1,146 research outputs found

    UK Large-scale Wind Power Programme from 1970 to 1990: the Carmarthen Bay experiments and the Musgrove Vertical-Axis Turbines

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    This article describes the development of the Musgrove Vertical Axis Wind Turbine (VAWT) concept, the UK ‘Carmarthen Bay’ wind turbine test programme, and UK government’s wind power programme to 1990. One of the most significant developments in the story of British wind power occurred during the 1970s, 1980s, and 1990s, with the development of the Musgrove vertical axis wind turbine and its inclusion within the UK Government’s wind turbine test programme. Evolving from a supervisor’s idea for an undergraduate project at Reading University, the Musgrove VAWT was once seen as an able competitor to the horizontal axis wind systems that were also being encouraged at the time by both the UK government and the Central Electricity Generating Board, the then nationalised electricity utility for England and Wales. During the 1980s and 1990s the most developed Musgrove VAWT system, along with three other commercial turbine designs was tested at Carmarthen Bay, South Wales as part of a national wind power test programme. From these developmental tests, operational data was collected and lessons learnt, which were incorporated into subsequent wind power operations.http://dx.doi.org/10.1260/03095240677860621

    Generalized Cauchy means

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    Given two means M and N, the operator MM,NMM,N assigning to a given mean ÎŒ the mean MM,N(ÎŒ)(x,y)=M(ÎŒ(x,N(x,y)),ÎŒ(N(x,y),y)) was defined in Berrone and Moro (Aequationes Math 60:1–14, 2000) in connection with Cauchy means: the Cauchy mean generated by the pair f, g of continuous and strictly monotonic functions is the unique solution ÎŒ to the fixed point equation MA(f),A(g)(ÎŒ)=ÎŒ, where A(f) and A(g) are the quasiarithmetic means respectively generated by f and g. In this article, the operator MM,NMM,N is studied under less restrictive conditions and a general fixed point theorem is derived from an explicit formula for the iterates MnM,NMM,Nn . The concept of class of generalized Cauchy means associated to a given family of mixing pairs of means is introduced and some distinguished families of pairs are presented. The question of equality in these classes of means remains a challenging open problem.Fil: Berrone, Lucio Renato. Universidad Nacional de Rosario. Facultad de Ciencias Exactas, IngenierĂ­a y Agrimensura; Argentina. Consejo Nacional de Investigaciones CientĂ­ficas y TĂ©cnicas; Argentin

    On Kedlaya type inequalities for weighted means

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    In 2016 we proved that for every symmetric, repetition invariant and Jensen concave mean M\mathscr{M} the Kedlaya-type inequality A(x1,M(x1,x2),
,M(x1,
,xn))≀M(x1,A(x1,x2),
,A(x1,
,xn)) \mathscr{A}\big(x_1,\mathscr{M}(x_1,x_2),\ldots,\mathscr{M}(x_1,\ldots,x_n)\big)\le \mathscr{M} \big(x_1, \mathscr{A}(x_1,x_2),\ldots,\mathscr{A}(x_1,\ldots,x_n)\big) holds for an arbitrary (xn)(x_n) (A\mathscr{A} stands for the arithmetic mean). We are going to prove the weighted counterpart of this inequality. More precisely, if (xn)(x_n) is a vector with corresponding (non-normalized) weights (λn)(\lambda_n) and Mi=1n(xi,λi)\mathscr{M}_{i=1}^n(x_i,\lambda_i) denotes the weighted mean then, under analogous conditions on M\mathscr{M}, the inequality Ai=1n(Mj=1i(xj,λj), λi)≀Mi=1n(Aj=1i(xj,λj), λi) \mathscr{A}_{i=1}^n \big(\mathscr{M}_{j=1}^i (x_j,\lambda_j),\:\lambda_i\big) \le \mathscr{M}_{i=1}^n \big(\mathscr{A}_{j=1}^i (x_j,\lambda_j),\:\lambda_i\big) holds for every (xn)(x_n) and (λn)(\lambda_n) such that the sequence (λkλ1+⋯+λk)(\frac{\lambda_k}{\lambda_1+\cdots+\lambda_k}) is decreasing.Comment: J. Inequal. Appl. (2018

