抑制型离子色谱法测定白酒中的F~-、CI~-、NO_2~-、H_2PO_4~-、NO_3~-

用抑制型离子色谱法测定白酒中的F~-、cl~-、NO_2~-、H_2PO_4~-、NO_3~-。流动相为4mmoL/L Na_2CO_3-3mmoL/L NaHCO_3混合溶液,流速为1.5mL/min,进样量为0.5mL,在最佳色谱条件下,5种无机阴离子10min内实现基线分离。F~-、cl~-、NO_2~-、H_2PO_4~-、NO_3~-的检出限分别为0.008、0.012、0.030、0.068、0.077mg/L。测定结果的相对标准偏差分别为1.86％、1.30％、2.06％、1.82％、1.50％,回收率分别为108.0％、94.0％、101.0％、98.7％、94.4％。     

离子色谱法测定大豆木质部汁液中的Cl-、SO42-、NO3-、PO43-、柠檬酸和苹果酸

建立了离子色谱法测定大豆木质部汁液中Cl~-、SO_4~(2-)、NO_3~-、PO_4~(3-)、柠檬酸和苹果酸的方法。Cl~-、SO_4~(2-)、NO_3~-、PO_4~(3-)、柠檬酸和苹果酸的检出限分别为0.01、0.04、0.05、0.05、0.30和0.10 mg/L,相对标准偏差分别为8.34％、4.68％、9.54％、6.86％、5.52％和7.50％,线性范围分别为0.5～50.0、1.0～100.0、0.5～50.0、1.0～100.0、5.0～100.0和1.0～100.0 mg/L,回收率分别为103％～106.7％、92％～98.7％、93％～95.5％、91.7％～92％、93.2％～106％和94％～108.3％。方法简便、快速,测定结果准确,无干扰。     

离子色谱法测定啤酒中的F~-、CI~-、SO_4~(2-)、NO_3~-和PO_4~(3-)

建立了以ASII-HC型阴离子交换柱分离、NaOH溶液为淋洗液、甲醇为有机改进剂、化学抑制电导检测测定啤酒中的F~-、cl~-、SO_4~(2-)、NO_3~-和PO_4~(3-)的离子色谱方法。各被测离子的线性关系良好,相关系数为0.9778～0.9991,测定结果的相对标准偏差为0.02％～3.60％,样品回收率为97.88％～103.80％。     

高效阴离子色谱法测定电催化氮气氧化中NO3-/NO2-的含量

开发了一种测定高浓度SO_4~(2-)电解液(0.5 mol/L)中NO_3~-/NO_2~-含量的高效阴离子色谱法。该方法不受催化剂溶出以及其它干扰离子的影响,可以应用于电催化氮气氧化制备NO_3~-/NO_2~-。通过改变流动相的流速、淋洗液浓度以及柱温实现了SO_4~(2-)与NO_3~-/NO_2~-色谱峰的完全分离。优化得到最佳检测条件:流动相流速1.0 mL/min,柱温30℃,淋洗液浓度25 mmol/L,淋洗液设置为等浓度梯度,冲洗因子:10,此条件下在较宽的检测范围内(0～300 mg/L)实现NO_3~-/NO_2~-的高灵敏度检测。其中,NO_3~-线性关系式为:Y_2=0.0107X_2-0.0255,相关系数R~2为0.9998; NO_2~-线性关系式为:Y_1=0.0127X_1+0.0107,相关系数R~2为0.9997。     

