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31.
Rob N. J. Comans Cornelis H. Van Der Weijden Simon P. Vriend 《Environmental Geology》1987,9(2):119-128
A hydrogeochemical study of the impact of land use on the composition of natural waters in the Vouzela region in northern
Portugal was carried out during the summer of 1983. Water samples were collected from spring and major streams in the area
and analyzed for major constituents and some trace elements. Analysis of variance and subsequent pairwise contrast tests demonstrated
that waters from agricultural areas are significantly enriched in constiluents such as Na, K, Ca, Mg, Sr, Cl, SO4, and NO3. High concentrations of these ions in agricultural areas are the result of both the application of fertilizers and enhanced
evaporation by the intensive irrigation of agricultural lands. Constitutents such as H4SiO4, HCO3, F, and probably Li, which are typically related to mineral weathering, were not affected by land use. In waters from forested
areas the concentration of most constituents was about 20% higher than in waters from uncultivated areas with mainly a grass
cover. This reflects the difference in the evapotranspiration of these two vegetation types. The chemistry of the Rio Zela
clearly reflects differences in land use in the Rio Zela valley. 相似文献
32.
Jungho Kim Laura Read Lynn E. Johnson David Gochis Rob Cifelli Heechan Han 《水文科学杂志》2020,65(10):1652-1666
ABSTRACT This study experiments with reservoir representation schemes to improve the ability to model active water management in the National Water Model (NWM). For this purpose, we developed an integrated water management model, NWM-ResSim, by coupling the NWM with HEC-ResSim, and two reservoir representation schemes are tested: simulation of reservoir operations and retrieval of scheduled operations. The experiments focus on a pilot reservoir domain in the Russian River basin – Lake Mendocino, California – and its contributing watershed. The evaluation results suggest that the NWM-ResSim improves the simulation performance of reservoir outflow from this managed reservoir over the NWM default level pool routing scheme. The degree of this improvement depends on the suitability of the operation guidance; the reservoir operations simulation scheme could have acceptable errors for the purposes of water resources management, but not for flood operations. Results of the retrieval scheme of scheduled operations demonstrated better performance for sub-daily flood operations. 相似文献
33.
34.
Building comparable global change vulnerability assessments: The vulnerability scoping diagram 总被引:29,自引:1,他引:29
Advancing vulnerability science depends in part on identifying common themes from multiple, independent vulnerability assessments. Such insights are difficult to produce when the assessments use dissimilar, often qualitative, measures. The Vulnerability Scoping Diagram is presented to facilitate the comparison of assessments with dissimilar measures. The diagram is illustrated with recent research on drought vulnerabilities, showing that common insights into vulnerability may emerge if independent research teams use a common structure for organizing information about exposure, sensitivity and adaptive capacity—even if the underlying measures differ between assessments. Broadly adopting this technique, which is grounded in the “Eight Steps” methodological protocol [Schröter, D., Polsky, C., Patt, A., 2005. Assessing vulnerabilities to the effects of global change: an eight step approach. Mitigation and Adaptation Strategies for Global Change 10(4), 573–595], will enable a vulnerability meta-analysis, the lessons from which may permit places to identify helpful adaptation or mitigation options without first having to conduct their own vulnerability assessments. 相似文献
35.
Rob M. Ellam Brian G. J. Upton J. Godfrey Fitton 《Contributions to Mineralogy and Petrology》1998,133(1-2):51-59
The Myggbukta caldera complex and a swarm of basic dykes constitute the latest Tertiary magmatism in the Hold with Hope region,
East Greenland. The Sr and Nd isotope ratios of these rocks show coherent variations which extend to high 87Sr/86Sr and low 143Nd/144Nd values and require a contribution from continental lithosphere. Broad correlations with major element differentiation indices
suggest that the continental component was incorporated during magmatic differentiation thereby favouring a crustal contamination
process. Trace element concentrations are strongly correlated with isotopic compositions but display ranges for many incompatible
elements which extend beyond likely crustal contaminant compositions. This is readily modelled by AFC processes in which the
dominant cause of trace element enrichment is the concentration effect of fractional crystallisation rather than the composition
of the contaminant. The simplest such models still require unrealistically high degrees of fractional crystallisation to explain
the ten-fold enrichment of some trace elements. This can be overcome if the primary magmas entering the crust already had
highly variable trace element compositions. Such variability is readily achieved if melts from different parts of the melting
column escape without thorough homogenization. An AFC model which incorporates variability in parental magma composition is
then able to simulate the range of compositions observed at Hold with Hope. This carries the implication that the variations
observed are more readily attributed to changes in uncontaminated parental magma than to variations in the composition or
amount of contaminant.
