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Biologically inspired aero/hydrodynamics attracts considerable interest because of promising efficiency and manoeuvring capabilities. Yet, the influence that external perturbations, typical of realistic environments, can have over the flow physics and aerodynamic performance remains a scarcely investigated issue. In this work, we focus on the impact of free stream turbulence (FST) on the aerodynamics of a flapping wing with a prescribed (heaving and pitching) motion at a chord-based Reynolds number of 1000. The problem is tackled by means of direct numerical simulations using an immersed boundary method and a synthetic turbulence generator. The effect of two key parameters, i.e. the turbulence intensity and integral length scale of FST, is described by characterising the phase- and spanwise-averaged flows and aerodynamic coefficients. In particular, we show how FST effectively enhances the dissipation of the vortices generated by the flapping wing once they are sufficiently downstream of the leading edge. The net (i.e. time-averaged) thrust is found to be marginally sensitive to the presence of FST, whereas the characteristic aerodynamic fluctuations appear to scale linearly with the turbulence intensity and sublinearly with the integral length scale. Moreover, we reveal a simple mechanism where FST triggers the leading-edge vortex breakup, which in turns provides the main source of aerodynamic disturbances experienced by the wing. Finally, we show how the frequency spectra of the aerodynamic fluctuations are governed by the characteristic time scales involved in the problem.
Interactions between shock waves and gas bubbles in a liquid can lead to bubble collapse and high-speed liquid jet formation, relevant to biomedical applications such as shock wave lithotripsy and targeted drug delivery. This study reveals a complex interplay between acceleration-induced instabilities that drive jet formation and radial accelerations causing overall bubble collapse under shock wave pressure. Using high-speed synchrotron X-ray phase contrast imaging, the dynamics of micrometre-sized air bubbles interacting with laser-induced underwater shock waves are visualised. These images offer full optical access to phase discontinuities along the X-ray path, including jet formation, its propagation inside the bubble, and penetration through the distal side. Jet formation from laser-induced shock waves is suggested to be an acceleration-driven process. A model predicting jet speed based on the perturbation growth rate of a single-mode Richtmyer–Meshkov instability shows good agreement with experimental data, despite uncertainties in the jet-driving mechanisms. The jet initially follows a linear growth phase, transitioning into a nonlinear regime as it evolves. To capture this transition, a heuristic model bridging the linear and nonlinear growth phases is introduced, also approximating jet shape as a single-mode instability, again matching experimental observations. Upon piercing the distal bubble surface, jets can entrain gas and form a toroidal secondary bubble. Linear scaling laws are identified for the pinch-off time and volume of the ejected bubble relative to the jet’s Weber number, characterising the balance of inertia and surface tension. At low speeds, jets destabilise due to capillary effects, resulting in ligament pinch-off.
We present the mineralogy and whole rock geochemistry of the lamproites dykes from the Kawardha area of the Western Bastar Craton. These dykes are characterized by phenocrysts and microphenocrysts of olivine, phlogopite, ulvo-spinel, Cr-spinel and magnetite within the chlorite and carbonate-rich groundmass with rutile and apatite as accessory phases. Mineral chemistry indicates that the lamproites in Kawardha are similar to olivine-phlogopite lamproites and are geochemically similar to other lamproites in the eastern Bastar craton. The Kawardha lamproites are characterized by higher concentrations of MgO (12–20.29 wt%), V (193–502 ppm), Ni (206–823 ppm), Cr (146–1130 ppm), Nb (101–260 ppm), Zr (301–635 ppm), Hf (6–13 ppm) and LREEs. Positive Nb-Ta anomalies and Th, Hf and Zr variations are comparable to other intra-cratonic rift-related lamproites. The geochemical variations (such as REE, HFSE and LILE) are consistent with an asthenospheric mantle source similar to the other lamproites in Bastar craton. Trace element modelling implies a low-degree partial melting (0.1–2%) of phlogopite-bearing garnet-lherzolite and/or phlogopite-bearing spinel-lherzolite mantle source. The widespread Proterozoic rifting events in the Bastar craton likely led to the melting and upwelling of the asthenospheric mantle and which further interacted with the metasomatized lithospheric mantle to form the parental melts of the lamproite dykes of the Kawardha area.