离子色谱法测定纯净水中F~-,BrO_3~-等6种阴离子

建立阴离子分离柱离子色谱法测定纯净水中F~-,BrO_3~-,Cl~-,NO_2~-,Br~-,NO_3~- 6种微量阴离子的方法。以SH-AC-1型阴离子柱为分离柱,柱箱温度为35℃,以1.0 mmol/L Na_2CO_3为淋洗液,流量为1.5 mL/min。F~-,BrO_3~-,Cl~-,NO_2~-,Br~-,NO_3~-的线性范围分别为20~320,40~800,40~640,10~200,50~1 000,50~1 000μg/L,线性相关系数均大于0.999,检出限为0.7~7.5μg/L,加标回收率在95.0%~106.3%之间,测定结果的相对标准偏差为1.41%~4.27%(n=5)。该方法测定结果准确、可靠,操作简便、快速,适用于纯净水中BrO_3~-,F~-,Cl~-,NO_2~-,Br~-,NO_3~- 6种阴离子的测定。     

离子色谱法测定核电站一回路冷却剂中痕量F~-,Cl~-和SO_4~(2-)

建立离子色谱法测定核电站一回路冷却剂中痕量氟离子F~-,氯离子Cl~-,硫酸根离子SO_4~(2-)的方法。采用80 mmol/L硼酸溶液配合氢氧化钾淋洗液发生器在线生成淋洗液,梯度洗脱,淋洗液流量为1.2 mL/min,在选定的分析条件下,NO_2~-,NO_3~-,PO_4~(3-)和CO_3~(2-)不干扰F~-,Cl~-,SO_4~(2-)的测定。F~-,Cl~-,SO_4~(2-)的质量浓度与其色谱峰面积呈良好的线性关系,线性相关系数分别为0.999 8,0.999 5,0.999 7,线性范围分别为0.85~30.0,2.65~30.0,2.00~30.0μg/L。F~-,Cl~-,SO_4~(2-)测定结果的相对标准偏差分别为0.56%~1.58%,0.85%~3.62%,1.21%~4.60%(n=7)。F~-,Cl~-,SO_4~(2-)的加标回收率分别为98%~104%,98%~108%,93%~108%。该方法快速、准确,满足核电站一回路冷却剂中痕量F~-,Cl~-,SO_4~(2-)的检测要求。     

离子色谱法测定油田灌注污水中的Cl~-、NO_3~-、SO_4~(2-)

采用二氯甲烷萃取、活性炭吸附、Na_2CO_3/NaHCO_3淋洗液储备液沉淀等预处理方法,有效地除去了油田灌注污水样中的有机物质和可能存在的高含量的钙镁离子,进而用离子色谱法同时测定了Cl~-、NO_3~-、SO_4~(2-)三种离子,相对标准偏差分别为0.06、4.6、2.2,NO_3~-、SO_4~(2-)离子的加标回收率分别为97.9％和97.1％。     

NO3^—,NO2^—同时测定的研究进展

综述了近年来农业、环境科学和食品科学中NO_3~-、NO_2~-同时测定方法的研究进展。     

电导-紫外检测器联用离子色谱法测定水样中的7种阴离子

以电导-紫外检测器联用离子色谱法同时测定水中的F~-、Cl~-、NO_2~-、Br~-、NO_3~-、I~-和SO_4~(2-)。样品经TSK gel guard column Suppe IC-Anion HS保护柱以及TSK gel Suppe IC-Anion HS分离柱分离,以NaHCO3(2.0mmol/L)-Na_2CO_3(3.0mmol/L)为流动相,流速1.5mL/min,柱温40℃,采用抑制电导检测器与紫外可见检测器串联检测。其中,F~-、Cl~-、Br~-和SO_4~(2-)使用电导检测器,NO_2~-、NO_3~-和I-采用紫外检测器。7种离子均具有较宽的线性范围,其线性相关系数r>0.999。对饮用纯净水以及海水两种实际样品进行测定和加标回收实验,加标回收率在92.8%~107%,测定值的相对标准偏差(n=6)在0.89%~5.7%。方法具有分析速度快,检出限低,精密度好等优点。在实际工作中具有很强的实用性和推广应用价值。     

