Details
Original language | English |
---|---|
Pages (from-to) | 2747-2758 |
Number of pages | 12 |
Journal | Environmental science: Nano |
Volume | 7 |
Issue number | 9 |
Publication status | Published - 31 Jul 2020 |
Abstract
The emerging consensus on organic matter (OM) cycling in soil and sediment proposes that a continuum of biological and geochemical processes in the micro-environment controls the fate of OM. However, spatio-temporal observation of the biogeochemical nature and behaviour of OM at the soil-water interfaces (SWIs) is impeded by the heterogonous and opaque nature of their microenvironment. Herein, we used a novel SoilChip method (soil microarrays incubated with a predefined solution) to continuously mimic and trace the OM biogeochemistry at SWIs for 21 days. Combining X-ray photoelectron spectroscopy and ion sputtering on SoilChips, we provided the first direct evidence that a nanoscale organic film with a distinct composition and thickness gradually formed at the SWI within 21 days of cultivation. Although the OM coating on the SWI quickly reached equilibrium within 4 days, the formation of thicker mineral-organic association (MOA, 20-130 nm) and microbial biomass (>130 nm) continued, partially at the cost of the thin MOA (<20 nm). Consistent with the thickening SWI, the bioavailability of nutrients (dissolved organic C and ammonium) decreased gradually over 21 days, which restrained the microbial activities. Collectively, thickening SWIs act as a biogeochemical gate to regulate the bioavailability of specific organic compounds and determine their preservation or microbial mineralization. Further, thickening SWIs in thez-axis direction provide direct structural insight to increase carbon sequestration in soil and sediment.
ASJC Scopus subject areas
- Materials Science(all)
- Materials Science (miscellaneous)
- Environmental Science(all)
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In: Environmental science: Nano, Vol. 7, No. 9, 31.07.2020, p. 2747-2758.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - Direct evidence for thickening nanoscale organic films at soil biogeochemical interfaces and its relevance to organic matter preservation
AU - Huang, Xizhi
AU - Li, Yiwei
AU - Guggenberger, Georg
AU - Kuzyakov, Yakov
AU - Liu, Bi Feng
AU - Wu, Jinshui
N1 - Funding information: The authors gratefully acknowledge financial support from the National Natural Science Foundation of China (Grant number 41090283; Grant number 41430860; Grant number 41807051); Open funding from Key Laboratory of Agro-ecological Processes in subtropical region, Institute of Subtropical Agro-ecology, the Chinese Academy of Sciences (Grant number ISA2018301); China Postdoctoral Fund (Grant number 2019M662635). The publication was also supported by the Government Program of Competitive Growth of Kazan Federal University and the “RUDN University program 5-100”.
PY - 2020/7/31
Y1 - 2020/7/31
N2 - The emerging consensus on organic matter (OM) cycling in soil and sediment proposes that a continuum of biological and geochemical processes in the micro-environment controls the fate of OM. However, spatio-temporal observation of the biogeochemical nature and behaviour of OM at the soil-water interfaces (SWIs) is impeded by the heterogonous and opaque nature of their microenvironment. Herein, we used a novel SoilChip method (soil microarrays incubated with a predefined solution) to continuously mimic and trace the OM biogeochemistry at SWIs for 21 days. Combining X-ray photoelectron spectroscopy and ion sputtering on SoilChips, we provided the first direct evidence that a nanoscale organic film with a distinct composition and thickness gradually formed at the SWI within 21 days of cultivation. Although the OM coating on the SWI quickly reached equilibrium within 4 days, the formation of thicker mineral-organic association (MOA, 20-130 nm) and microbial biomass (>130 nm) continued, partially at the cost of the thin MOA (<20 nm). Consistent with the thickening SWI, the bioavailability of nutrients (dissolved organic C and ammonium) decreased gradually over 21 days, which restrained the microbial activities. Collectively, thickening SWIs act as a biogeochemical gate to regulate the bioavailability of specific organic compounds and determine their preservation or microbial mineralization. Further, thickening SWIs in thez-axis direction provide direct structural insight to increase carbon sequestration in soil and sediment.
AB - The emerging consensus on organic matter (OM) cycling in soil and sediment proposes that a continuum of biological and geochemical processes in the micro-environment controls the fate of OM. However, spatio-temporal observation of the biogeochemical nature and behaviour of OM at the soil-water interfaces (SWIs) is impeded by the heterogonous and opaque nature of their microenvironment. Herein, we used a novel SoilChip method (soil microarrays incubated with a predefined solution) to continuously mimic and trace the OM biogeochemistry at SWIs for 21 days. Combining X-ray photoelectron spectroscopy and ion sputtering on SoilChips, we provided the first direct evidence that a nanoscale organic film with a distinct composition and thickness gradually formed at the SWI within 21 days of cultivation. Although the OM coating on the SWI quickly reached equilibrium within 4 days, the formation of thicker mineral-organic association (MOA, 20-130 nm) and microbial biomass (>130 nm) continued, partially at the cost of the thin MOA (<20 nm). Consistent with the thickening SWI, the bioavailability of nutrients (dissolved organic C and ammonium) decreased gradually over 21 days, which restrained the microbial activities. Collectively, thickening SWIs act as a biogeochemical gate to regulate the bioavailability of specific organic compounds and determine their preservation or microbial mineralization. Further, thickening SWIs in thez-axis direction provide direct structural insight to increase carbon sequestration in soil and sediment.
UR - http://www.scopus.com/inward/record.url?scp=85091867626&partnerID=8YFLogxK
U2 - 10.1039/d0en00489h
DO - 10.1039/d0en00489h
M3 - Article
AN - SCOPUS:85091867626
VL - 7
SP - 2747
EP - 2758
JO - Environmental science: Nano
JF - Environmental science: Nano
SN - 2051-8153
IS - 9
ER -