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Microstructural Kinetics Group

Department of Materials Science & Metallurgy
 

Fri 01 Nov 16:00: TBA

School of Physical Sciences - Tue, 23/04/2024 - 12:44
TBA

Abstract not available

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Wed 22 May 16:00: TBA

School of Physical Sciences - Tue, 23/04/2024 - 11:40
TBA

TBA

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Mon 20 May 15:00: Jet dynamics in topographically-forced shallow-water planetary atmospheres ADIW03 - Climate Applications of Layering

School of Physical Sciences - Tue, 23/04/2024 - 11:30
Jet dynamics in topographically-forced shallow-water planetary atmospheres

This talk examines the emergence of jets and their long-time dynamics in global spherical rotating shallow-water flows.  Departing from many past studies, we apply space and time-varying (time-correlated) topographic-like forcing exclusively, and weakly damp thermally.  Results are presented using Contour Advection, a numerical approach designed to have extremely weak numerical damping, and thus suitable for investigating long-time dynamics.  The response to topographic forcing differs significantly from previously-considered vorticity forcing, with a much larger role played by divergent motions (imbalance).  Like in previous studies, well-defined quasi-zonal jets emerge, but these jets can drift meridionally, which appears to be an effect induced by the divergent motions. Authors: David Dritschel, Richard Scott & Mahdi Jalali  

ADIW03 - Climate Applications of Layering

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Mon 29 Apr 14:00: Can a computer judge interestingness? (NOTE UNUSUAL DAY/TIME)

School of Physical Sciences - Tue, 23/04/2024 - 10:16
Can a computer judge interestingness?

Mathematics is made up of provable interesting statements about numbers, geometry and abstract structures. While proof can be precisely defined, interestingness remains mysterious, a matter of intuition. In this talk we discuss ways to implement interestingness on a computer, both in symbolic and formal terms, and using state of the art AI.

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Fri 26 Apr 13:35: Privacy with Synthetic Data: Applications and Developments OFBW65 - Connecting Heavy Tails and Differential Privacy in Machine Learning

School of Physical Sciences - Tue, 23/04/2024 - 09:30
Privacy with Synthetic Data: Applications and Developments

OFBW65 - Connecting Heavy Tails and Differential Privacy in Machine Learning

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Fri 31 May 16:00: Title to be confirmed

School of Physical Sciences - Tue, 23/04/2024 - 09:14
Title to be confirmed

Abstract not available

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Fri 24 May 16:00: Title to be confirmed

School of Physical Sciences - Tue, 23/04/2024 - 09:12
Title to be confirmed

Abstract not available

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Fri 03 May 16:00: Title to be confirmed

School of Physical Sciences - Tue, 23/04/2024 - 09:10
Title to be confirmed

Abstract not available

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Fri 17 May 16:00: PhD students' talks

School of Physical Sciences - Tue, 23/04/2024 - 09:00
PhD students' talks

Abstract not available

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Thu 02 May 14:00: The entanglement membrane in exactly solvable lattice models

School of Physical Sciences - Tue, 23/04/2024 - 08:36
The entanglement membrane in exactly solvable lattice models

Entanglement membrane theory is an effective coarse-grained description of entanglement dynamics and operator growth in chaotic quantum many-body systems. The fundamental quantity characterizing the membrane is the entanglement line tension. However, determining the entanglement line tension for microscopic models is in general exponentially difficult. We compute the entanglement line tension in a recently introduced class of exactly solvable yet chaotic unitary circuits, so-called generalized dual-unitary circuits, obtaining a non-trivial form that gives rise to a hierarchy of velocity scales with $v_E DU2 circuits, the entanglement line tension can be computed entirely, while for the higher levels the solvability is reduced to certain regions in spacetime. This partial solvability nevertheless constrains the dynamics inside the inaccessible region. Finally, we discuss a general framework of constructing lattice models with solvable dynamics. Our results shed light on entanglement membrane theory in microscopic Floquet lattice models and enable us to perform non-trivial checks on the validity of its predictions by comparison to exact and numerical calculations. Moreover, they demonstrate that generalized dual-unitary circuits display a more generic form of information dynamics than dual-unitary circuits.