电导-紫外检测器联用离子色谱法测定水样中的7种阴离子

以电导-紫外检测器联用离子色谱法同时测定水中的F~-、Cl~-、NO_2~-、Br~-、NO_3~-、I~-和SO_4~(2-)。样品经TSK gel guard column Suppe IC-Anion HS保护柱以及TSK gel Suppe IC-Anion HS分离柱分离,以NaHCO3(2.0mmol/L)-Na_2CO_3(3.0mmol/L)为流动相,流速1.5mL/min,柱温40℃,采用抑制电导检测器与紫外可见检测器串联检测。其中,F~-、Cl~-、Br~-和SO_4~(2-)使用电导检测器,NO_2~-、NO_3~-和I-采用紫外检测器。7种离子均具有较宽的线性范围,其线性相关系数r0.999。对饮用纯净水以及海水两种实际样品进行测定和加标回收实验,加标回收率在92.8%~107%,测定值的相对标准偏差(n=6)在0.89%~5.7%。方法具有分析速度快,检出限低,精密度好等优点。在实际工作中具有很强的实用性和推广应用价值。     

离子色谱法测定农村饮用水中阴离子

采用离子色谱法测定农村饮用水中F-、Cl-、NO2-、Br-、NO3-和SO42-等6种阴离子的含量。水样经Ion Pac AG19保护柱及Ion Pac AS19分离柱分离,以20.00mmol·L-1氢氧化钾溶液为淋洗液,采用抑制电导器检测。F-、NO2-和Br-在4mg·L-1以内,Cl-、NO3-和SO42-在40mg·L-1以内呈线性关系,检出限(2S/N)在0.002～0.012mg·L-1之间。方法用于水样中6种阴离子的测定,加标回收率在98.0%～101.3%之间,相对标准偏差(n=6)在0.83%～2.7%之间。     

离子色谱法同时测定大气降水中的5种阴离子

以保留时间定性、峰面积外标法定量,建立了离子色谱同时测定大气降水中F–,Cl–,NO2–,NO3–,SO42–5种阴离子的分析方法。结果表明,5种阴离子标准曲线线性相关系数均大于0.999 8,检出限(3s/k)在0.000 3~0.006 6 mg/L之间。F–,Cl–,NO2–,NO3–,SO42–测定结果的相对标准偏差(n=10)分别为1.70%,2.46%,9.30%,0.73%,0.67%。用该方法对水样进行测定并进行加标回收试验,5种阴离子加标回收率在91.2%~102.7%之间。该方法灵敏度高,简便、快速,能满足大气降水中阴离子分析的要求。     

离子色谱法测定生活饮用水中4种阴离子

对离子色谱法测定饮用水中的F-,C1-,NO3- -N,SO4^2--4种阴离子的分析方法进行了优化。用正交试验法选择最优实验条件为：流速0．9mL／min,柱温32℃。4种阴离子检出限：F-0．02mg／L,Cl-0．04mg／L,NO3--N0．04mg／L,SO4^2- 0．16mg／L。测定结果相对标准偏差均小于5％,回收率为91.3％～106．1％,相关系数大于0．999。该方法操作简便,灵敏度、准确度高,标准工作曲线线性良好,可用于饮用水中F-,C1-,NO3^- —N,SO4^2—4种离子的同时分析。     

碱化底液消除水负峰离子色谱法测定水中F~–,Cl~–等7种阴离子

在研究消除水负峰的基础上,建立离子色谱法测定水中F–,Cl–,NO2–,H2PO4–,Br–,NO3–,SO42–7种阴离子的方法。经实验确定淋洗液为4.5 mmol/L NaHCO3–4.0 mmol/L Na2CO3,淋洗液流量为1.0 mL/min,柱箱温度为35℃。在底液中加入与淋洗液同浓度的Na2CO3–NaHCO3可有效消除水负峰。该方法对7种阴离子的检出限为0.004~0.034 mg/L,测定结果的相对标准偏差为0.69%~3.57%(n=6),加标回收率为95%~105%。该法能有效消除水负峰及其对F–测定的影响,操作简便、测定结果准确可靠,适用于水中F–、Cl–等7种阴离子的测定。     

