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This new edition of a widely used and cited introduction to ethics and the environment offers a broad and lively discussion of nature's future, focusing on climate change, conservation, and justice for both our contemporaries and future generations. It discusses the nature of environmental problems and their relationship to economics, religion, technology, and aesthetics. It includes incisive discussions of our moral relations with other animals, and of how animals are used in our food systems. It also provides a deep discussion of the value of nature, which takes up ecofeminist and deep ecology views as well as sentientism and biocentrism. It discusses the plurality of values, and applies this analysis to some conflicts from the author's home state of California. The volume is comprehensively revised and updated, with several new chapters, and concludes with a compelling discussion of the question “How should I live?” in this new epoch of the Anthropocene.
The flow near a moving contact line depends on the dynamic contact angle, viscosity ratio and capillary number. We report experiments involving immersing a plate into a liquid bath, concurrently measuring the interface shape, interfacial velocity and fluid flow using digital image processing and particle image velocimetry. All experiments were performed at low plate speeds to maintain small Reynolds and capillary numbers for comparison with viscous theories. The dynamic contact angle, measured in the viscous phase, was kept below $90^{\circ }$ and the viscosity ratio, $\lambda < 1$. This region of parameter space is largely unexplored for advancing contact lines. An important aim of the present study is to provide new experimental data against which new contact line models can be developed. The flow field is directly compared against the prediction from the viscous theory of Huh & Scriven (J. Colloid Interface Sci., vol. 35, issue 1, 1971, pp. 85–101) but with a slight modification involving the curved interface. Remarkable agreement is found between experiments and theory across a wide parameter range. The prediction for interfacial speed from Huh & Scriven is also in excellent agreement with experiments except in the vicinity of the contact line. Material points along the interface were found to rapidly slow down near the contact line, thus alleviating the singularity at the moving contact line. To the best of our knowledge, such a detailed test of theoretical models has not been performed before and we hope the present study will spur new modelling efforts in the field.
The emergence of vascular plants, such as Cooksonia, had a profound impact on Earth’s Early Paleozoic biogeochemical cycles (e.g. atmospheric oxygen, nitrogen and CO2), potentially triggering global environmental and biological changes. However, the timing of Cooksonia’s terrestrial emergence remains elusive as phylogenetic models, microfossils and macrofossils provide different timings for land colonization by vascular plants. Here, hundreds of zircon grains from three siltstones were dated using Laser Ablation-Inductively Couple Plasma-Mass Spectrometry (LA-ICP-MS). The study presents detrital zircon U-Pb dates, which refine the current biostratigraphy ages assigned to Cooksonia macrofossils from the three oldest sites globally. Specifically, siltstones hosting Cooksonia macrofossils from Borrisnoe Mountain (Ireland) and Capel Horeb (Wales) yield Gorstian–Homerian maximum depositional ages (MDAs) of 426 ± 2 Ma and 427 ± 2 Ma, respectively. Additionally, Cwm Graig Ddu (Wales) yields a (Pridoli-Ludlow) maximum age of 423 ± 3 Ma. The findings provide the first detrital zircon U-Pb dates for the oldest Cooksonia macrofossils globally and contribute crucial maximum ages. These maximum ages are instrumental in refining future calibrations of molecular clocks and improving phylogenetic models, thus contributing significantly to a better understanding of Cooksonia’s evolutionary history, including its environmental and ecological impacts.
In the Triassic Mercia Mudstone Group of the Bristol Channel area, SW Britain, yellow micritic-oolitic dolomites deposited in a near-shore location of an extensive shallow saline alkaline lake, pass landwards into conglomerates and sandstones of colluvial-fluvial origin (Dolomitic Conglomerate). Offshore facies are red marl (Branscombe Fm.) and grey-green marl (Blue Anchor Fm.) of shallow lake-playa origin. Conspicuous red silicified bands and nodules (cherts) occur within the shoreline dolomites cropping out at Clevedon, 30 km SW of Bristol. The originally aragonitic ooids and lime mud were dolomitized very early on the lake floor and just below, and the presence of pyrite indicates anoxic conditions therein. The silicification is attributed to the influx of meteoric water with near-neutral pH, provided by flash floods and rainstorms as hyperpycnal and hypopycnal flows, interacting with the silica-rich, saline, alkaline lake water and porewater within the lake sediment. Aragonitic ooids picked up in the flows underwent dissolution, then slight compaction of outer dolomitic lamellae, before silica precipitation. The red colour of the chert from detrital finely disseminated hematite also indicates very early precipitation, before suboxic-anoxic conditions developed in the enclosing lake carbonates. These Triassic sediments show features of soft-sediment deformation, attributed to the formation of chert via a silica gel and/or density contrasts of rapid deposition-dewatering, plus possible seismic activity connected to a nearby basin-margin fault.
