†Environmental Molecular Sciences Laboratory and Biological Sciences Division, Pacific Northwest National Laboratory, Richland, Washington 99354, United States.
Anal Chem. 2015;87(10):5206-15. doi: 10.1021/acs.analchem.5b00116. Epub 2015 Apr 30.
Soil organic matter (SOM), a complex, heterogeneous mixture of above and belowground plant litter and animal and microbial residues at various degrees of decomposition, is a key reservoir for carbon (C) and nutrient biogeochemical cycling in soil based ecosystems. A limited understanding of the molecular composition of SOM limits the ability to routinely decipher chemical processes within soil and accurately predict how terrestrial carbon fluxes will respond to changing climatic conditions and land use. To elucidate the molecular-level structure of SOM, we selectively extracted a broad range of intact SOM compounds by a combination of different organic solvents from soils with a wide range of C content. Our use of electrospray ionization (ESI) coupled with Fourier transform ion cyclotron resonance mass spectrometry (FTICR MS) and a suite of solvents with varying polarity significantly expands the inventory of the types of organic molecules present in soils. Specifically, we found that hexane is selective for lipid-like compounds with very low O/C ratios (<0.1); water (H2O) was selective for carbohydrates with high O/C ratios; acetonitrile (ACN) preferentially extracts lignin, condensed structures, and tannin polyphenolic compounds with O/C > 0.5; methanol (MeOH) has higher selectivity toward compounds characterized with low O/C < 0.5; and hexane, MeOH, ACN, and H2O solvents increase the number and types of organic molecules extracted from soil for a broader range of chemically diverse soil types. Our study of SOM molecules by ESI FTICR MS revealed new insight into the molecular-level complexity of organics contained in soils. We present the first comparative study of the molecular composition of SOM from different ecosystems using ultra high-resolution mass spectrometry.
土壤有机质(SOM)是一种复杂的、异质的地上和地下植物凋落物以及动物和微生物残体的混合物,处于不同程度的分解状态,是土壤基生态系统中碳(C)和养分生物地球化学循环的关键储库。对 SOM 分子组成的了解有限,限制了我们常规解析土壤内化学过程的能力,并准确预测陆地碳通量将如何响应不断变化的气候条件和土地利用。为了阐明 SOM 的分子水平结构,我们使用不同极性的一系列溶剂,通过不同有机溶剂的组合,从具有广泛 C 含量的土壤中选择性地提取了广泛的完整 SOM 化合物。我们使用电喷雾电离(ESI)与傅里叶变换离子回旋共振质谱(FTICR MS)相结合,并使用一系列具有不同极性的溶剂,显著扩展了土壤中存在的有机分子类型的清单。具体来说,我们发现正己烷对 O/C 比值非常低(<0.1)的类脂化合物具有选择性;水(H2O)对 O/C 比值高的碳水化合物具有选择性;乙腈(ACN)优先提取 O/C>0.5 的木质素、缩合结构和单宁多酚化合物;甲醇(MeOH)对 O/C<0.5 的化合物具有更高的选择性;正己烷、MeOH、ACN 和 H2O 溶剂增加了从更广泛的化学多样土壤类型中提取的土壤中有机分子的数量和类型。我们通过 ESI FTICR MS 对 SOM 分子的研究揭示了土壤中有机物分子水平复杂性的新见解。我们使用超高分辨率质谱对不同生态系统的 SOM 分子组成进行了首次比较研究。