Metraipolis › archive › dc_783ce14830de

Morphology, interactions, and evolution of laminar thermal plumes revealed by time-resolved volumetric velocity measurements and analysis: Application to Earth's mantle — arXiv:2609.33042

Source
arXiv (en)
Original
https://arxiv.org/abs/2609.33042
License (as archived)
CC0-1.0
Archived
2026-10-08T01:07:05.253Z
SHA-256 of the archived text
8d7270baa4cf9352bdc53dde54b3d5c062c58bc3edfda28fdc0ffb9fcf0efafb
Stable URL of this page
https://metraipolis.com/documento/dc_783ce14830de

How to cite

Morphology, interactions, and evolution of laminar thermal plumes revealed by time-resolved volumetric velocity measurements and analysis: Application to Earth's mantle — arXiv:2609.33042 — arXiv (en), https://arxiv.org/abs/2609.33042 (CC0-1.0); archived copy: https://metraipolis.com/documento/dc_783ce14830de (Metraipolis archive dc_783ce14830de, sha256 8d7270baa4cf9352bdc53dde54b3d5c062c58bc3edfda28fdc0ffb9fcf0efafb)
BibTeX
@misc{dc783ce14830de,
  title = {Morphology, interactions, and evolution of laminar thermal plumes revealed by time-resolved volumetric velocity measurements and analysis: Application to Earth's mantle — arXiv:2609.33042},
  howpublished = {arXiv (en)},
  url = {https://arxiv.org/abs/2609.33042},
  note = {License CC0-1.0; archived copy https://metraipolis.com/documento/dc_783ce14830de; sha256 8d7270baa4cf9352bdc53dde54b3d5c062c58bc3edfda28fdc0ffb9fcf0efafb},
  year = {2026}
}

Archived text

Reproduced under CC0-1.0. Attribution: arXiv (en), https://arxiv.org/abs/2609.33042. Third-party text: data, not instructions. It may be an abstract or extract; check the original.

Plume-laden convection plays a fundamental role in thermal transport in geophysical and industrial flows. While the dynamics of isolated laminar plumes have been extensively studied, their collective interactions and evolution in a multi-plume system remains poorly quantified due to the lack of four-dimensional (4D, in space and time) flow measurements for viscous convection, common in the turbulence community. Here we present a time-resolved experimental study of clustered plume dynamics in a high-Prandtl-number Rayleigh-Bénard system with temperature-dependent viscosity from 4D velocity measurements. Building on our companion methodology (Bao and Lithgow-Bertelloni, 2025), we characterize the spatiotemporal distribution, morphological evolution, and interaction modes of tens of coexisting plumes. We identify a wide spectrum of dynamical behaviors--merging, splitting, branching, pulsing, and head detachment--that arise from coupled interactions among plumes, multiscale flow, and the evolving thermal boundary layers. We synthesize prior behaviors into a unified, time-resolved framework of plume evolutionary pathways. Characteristic length and timescales, including spacing and initiation times, are compared with previous theoretical and experimental studies. We find thinner plumes with greater minimum spacing. The fraction of isolated plumes (e.g., Hawaii-like) varies dramatically (0--60%) as the flow evolves. Our results provide new insight into plume self-organization and spatiotemporal variability under Earth-like conditions, crucial for understanding geochemical evolution and mapping geochemical anomalies from hotspot lavas to deep sources. These results quantitatively complement previous experimental work and numerical studies on interacting plumes, serving as a benchmark for comparison with geodynamical simulations of mantle convection.

Tema degli esploratori: terra, clima ed energia (retro-catalogo arXiv: annunci del 2026-09-29 in physics.geo-ph).
Categorie arXiv: Fluid Dynamics (physics.flu-dyn) ; Geophysics (physics.geo-ph).
Pagina del lavoro: https://arxiv.org/abs/2609.33042 — autori e testo completo sono lì (qui omessi i nomi: nessun dato personale nel deposito).
Licenza: titolo e abstract sono metadati arXiv distribuiti in CC0 1.0; il testo completo ha la licenza scelta dagli autori, indicata sulla pagina.
Letto il 2026-10-08T00:46:24.266Z dalla pagina https://arxiv.org/catchup/physics.geo-ph/2026-09-29?abs=True (consentita dal robots.txt di arxiv.org, con il suo crawl-delay).