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4D Surface Reconstructions to Study Microscale Structures and Functions in Soil Biogeochemistry.
Ost, Alexander D; Wu, Tianyi; Höschen, Carmen; Mueller, Carsten W; Wirtz, Tom; Audinot, Jean-Nicolas.
Afiliação
  • Ost AD; Advanced Instrumentation for Nano-Analytics (AINA), Materials Research and Technology Department (MRT), Luxembourg Institute of Science and Technology (LIST), 4422 Belvaux, Luxembourg.
  • Wu T; University of Luxembourg, 4365 Esch-sur-Alzette, Luxembourg.
  • Höschen C; Soil Science, TUM School of Life Sciences, Technical University of Munich, 85354 Freising-Weihenstephan, Germany.
  • Mueller CW; Soil Science, TUM School of Life Sciences, Technical University of Munich, 85354 Freising-Weihenstephan, Germany.
  • Wirtz T; Department of Geosciences and Natural Resource Management Geography, University of Copenhagen, 1350 Copenhagen, Denmark.
  • Audinot JN; Advanced Instrumentation for Nano-Analytics (AINA), Materials Research and Technology Department (MRT), Luxembourg Institute of Science and Technology (LIST), 4422 Belvaux, Luxembourg.
Environ Sci Technol ; 55(13): 9384-9393, 2021 07 06.
Article em En | MEDLINE | ID: mdl-34165287
ABSTRACT
The development of high-resolution microscopy and spectroscopy techniques has allowed the analysis of microscopic 3D objects in fields like nanotechnology and life and soil sciences. Soils have the ability to incorporate and store large amounts of organic carbon. To study this organic matter (OM) sequestration, it is essential to analyze its association with soil minerals at the relevant microaggregate scale. This has been previously studied in 2D. However, 3D surface representations would allow a variable angle and magnification analysis, providing detailed insight on their architecture. Here we illustrate a 4D surface reconstruction workflow able to locate preferential sites for OM deposition with respect to microaggregate topography. We used Helium Ion Microscopy to acquire overlapping Secondary Electron (SE) images to reconstruct the soil topography in 3D. Then we used nanoscale Secondary Ion Mass Spectrometry imaging to chemically differentiate between the OM and mineral constituents forming the microaggregates. This image was projected onto the 3D SE model to create a 4D surface reconstruction. Our results show that organo-mineral associations mainly form at medium curvatures while flat and highly curved surfaces are avoided. This method presents an important step forward to survey the 3D physical structure and chemical composition of microscale biogeochemical systems correlatively.
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Texto completo: 1 Base de dados: MEDLINE Assunto principal: Solo / Minerais Idioma: En Ano de publicação: 2021 Tipo de documento: Article

Texto completo: 1 Base de dados: MEDLINE Assunto principal: Solo / Minerais Idioma: En Ano de publicação: 2021 Tipo de documento: Article