Borowitzka, MA & Larkum, AWD 1974, 'Chloroplast development in the caulerpalean algaHalimeda', Protoplasma, vol. 81, no. 2-3, pp. 131-144.
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Larkum, AWD & Boardman, NK 1974, 'The effect of nigericin and valinomycin on CO2 fixation electron transport and P518 in intact spinach chloroplasts', FEBS Letters, vol. 40, no. 1, pp. 229-232.
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Leitch, EC 1974, 'The geological development of the southern part of the New England Fold Belt', Journal of the Geological Society of Australia, vol. 21, no. 2, pp. 133-156.
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Two major divisions of the New England Fold Belt, Zone A and Zone B, are separated by the Peel Fault. Deposition in these two zones was probably contemporaneous (Lower Palaeozoic - Lower Permian). Terminal orogenesis in both zones was also contemporaneous (Middle Permian) but whereas in Zone A deformation was only moderate, metamorphism was of burial type, and granitic emplacement was uncommon, in Zone B many rocks were severely deformed and regionally metamorphosed, and both syn-tectonic and post-tectonic granites are widespread. Pre-orogenic palaeogeography is envisaged in terms of an evolving volcanic chain - fore-chain basin - trench system, with an outer non-volcanic arc developed in the Carboniferous. Cessation of movement on a subduction zone dipping westward beneath the volcanic chain is believed to have caused the Middle Permian deformation, but neither metamorphism nor the granitic rocks are directly related to subduction. © Taylor & Francis Group, LLC.
LESLIE, LM & SMITH, RK 1974, 'A NUMERICAL STUDY OF KATABATIC WINDS AND THEIR EFFECT ON POLLUTANT DISPERSAL IN URBAN AREAS.', PROCS. 5TH AUSTRALASIAN CONF. ON HYDRAULICS AND FLUID MECH., SPONSORED BY, AND HELD AT, CANTERBURY UNIV., NEW ZEALAND, vol. 2, no. (DECEMBER 9-13, 1974), pp. 553-560.
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THIS PAPER DESCRIBES A SERIES OF NUMERICAL EXPERIMENTS DESIGNED TO SIMULATE THE KATABATIC WIND PRODUCED BY NOCTURNAL COOLING OF AN ISOLATED HILL.IT AIMS TO EXPLORE THE FACTORS WHICH DETERMINE THE INTENSITY, STRUCTURE AND EXTENT OF SUCH WINDS.THESE FACTORS ARE RELEVANT NOT ONLY TO AN UNDERSTANDING OF THE CLIMATOLOGY OF AREAS ADJACENT TO HILLY OR MOUNTAINOUS TERRAIN BUT ALSO TO AN UNDERSTANDING OF THE FLUSHING AND DISPERSAL OF POLLUTANT BUILD-UP IN VALLEYS AND ABOVE PLAINS BORDERING ON HILLS.FOR THIS REASON, AN ATTEMPT IS MADE TO ASSESS THE EFFECTIVENESS OF THE KATABATIC CIRCULATION IN DISPERSING A POLLUTANT EMITTED OVER THE PLAIN AREA ADJACENT TO AN ISOLATED HILL PRIOR TO THE ONSET OF COOLING AND TO ESTIMATE THE RANGE OVER WHICH POLLUTANT CONCENTRATION IS SIGNIFICANTLY REDUCED.THE CALCULATIONS PROVIDE A CLEAR DEMONSTRATION OF THE IMPORTANCE OF THE ADVECTION OF MOMENTUM AND HEAT IN THE FLOW, EFFECTS WHICH HAVE BEEN IGNORED IN MOST PREVIOUS THEORETICAL STUDIES.IT HAS ALSO BEEN FOUND THAT NON-UNIFORMITIES IN GROUND COOLING HAVE A VERY LARGE INFLUENCE ON THE STRENGTH OF THE DOWNSLOPE WIND WHEN OTHER FACTORS ARE UNCHANGED.(A)
Leslie, LM & Smith, RK 1974, 'NUMERICAL STUDY OF KATABATIC WINDS AND THEIR EFFECT ON POLLUTANT DISPERSAL IN URBAN AREAS.', pp. 553-560.
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Description of a series of numerical experiments designed to simulate the katabatic wind produced by nocturnal cooling of an isolated hill. The factors which determine the intensity, structure and extent of such winds are explored. These factors are relevant not only to an understanding of the climatology of areas adjacent to hilly or mountainous terrain but also to an understanding of the flushing and dispersal of pollutant build-up in valleys and above plains bordering on hills. An assessment is also made of the katabatic circulation in dispersing a pollutant emitted over the plain area adjacent to an isolated hill prior to the onset of cooling and to estimate the range over which pollutant concentration is significantly reduced. Calculations show the importance of the advection of momentum and heat in the flow, effects which have been ignored in most previous theoretical studies.
Mueller, PH & Platen, E 1974, 'Rank Strategies in Sequential Selection Problems.', Wiss Z Tech Univ Dres, vol. 23, no. 5, pp. 1069-1076.
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A Bellman equation for the determination of an optimal strategy is derived for the so-called ″optimum selection problem″ , under the assumption of an existing rank sequence for individual objects. This ″optimum selection problem″ involves the selection of m from n sequentially observable objects without the possibility of supplementary examination. the method is based on an additive result functional whose The results, in case of the selection of an object, depend on their rank number, on the number of the already observed and on the number of the already selected objects. In the majority of practical applications, the elementary result is a monotonous function of the rank number. It is shown that optimum strategy is pure strategy and, in the case of a monotonous results functional, it is, moreover, a so-called simple strategy. These optimal simple strategies can be relatively easily represented. Some special sequential selection problems are solved.
SABINE, TM, SMITH, GB & REEVE, KD 1974, 'CRITICAL CONCENTRATION FOR MAGNETIC ORDER IN SOLID-SOLUTIONS OF UO2 WITH THO2 AND ZRO2', JOURNAL OF PHYSICS C-SOLID STATE PHYSICS, vol. 7, no. 24, pp. 4513-4521.
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