Ma Chao, Ni Hong-Xing, Qi Yu-Lin
Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300072, China.
Sinochem Asset Management Co., Ltd., Beijing 100045, China.
Se Pu. 2023 Aug;41(8):662-672. doi: 10.3724/SP.J.1123.2023.03012.
Dissolved organic matter (DOM) is a highly complex and heterogeneous mixture that exists in various environments, including rivers, oceans, soils, and atmospheric aerosols. DOM plays a crucial role in biogeochemical cycles and significantly influences the environment by regulating water quality, changing the climate, and transporting pollutants. Therefore, clarifying the detailed molecular composition of DOM is essential to obtain a better understanding of its physical and chemical properties, thereby enabling further elucidation of its biogeochemical behavior. In this study, Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) combined with quadrupole detection (QPD) was used to conduct the online ultra performance liquid chromatography (UPLC)-MS analysis of DOM in water, aerosol, and soil samples collected in Tianjin, China. The samples were extracted with pure water and filtered through a glass fiber membrane (0.45 μm). The DOM in the samples was then enriched by solid-phase extraction (SPE) and redissolved in water-acetonitrile (1∶1, v/v) at mass concentration of 200 mg/L for the LC-MS experiments. The mobile phases used for UPLC were water containing 0.1% (v/v) formic acid (A) and acetonitrile containing 0.1% (v/v) formic acid (B). The gradient elution procedure was as follows: 0-5 min, 0B; 5-11 min, 0B-95%B; 11-25 min, 95%B; 25-28 min, 95%B-0B; 28-30 min, 0B. The flow rate was 0.1 mL/min, and the injection volume was 10 μL. The UV wavelength was set at 274 nm. MS detection was performed in negative electrospray ionization (ESI(-)) mode with a capillary voltage of 5.0 kV, and the MS data were collected in broadband ( 150-1000) and QPD modes. The transient data size was set to 2M, the free induction decay signal length was 0.74 s, and the ion accumulation time was 0.030 s. Four chromatographic peaks were observed in the chromatograms. The first peak was identified as salt adduct compounds containing sodium formate. The three other peaks contained complex components, such as oxygen-rich, unsaturated tannin-like compounds, as well as low-oxygen, highly saturated lignin-like and protein/amino-like compounds. UPLC-FT-ICR MS was suitable for assigning the detailed elemental compositions of the DOM samples. UPLC effectively improved the ionization efficiency of difficult-to-ionize compounds and enhanced the detection accuracy of MS. Indeed, MS peaks with a mass difference of as small as 3.4 mDa were well identified. A total of 12027, 15593, and 8029 peaks in the mass spectra of the water, aerosol, and soil samples, respectively, were assigned to known elemental formulae. Peaks Ⅱ and Ⅲ were hydrophilic components mainly including CHNO and CHO compounds. Compared with peak Ⅱ, peak Ⅲ exhibited a significant increase in CHNOS and CHOS, indicating that UPLC exerted a certain separation effect on these compounds. Furthermore, the aerosol samples contained a higher concentration of sulfur-containing compounds than the water and soil samples, primarily because of the abundance of organic sulfates present in atmospheric and cloud water. Data processing and graphic visualization revealed that the unique components in the water samples mainly appeared in the area of 0.1<O/C<0.5 and 1.0 <H/C<1.7. The compounds detected were low-oxygen and highly condensed lignin-like compounds. The unique components in the aerosol samples appeared in the area of 0.4<O/C<1.0 and 1.5<H/C<2.0, and were classified as carbohydrates. The unique components in the hydrophilic fraction of the soil samples were found in the area of 0.6<O/C<1.0 and 0.5<H/C<1.0, and were determined to be tannin-like compounds. By contrast, the components in the hydrophobic fraction were similar to those found in the water samples and appeared in the region containing lignin-like compounds. In summary, this study proposed a novel analytical protocol to characterize DOM from different ecosystems using UPLC-FT-ICR MS. This method could separate DOM components using UPLC with eluents of different polarities and analyze them using high-resolution FT-ICR MS to reveal their molecular compositions and possible chemical types. This protocol offers solid technical support for the comprehensive profiling of DOM at the molecular level.