Received: 5 March 1998 / Accepted: 16 June 1998 相似文献
36.
Thermal demagnetization of red and drab sandstones from the St. Bees Sandstone shows a wide range of directional stability. After the removal of a metastable secondary magnetization at temperatures up to 300°C red sandstones may show stable or unstable magnetization. Experiments indicate that both the stable and unstable magnetization is carried by coarse haematite particles (specularite).Drab sandstones, which have been subject to reduction and dissolution of haematite are generally unstable but specimens with a stable NRM occur and this must be carried by specularite because the pigment has been removed from these specimens.The stable magnetization is believed to have developed during deposition and early diagenesis by the oxidation of detrital iron oxides. Pole positions correspond to known Triassic poles and there are abundant normal and reversed zones typical of the Lower Triassic.The unstable magnetization of the red sandstones is apparently due to the development of authigenic overgrowths of haematite on the detrital specularites. This phase of authigenesis may have taken place over a long time, and after significant changes in the ambient geomagnetic field resulting in complex magnetizations in individual grains and hence whole rocks. 相似文献
37.
Pleistocene sediments and soils exposed at Stebbing in central Essex, England are described, analysed and interpreted. The sand and gravel units above Eocene London Clay and Upper Pliocene Red Crag are shown to be a high level member of the Kesgrave Formation, with a surface immediately beneath that of the Westland Green Gravels, which are tentatively assigned to the Pre-Pastonian ‘a’ Stage of the British Quaternary succession. The rubified, argillic soil developed in the surface of these fluvial deposits is a composite of the Valley Farm and Barham Soils and displays micromorphological evidence of several phases of clay illuviation, gleying and clay coating disruption. Originally truncated and buried beneath Anglian gelifluction deposits, cover sand and till, the soil has been exhumed in most places by subsequent erosion. The full succession, however, is preserved within large gulls that formed by periglacial cambering prior to this erosion. More recent loess incorporation and pedogenesis have modified the exhumed soil and the materials within the gulls. 相似文献
38.
Kim Vermonden Marion A. A. Hermus Marije van Weperen Rob S. E. W. Leuven Gerard van der Velde Alfons J. P. Smolders Jan G. M. Roelofs A. Jan Hendriks 《水文研究》2009,23(21):3110-3120
The water quality of urban drainage ditches in lowlands in the Rhine‐Meuse delta was analysed with principal component analysis (PCA) during a dry period and a rain storm, and related to the seepage of polluted river water and effective impervious area (EIA). This was done in order to test the hypothesis that seepage of river water and storm water runoff from impervious areas strongly determine the water quality of urban drainage systems along large lowland rivers. Our analysis revealed that upward seepage of groundwater originating from rivers Rhine and Meuse was positively correlated with nitrate, potassium, sodium and chloride and negatively correlated with alkalinity, calcium, magnesium and iron. EIA was correlated with very few environmental variables (i.e. phosphate, pH and iron in the dry period and iron during the rain storm). Nickel and zinc concentrations generally exceeded the maximum allowable concentrations (MAC), while lead and phosphorus concentrations were just above the nutrient standards and MAC in a few locations during the rain storm. To optimize water quality in urban water systems, attention should be paid to all sources of pollution and not only to EIA. The impact of local groundwater seepage originating from large rivers in lowlands on the chemistry of urban water systems is often underestimated and should be taken into account when assessing water quality and improving water quality status. Copyright © 2009 John Wiley & Sons, Ltd. 相似文献
39.
Some things old, some things new: The spatial representations and politics of change of the peak oil relocalisation movement 总被引:1,自引:0,他引:1
Despite continued uncertainty about the physical realities and political, economic and social implications of peak oil, combined concerns about oil scarcity, climate change and globalisation has spawned an energetic relocalisation movement dedicated to achieving a comprehensive reduction in oil dependency through community-scale initiatives. This paper uses a discourse approach to examine the emergence, geographical spread and practices of the Transition Network, a UK-originated relocalisation movement now involving 186 local initiatives in the UK and other countries. We trace the movement’s drawing upon, and innovation from, discourses and techniques used by other grassroots environmental movements to promote a spatial representation of peak oil as an inevitable and geographically undiscriminating problem, and its use of addiction metaphors and participatory techniques to promote personal and community-scale energy descent initiatives as a viable and necessary alternative to globalisation. We also analyse the spatial representations and techniques used in the Network’s “rhizomic” spread across multiple localities around the world and embedding in communities where relocalisation initiatives are established. We conclude by examining the future challenges these spatial constructions of peak oil pose for the relocalisation movement. 相似文献
40.