This paper theoretically introduces a new architecture for pumping leaky-dielectric fluids. For two such fluids layered in a channel, the mechanism utilises Maxwell stresses on fluid interfaces (referred to as menisci) induced by a periodic array of electrode pairs inserted between the two fluids and separated by the menisci. The electrode pairs are asymmetrically spaced and held at different potentials, generating an electric field with variation along the menisci. To induce surface charge accumulation, an electric field (and thus current flow) is also imposed in the direction normal to the menisci, using flat upper and lower electrodes, one in each fluid. The existence of both normal and tangential electric fields gives rise to Maxwell stresses on each meniscus, driving the flow in opposite directions on adjacent menisci. If the two menisci are the same length, then a vortex array is generated that results in no net flow; however, if the spacing is asymmetric, then the longer meniscus dominates, causing a net pumping in one direction. The pumping direction can be controlled by the (four) potentials of the electrodes, and the electrical properties of the two fluids. In the analysis, an asymptotic approximation is made that the interfacial electrode period is small compared to the fluid layer thicknesses, which reduces the analytical difficulty to an inner region close to the menisci. Closed-form solutions are presented for the potentials, velocity field and resulting pumping speed, for which maximum values are estimated, with reference to the electrical power required and feasibility.
We present a theoretical approach that derives the wavenumber $k^{-1}$ spectral scaling in turbulent velocity spectra using random field theory without assuming specific eddy correlation forms or Kolmogorov’s inertial-range scaling. We argue for the mechanism by Nikora (1999 Phys. Rev. Lett.83 (4), 734), modelling turbulence as a superposition of eddy clusters with eddy numbers inversely proportional to their characteristic length scale. Statistical mixing of integral scales within these clusters naturally yields the $k^{-1}$ scaling as an intermediate asymptotic regime. Building on the spectrum modelling introduced in Jetti et al. (2025b Z. Angew. Math. Physik.74 (3), 123), we develop and apply an integral formulation of the general velocity spectrum that reproduces the $k^{-1}$ regime observed in field spectra, thereby bridging theoretical derivation and empirical observations. The model is validated using wind data at a coastal site, and tidal data in a riverine environment where the –1 scaling persists beyond the surface layer logarithmic region. The results confirm the robustness of the model at various flow conditions, offering new insights into the spectral energy distribution in geophysical and engineering flows.
Crystallisation of the earliest minerals typically affects the composition of minerals subsequently formed, being controlled by their abundance and the compatibility/incompatibility of the relevant elements. Here we have investigated the effects of early tourmaline crystallisation on the formation of primary Be minerals (beryl and helvine–danalite) in metaluminous intragranitic NYF pegmatites of the Třebíč Pluton, Czech Republic. Tourmaline occurs in different textural-paragenetic types: (a) coarse- to medium-grained aggregates; (b) graphic (Tur+Qz) intergrowths; (c) fine-grained nodules (Tur+Qz+Pl+Kfs); (d) tourmaline pseudomorphs after biotite; (e) interstitial tourmaline; and (f) replacing helvine–danalite. The compositions of primary tourmalines (a), (b) and (c) vary from Ca- and Ti-rich Fe-dravite to Mg-poor schorl and dutrowite, and to magnesio-dutrowite, showing low to moderate Al (5.1–6.1 apfu), variable Mg (0.1–1.9 apfu) and Fe (1.3–2.2 apfu), low Mn (≤0.1 apfu), low to moderate Ca (0.1–0.4 apfu), and high Ti (≤0.55 apfu). Type (f) secondary tourmaline is poor in Mg, Ca and Ti (all ≤0.07 apfu), but rich in Na (0.64–0.81 apfu), Fe (0.68–2.17 apfu), Mn (0.31–0.80 apfu), Al (6.57–7.61 apfu), and F (0.37–0.58 apfu). Two distinct assemblages of early-formed Be minerals were recognised: the assemblage beryl ± phenakite occurs in pegmatites with rare interstitial tourmaline (e), whereas the assemblage helvine–danalite ± phenakite is characteristic of pegmatites with abundant early tourmaline (a). The assemblages of primary Be minerals in the individual pegmatites reflect how crystallisation and abundance of early tourmaline control the origin and composition of successive primary Be minerals. The crystallisation of abundant early-formed tourmaline depletes the residual melt of elements that are incorporated preferentially into the tourmaline structure (Al, Mg, Zn), whereas incompatible Mn accumulates, leading to the formation of Mn-rich helvine–danalite. In contrast, beryl only occurs in pegmatites where early-formed tourmaline is absent. The early crystallisation of tourmaline might thus affect the species and composition of later crystallising minerals.