We introduce a novel recursive procedure to a neural-network-based subgrid-scale (NN-based SGS) model for large eddy simulation (LES) of high-Reynolds-number turbulent flow. This process is designed to allow an SGS model to be applicable to a hierarchy of different grid sizes without requiring expensive filtered direct numerical simulation (DNS) data: (1) train an NN-based SGS model with filtered DNS data at a low Reynolds number; (2) apply the trained SGS model to LES at a higher Reynolds number; (3) update this SGS model with training data augmented with filtered LES (fLES) data, accommodating coarser filter size; (4) apply the updated NN to LES at a further higher Reynolds number; (5) go back to Step (3) until a target (very coarse) filter size divided by the Kolmogorov length scale is reached. We also construct an NN-based SGS model using a dual NN architecture whose outputs are the SGS normal stresses for one NN and the SGS shear stresses for the other NN. The input is composed of the velocity gradient tensor and grid size. Furthermore, for the application of an NN-based SGS model trained with one flow to another flow, we modify the NN by eliminating bias and introducing a leaky rectified linear unit function as an activation function. The present recursive SGS model is applied to forced homogeneous isotropic turbulence (FHIT) and successfully predicts FHIT at high Reynolds numbers. The present model trained from FHIT is also applied to decaying homogeneous isotropic turbulence and shows an excellent prediction performance.
The Cambridge Handbook of Hydrogen and the Law is the first comprehensive reference work on the regulation of this key area in the energy transition. It is global in scope, featuring chapters that explain the legal situation on hydrogen regulation in Europe, the USA, Latin America, Oceania, the Middle East / North Africa, and Southeast Asia. It includes chapters covering all relevant legal aspects of the hydrogen value chain from production to end use, making it the first in-depth work on the interplay of hydrogen and the law. Leading scholars and practitioners discuss the creation of hydrogen markets, the role of local authorities, sustainability and public participation in hydrogen regulation, the permitting regimes for electrolysers, offshore hydrogen, the regulation on hydrogen transportation and storage, indigenous perspectives on hydrogen, the regulation of hydrogen in heating and the regulation of electricity storage in the form of hydrogen. This title is also available as Open Access on Cambridge Core.
Orbital motions have always been used to test gravitational theories which, from time to time, have challenged the then-dominant paradigms. This book provides a unified treatment for calculating a wide variety of orbital effects due to general relativity and modified models of gravity, to its first and second post-Newtonian orders, in full generality. It gives explicit results valid for arbitrary orbital configurations and spin axes of the sources, without a priori simplifying assumptions on either the orbital eccentricity or inclination. These general results apply to a range of phenomena, from Earth's artificial satellites to the S-stars orbiting the supermassive black hole in the Galactic Centre to binary and triple pulsars, exoplanets, and interplanetary probes. Readers will become acquainted with working out a variety of orbital effects other than the time-honoured perihelion precession, designing their own space-based tests, performing effective sensitivity analyses, and assessing realistic error budgets.
We provide scaling relations for the Nusselt number $Nu$ and the friction coefficient $C_{S}$ in sheared Rayleigh–Bénard convection, i.e. in Rayleigh–Bénard flow with Couette- or Poiseuille-type shear forcing, by extending the Grossmann & Lohse (J. Fluid Mech., vol. 407, 2000, pp. 27–56, Phys. Rev. Lett., vol. 86, 2001, pp. 3316–3319, Phys. Rev. E, vol. 66, 2002, 016305, Phys. Fluids, vol. 16, 2004, pp. 4462–4472) theory to sheared thermal convection. The control parameters for these systems are the Rayleigh number $Ra$, the Prandtl number $Pr$ and the Reynolds number $Re_S$ that characterises the strength of the imposed shear. By direct numerical simulations and theoretical considerations, we show that, in turbulent Rayleigh–Bénard convection, the friction coefficients associated with the applied shear and the shear generated by the large-scale convection rolls are both well described by Prandtl's (Ergeb. Aerodyn. Vers. Gött., vol. 4, 1932, pp. 18–29) logarithmic friction law, suggesting some kind of universality between purely shear-driven flows and thermal convection. These scaling relations hold well for $10^6 \leq Ra \leq 10^8$, $0.5 \leq Pr \leq 5.0$, and $0 \leq Re_S \leq 10^4$.
The unsteady flow physics of wind-turbine wakes under dynamic forcing conditions are critical to the modelling and control of wind farms for optimal power density. Unsteady forcing in the streamwise direction may be generated by unsteady inflow conditions in the atmospheric boundary layer, dynamic induction control of the turbine or streamwise surge motions of a floating offshore wind turbine due to floating-platform oscillations. This study seeks to identify the dominant flow mechanisms in unsteady wakes forced by a periodic upstream inflow condition. A theoretical framework for the problem is derived, which describes travelling-wave undulations in the wake radius and streamwise velocity. These dynamics encourage the aggregation of tip vortices into large structures that are advected along in the wake. Flow measurements in the wake of a periodically surging turbine were obtained in an optically accessible towing-tank facility, with an average diameter-based Reynolds number of 300 000 and with surge-velocity amplitudes of up to 40 % of the mean inflow velocity. Qualitative agreement between trends in the measurements and model predictions is observed, supporting the validity of the theoretical analyses. The experiments also demonstrate large enhancements in the recovery of the wake relative to the steady-flow case, with wake-length reductions of up to 46.5 % and improvements in the available power at 10 diameters downstream of up to 15.7 %. These results provide fundamental insights into the dynamics of unsteady wakes and serve as additional evidence that unsteady fluid mechanics can be leveraged to increase the power density of wind farms.
