Characterizing sedimentary processes in abandoned channel using compositional data analysis and wavelet transform

Grain size distribution (GSD) is essential for characterizing the deposition process. However, it is necessary to consider its compositional constraint to comprehend the statistical distribution of size fractions within the sediments. Compositional data analysis (CoDA) and wavelet transform (WT) rep...

Teljes leírás

Elmentve itt :
Bibliográfiai részletek
Szerzők: Eltijani Abdelrhim
Molnár Dávid
Geiger János
Dokumentumtípus: Cikk
Megjelent: 2023
Sorozat:GEM - INTERNATIONAL JOURNAL ON GEOMATHEMATICS 14 No. 1
Tárgyszavak:
doi:10.1007/s13137-023-00223-y

mtmt:33992807
Online Access:http://publicatio.bibl.u-szeged.hu/29334
Leíró adatok
Tartalmi kivonat:Grain size distribution (GSD) is essential for characterizing the deposition process. However, it is necessary to consider its compositional constraint to comprehend the statistical distribution of size fractions within the sediments. Compositional data analysis (CoDA) and wavelet transform (WT) represent alternative methods beyond traditional approaches, e.g., probability density function (PDF). This paper introduces a quantitative approach for characterizing Quaternary depositional and environmental changes using abandoned channel infill sediments. The proposed approach integrates CoDA and WT to thoroughly comprehend the depositional patterns observed in abandoned channels and the underlying environmental variability. The depositional model constructed based on CoDA showed coarsening-upward sequences, suggesting a periodic connection between the main channel and the oxbow lake. Three scales of cycles consistent with the depositional model constructed using CoDA were identified based on WT: small, medium, and large-scale cycles of processes. The large-scale cycles indicate the main depositional events, while the medium and small scale reflects the variation within and during deposition. CoDA and WT demonstrate excellent potential in characterizing the GSD and interpreting oxbow lakes' deposition and sedimentation processes.
Terjedelem/Fizikai jellemzők:16
ISSN:1869-2672