Interactions between hyperelastic bio-membranes and fluid play a crucial role in the flight (or swimming) motion of many creatures, such as bats, flying squirrels and lemurs. Bio-membranes are characterised by high stretchability and micro-bending stiffness, leading to unique fluid–solid coupling properties (Mathai et al., 2023, Phys. Rev. Lett., vol. 131, 114003). This study presents a high-fidelity numerical exploration of the hyperelastic characteristics of a pitching foil inspired by bio-membranes in fluid within a low Reynolds number regime. The focus is on the effect of foil compliance on its self-propulsion performance, mimicking natural propulsion mechanisms, with the foil free to move in the horizontal direction. We find that with certain compliance, the foil may experience a velocity crisis, meaning that its propulsive capability is completely lost. This phenomenon is caused by the loss of beat speed when the foil’s passive deformation is out of phase with the pitching motion. By contrast, the two motions can be in phase at proper compliance, leading to an increased beat speed. This will significantly enhance propulsive velocity up to $33\,\%$ compared with the rigid case. The results demonstrate the feasibility of compliance tuning to circumvent the velocity crisis and improve the propulsive speed, which are helpful in the design of micro aerial robots using biomimetic membranes.
This Element supports Gwich'in, Iñupiat, and all Alaska Natives' collective continuance and reparative justice from the perspective of a settler in the traditional territories of lower Tanana Dene Peoples. It stands with Alaska Natives' recovering and safe-keeping: kinships obstructed by settler-colonialism; ontologies and languages inseparable from land-relations and incommensurable with English-language perspectives; and epistemologies not beholden to any colonialist standard. These rights and responsibilities clash with Leopoldian conservation narratives still shaping mind-sets and institutions that eliminate Indigenous Peoples by telling bad history and by presuming entitlements to lands and norm-making authority. It models an interlocking method and methodology – surfacing white supremacist settler-colonialist assumptions and structures of Leopoldian conservation narratives – that may be adapted to critique other problematic legacies. It offers a pra xis of anti-colonialist, anti-racist, liberatory environmental-narrative critical-assessment centering Indigenous experts and values, including consent, diplomacy, and intergenerational respect needed for stable coalitions-making for climate and environmental justice.
Xandarellida is a clade of artiopodan euarthropods known exclusively from the early Cambrian (Series 2, Stage 3) Chengjiang biota of South China, apart from the possible inclusion of Phytophilaspis Ivantsov, 1999 from the early Cambrian Sinsk Biota of Siberia. A rare euarthropod taxon represented by four specimens from the Emu Bay Shale (Cambrian Series 2, Stage 4) of Kangaroo Island, South Australia, represents the first record of Xandarellida from East Gondwana. A new monotypic genus, Austroxandarella n. gen., is based on A.poikar n. sp., being most readily distinguished by its elongate pygidium. Close affinities to Xandarella Hou et al., 1991 are suggested by a thorax of 10 tergites, with progressive elongation of the posterior three tergites relative to the seven anterior tergites of subequal length—this elongation representing the dorsoventral decoupling of biramous appendage pairs and tergites shared by all xandarellids. Discovery of an Australian xandarellid adds more support for biogeographic affinities between East Gondwana and South China in the early Cambrian.
The objective of this chapter is to more fully explore how urban environmental change takes place. The role and significance of economic development and normative planning efforts are explored. These conditions further help refine understanding of how different drivers and social and economic forces influence how cities both create and respond to the environmental crises and how transitions are manifested. Several different narratives of urban transitions are defined. These include urban transitions as sequence, collapse, advance, futures, and just sustainability. An integrated framework that links the different elements of urban environmental transitions is presented and discussed. The framework includes four steps – stress, crisis, transition, and transformation – with coupled components and elements such as drivers, spheres of action, and process and product outcomes. A review of the application areas and specific cases are presented as an introduction to the next section of the book.
Gamero-Castaño and colleagues have reported that a large number of calculated shapes for electrified cone jets collapse into a nearly universal geometry when scaled with a characteristic length $R_G$ previously introduced by Gañán-Calvo et al. (J. Aerosol Sci., vol. 25, 1994, pp. 1121–1142). The theoretical reasons for that unexpected success were, however, unclear. Recently, Pérez-Lorenzo & Fernández de la Mora (J. Fluid Mech., vol. 931, 2022, A4) have noted that a slightly different length scale $L_j$ is suggested by the asymptotic jet structure inferred by Gañán-Calvo (Phys. Rev. Lett., vol. 79, 1997, pp. 217–220) from energy conservation and the hypothesis that the asymptotic electric field is that given by Taylor’s static model. This article aims to identify which of these two scales best collapses calculated cone-jet structures, and whether there is an alternative superior one. The characteristic lengths are tested against a large set of numerical solutions of a cone-jet model. The effectiveness of each scaling is determined through analyses based on the standard deviation of the numerical solutions. Despite the slight difference between $R_G$ and $L_j$, this analysis clearly identifies $L_j$ as the most accurate scaling for all cone-jet parameters tested. Differentiating between both scales would not have been possible with experimental measurements, but requires the use of high-fidelity numerical solutions. Surprisingly, the success of $L_j$ is not limited to the jet region, but extends to the cone and the neck. These findings provide a slightly superior scaling enjoying a considerably firmer theoretical basis.
