“…To further identify the types and spatial distribution of functional groups of mineral-associated organic matter in the contrasting fertilization treatments, the high resolution of spatially-related SR-FTIR spectromicroscopy (with the fine scan model, 1 µm step −1 ) was used to collect the spectra through the soil particles (Figure 3). Obviously, the N-H stretching of amines (∼3,200-3,400 cm −1 ) (36, 37), C-H stretching of lipids (∼2,920 cm −1 ) (36), and aromatic C=C vibrations and amide N-C stretch (∼1,650 and 1,530 cm −1 , respectively) (37) were stronger in the long-term manure fertilized soil (i.e., M) than those in the long-term inorganic fertilized soil (i.e., NPK) (Figure 3). Notably, the strong absorbance of functional groups from secondary minerals (<950 cm −1 ) (38) supported that secondary minerals (e.g., Fe-O and Al-O) played a vital role in the SOC storage, which was supported by the results from NanoSIMS images (Figure 2).…”