Journal
SCIENCE OF THE TOTAL ENVIRONMENT
Volume 563, Issue -, Pages 237-246Publisher
ELSEVIER
DOI: 10.1016/j.scitotenv.2016.03.245
Keywords
Charcoal; Density; Porosity; Imbibition; XPS; Ageing
Categories
Funding
- US NSF [EAR 0911685, 0949337]
- Division Of Earth Sciences
- Directorate For Geosciences [0949337] Funding Source: National Science Foundation
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To best use biochar as a sustainable soil management and carbon (C) sequestration technique, we must understand the effect of environmental exposure on its physical and chemical properties because they likely vary with time. These properties play an important role in biochar's environmental behavior and delivery of ecosystem services. We measured biochar before amendment and four years after amendment to a commercial nectarineorchard at rates of 5, 15 and 30 t ha(-1). We combined two pycnometry techniques to measure skeletal (rho(s)) and envelope (rho(e)) density and to estimate the total pore volume of biochar particles. We also examined imbibition, which can provide information about soil hydraulic conductivity. Finally, we investigated the chemical properties, surface, inner layers atomic composition and C1s bonding state of biochar fragments through X-ray photoelectron spectroscopy (XPS). Ageing increased biochar skeletal density and reduced the water imbibition rate within fragments as a consequence of partial pore clogging. However, porosity and the volume of water stored in particles remained unchanged. Exposure reduced biochar pH, EC, and total C, but enhanced total N, nitrate-N, and ammonium-N. X-ray photoelectron spectroscopy analyses showed an increase of O, Si, N, Na, Al, Ca, Mn, and Fe surface (0-5 nm) atomic composition (at%) and a reduction of C and K in aged particles, confirming the interactions of biochar with soil inorganic and organic phases. Oxidation of aged biochar fragments occurred mainly in the particle surface, and progressively decreased down to 75 nm. Biochar surface chemistry changes included the development of carbonyl and carboxylate functional groups, again mainly on the particle surface. However, changes were noticeable down to 75 nm, while no significant changes were measured in the deepest layer, up to 110 nm. Results show unequivocal shifts in biochar physical and chemical properties/characteristics over short (similar to years) timescales. (c) 2016 Elsevier B.V. All rights reserved.
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