Daily life in cities is often about balance and compromise. Urban densities facilitate things being in close proximity and provide convenience for residents, but they also create an opportunity for traffic congestion and increased social and environmental inequity, and the possibility of lower-density suburban sprawl. To promote urban sustainability, a careful balance of economic development, ecology, and equity is required. In this chapter, four examples of urban sustainability crises and the dramatic response to them are examined. The cases include Miami, US; Oslo, Norway; St. Georges, Grenada; and Shenzhen, China. In each situation, the sustainability crisis emerges from a deeply set awareness of diminishing environmental quality of life and a feeling that the residents’ sense of place is under threat. The drivers of this threat are deeply embedded in social and economic factors. In each city, the policy switch to enhanced sustainability results from an aggressive, multi-scalar effort to alter and redirect the pattern of urban spatial development.
A pressing need exists to understand how, when, and why to adjust and build upon urban environmental policies that can influence a city’s capacity to foster and enact climate adaptation and mitigation. The objective of this book has been to define what we can learn from past urban environmental crises and resulting policy transitions that might be applicable to understand how climate change will manifest as crises in cities and what can be done to help accelerate urban climate action. In this chapter, we more directly turn our attention to learning what the book’s case studies reveal about these objectives. The case studies illustrate how existing urban environmental practices can be adjusted and enhanced to better grapple with the challenges of climate change. The analysis provides the groundwork for a set of innovative recommendations on how to perceive the urban climate crisis and how to consider new urban climate change policies. A key overall conclusion is that we should do all we can to learn from previous urban environmental crises as they will continue to inform us moving into the future.
The chapter lays out the goal and objectives of the project by introducing the framing of the book, key terms and concepts, and the structure of the argument. A central element of the chapter is to lay out how the growing climate crisis and the impact on cities can be situated within the broader set of challenges the cities have faced with their growth and development. Explicit here is the assertion that to address the current waves of dynamic climate risk affecting cities and their residents, one can benefit from looking back into their collective histories to understand how and why cities were able to address, and in some cases overcome, past environmental trials. The book presents how these narratives of “solving” urban environmental problems can be set and analyzed within a several-step process of stress, crisis, transition, and transformation. The steps are bounded by a range of conditions through which fundamental issues of impact and vulnerability and resilience of environmental policy regimes come into question. How urban environmental crises build and reach significant tipping points with associated policy transitions are specific turn key components of the book’s storyline.
Urbanization and the concentration of population and activity traditionally have brought cities an array of environmental quality and pollution issues. The process through which cities have responded to their air pollution problems are equally varied. This application chapter focuses on the narratives of three cities and an urbanized region: London, UK; Los Angeles, US; Rhine-Ruhr River Valley, Germany; and Tokyo, Japan. In all cases, worsening air pollution began to have clear and often immediate economic consequences and human health impacts. While different, several important similarities were present among the crisis-to-transformation processes for each city. These include an extended history of ever-worsening air quality conditions, often punctuated or accelerated through large-scale social or environmental trauma, the emergence and rapid application of new science and technology, and the concomitant innovation in public policy and governance capacity to address the problem of urban air pollution. The desire to address urban air pollution became both an economic imperative and an ambition to protect the well-being of the cities’ residents and to restore the sentiment that the communities were pleasant and healthy places in which to live.
The growth and impact of urban environmental problems can manifest as significant stress and eventual crises for cities and their residents. The focus of this chapter is on how and why these stressors and crises are addressed in cities and the conditions under which the crises can eventually result in significant environmental policy transitions and follow-on transformations. Several different types of documented urban crises (including ecological-resource, urban spatial development, socio-economic, and extreme events) are discussed and analyzed in the chapter. Social, environmental/ecological, and infrastructural/technological drivers influence the connection between urban environmental stress, crisis, transition, and transformation. The actual mechanisms that set up and orchestrate the transition process reflect the resilience of the existing environmental and policy management regime and the magnitude of the stress and crisis. The chapter focuses on describing each of the steps in the transition and the mechanisms that connect each step, as well as the key terms and concepts associated with the process. The importance of policy system tipping points or regime shifts is illustrated.