Minero Claudio, Lauri Vittorio, Falletti Gianpaolo, Maurino Valter, Pelizzetti Ezio, Vione Davide
Dipartimento di Chimica Analitica, Università di Torino, Via Pietro Giuria 5, 10125 Torino, Italy.
Ann Chim. 2007 Oct;97(10):1107-16. doi: 10.1002/adic.200790094.
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 (micro +/- sigma = 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 by means 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.
主要采自意大利西北部皮埃蒙特大区都灵省的湖水过滤样本,从分光光度法的角度进行了特征分析。然后,光谱数据被用于通过三波长光度法直接测定硝酸盐,该方法应能解释溶解有机物(DOM)造成的光谱干扰,并将结果与离子色谱法测定的硝酸盐含量进行比较。分光光度法被证明非常适合用于硝酸盐测量,在硝酸盐浓度高达0.1 mM时,相关图(光谱数据与离子色谱数据)的斜率为1(微 +/- 西格玛 = 0.99 +/- 0.03),26个数据点的r2 = 0.97。湖水光谱还通过285和254 nm处的特定吸光度(吸光度与NPOC,后者用于量化DOM含量)以及E2/E3和E3/E4指数来表征DOM。后两者仅利用辐射吸收数据(250与365以及300与400 nm)。可以得出结论,湖水DOM主要由自生源物质(生物产生的脂肪族化合物,只有一小部分芳香族基团)组成,通常分子量和芳香度较低。在高山湖泊中可能会发现一些例外情况,但也应该考虑到,如果要研究DOM的来源,NPOC测量是无法避免的。仅从吸收光谱就可以了解吸收辐射的DOM的芳香度,但大多数自生源DOM会逃过分光光度法的表征。