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Reply to comment on ‘Up‐scaling potential impacts on water flows from agricultural water interventions: opportunities and trade‐offs in the Osman Sagar catchment,Musi sub‐basin,India’. Hydrological Processes 27: 3905–3921 by Bouma et al., 
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下载免费PDF全文 Kaushal K. Garg Suhas P. Wani Jennie Barron Louise Karlberg Johan Rockstrom 《水文研究》2014,28(8):3352-3355
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Katy Mee Jennie S. Gilbert David W. McGarvie José A. Naranjo Malcolm S. Pringle 《Bulletin of Volcanology》2009,71(8):933-952
Nevados de Chillán Volcanic Complex, central Chile, has been active for at least 640 ka—a period spanning a number of glacial
and interglacial periods. Geologic mapping, radiometric dating and geochemical analysis have identified six new volcanic units
and produced four new 40Ar/39Ar ages for Cerro Blanco, the northern subcomplex of Nevados de Chillán volcano. Compositions range from dacite to basaltic-andesite
and a new geologic map is presented. Examination of lava fracture structures on both newly mapped lavas and those mapped during
previous studies has enabled interpretations of former eruptive environments. Palaeoenvironment reconstructions, combined
with 40Ar/39Ar ages and comparison with the marine oxygen isotope record, show that at least three phases of volcanic activity have occurred
during the evolution of Cerro Blanco: (1) a constructive, pre-caldera collapse period; (2) a period of caldera formation and
collapse; and (3) a constructive period of dome growth forming the modern day volcanic centre. This style of volcanic evolution,
whereby large-scale caldera collapse is followed by growth of a new stratocone is common at Andean volcanoes. 相似文献
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Jashar?ArfaiEmail author Dieter?Franke Christoph?Gaedicke Rüdiger?Lutz Michael?Schnabel Stefan?Ladage Kai?Berglar Mario?Aurelio Jennie?Montano Nicole?Pellejera 《Marine Geophysical Researches》2011,32(3):349-362
Interpretation of deep 2-D multi-channel seismic data sheds insights into the geological evolution of the West Luzon Basin,
Philippines. This basin is a sediment-filled trough that is located between the island of Luzon and the outer arc high of
the west Luzon subduction zone. High-amplitude, low-frequency reflection bands mark the acoustic basement. The basement, at
about 6 s (TWT), is dissected by normal faults with some of them being inverted in a later phase of deformation. The sedimentary
successions, overlying the basement are stratified with partly chaotic structures and discontinuous reflectors. Five regional
unconformities separate major stratigraphic units. Grid calculations of our seismic data reveal variations in the sedimentation
pattern of the basin with a shift of the deposition centre from east to west and backwards during formation. A distinct bottom-simulating
reflector is commonly observed. Because the northern boundary of the continental fragments to the South of the West Luzon
Basin is unclear we speculate that the basin may be (partly) underlain by continental crust. The continental crust was affected
by rifting prior to and during the opening of the South China Sea and the basin was overprinted at a later stage by a forearc
structural setting when subduction was initiated. 相似文献
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Selection of ground motion time series and limits on scaling 总被引：4，自引：0，他引：4
Jennie Watson-Lamprey Norman Abrahamson 《Soil Dynamics and Earthquake Engineering》2006,26(5):477-482
A procedure to select time series for use in non-linear analyses that are intended to result in an average response of the non-linear system is proposed that is not based simply on magnitude, distance, and spectral shape. A simple model of a yielding system is used as a proxy for the non-linear behavior of a more complicated yielding system. As an example, Newmark displacements are used as a proxy for more complex slope-stability models. The candidate scaled time series are evaluated to find those that yield a response of the simple non-linear system that is near the expected response for the design event. Those scaled time series with responses near the expected value are selected as the optimum time series for defining average response even if the scale factors are larger than commonly accepted (e.g. scale factors >factor of 2). 相似文献
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Alistair Simon Bargery Alexander Barrett Lionel Wilson Jennie S. Gilbert 《Icarus》2010,210(1):488-506