离子色谱法测定火场爆炸残留物中7种阴离子

建立了离子色谱法测定爆炸残留物中F,Cl,NO_2,SO_4,Br,NO_3,PO_47种阴离子的方法。采用抑制电导检测器,以DIONEX Ion Pac~?AS11–HC型阴离子交换柱为分离柱,柱箱温度为40℃,以22 mmol/L KOH溶液为淋洗液,流量为1.20 m L/min。F~–,Cl~–,NO_2~–,SO_4~(2–),Br~–,NO_3~–,PO_4~(3–)在各自范围内均呈良好的线性关系,相关系数均大于0.999,检出限在0.06~0.15 mg/L之间,加标回收率为92.5%~101.3%,测定结果的相对标准偏差为1.86%~2.79%(n=7)。该方法简便、快捷,选择性好,灵敏度高,可满足分析要求。     

离子色谱法测定水中的F-、Cl-、NO2--N、NO3--N、SO42-

应用DX－102型离子色谱仪测定水中的F^-、Cl^-、NO2^-－N、NO3^-－N及SO4^2-，淋洗液为1.42mmol/L NaHCO3-1.50mmol/L Na2CO3溶液，淋洗液流速为1.8mL/min，进样量为25μL。5种离子在上述实验条件下分离良好，定量测定的线性相关系数均在0.9995以上。     

The reaction of Li[Al(OR)4] R = OC(CF3)2Ph, OC(CF3)3 with NO/NO2 giving NO[Al(OR)4], Li[NO3] and N2O. The synthesis of NO[Al(OR)4] from Li[Al(OR)4] and NO[SbF6] in sulfur dioxide solution

NO[Al(OC(CF(3))(2)Ph)(4)] 1 and NO[Al(OC(CF(3))(3))(4)] 2 were obtained by the metathesis reaction of NO[SbF(6)] and the corresponding Li[Al(OR)(4)] salts in liquid sulfur dioxide solution in ca 40% (1) and 85% (2) isolated yield. 1 and 2, as well as Li[NO(3)] and N(2)O, were also given by the reaction of an excess of mixture of (90 mol%) NO, (10 mol%) NO(2) with Li[Al(OR)(4)] followed by extraction with SO(2). The unfavourable disproportionation reaction of 2NO(2)(g) to [NO](+)(g) and [NO(3)](-)(g)[DeltaH degrees = +616.2 kJ mol(-1)] is more than compensated by the disproportionation energy of 3NO(g) to N(2)O(g) and NO(2)(g)[DeltaH degrees =-155.4 kJ mol(-1)] and the lattice energy of Li[NO(3)](s)[U(POT)= 862 kJ mol(-1)]. Evidence is presented that the reaction proceeds via a complex of [Li](+) with NO, NO(2)(or their dimers) and N(2)O. NO(2) and Li[Al(OC(CF(3))(3))(4)] gave [NO(3)(NO)(3)][Al(OC(CF(3))(3))(4)](2), NO[Al(OC(CF(3))(3))(4)] and (NO(2))[Al(OC(CF(3))(3))(4)] products. The aluminium complex [Li[AlF(OC(CF(3))(2)Ph)(3)]](2) 3 was prepared by the thermal decomposition of Li[Al(OC(CF(3))(2)Ph)(4)]. Compounds 1 and 3 were characterized by single crystal X-ray structural analyses, 1-3 by elemental analyses, NMR, IR, Raman and mass spectra. Solid 1 contains [Al(OC(CF(3))(2)Ph)(4)](-) and [NO](+) weakly linked via donor acceptor interactions, while in the SO(2) solution there is an equilibrium between the associated [NO](+)[Al(OC(CF(3))(2)Ph)(4)](-) and separated solvated ions. Solid 2 contains essentially ionic [NO](+) and [Al(OC(CF(3))(3))(4)](-). Complex 3 consists of two [Li[AlF(OC(CF(3))(2)Ph)(3)]] units linked via fluorine lithium contacts. Compound 1 is unstable in the SO(2) solution and decomposes to yield [AlF(OC(CF(3))(2)Ph)(3)](-), [(PhC(CF(3))(2)O)(3)Al(mu-F)Al(OC(CF(3))(2)Ph)(3)](-) anions as well as (NO)C(6)H(4)C(CF(3))(2)OH, while compound 2 is stable in liquid SO(2). The [small nu](NO(+)) in 1 and [NO](+)(toluene)[SbCl(6)] are similar, implying similar basicities of [Al(OC(CF(3))(2)Ph)(4)](-) and toluene.     