The development of blue and green hydrogen has been identified as national priorities in a number of Middle East and North Africa (MENA) countries, most notably Gulf Cooperation Council (GCC) states such as Saudi Arabia, United Arab Emirates (UAE), Oman, and Qatar. For example, Qatar announced plans for a US$1 billion plant to make blue ammonia, while Saudi Arabia already commenced work on the NEOM Green Ammonia project, a $US5 billion green hydrogen plant and one of the world’s largest hydrogen projects. With increasing investment and capital outlay on hydrogen projects, the MENA region is projected to become one of the world’s largest exporters of green hydrogen by the year 2050 with an approximate export value of US$200 billion. Despite the rise in hydrogen investments, corresponding law, governance, and institutional frameworks to support hydrogen production are yet to be formulated and communicated, and key vectors for implementation remain, at best, loosely articulated, including mission-critical public–private partnerships (P3), which have been so successful in similar contexts. There is a rather limited legal and/or policy framework that specifically relates to hydrogen across the MENA region. The injection of significant amounts of hydrogen into the national energy networks and grids comes with a wide range of questions across the entire hydrogen production and supply chain. A comprehensive legal framework is required to clarify licensing and permitting processes for hydrogen production, storage, commercialization, and export; while health, safety and design standards for hydrogen infrastructure will need to be elaborated upon to limit environmental, social and governance risks. The chapter explores the guiding principles of an optimal hydrogen regulation framework for MENA countries. It analyses current regulatory uncertainties and gaps in the design and implementation of hydrogen projects across the MENA region and draws upon experiences from other regions with legal pathways for addressing those challenges.
This chapter employs a survey to ask whether the efforts of various climate networks as part of collaborative climate governance are perceived as effective. Sweden is known for being a corporatist state in which dialogue with stakeholders is a key feature of policy development. This can also be seen in the way that the Swedish government has developed its policies for decarbonization by establishing the multi-stakeholder initiative Fossil Free Sweden as a flagship. However, there are numerous other climate networks that are led by non-state and sub-state actors and operate independently of state action. This chapter outlines a set of multi-actor networks that work to contribute to achieve Sweden’s climate targets and assesses them in terms of perceived effectiveness. By studying the perceptions of key stakeholders, this chapter seeks to understand the contributions of various climate networks to Swedish decarbonization beyond measurable emission reductions, thereby paving the way for critical reflections about the role of collaborative climate action in broader governance arrangements.
The effects of the evolution of vortices on the aeroacoustics generated by a hovering wing are numerically investigated by using a hybrid method of an immersed boundary–finite difference method for the three-dimensional incompressible flows and a simplified model based on the Ffowcs Williams-Hawkings acoustic analogy. A low-aspect-ratio ($AR=1.5$) rectangular wing at low Reynolds ($Re=1000$) and Mach ($M=0.04$) numbers is investigated. Based on the simplified model, the far-field acoustics is shown to be dominated by the time derivative of the pressure on the wing surface. Results show that vortical structure evolution in the flow fields, which is described by the divergence of the convection term of the incompressible Navier–Stokes equations in a body-fixed reference frame, determines the time derivative of the surface pressure and effectively the far-field acoustics. It dominates over the centrifugal acceleration and Coriolis acceleration terms in determining the time derivative of the surface pressure. The position of the vortex is also found to affect the time derivative of the surface pressure. A scaling analysis reveals that the vortex acoustic source is scaled with the cube of the flapping frequency.
This chapter focuses on three case studies from California that provide a laboratory for investigating value conflicts. One case involves feral goats and endemic plants on San Clemente Island. What initially presents as a textbook conflict between sentientism and biocentrism turns out to engage a host of other values. A second case concerns tule elk and cattle in Point Reyes National Seashore. A variety of values are in play, but the primary conflict is between an endangered species and a population of animals that humans use for food. The third case involves Sierra Nevada bighorn sheep and mountain lions. Both of these species have depleted populations and restricted ranges due to human action, and both are under intensive management. Their interests conflict and humans cannot remove themselves from the conflict.
This chapter focuses on legal approaches in the intersection between hydrogen storage and the electricity sector. With the increase of intermittent renewable energy sources in the electricity markets, new solutions are needed to ensure a reliable supply of electricity when renewable sources are not available. While technologies such as batteries are able to store electricity for short periods of time, medium- to long-term storage of electricity continues to be a challenge. Hydrogen storage has been presented as a potential solution to address this need. This chapter analyses the legal questions that emerge in using hydrogen as a storage medium to balance the intermittency of renewable energy sources in the low-carbon energy transition. It reviews the legal challenges and opportunities of using hydrogen as an energy storage medium and the definition of end use in this context. The discussion draws on the European Union (EU) legal frameworks for electricity and hydrogen as an illustrative case study to demonstrate how these legal questions can be governed through a transnational legal framework. The chapter concludes with an assessment of the principal gaps in the EU legal framework and evaluates the likely future directions of regulating hydrogen as an energy storage medium in the Union’s low-carbon energy transition.