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11.
12.
Marcus B. Lane 《The Australian geographer》2005,36(3):283-299
This paper tracks the changing role of public participation in planning thought. In doing so, the paper shows that the role of public participation in planning is largely determined by the nature of the planning enterprise being undertaken. The definition of the planning problem, the kinds of knowledge used in planning practice, and the conceptualisation of the planning and decision-making context are the important determinants of the extent of participation offered to the public. The paper therefore contributes to thinking about how to evaluate public participation by showing that it can only be understood in terms of the decision-making context in which it is embedded. Specifically, it makes little sense to evaluate public participation in terms that are not shared by the planning model itself 相似文献
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Marcus Schulz Jan Priegnitz Jörg Klasmeier Stefan Heller Stefan Meinecke Michael Feibicke 《水文研究》2012,26(2):272-280
In several empirical and modelling studies on river hydraulics, dispersion was negatively correlated to surface roughness. In this study, it was aimed to investigate the influence of surface roughness on longitudinal dispersion under controlled conditions. In artificial flow channels with a length of 104 m, tracer experiments with variations in channel bed material were performed. By use of measured tracer breakthrough curves, average flow velocity, mean longitudinal dispersion, and mean longitudinal dispersivity were calculated. Longitudinal dispersion coefficients ranged from 0·018 m2 s?1 in channels with smooth bed surface up to 0·209 m2 s?1 in channels with coarse gravel as bed material. Longitudinal dispersion was linearly related to mean flow velocity. Accordingly, longitudinal dispersivities ranged between 0·152 ± 0·017 m in channels with smooth bed surface and 0·584 ± 0·015 m in identical channels with a coarse gravel substrate. Grain size and surface roughness of the channel bed were found to correlate positively to longitudinal dispersion. This finding contradicts several existing relations between surface roughness and dispersion. Future studies should include further variation in surface roughness to derive a better‐founded empirical equation forecasting longitudinal dispersion from surface roughness. Copyright © 2011 John Wiley & Sons, Ltd. 相似文献
15.
Paola De Rossi Fontanelli Luiz Fernando De Ros Marcus Vinicius Dorneles Remus 《Marine and Petroleum Geology》2009
The provenance of the Maastrichtian deep-water reservoir sandstones from the Jubarte oil field (Campos Basin, eastern Brazil), was studied using an integrated approach that included quantitative petrography, conventional heavy mineral analysis, garnet mineral chemistry and zircon geochronology. The reservoirs are predominantly coarse, poorly-sorted sandstones with feldspathic composition derived from uplifted basement terrains. The fourth- and fifth-order depositional sequences analyzed show no major variations in composition or in provenance through time. However, variations in apatite:tourmaline presents potential to be used as a parameter for sandstone correlation within the field. The composition of heavy minerals indicates derivation from high temperature and low-to-medium pressure aluminous metapelitic rocks, from granites and subordinate mafic rocks, derived from the Cabo Frio Tectonic Domain and the Oriental terrain of Ribeira orogen, characterizing a supply route from SW to NE. The low ZTR index, as well as the absence of low-grade stable heavy minerals and of metasedimentary rock fragments, suggest that by the end of Cretaceous all supracrustal, low-grade terrains had already been totally eroded, and that plutonic, infracrustal rocks were exposed, similarly to the present situation. 相似文献
16.
We present the finalized catalog of solar energetic proton events detected by the Wind/EPACT instrument over the period 1996?–?2016. Onset times, peak times, peak proton intensity and onset-to-peak proton fluence are evaluated for the two available energy channels, at about 25 and 50 MeV. We describe the procedure utilized to identify the proton events and to relate them to their solar origin (in terms of flares and coronal mass ejections). The statistical relationships between the energetic protons and their origin (linear and partial correlation analysis) are reported and discussed in view of earlier findings. Finally, the different trends found in the first 8 years of Solar Cycles 23 and 24 are discussed. 相似文献
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Differences in trace metal concentrations among fluvial morphologic units and implications for sampling 总被引:2,自引:0,他引:2
This study examines the segregation of trace metals within and between fluvial morphologic units in sand-sized and finer
bed sediments in a cobble bed stream. The types of fluvial morphologic units sampled are low gradient riffles, high gradient
riffles, glides, eddy drop zones, lateral scour pools, attached bars, and detached bars. Three to nine samples were collected
from ten of each type of morphologic unit. All 12 metals show significantly different concentrations between some morphologic
units in sediments smaller than 2 mm. Eddy drop zones and attached bars consistently have the highest metal concentrations,
while low gradient riffles, high gradient riffles, and glides typically have the lowest concentrations. Metals showing the
greatest between-unit variability are Al, Cr, Fe, Cu, and Ti, followed by Co, Mn, and Pb, while Mg, Mn, V, and Zn display
relatively few differences between units. Lateral and longitudinal variations of metals within units are not significant,
and there was no consistent, predictable variation in metal concentrations with distance downstream. Results indicate that
metal studies in other gravel- and cobble-bed streams should include a reconnaissance survey to determine variations between
morphologic units, stratify sampling by morphologic unit, and analyze spatial autocorrelation to determine sample spacing.
Received: October 1997 · Accepted: 23 March 1998 相似文献
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20.
Y Marcus 《Geochimica et cosmochimica acta》1977,41(12):1739-1744
The activities of KCl and of H2O in Dead Sea water were estimated according to several approaches dealing with multicomponent electrolyte solutions. The activity of H2O, both measured directly via its vapor pressure and calculated theoretically, is 0.754 ± 0.004 for brine of density 1.207 ± 0.003gcm?3 at 25°C. The mean ionic activity of KCl in this brine ranges from 0.876 to 1.199 according to various treatments. These correspond to binary aqueous solutions 8.6–12.1 times richer than the brine. The brine cannot be simultaneously in equilibrium with respect to both H2O and KCl with such binary solutions, so a hypothetically perfect semipermeable membrane cannot lead to a state of equilibrium between the brine and aqueous KCl of any concentration. 相似文献