Determination of inorganic anions by ion chromatography using a graphitized carbon column dynamically coated with cetyltrimethylammonium ions.

The simultaneous determination of inorganic anions by ion chromatography using a dynamically coated graphitized carbon column with cetyltrimethylammonium (CTA) ions was investigated with suppressed conductivity detection. Column preparations with CTA and sodium carbonate-sodium hydrogencarbonate concentration in the eluent were examined to optimize the separation of seven common anions (F-, Cl-, NO2-, Br-, NO3-, HPO(4)2- and SO(4)2-). Calibration curves were linear from 0.5 to 5 micrograms/ml for F-, from 1.0 to 10 micrograms/ml for Cl-, from 1.5 to 15 micrograms/ml for NO2-, from 2.0 to 20 micrograms/ml for Br- and NO3-, from 5.0 to 50 micrograms/ml for HPO(4)2- and from 3.0 to 30 micrograms/ml for SO(4)2- with correlation coefficients (r) of 0.999 or better. The relative standard deviations of peak areas were between 0.3 and 0.9% for 10 repeated measurements. The application of this newly developed method was demonstrated by the determination of inorganic anions in the water for pharmaceutical purposes. Using CTA-Br as the coating agent, a permanently coated ion-exchange column was obtained, which allowed efficient separations of seven anions without adding any coating agent to the eluent.     

Nitrogen-15 in NO3- characterises differently reactive soil organic N pools

Intercropping with legumes is known to increase the plant-available nitrogen (N) in soil, but can also increase leaching of NO3- to the groundwater. To minimise NO3- leaching risks, knowledge of the N-release processes is essential, including an estimate of the contribution of legumes to total NO3- concentrations in soil. Our objectives were to answer the questions: (1) whether the presence of legume roots increases N mineralisation, and (2) whether the proportion of legume-derived N in NO3- could be calculated with the help of natural abundance 15N in NO3-. We sampled soil monoliths of a Medicago x varia Martyn monoculture in August 2004 and set up three treatments: 'disturbance' (sieved to <2 mm), 'disturbance-roots' (sieved to <2 mm and visible roots removed), and 'control' (left untreated). During an incubation period of 70 days, an N-free nutrient solution was leached through the samples weekly. In the leachates we measured total N, total organic carbon, NO3-, and NH4+ concentrations. Six of the 13 sampling dates were chosen for N isotope analysis in NO3-. Nitrate was separated as AgNO3. During the incubation, 3 to 6% of the initial total mass of total N (192 to 274 mg N) in soil was mineralised. Nitrogen mineralisation followed zero-order kinetics independent of treatments. Mineralisation rates decreased in the order control (day 70: 3.7 microg NO3-N (mg Ninitial)-1)>disturbance-roots (2.6 microg NO3-N (mg Ninitial)-1)>disturbance (1.9 microg NO3-N (mg Ninitial)-1), indicating that mineralisation of legume roots did not play a major role in N mineralisation. The delta15N values jumped from ca. 3 per thousand to ca. 8 per thousand after 2 weeks of incubation, which we attributed to the contribution of two N pools. An exponential two-pool model could not be fitted to the data. Legume-derived soil organic matter, SOM (pool 1), was mineralised at the same rate as SOM accumulated before establishment of the legumes (pool 2). Fresh legume roots did not contribute significantly to N mineralisation.