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We model filtration of a feed solution, containing both small and large foulant particles, by a membrane filter. The membrane interior is modelled as a network of pores, allowing for the simultaneous adsorption of small particles and sieving of large particles, two fouling mechanisms typically observed during the early stages of commercial filtration applications. In our model, first-principles continuum partial differential equations model transport of the small particles and adsorptive fouling in each pore, while sieving particles are assumed to follow a discrete Poisson arrival process with a biased random walk through the pore network. Our goals are to understand the relative influences of each fouling mode and highlight the effect of their coupling on the performance of filters with a pore-size gradient (specifically, we consider a banded filter with different pore sizes in each band). Our results suggest that, due to the discrete nature of pore blockage, sieving alters qualitatively the rate of the flux decline. Moreover, the difference between sieving-particle sizes and the initial pore size (radius) in each band plays a crucial role in indicating the onset and disappearance of sieving–adsorption competition. Lastly, we demonstrate a phase transition in the filter lifetime as the arrival frequency of sieving particles increases.
The paper discusses the possibility of dust particles containing living bacteria ejected from Earth reaching Europa and landing on its surface. It is shown that, taking certain factors into account, over a period of 30 − 80 Myr (the estimated age of Europa’s ocean), Jupiter’s moon would have been impacted by approximately 3 × 1023 to 8 × 1023 particles in total, within which a bacterium could have survived. In the paper, we discuss the possibility of dust grains entering liquid water beneath the surface.
We investigate the oscillation of the large-scale circulation (LSC) in turbulent Rayleigh–Bénard convection by combining laboratory experiments and numerical simulations. The experiments are conducted mainly in a laterally confined rectangular cell, and the flow fields are measured by particle image velocimetry in the vertical mid-plane. It is found that the velocity field exhibits not only the commonly observed oscillation frequencies $(f\tau _o=1,2)$ but also higher-order harmonic frequencies $(f\tau _o\gt 2)$, where $\tau _o$ is the turnover time of the LSC. Spectral proper orthogonal decomposition (SPOD) reveals that the coherent structures underlying these frequencies display an approximate azimuthal periodicity when viewed in polar coordinates. These structures can be interpreted as travelling waves, consistent with the advected-oscillation picture proposed by Brown & Ahlers (2009 J. Fluid Mech., vol. 638, pp. 383–400). A data-driven resolvent analysis, used here as an effective input–output model inferred from the experimental data, yields response modes and gain peaks that are consistent with the SPOD results, and support the interpretation that the dominant oscillations are selected through linear amplification about the mean circulation. This perspective is further supported by direct numerical simulation in a rectangular cell and by velocity measurements in a cylindrical cell. These findings provide an additional viewpoint for understanding the oscillation mechanism of the LSC in turbulent Rayleigh–Bénard convection.
Obtaining accurate field statistics continues to be one of the major challenges in turbulence theory and modelling. From the various existing modelling approaches, multifractal models have been successful in capturing intermittency in velocity gradient and increment distributions. Moreover, superstatistical models from non-equilibrium statistical mechanics have shown the capacity to model probability density functions (p.d.f.s) of various statistical turbulent quantities as ensembles of simpler stochastic processes. Here, we present an approach that generates field statistics in the form of a characteristic functional by promoting a model for multifractal increment statistics to an ensemble of Gaussian fields. By carefully designing the correlation function and the corresponding weight of each subensemble, we are able to define a functional that exhibits multifractal two-point inertial-range and dissipation-range statistics, and that blends into realistic large-scale behaviour. Additionally, the method is capable of producing multifractal statistics with any of the widely used singularity spectra. We characterise the fidelity of our approach through comparisons to literature results from direct numerical simulations. Overall, our framework thereby bridges between three different perspectives: superstatistics, multifractals and functional approaches to turbulence.
The Benedictine Abbey in Tyniec is the oldest existing monastery in Poland (11th cent. AD). The historic walls of the Monastery have survived to this day and crown the limestone hill on the Vistula River. The geological structure of the surrounding area is reflected in the composition of the mortars.
In vicinity of Tyniec one may observe outcrops of Upper Jurassic limestones represented by two facies: bedded limestones with cherts and massive limestones. Recently, it was discovered that the monks not only fortified the Tyniec hill but also partly built it up with loess. Additionally, a massive “stepped” stone platform was later built to strengthen the edge of the hill. The mortars radiocarbon dating provides the first attempt to obtain the wide chronology of the extension of Tyniec. For this purpose, the chronologically oldest layers were analyzed.
Sequential dissolution of mortars was applied to separate the carbonates of different origin. The obtained results illustrated the huge influence of mortar components and the local geological structure on the 14C measurements. In addition to the mortar, 14C measurements were also made for charcoal from Tyniec Abbey. Radiocarbon dating was performed on the selected fractions using accelerator mass spectrometry (AMS). Radiocarbon dating results of samples from the oldest part of the stone platform make it possible to associate its construction with the earliest monastery buildings.
