Abstract:Carbon particles containing mineral matter promote soil fertility, helping it to overcome the rather unfavorable climate conditions of the humid tropics. Intriguing examples are the Amazonian Dark Earths, anthropogenic soils also known as "Terra Preta de Índio'' (TPI), in which chemical recalcitrance and stable carbon with millenary mean residence times have been observed. Recently, the presence of calcium and oxygen within TPI-carbon nanoparticles at the nano- and mesoscale ranges has been demonstrated. In th… Show more
“…In this fraction, the C 1s photoelectron peak was composed of four components (Supplementary Table 10): C1s A in 284.6 eV from aromatic C (C=C); C1s B in 286.2 ± 0.2 eV, which may be assigned to phenol or hydroxyl (C-OH) groups, ether (C-O-C) or pyrrolic (C-N) groups; C 1s C in 287.5 ± 0.4 eV, assigned to carbonyl (C=O) groups; and C 1s D in 289.1 ± 0.3 eV, assigned to the carboxyl (COOH) groups 43,44 .…”
Section: Spectroscopic Insights Into Primingmentioning
Biochar can increase the stable C content of soil. However, studies on the longer-term role of plant-soil-biochar interactions and the consequent changes to native soil organic carbon (SOC) are lacking. Periodic 13 CO 2 pulse labelling of ryegrass was used to monitor belowground C allocation, SOC priming, and stabilization of root-derived C for a 15-month period-commencing 8.2 years after biochar (Eucalyptus saligna, 550 • C) was amended into a subtropical ferralsol. We found that field-aged biochar enhanced the belowground recovery of new root-derived C ( 13 C) by 20%, and facilitated negative rhizosphere priming (it slowed SOC mineralization by 5.5%, that is, 46 g CO 2 -C m −2 yr −1 ). Retention of root-derived 13 C in the stable organo-mineral fraction (<53 µm) was also increased (6%, P < 0.05). Through synchrotron-based spectroscopic analysis of bulk soil, fieldaged biochar and microaggregates (<250 µm), we demonstrate that biochar accelerates the formation of microaggregates via organo-mineral interactions, resulting in the stabilization and accumulation of SOC in a rhodic ferralsol.
“…In this fraction, the C 1s photoelectron peak was composed of four components (Supplementary Table 10): C1s A in 284.6 eV from aromatic C (C=C); C1s B in 286.2 ± 0.2 eV, which may be assigned to phenol or hydroxyl (C-OH) groups, ether (C-O-C) or pyrrolic (C-N) groups; C 1s C in 287.5 ± 0.4 eV, assigned to carbonyl (C=O) groups; and C 1s D in 289.1 ± 0.3 eV, assigned to the carboxyl (COOH) groups 43,44 .…”
Section: Spectroscopic Insights Into Primingmentioning
Biochar can increase the stable C content of soil. However, studies on the longer-term role of plant-soil-biochar interactions and the consequent changes to native soil organic carbon (SOC) are lacking. Periodic 13 CO 2 pulse labelling of ryegrass was used to monitor belowground C allocation, SOC priming, and stabilization of root-derived C for a 15-month period-commencing 8.2 years after biochar (Eucalyptus saligna, 550 • C) was amended into a subtropical ferralsol. We found that field-aged biochar enhanced the belowground recovery of new root-derived C ( 13 C) by 20%, and facilitated negative rhizosphere priming (it slowed SOC mineralization by 5.5%, that is, 46 g CO 2 -C m −2 yr −1 ). Retention of root-derived 13 C in the stable organo-mineral fraction (<53 µm) was also increased (6%, P < 0.05). Through synchrotron-based spectroscopic analysis of bulk soil, fieldaged biochar and microaggregates (<250 µm), we demonstrate that biochar accelerates the formation of microaggregates via organo-mineral interactions, resulting in the stabilization and accumulation of SOC in a rhodic ferralsol.
“…Therefore we believe that Ca ions are reducing the GO-Ca containing samples mainly through epoxy functional group. Indeed, the Ca ion epoxy interaction in oxide nanographene was previously theoretical studied showing the adsorption energies of −147 kcal/mol [78,79], hence making the GO structure more stable.…”
“…Biochar known through studies in the Amazonia Dark Earth, has been evidenced in the literature as a direct contributor in the chemical, physical and biological aspects of the soil (ARCHANJO et al, 2014;LIMA et al 2016). Due to its polycyclic aromatic chemistry, its use in soils has promoted immobilization of inorganic and organic pollutants, increased microbiological activity and greater availability of water and nutrients (LEHMANN et al, 2011).…”
Section: Introductionmentioning
confidence: 99%
“…Due to the release of volatile compounds of the biochar, micro, meso and macropores, respectively, smaller than 2.00 nm, between 2.00 nm -50.00 nm and greater than 50.00 nm originate, which interfere in the increase of their surface area, increasing water storage in their spaces (ARCHANJO et al, 2014). This effect was verified with the use of biochar in a sandy texture plintite soil by Carvalho et al (2014), where they obtained an increase of about 1% of water available to the plants at each T ha -1 of biochar.…”
The objective of this study was to evaluate the influence of biochar saturation doses on the cumulative loss of water in a Yellow Latosol typical of Central Amazonia. The experiment was conducted in a greenhouse of the National Institute of Research of the Amazon -INPA, in Manaus-AM. Biochar was used from the pyrolysis of brown urchins and a secondary forest soil. A completely randomized design with five biochar doses (0, 20, 40, 60 and 80 t ha -1 ) was used with four replicates, each experimental unit consisting of a plastic vessel with 2500 g of soil with biochar. The observed variables were the amount of water required for soil saturation and the cumulative loss of water in seven periods (24 h, 48 h, 72 h, 96 h, 120 h, 144 h and 168 h). The water measurements required for saturation were based on dry soil and, while losses were calculated based on the subtraction of the saturated soil mass and the wet mass of each period. The biochar doses did not significantly influence the amount of water required for saturation of the studied soil. Attenuated water losses were observed with the application of 20 and 40 t ha -1 of biochar. The higher doses of 60 and 80 t ha -1 of biochar promoted the greatest accumulated losses of soil water.
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