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排序方式: 共有129条查询结果,搜索用时 15 毫秒
51.
Towards sustainable groundwater use: setting long-term goals, backcasting, and managing adaptively 总被引:7,自引:0,他引:7
Gleeson T Alley WM Allen DM Sophocleous MA Zhou Y Taniguchi M VanderSteen J 《Ground water》2012,50(1):19-26
The sustainability of crucial earth resources, such as groundwater, is a critical issue. We consider groundwater sustainability a value-driven process of intra- and intergenerational equity that balances the environment, society, and economy. Synthesizing hydrogeological science and current sustainability concepts, we emphasize three sustainability approaches: setting multigenerational sustainability goals, backcasting, and managing adaptively. As most aquifer problems are long-term problems, we propose that multigenerational goals (50 to 100 years) for water quantity and quality that acknowledge the connections between groundwater, surface water, and ecosystems be set for many aquifers. The goals should be set by a watershed- or aquifer-based community in an inclusive and participatory manner. Policies for shorter time horizons should be developed by backcasting, and measures implemented through adaptive management to achieve the long-term goals. Two case histories illustrate the importance and complexity of a multigenerational perspective and adaptive management. These approaches could transform aquifer depletion and contamination to more sustainable groundwater use, providing groundwater for current and future generations while protecting ecological integrity and resilience. 相似文献
52.
We have devised a new, simple and easy technique to measure the viscosity of hydrous silicate melts by combining an autoclave for melt hydration and the fiber elongation method for viscosity measurement. Using this, we measured the viscosity of hydrous rhyolitic melts whose water content ranges from 0.02 to 0.58 wt%. We observed a drastic decrease in viscosity against water content: 0.1 wt% water decreases the viscosity about an order of magnitude. Even when the water content is only 0.02 wt%, the viscosity decreased about half an order of magnitude. These results clearly demonstrate that the effect of water on viscosity should not be ignored even when it occurs as a trace constituent. We compared our experimental data with those derived from a non-Arrhenian viscosity model, which is considered to be applicable to calc-alkaline samples. This model succeeded in expressing the viscosity variation against water content but was unable to accurately predict the measured viscosity of liquids.Editorial responsibility: D. Dingwell 相似文献
53.
54.
Richard N. Peterson William C. Burnett Makoto Taniguchi Jianyao Chen Isaac R. Santos Sambuddha Misra 《Continental Shelf Research》2008
In light of the current problems facing the Yellow River and surrounding areas (e.g., periods of zero river discharge, increasing nitrate concentrations of the Bohai Sea), we examined the coastal mixing dynamics around the mouth of the Yellow River. Naturally occurring radium isotopes (223Ra, 224Ra, 226Ra, and 228Ra) and other geochemical tracers (Ba, Si, and salinity) were employed to determine river plume transport scales and rates. Barium and radium exhibit elevated concentrations within the salinity gradient where they are desorbed from particles via ion-exchange. Once they are added to the system, they decrease offshore from dilution with lower concentration Bohai Sea water, and in the case of 224Ra and 223Ra, by radioactive decay. Using radium “ages” to assess the dissolved material transport scales and rates proved to be a useful tool in this environment. The ages based on the 224Ra/228Ra activity ratio increased gradually until salinities reached ∼25 when they rapidly increased due to decreased mixing at higher salinities. Integrated net transport rates through the salinity front ranged from 1.4 to 1.6 cm/s and did not vary significantly with river discharge. Thus, tidal mixing appears to dominate in this system, at least over the range of discharges investigated (80–600 m3/s). Determining the temporal scale of flow across the coastal zone in this region is a valuable first step toward examining whether the Yellow River is contributing to the increasing inorganic nitrogen concentrations in the central Bohai Sea. 相似文献
55.
R. R. Giri Ph.D. H. Ozaki Y. Takayanagi S. Taniguchi M. Eng. R. Takanami M. Eng. 《International Journal of Environmental Science and Technology》2011,8(1):19-30
Ultraviolet photolysis and ultraviolet and hydrogen peroxide oxidation of fourteen commonly used pharmaceutical compounds and two personal care products in mixed solution using low pressure ultraviolet lamp was investigated in laboratory batch experiments. Removal of the compounds followed the first-order reaction kinetic. Three distinct impacts of hydrogen peroxide on ultraviolet and hydrogen peroxide oxidation of the compounds (positive, negative and no significant effect) were observed. Removal behavior of the several tested compounds in mixed solution varied significantly than their respective behavior in absence of coexisting compounds. Clofibric acid, diclofenac, fenoprofen, isopropylantipyrine, ketoprofen, phenytoin and triclosan were removed very efficiently (> 96 %) by ultraviolet photolysis alone. Residual hydrogen peroxide during ultraviolet and hydrogen peroxide oxidation was quantitated for the first time. Hydrogen peroxide addition to ultraviolet photolysis was not worthy for majority of the tested compounds as their removal did not increase significantly and very big fractions (> 85 %) of the added hydrogen peroxide (0.29 ~ 1.47 mM) remained unused presumably due to small fluence of the lamp, very small molar absorption for hydrogen peroxide at 254 nm (27.06 /M.cm) and acidic pH of reaction solution (< 5.7). Further exploration on ultraviolet and hydrogen peroxide oxidation with higher fluence lamp and alkaline solution pH will clarify usefulness of the method to treat pharmaceutical contaminated waters. 相似文献
56.