Human activity in the Antarctic is supported by a wide network of government agencies, policies, businesses and workers back home. This polar workforce is particularly important in the so-called ‘Antarctic gateway cities’, which foreground their economic and cultural connections with the far south. Rather than focusing just on the Antarctic continent as the place of work, this paper therefore takes a broader approach by turning attention to the people back home that enable Antarctic logistics, modelling, policymaking and public awareness to be executed successfully. The paper outlines a matrix for mapping polar work capacity, with Antarctic roles classified as direct or indirect and as in situ or ex situ. By bringing together stakeholders from a range of Antarctic workplaces (including local and national government, academia, tourism and local business owners and training providers) from Christchurch (New Zealand) in October 2024, a workshop event identified the key challenges facing the Antarctic sector over the coming 5 years and highlighted areas where international collaboration could help to address these challenges into the future. Key suggestions include the implementation of an overarching Antarctic strategy; training and education to improve local talent and pathways; enhanced visibility of existing skillsets; establishing exchange opportunities across the Antarctic gateway cities; and developing Antarctic identities, including through tourism opportunities.
In this paper, we investigate the influences of wall temperature on compressible turbulent boundary layers at free-stream Mach number 6.0 and moderate Reynolds numbers. The findings demonstrate that turbulent statistics, including the logarithmic scaling of Reynolds stresses in the overlap region, the presence of very-large-scale motions in the outer layer, and their superposition on near-wall turbulence, exhibit qualitative invariance across varying wall temperatures. However, the reduced scale separation between near-wall small-scale motions and outer-layer large-scale motions leads to a contraction in the vertical extent of Reynolds stresses adhering to the logarithmic law. Very-large-scale motions are attenuated in viscous units but intensified in global scalings due to the lower free-stream Reynolds number, following approximately the power law. Their superposition effects on near-wall turbulence, when weighted by density, show only weak dependence on wall temperature. Conversely, the modulation of near-wall velocity and temperature fluctuations by very-large-scale motions diminishes with decreasing wall temperature. Through detailed analysis of spanwise spectra in the outer region, a distinct inertial subrange obeying the classical $-5/3$ scaling law is identified, alongside a universal scaling over the dissipative range. These observations suggest that the mechanisms governing energy cascade processes and the associated small-scale turbulent fluctuations remain independent of wall temperature variations.
Field research in the Petites Pyrénées (France) yielded new Late Cretaceous continental microvertebrates, including some of the few known mammals from Europe from this time. They come from the well-dated late Maastrichtian Auzas Marls Formation which has yielded some of the latest European Mesozoic vertebrates. Here, we report new discoveries, including for the first time a co-occurrence of multituberculate and eutherian mammals in the Cretaceous of Western Europe, breaking previously known strong provincialism of Late Cretaceous mammals in Europe. Two new mammals are described. The kogaionid species Hainina cassagnauensis n. sp. is the first multituberculate known from the Late Cretaceous of Western Europe and the earliest record of Hainina. It makes Hainina one of the only known vertebrate genera crossing the K/Pg boundary in Europe. H. cassagnauensis n. sp. is the first described evidence for a mammal dispersal between the Eastern and Western parts of the European Archipelago at the end of the Cretaceous. Mammals from Tricouté also include an upper molar of the new eutherian cf. Azilestes yvettae n. sp. It exhibits an advanced morphology showing affinities to other specialized endemic eutherians from the Cretaceous of Europe such as Valentinella vitrollense and Azilestes ragei. These three European species have a basic zhelestid dental morphology, but their specializations suggest a new, at least subfamilial, European clade. As with other vertebrates from the European Archipelago, the kogaionid multituberculates and the zhelestid eutherians are ancient relict lineages that belong to the «old European faunal core».
The first bifurcation of the flow around a spheroid is analysed using global stability analysis to understand the development of flow asymmetry despite the symmetry of the configuration. The base flow, perturbations, adjoint modes, vorticity fields, structural sensitivity and skin friction lines are analysed to characterise the flow. The study of aspect ratio effects at zero angle of attack establishes that the structure of the asymmetry is the same whether the axisymmetric body is bluff or more streamlined. Stability of the flow field around the 6 : 1 spheroid is then investigated for angles of attack $\alpha \in [0{-}90]^\circ$ as a function of Reynolds number. Comparison of the low angle of attack results with the DARPA SUBOFF experiments of Ashok et al. (J. Fluid Mech., 2015, vol. 774, pp. 416–442) shows that the asymmetry observed in the experiments is similar to the global mode predicted by the stability calculations. It is conjectured that the experimental asymmetry is triggered by the weak cross-stream circulating flow. The leading eigenmode is a stationary asymmetric mode in the angle of attack $\alpha \in [0{-}65]^\circ$ range, while above $\alpha =65^\circ$, the leading mode is an oscillatory shedding mode. The rapid decrease in the critical Reynolds number between cases $\alpha =49.25^\circ$ and $49.5^\circ$ is attributed to coexisting symmetric flow states that have different susceptibilities to asymmetry; there exists a symmetric stationary mode that does not become unstable first, but appears to be the difference between the base flows at the same Reynolds number at the two angles of attack. The change from a stationary to an oscillatory instability between $\alpha =65^\circ$ and $70^\circ$ is linked to the ability/inability of the vortex sheets to roll up and reattach to the body in the former/latter cases, respectively. The difference in the separation patterns and the similarity between the eigenmodes indicate that asymmetry of the flow field is governed by the same mechanism across a wide angle of attack range, regardless of whether the flow is like a bluff body wake, a streamlined body wake or a vortex wake. Previous studies have argued that the asymmetry of vortex pairs emerges either because of a vortex instability or a separation/reattachment related mechanism; since the development of the asymmetry cannot be linked to specific features in the separation pattern in the investigated configurations, our results support the former argument.
