{"title":"表层湖水样品的分光光度表征:对硝酸盐定量和溶解有机物性质的影响","authors":"Claudio Minero, Vittorio Lauri, Gianpaolo Falletti, Valter Maurino, Ezio Pelizzetti, Davide Vione","doi":"10.1002/adic.200790094","DOIUrl":null,"url":null,"abstract":"<p>Filtered lakewater samples, mainly collected in the province of Torino (Piedmont, NW Italy) were characterised from a spectrophotometric point of view. Spectral data were then used for the direct determination of nitrate by three-wavelength photometry, which should account for the spectral interference by dissolved organic matter (DOM), and the results compared with nitrate quantification by ion chromatography. The spectrophotometric method proved very suitable for nitrate measurement, with unity slope (μ±σ = 0.99±0.03) of the correlation plot (spectral vs. ion chromatography data) up to 0.1 mM nitrate, and with r<sup>2</sup> = 0.97 for 26 data points. Lakewater spectra were also used for the characterisation of DOM bymeans of the specific absorption at 285 and 254 nm (absorbance vs. NPOC, the latter to quantify the DOM amount), and the E<sub>2</sub>/E<sub>3</sub> and E<sub>3</sub>/E<sub>4</sub> indexes. The latter two make only use of radiation absorption data (250 vs. 365 and 300 vs. 400 nm). It could be concluded that lakewater DOM is mainly composed of autochthonous material (biologically produced aliphatic compounds and only a minor fraction of aromatic groups), with generally low molecular weight and degree of aromaticity. Some exceptions could be found in high-mountain lakes, but it should also be considered that NPOC measurement cannot be avoided if DOM origin is to be studied. From the absorption spectrum alone it is possible to get indication on the aromaticity degree of radiation-absorbing DOM, but most of the autochthonous DOM would escape spectrophotometric characterisation.</p>","PeriodicalId":8193,"journal":{"name":"Annali di chimica","volume":"97 10","pages":"1107-1116"},"PeriodicalIF":0.0000,"publicationDate":"2007-09-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1002/adic.200790094","citationCount":"37","resultStr":"{\"title\":\"Spectrophotometric Characterisation of Surface Lakewater Samples: Implications for the Quantification of Nitrate and the Properties of Dissolved Organic Matter\",\"authors\":\"Claudio Minero, Vittorio Lauri, Gianpaolo Falletti, Valter Maurino, Ezio Pelizzetti, Davide Vione\",\"doi\":\"10.1002/adic.200790094\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Filtered lakewater samples, mainly collected in the province of Torino (Piedmont, NW Italy) were characterised from a spectrophotometric point of view. Spectral data were then used for the direct determination of nitrate by three-wavelength photometry, which should account for the spectral interference by dissolved organic matter (DOM), and the results compared with nitrate quantification by ion chromatography. The spectrophotometric method proved very suitable for nitrate measurement, with unity slope (μ±σ = 0.99±0.03) of the correlation plot (spectral vs. ion chromatography data) up to 0.1 mM nitrate, and with r<sup>2</sup> = 0.97 for 26 data points. Lakewater spectra were also used for the characterisation of DOM bymeans of the specific absorption at 285 and 254 nm (absorbance vs. NPOC, the latter to quantify the DOM amount), and the E<sub>2</sub>/E<sub>3</sub> and E<sub>3</sub>/E<sub>4</sub> indexes. The latter two make only use of radiation absorption data (250 vs. 365 and 300 vs. 400 nm). It could be concluded that lakewater DOM is mainly composed of autochthonous material (biologically produced aliphatic compounds and only a minor fraction of aromatic groups), with generally low molecular weight and degree of aromaticity. Some exceptions could be found in high-mountain lakes, but it should also be considered that NPOC measurement cannot be avoided if DOM origin is to be studied. 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引用次数: 37
摘要
过滤的湖水样本,主要收集在都灵省(皮埃蒙特,意大利西北部)从分光光度法的角度进行了表征。然后利用光谱数据进行三波长光度法直接测定硝酸盐,该方法应考虑溶解有机物(DOM)的光谱干扰,并将结果与离子色谱法测定硝酸盐进行比较。结果表明,分光光度法非常适用于硝酸盐的测定,相关图(光谱与离子色谱数据)的统一斜率(μ±σ = 0.99±0.03)可达0.1 mM硝酸盐,26个数据点的r2 = 0.97。通过285 nm和254 nm的比吸收(吸光度vs. NPOC,后者用于量化DOM的量)以及E2/E3和E3/E4指标,利用湖水光谱对DOM进行表征。后两种方法仅使用辐射吸收数据(250 nm vs. 365 nm和300 nm vs. 400 nm)。结果表明,湖水DOM主要由天然物质(生物生成的脂肪族化合物和少量芳香族)组成,分子量普遍较低,芳香度较低。在高山湖泊中可以发现一些例外,但也应该考虑到,如果要研究DOM的起源,NPOC的测量是无法避免的。仅从吸收光谱就可以得到吸收辐射的DOM的芳香度的指示,但大多数原生DOM会逃避分光光度表征。
Spectrophotometric Characterisation of Surface Lakewater Samples: Implications for the Quantification of Nitrate and the Properties of Dissolved Organic Matter
Filtered lakewater samples, mainly collected in the province of Torino (Piedmont, NW Italy) were characterised from a spectrophotometric point of view. Spectral data were then used for the direct determination of nitrate by three-wavelength photometry, which should account for the spectral interference by dissolved organic matter (DOM), and the results compared with nitrate quantification by ion chromatography. The spectrophotometric method proved very suitable for nitrate measurement, with unity slope (μ±σ = 0.99±0.03) of the correlation plot (spectral vs. ion chromatography data) up to 0.1 mM nitrate, and with r2 = 0.97 for 26 data points. Lakewater spectra were also used for the characterisation of DOM bymeans of the specific absorption at 285 and 254 nm (absorbance vs. NPOC, the latter to quantify the DOM amount), and the E2/E3 and E3/E4 indexes. The latter two make only use of radiation absorption data (250 vs. 365 and 300 vs. 400 nm). It could be concluded that lakewater DOM is mainly composed of autochthonous material (biologically produced aliphatic compounds and only a minor fraction of aromatic groups), with generally low molecular weight and degree of aromaticity. Some exceptions could be found in high-mountain lakes, but it should also be considered that NPOC measurement cannot be avoided if DOM origin is to be studied. From the absorption spectrum alone it is possible to get indication on the aromaticity degree of radiation-absorbing DOM, but most of the autochthonous DOM would escape spectrophotometric characterisation.