2011
DOI: 10.1111/j.1365-2818.2011.03553.x
|View full text |Cite
|
Sign up to set email alerts
|

Analytical electron microscopy of black carbon and microaggregated mineral matter in Amazonian dark Earth

Abstract: Black carbon (BC) is one of the most stable forms of soil organic matter. Its surface functional groups and structure have been well characterized by a range of analytical methods. However, little is known about the mechanisms of interactions between the BC particles and the surrounding mineral matter. In this paper a range of microscopy techniques, such as transmission electron microscopy and scanning transmission electron microscopy, were used to investigate the possible reactions of BC particles within micr… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

2
16
0

Year Published

2013
2013
2021
2021

Publication Types

Select...
8
1

Relationship

1
8

Authors

Journals

citations
Cited by 21 publications
(18 citation statements)
references
References 40 publications
2
16
0
Order By: Relevance
“…Similarly, the D-G bands in the Raman spectra of the BCC were fitted to five mixed Gaussian-Lorenzian functions, then the cross sectional particle size for a bimodal distribution calculated using a G1 peak at 1598 cm −1 , FWHM 63 cm −1 = 11 nm, G2 1542 cm −1 , FWHM 226 cm −1 = 3 nm . The crystallite size range of the BC of 9-15 nm is typical of charcoals (7-11 nm) (Ribeiro-Soares et al, 2013) whereas the BCC 3-11 nm is more typical of biochars and black carbon that have a significant coating of organomineral micro aggregates as found in Terra Preta soil particles (2-8 nm) (Chia et al, 2012b;Ribeiro-Soares et al, 2013).…”
Section: Analysis Of Surface Functional Groups Using Xps Ftir Raman mentioning
confidence: 99%
“…Similarly, the D-G bands in the Raman spectra of the BCC were fitted to five mixed Gaussian-Lorenzian functions, then the cross sectional particle size for a bimodal distribution calculated using a G1 peak at 1598 cm −1 , FWHM 63 cm −1 = 11 nm, G2 1542 cm −1 , FWHM 226 cm −1 = 3 nm . The crystallite size range of the BC of 9-15 nm is typical of charcoals (7-11 nm) (Ribeiro-Soares et al, 2013) whereas the BCC 3-11 nm is more typical of biochars and black carbon that have a significant coating of organomineral micro aggregates as found in Terra Preta soil particles (2-8 nm) (Chia et al, 2012b;Ribeiro-Soares et al, 2013).…”
Section: Analysis Of Surface Functional Groups Using Xps Ftir Raman mentioning
confidence: 99%
“…Detailed evaluation of biochar after incorporating into the soil for more than one year has been carried out using a range of techniques including transmission electron microscopy (TEM) and scanning electron microscopy (SEM). Chia et al (2012) characterized the interfaces between carbon-rich and mineral-rich regions of particles collected from the Terra Preta soils from the Amazon. A key finding was the appearance of Fe and Mn nanoparticles around the surface of the carbon-rich regions and the high concentration of Ca in the amorphous carbon that surrounded mineral phases.…”
Section: Introductionmentioning
confidence: 99%
“…For instance, O K-edges observed in Figure 6 and Figure 7 display a prepeak for Ti and Fe particles that is absent for the O K-edge associated with clays, consistent with previous studies on similar systems. 35 This prepeak is associated with O bonded to Fe and Ti. A preliminary analysis (not shown) of the near-edge structure in EELS spectra for C K-edge was performed with an energy resolution of 0.6 eV.…”
Section: Energy and Fuelsmentioning
confidence: 99%