    Solar System Processes Underlying Planetary Formation, Geodynamics, and the Georeactor

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    Only three processes, operant during the formation of the Solar System, are responsible for the diversity of matter in the Solar System and are directly responsible for planetary internal-structures, including planetocentric nuclear fission reactors, and for dynamical processes, including and especially, geodynamics. These processes are: (i) Low-pressure, low-temperature condensation from solar matter in the remote reaches of the Solar System or in the interstellar medium; (ii) High-pressure, high-temperature condensation from solar matter associated with planetary-formation by raining out from the interiors of giant-gaseous protoplanets, and; (iii) Stripping of the primordial volatile components from the inner portion of the Solar System by super-intense solar wind associated with T-Tauri phase mass-ejections, presumably during the thermonuclear ignition of the Sun. As described herein, these processes lead logically, in a causally related manner, to a coherent vision of planetary formation with profound implications including, but not limited to, (a) Earth formation as a giant gaseous Jupiter-like planet with vast amounts of stored energy of protoplanetary compression in its rock-plus-alloy kernel; (b) Removal of approximately 300 Earth-masses of primordial gases from the Earth, which began Earth's decompression process, making available the stored energy of protoplanetary compression for driving geodynamic processes, which I have described by the new whole-Earth decompression dynamics and which is responsible for emplacing heat at the mantle-crust-interface at the base of the crust through the process I have described, called mantle decompression thermal-tsunami; and, (c)Uranium accumulations at the planetary centers capable of self-sustained nuclear fission chain reactions.Comment: Invited paper for the Special Issue of Earth, Moon and Planets entitled Neutrino Geophysics Added final corrections for publicatio

    Thermal conductivity of amorphous carbon thin films

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    Thermal conductivities Λ\Lambda of amorphous carbon thin films are measured in the temperatures range 80--400 K using the 3ω3\omega method. Sample films range from soft a-C:H prepared by remote-plasma deposition (Λ=0.20\Lambda = 0.20 W m−1^{-1} K−1^{-1} at room temperature) to amorphous diamond with a large fraction of sp3sp^3 bonded carbon deposited from a filtered-arc source (Λ=2.2\Lambda = 2.2 W m−1^{-1} K−1^{-1}). Effective-medium theory provides a phenomenological description of the variation of conductivity with mass density. The thermal conductivities are in good agreement with the minimum thermal conductivity calculated from the measured atomic density and longitudinal speed of sound.Comment: 4 pages, 4 figure

    From Deficit to Strength-Based Aboriginal Health Research—Moving toward Flourishing

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    Aboriginal Australians have a fundamental human right to opportunities that lead to healthy and flourishing lives. While the impact of trauma on Aboriginal Australians is well-documented, a pervasive deficit narrative that focuses on problems and pathology persists in research and policy discourse. This narrative risks further exacerbating Aboriginal disadvantage through a focus on 'fixing what is wrong' with Aboriginal Australians and the internalising of these narratives by Aboriginal Australians. While a growing body of research adopts strength-based models, limited research has sought to explore Aboriginal flourishing. This conceptual paper seeks to contribute to a burgeoning paradigm shift in Aboriginal research, seeking to understand what can be learned from Aboriginal people who flourish, how we best determine this, and in what contexts this can be impactful. Within, we argue the case for a new approach to exploring Aboriginal wellbeing that integrates salutogenic, positive psychology concepts with complex systems theory to understand and promote Aboriginal wellbeing and flourishing. While deeper work may be required to establish the parameters of a strength-based, culturally aligned Aboriginal conceptualisation of positive psychology, we suggest the integration of Aboriginal and Western methodologies offers a unique and potent means of shifting the dial on seemingly intractable problems.Jonathan Bullen, Trish Hill-Wall, Kate Anderson, Alex Brown, Clint Bracknell, Elizabeth A. Newnham, Gail Garvey, and Lea Water
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