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Fri 10 May 16:00: Geometry and learning of dynamical systems

School of Physical Sciences - Tue, 23/04/2024 - 08:32
Geometry and learning of dynamical systems

Abstract not available

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Fri 14 Jun 16:00: Entrainment across a turbulent/turbulent interface

School of Physical Sciences - Tue, 23/04/2024 - 08:29
Entrainment across a turbulent/turbulent interface

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Mon 29 Apr 14:00: Title to be confirmed (NOTE UNUSUAL DAY/TIME)

School of Physical Sciences - Tue, 23/04/2024 - 00:04
Title to be confirmed

Abstract not available

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Wed 01 May 16:00: Chirality and Topology

School of Physical Sciences - Mon, 22/04/2024 - 19:57
Chirality and Topology

Chirality is a very active field of research in organic chemistry, closely linked to the concept of symmetry. Topology, a well-established concept in mathematics, has nowadays become essential to describe condensed matter [1,2]. At its core are chiral electron states on the bulk, surfaces and edges of the condensed matter systems, in which spin and momentum of the electrons are locked parallel or anti-parallel to each other. Magnetic and non-magnetic Weyl semimetals, for example, exhibit chiral bulk states that have enabled the realization of predictions from high energy and astrophysics involving the chiral quantum number, such as the chiral anomaly, the mixed axial-gravitational anomaly and axions [3-5]. Chiral topological crystals exhibit excellent chiral surface states [6,7] and different orbital angular momentum for the enantiomers, which can be advantageous in catalysis. The potential for connecting chirality as a quantum number to other chiral phenomena across different areas of science, including the asymmetry of matter and antimatter and the homochirality of life, brings topological materials to the fore [8].

References:

[1] M. G. Vergniory, B. J. Wieder, L. Elcoro, S. S. P. Parkin, C. Felser, B. A. Bernevig, N. Regnault, Science 2022, 376, 6595.

[2] P. Narang, C. A. C. Gracia and C. Felser, Nat. Mater. 2021, 20, 293.

[3] J. Gooth et al., Nature 2017, 547, 324.

[4] J. Gooth et al., Nature 2019, 575, 315.

[5] D. M. Nenno, et al., Nat Rev Phys 2022, 2, 682.

[6] B. Bradlyn, J. Cano, Z. Wang, M. G. Vergniory, C. Felser, R. J. Cava and B. A. Bernevig, Science 2016, 353, aaf5037.

[7] N. B. M Schröter, et al., Science 2020, 369, 179.

[8] C. Felser, J. Gooth, preprint arXiv:2205.05809.

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Fri 26 Apr 13:00: Uniqueness of extremal black holes in de Sitter

School of Physical Sciences - Mon, 22/04/2024 - 17:49
Uniqueness of extremal black holes in de Sitter

Uniqueness theorems for black holes with a cosmological constant are only known in a few limited cases. In my talk I present a recent uniqueness theorem for the extremal Schwarzschild-de Sitter black hole within the class of analytic vacuum spacetimes with a positive cosmological constant containing a static extremal Killing horizon. The proof is based on establishing the uniqueness of transverse deformations to the near-horizon geometry at each order in the transverse parameter. I also present a generalisation to charged extremal black holes in de Sitter and discuss the analogous problem in the case of negative cosmological constant. The talk is based on 2309.04238 [gr-qc] and 2403.08467 [gr-qc].

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Mon 20 May 12:00: Arctic Transitions: The Beaufort Gyre’s Diffusive Staircase ADIW03 - Climate Applications of Layering

School of Physical Sciences - Mon, 22/04/2024 - 17:30
Arctic Transitions: The Beaufort Gyre’s Diffusive Staircase

Diffusive staircases in the Arctic Ocean are structures that consist of mixed layers separated by thin interfaces in temperature and salinity. These staircases are prevalent in the Arctic and can occur when warm and salty water underlies cooler, fresher water. In this talk, I will focus on staircases in a particular region of the western Arctic Ocean, known as the Beaufort Gyre. Staircase layer thicknesses exhibit distinct differences across the Gyre, with a jump from thinner layers in the western Gyre to thicker layers on the eastern side. We will discuss how this sharp transition may be linked to a warm water influx into the Gyre and subsequent propagation across the region. The results may be of interest for interpreting how staircases may change under Arctic warming. 

ADIW03 - Climate Applications of Layering

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Thu 23 May 15:00: How Dirty Icebergs Melt ADIW03 - Climate Applications of Layering

School of Physical Sciences - Mon, 22/04/2024 - 16:30
How Dirty Icebergs Melt

ADIW03 - Climate Applications of Layering

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