Tomoyuki Sato Keisuke Taniguchi Tomohiro Takagawa Fujio Masuda 《Geo-Marine Letters》2011,31(2):101-108
Flume experiments aimed to produce flaser bedding were conducted using fine sand and clay in a circular flume. The formation
process of mud drapes during the slack-water stage was revealed in detail. When the tidal current declines, a uniform mobile
mud layer initially settles from suspension and drapes the entire rippled sand bed (type A mud). When the remaining flow velocity
is very low, a more fluid mud begins to settle out (type B mud) that preferentially fills the ripple troughs, the ripples
and mud together forming a flat surface. At slack tide, the two-phase mud drape is temporarily stationary. After the onset
of the reversed flow phase, most of the type B mud is resuspended, while the type A mud is eroded from the crests, leaving
behind a remnant mud drape (flaser) in the troughs that is subsequently buried by migrating ripples. Type B mud generally
contains variable amounts of sand derived from eroded ripple crests, but does not show any visible internal sedimentary structures.
Type A mud represents the ‘mud drapes’ commonly described in the literature, the temporary existence of type B mud having
gone unnoticed because of its low preservation potential. When present, it can be recognized by its sand content and the occurrence
of flame structures in ripple troughs. Tidal deposits reflecting the existence and depositional characteristics of both type
A and type B mud are found in, for example, the macrotidal Oligocene Ashiya Group, Japan. 相似文献
57.
.Dr H. Taniguchi 《Mineralogy and Petrology》1993,49(1-2):13-25
Summary Density and viscosity measurements of three melts of volcanic rock composition (basalt and andesite) at low temperatures were carried out to understand the role of free volume in the viscous behavior of a magma and to estimate the flow unit in the melts. The data combined with literature data suggest the following conclusion: free-volume theory is not applicable to these silicate melts; the relation between viscosity and the inverse of free volume does not yield a straight line in a wide temperature range from the glass-transion temperature to 1550°C. However, two depolymerized melts, diopside and Oki-Dozen alkali basalt (OAB), yield almost linear relationships. Thus, the free-volume theory should hold to a fairly good approximation for these two melts. Based on this approximation, the radius of flow unit for diopside melt was calculated to be about 4.7 Å, and that for Oki-Dozen alkali basalt to be about 4.2 Å. The three-dimensional silicate anions which may correspond to the flow unit are Si14O35
14– and Si16O40
16– for diopside melt, and Si10O25
10– and Si12O30
12– for OAB melt. The temperature effect on the initial slope of the viscosity-pressure relation has also been examined in the frame of free-volume theory. It was concluded that the relative increase of the initial slope of the relation with increasing temperature might be caused by the increase of free volume.With 6 Figures 相似文献
58.
Geometric modelling and object-oriented software concepts applied to a heterogeneous fractured network from the Grimsel rock laboratory 总被引:2,自引:0,他引:2
Thomas Kalbacher Ralph Mettier Chris McDermott Wenqing Wang Georg Kosakowski Takeo Taniguchi Olaf Kolditz 《Computational Geosciences》2007,11(1):9-26
Discrete fracture network simulations are computationally intensive and usually time-consuming to construct and configure.
This paper presents a case study with techniques for building a 3D finite element model of an inhomogeneous fracture network
for modelling flow and tracer transport, combining deterministic and stochastic information on fracture aperture distributions.
The complex intersected fractures represent a challenge for geometrical model design, mesh quality requirements and property
allocations. For the integrated and holistic modelling approach, including the application of numerical and analytical simulation
techniques, new object-oriented concepts in software engineering are implemented to ensure a resourceful and practicable software
environment. 相似文献
59.
60.
R. Feldmann C. M. Carollo C. Porciani S. J. Lilly P. Capak Y. Taniguchi O. Le Fèvre A. Renzini N. Scoville M. Ajiki H. Aussel T. Contini H. McCracken B. Mobasher T. Murayama D. Sanders S. Sasaki C. Scarlata M. Scodeggio Y. Shioya J. Silverman M. Takahashi D. Thompson G. Zamorani 《Monthly notices of the Royal Astronomical Society》2006,372(2):565-577