P is 242.98MHz, the detection temperature is 25 ℃, the pulse program is 90-degree pulse, the signal acquisition time is 0.845s, and the pulse interval time is 0.1s.
2. The method for rapidly and quantitatively detecting organic phosphorus in soil according to claim 1, wherein in the step (1), the rotation speed of the centrifugation is 10000rpm and the time is 10min.
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