Experiments have been performed to simulate the shallow ascent and surface release of water and brines under low atmospheric pressure. Atmospheric pressure was treated as an independent variable and water temperature and vapor pressure were examined as a function of total pressure variation down to low pressures. The physical and thermal responses of water to reducing pressure were monitored with pressure transducers, temperature sensors and visible imaging. Data were obtained for pure water and for solutions with dissolved NaCl or CO2. The experiments showed the pressure conditions under which the water remained liquid, underwent a rapid phase change to the gas state by boiling, and then solidified because of removal of latent heat. Liquid water is removed from phase equilibrium by decompression. Solid, liquid and gaseous water are present simultaneously, and not at the 611 Pa triple point, because dynamic interactions between the phases maintain unstable temperature gradients. After phase changes stop, the system reverts to equilibrium with its surroundings. Surface and shallow subsurface pressure conditions were simulated for Mars and the icy satellites of the outer Solar System. Freezing by evaporation in the absence of wind on Mars is shown to be unlikely for pure water at pressures greater than c. 670 Pa, and for saline solutions at pressures greater than c. 610 Pa. The physical nature of ice that forms depends on the salt content. Ice formed from saline water at pressures less than c. 610 Pa could be similar to terrestrial sea ice. Ice formed from pure water at pressures less than c. 100 Pa develops a low thermal conductivity and a ‘honeycomb’ structure created by sublimation. This ice could have a density as low as c. 450 kg m−3 and a thermal conductivity as low as 1.6 W m−1 K−1, and is highly reflective, more akin to snow than the clear ice from which it grew. The physical properties of ice formed from either pure or saline water at low pressures will act to reduce the surface temperature, and hence rate of sublimation, thereby prolonging the lifespan of any liquid water beneath. 相似文献
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John A. Stevenson Jennie S. Gilbert David W. McGarvie John L. Smellie 《Quaternary Science Reviews》2011,30(1-2):192-209
Rhyolite eruptions in Iceland mostly take place at long-lived central volcanoes, examples of which are found associated with each of the present-day rift-zone ice caps. Subglacial eruptions at Kerlingarfjöll central volcano produced rhyolite tuyas that are notable for their exposures of early-erupted pyroclastic material. Observations from a number of these edifices are synthesised into a general model for explosive rhyolite tuya formation. Eruptions begin with violent phreatomagmatic explosions that generate massive tuff (mT), but the influence of water quickly declines, leading to the formation of massive lapilli-tuffs (mLT) containing magmatically-fragmented vesicular pumice and ash. These are deposited rapidly near the vent, probably by moist pyroclastic density currents, confined by ice but not within a meltwater lake. The explosive-effusive transition is controlled by the ascent rate and gas content of the magma. An unusual obsidian-rich massive lapilli-tuff lithofacies (omLT) is identified and interpreted as pyroclastic material that was intruded into gas-fluidised deposits at the explosive-effusive transition. The effusive phase of eruption involves the emplacement of intrusions and lava caps. Intrusions of lava into the early-erupted phreatomagmatic deposits are characterised by peperitic margins and the formation of hyaloclastite. Intrusions into stratigraphically higher levels of the pyroclastic material show more limited interaction with the host tephra and have microcrystalline cores. Large lava bodies with columnar-jointed margins cap the tuyas and have intrusive basal contacts with the tephras. The main influence of the ice is to confine the rhyolite eruptive products to immediately above the vent region. This is in contrast to subglacial basaltic tuya-forming eruptions, which are characterised by the formation of meltwater lakes, phreatomagmatic fragmentation and subaqueous deposition. The lack of meltwater storage may reduce the potential for large jökulhlaups. 相似文献
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The last decade has witnessed a surge of interest in ‘sustainable communities’ within the UK. This has stimulated a plethora of research aimed at acquiring a better understanding of what ‘sustainable communities’ might look like and how they can be achieved. However, this has not been accompanied by a reflection and interrogation of the actual processes, challenges and politics of doing ‘sustainable communities’ research. This paper addresses this gap by highlighting the importance of paying attention to the on-going process of negotiating access when carrying out sustainability research at the community level. We draw on a recent study of skills and knowledge for ‘sustainable communities’ in Stroud Gloucestershire, UK, to illustrate the importance of sensitivity to social relationships throughout and beyond the research trajectory within sustainability research. Our experience raises important questions about the politics of research practices when doing sustainability research ‘with’ communities and the challenges associated with participatory approaches as a means to demonstrate research impact. We argue that in developing a fuller understanding of why and how different types of community level initiatives can contribute to the ‘sustainable communities’ agenda, greater consideration needs to be given to how these community practices can be better supported through the process of doing academic research. 相似文献