arXiv subjects

Ricardo Ivan Ferreira Trindade

Publications and source records attributed to Ricardo Ivan Ferreira Trindade.

3 recordsLinked to original sources

arXiv2024

Coupling nanoscopic tomography and micromagnetic modelling to assess the stability of geomagnetic recorders

The recording of planetary magnetic fields is often attributed to uniformly-magnetised nanoscopic iron oxides, called single-domain (SD). Yet, the main magnetic constituents of rocks are more complex, non-uniformly magnetised grains in single or multi-vortex states. We know little about their behaviour due to limitations in defining their precise shape and internal magnetic structure. We propose a novel approach combining non-destructive synchrotron-based ptychographic nanotomography with micromagnetic modelling to explore the magnetic stability of remanence-bearing minerals. Applied to a microscopic rock sample, we identified hundreds of nanoscopic grains of magnetite/maghemite with diverse morphologies. For some grains, shape irregularities near the transition from SD to the single-vortex state allow for multiple domain states, some unstable and unable to record the field for significant periods. Additionally, some other grains exhibit temperature-dependent occupancy probabilities, potentially hampering experiments to recover the intensity of past magnetic fields.

physics.geo-ph↗

arXiv2020

Geomagnetic reversals at the edge of regularity

Geomagnetic field reversals remain as one of the most intriguing problems in geophysics and are regarded as chaotic processes resulting from a dynamo mechanism. In this article, we use the polarity scale data set for the last 170 Myr from the ocean's floor to provide robust evidence for an inverse relationship between the complexity of sequences of consecutive polarity intervals and the respective reversal rate. In particular the variability of sequences of polarity intervals reaches a minimum in the mid-Jurassic when a maximum reversal rate is found. This raises the possibility of epochs of high regularity in the reversal process geodynamo. To shed light on this process, We investigate the transition from regular to chaotic regime in a minimal model for geomagnetic reversals. We show that even in a chaotic regime, near to the transition the system retains the signature of regular behavior. We suggest that geomagnetic reversals have switched between different degrees of irregularity, with a dominant periodicity around 70 kyrs that results from a "ghost" limit cycle.

physics.geo-ph↗

arXiv2019

Evidence for crisis-induced intermittency during geomagnetic superchron transitions

The geomagnetic field's dipole undergoes polarity reversals in irregular time intervals. Particularly long periods (of the order of $10^7$yrs) without reversals, named superchrons, have occurred at least three times in history. We provide observational evidence for high non-Gaussianity in the vicinity of a transition to and from a geomagnetic superchron, consisting of a sharp increase in high-order moments (skewness and kurtosis) of the dipole's distribution. Such increase in the moments is a universal feature of crisis-induced intermittency in low-dimensional dynamical systems undergoing global bifurcations. This suggests temporal variation of the underlying parameters of the physical system. Through a low dimensional system that models the geomagnetic reversals we show that the increase in the high-order moments during transitions to geomagnetic superchrons is caused by the progressive destruction of global periodic orbits exhibiting both polarities as the system approaches a merging bifurcation. We argue that the non-gaussianity in this system is caused by the redistribution of the attractor around local cycles as global ones are destroyed.

physics.geo-ph↗