溶解有机物(DOM)是一种高度复杂且异质的混合物,存在于各种环境中,包括河流、海洋、土壤和大气气溶胶。DOM在生物地球化学循环中起着至关重要的作用,并通过调节水质、改变气候和传输污染物对环境产生重大影响。因此,阐明DOM的详细分子组成对于更好地理解其物理和化学性质至关重要,从而能够进一步阐明其生物地球化学行为。在本研究中,采用傅里叶变换离子回旋共振质谱(FT-ICR MS)结合四极杆检测(QPD)对在中国天津采集的水、气溶胶和土壤样品中的DOM进行在线超高效液相色谱(UPLC)-MS分析。样品用纯水提取,通过玻璃纤维膜(0.45μm)过滤。然后通过固相萃取(SPE)对样品中的DOM进行富集,并以质量浓度200mg/L重新溶解于水-乙腈(1∶1,v/v)中用于LC-MS实验。UPLC使用的流动相为含0.1%(v/v)甲酸的水(A)和含0.1%(v/v)甲酸的乙腈(B)。梯度洗脱程序如下:0 - 5分钟,0%B;5 - 11分钟,0%B - 95%B;11 - 25分钟,95%B;25 - 28分钟,95%B - 0%B;28 - 30分钟,0%B。流速为0.1mL/min,进样量为10μL。紫外波长设定为274nm。MS检测在负电喷雾电离(ESI(-))模式下进行,毛细管电压为5.0kV,MS数据在宽带(150 - 1000)和QPD模式下采集。瞬态数据大小设定为2M,自由感应衰减信号长度为0.74s,离子累积时间为0.030s。在色谱图中观察到四个色谱峰。第一个峰被鉴定为含甲酸钠的盐加合物化合物。其他三个峰包含复杂成分,如富氧、不饱和的单宁类化合物,以及低氧、高饱和的木质素类和蛋白质/氨基类化合物。UPLC-FT-ICR MS适用于确定DOM样品的详细元素组成。UPLC有效提高了难电离化合物的电离效率,并增强了MS的检测准确性。实际上,质量差小至3.4mDa的MS峰也能被很好地识别。水、气溶胶和土壤样品的质谱图中分别共有12027、15593和8029个峰被指定为已知的元素分子式。峰Ⅱ和峰Ⅲ是亲水性成分,主要包括CHNO和CHO化合物。与峰Ⅱ相比,峰Ⅲ的CHNOS和CHOS显著增加,表明UPLC对这些化合物有一定的分离效果。此外,气溶胶样品中含硫化合物的浓度高于水和土壤样品,这主要是由于大气和云水相中存在大量有机硫酸盐。数据处理和图形可视化显示,水样中的独特成分主要出现在0.1 < O/C < 0.5和1.0 < H/C < 1.7的区域。检测到的化合物是低氧且高度缩合的木质素类化合物。气溶胶样品中的独特成分出现在0.4 < O/C < 1.0和1.5 < H/C < 2.0的区域,归类为碳水化合物。土壤样品亲水性部分的独特成分出现在0.6 < O/C < 1.0和0.5 < H/C < 1.0的区域,确定为单宁类化合物。相比之下,疏水性部分的成分与水样中的相似,出现在含木质素类化合物的区域。总之,本研究提出了一种新颖的分析方法,使用UPLC-FT-ICR MS对来自不同生态系统的DOM进行表征。该方法可以使用具有不同极性洗脱剂的UPLC分离DOM成分,并使用高分辨率FT-ICR MS对其进行分析,以揭示其分子组成和可能的化学类型。该方法为在分子水平上全面剖析DOM提供了坚实的技术支持。