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. 2022 Dec 13;6:96. Originally published 2022 Aug 4. [Version 2] doi: 10.12688/gatesopenres.13727.2

Table 2. Proposed band assignments of the FTIR spectra of biochar.

Wavenumbers
(cm -1)
Characteristic vibrations Reference
3670 - 3650 ν(OH) from non-hydrogen bonded O-H groups ( Sharma et al., 2004)
3600 - 3200 ν(OH) from sorbed water and hydrogen-bonded biochar O-H groups ( Keiluweit et al., 2010)
~2980 2990-2950 cm -1 asymmetric aliphatic v(CH) from terminal –CH 3 groups ( Socrates, 2001)
~2890 2870-2890 cm -1 symmetric aliphatic v(CH) from terminal –CH 3 groups ( Socrates, 2001)
2700-2100 P-OH groups produce one or two broad bands in the 2700 -2100 region
2100 - 2250cm -1 C≡C bonds
2100 - 2360cm 1 Silane Si-H
2100 - 2270cm -1 Dimides, Azides and Ketenes
( Stuart, 2004)
1700 v(C=O) from carboxylic acids amides, esters and ketones 1740- 1650 ( Socrates, 2001)
1540 - 1650 C==O stretching vibrations for amides, aromatic C=C stretching and carboxylate anion vibrations. ( Calderón et al., 2006)
1580 - 1600 vibration of C=C bonds ( Davis et al., 1999)
1424 Carbonate (ν 3; asymmetric stretch) ( Socrates, 2001)
1200- 950 P–O (asymmetric and symmetric stretching of PO 2 and P(OH) 2 in phosphate) ( Jiang et al., 2004)
1100-1000 Si-O-Si asymmetric stretching ( Falaras, 1999)
1020 - 1030 C–O stretching of ethers and primary amine C–N stretches ( Keiluweit et al., 2010)
( Claoston et al., 2014)
~875 Out-of-plane bending for CO 3 2− and – v(M-O-H) O-H bending bands from clay minerals associated with biochar ( Zhao et al., 2013)
( Farmer, 1974)
796 and 780 quartz doublet ( Farmer, 1974)
462-464 Si-O-Si ( Qian & Chen, 2013)
452 Si-O rocking Shahrokh Abadi et al., 2015