Understanding the diverse pathways between science and policy is crucial for assessing the impact of research. In this context, ‘research impact’ refers to the broader societal benefits of scientific research that extend beyond traditional research evaluation metrics. Metrics of academic and scientific excellence, such as h-indexes or bibliometric analyses, often fail to capture the impact of science on policy. To investigate one aspect of how research can influence policy, and therefore probably have impact, this study analysed ice core publications from the Australian Antarctic Program. A dataset of 266 Australian-authored and/or -funded East Antarctic ice core publications was examined, revealing that 123 were cited in 284 international and Australian (domestic) policy and policy-related documents. To analyse the policy influence of the research, key information was categorized into authoring countries, institutions, research themes and the contextual use of publications by the documents. This categorization highlighted the different uses of information and interpretations of ice core publications by separate forums, with some more active compared to passive uses. The ‘Active-Passive’ spectrum developed in this study provides a framework for understanding how research is being used, and it underscores the relevance of ice core science to local Australian governance. The results show that domestic uptake of ice core publications by some Australian states demonstrated more ‘Active’ inclusions in policy to support an area of national interest: water security. The mixed methods piloted in this study can be used to assess scientific publications from national Antarctic programmes with more nuance, thereby offering an improved avenue for measuring research impact.
Future generations, wildlife, and natural resources – collectively referred to as 'the voiceless' in this work – are the most vulnerable and least equipped populations to protect themselves from the impacts of global climate change. In this new edition of Climate Change and the Voiceless, Randall S. Abate provides comprehensive analysis of recent landmark strategic litigation to protect vulnerable communities, significant updates on legislative and judicial developments on rights of nature, and a detailed summary of the most important climate change advisory opinions and their implications for the protection of voiceless communities. As in the original work, he identifies the common vulnerabilities of the voiceless in the Anthropocene era and demonstrates how the law can evolve to protect their interests more effectively. This work should be read by anyone interested in how the law can be employed to mitigate the effects of climate change on those who stand to lose the most.
The optical theory of light scattering by nonspherical particles is fundamental to remote sensing of the atmosphere and ocean, as well as to other areas of computational physics, astrophysics, the biomedical sciences, and electromagnetics. At present, many training programs in light scattering are woefully lacking. This book fills the void in existing research on light scattering and training, particularly in the case of large scattering particles, and provides a solid foundation on which future research can be based, including suggestions for further directions in the field. With the elucidation of the theoretical basis for light scattering (particularly within the framework of the physical-geometric optics method) and the demonstration of practical applications, this book will be invaluable for training future scientists in the discipline of light scattering, as well as for researchers and professionals using remote-sensing techniques to analyze the properties of the atmosphere and oceans, and in the area of biophotonics.
The canonical scenario of two-degree-of-freedom vortex-induced vibration (VIV) of a circular cylinder is re-examined in this study through high-fidelity large-eddy simulations (LES) at a Reynolds number of 10 000. The in-line and cross-flow vibration amplitudes, frequency responses and hydrodynamic coefficients predicted by the present LES match classical experimental results better than previous numerical attempts. In particular, motivated by an inadequate study yet vital importance of the small-amplitude in-line response in offshore engineering design, we present the first numerical evidence for the existence of three in-line response regions. Furthermore, the present in-line response agrees well with the design guideline DNV-RP-F105. After validating the present results against DNV-RP-F105 and published experiments, the detailed LES datasets enable further analysis of new VIV characteristics and physical mechanisms that have not been explored previously. For example, we identify and explain (i) the existence of twin governing frequencies for several VIV branches with partial synchronisation, (ii) decoupled in-line and cross-flow vibrations in the first in-line branch with symmetric vortex-shedding pattern, where an in-line resonance may not induce a cross-flow resonance, (iii) existence of a new elliptic vibration trajectory for a perfectly in-line resonant condition, (iv) gradualness in the 2S ↔ 2T transition of the vortex-shedding pattern and thus a continuous variation in the vibration amplitudes and hydrodynamic coefficients amid this transition and (v) lowest spanwise correlation of vortex shedding in the super-upper and lower branches, which is induced by complex interactions among ≥4 shed vortices over a cylinder vibration period.