Direct evidence for thickening nanoscale organic films at soil biogeochemical interfaces and its relevance to organic matter preservation

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Autoren

Externe Organisationen

  • Huazhong University of Science and Technology
  • Chinese Academy of Sciences (CAS)
  • Massachusetts Institute of Technology (MIT)
  • Kazan Volga Region Federal University
  • Peoples' Friendship University of Russia (RUDN)
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Details

OriginalspracheEnglisch
Seiten (von - bis)2747-2758
Seitenumfang12
FachzeitschriftEnvironmental science: Nano
Jahrgang7
Ausgabenummer9
PublikationsstatusVeröffentlicht - 31 Juli 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.

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Direct evidence for thickening nanoscale organic films at soil biogeochemical interfaces and its relevance to organic matter preservation. / Huang, Xizhi; Li, Yiwei; Guggenberger, Georg et al.
in: Environmental science: Nano, Jahrgang 7, Nr. 9, 31.07.2020, S. 2747-2758.

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

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title = "Direct evidence for thickening nanoscale organic films at soil biogeochemical interfaces and its relevance to organic matter preservation",
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.",
author = "Xizhi Huang and Yiwei Li and Georg Guggenberger and Yakov Kuzyakov and Liu, {Bi Feng} and Jinshui Wu",
note = "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”.",
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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.

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U2 - 10.1039/d0en00489h

DO - 10.1039/d0en00489h

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JO - Environmental science: Nano

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SN - 2051-8153

IS - 9

ER -

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