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1.
Formation of saline groundwaters in the Baltic region through freezing of seawater during glacial periods 总被引：1，自引：0，他引：1
Typical Ca---Cl brines occur in crystalline and metamorphic rocks below freshwater horizons at various localities in Sweden and Finland. Total dissolved solids (TDS) range in concentration between 2 and 120 gl−1 and have long been thought to derive from water-rock interactions. The relationships between Na, Cl and Br in these brines suggest, however, that they were derived from freezing of seawater during glacial periods. The brines were subsequently diluted by meteoric waters and their Ca/Mg ratio was increased through water-rock interactions in the subsurface. The hydrogeological model for both the formation of freeze-derived marine brines and their lateral intrusion involves restricted inland marine basins in recent and subrecent polar climatic belts. Seawater in such basins gradually freezes in response to glaciation. The solutes which concentrate in the remaining water body are residual after precipitation of a sequence of minerals which include carbonates, mirabilite and hydrohalite. Hydraulic pressure of the growing ice sheet over the frozen seas is gradually added to the ambient hydrostatic pressure exerted on the brines. This, together with their increased density, increases the intrusional potential of the brines. As the land ice cannot exert hydraulic pressure on continental groundwater in the aquifers, the balance of pressure favours deep landward intrusion of brines. Post-glacial processes cause the subsurface dilution and replacement of the brines both by seawater and fresh waters. The presence of such brines also far from present-day coastal settings reflects the shifting of coastlines as a result of isostatic movements and eustatic sea-level changes associated with glaciation and deglaciation. 相似文献
2.
The effect of urbanization in an arid region: Formation of a perched water table that causes environmental damages 总被引：1，自引：0，他引：1
Construction in a new neighborhood in the israeli town of Dimona, situated in an arid region in the south of the country (150
mm average annual rainfall), resulted in a rise in groundwater levels during the subsequent rainy seasons This caused flooding
of shelter basements, soil sliding, and sagging which permanently damaged walls and buildings The neighborhood had been built
on continental sands and marls blanketed by loess, on a valley slope near a rocky anticlinal dip-slope
Subsurface studies, using piezometer holes and groundwater analyses, revealed the presence of sand lenses alternating with
plastic marls, which act as seasonal aquifers with perched water tables Groundwaters obtain high SO
4
−2
and Cl− corrosivity through contact with these nonflushed marls of the Neogene valley fill (Hazeva Formation)
The reasons for the rising of groundwater were found to be (a) artificial interference with the natural (pre-construction)
drainage system—interception of the hillside runoff by building plots, roads, etc, (b) partial denudation of the loess blanket,
increasing the local infiltration and the build-up of local, perched water tables, and (c) corrosion of concrete and steel
pipelines, as well as foundations, by prolonged contact with corrosive groundwater, resulting in haphazard but massive leakage
Guidelines are proposed for an environmental improvement plan, which would include terracing and planting of the watershed
above town to increase evapotranspiration, lowering of the water table by pumping, and diverting the water to suburban parks
(groves of saltresistant trees), and replacement of steel and cement pipes by a non-corrodable plastic pipe system 相似文献
3.
单窗算法的大气参数估计方法 总被引：95，自引：10，他引：95
根据地表热辐射传导方程,提出了一个简单可行且精度较高的专门用于从TM6数据中演算地表温度的方法——单窗算法.这一算法把大气和地表状态对地表热传导的影响直接包括在演算公式中.该方法需要两个大气参数进行地表温度的演算,即大气平均作用温度和大气透射率.本文论述这两个大气参数的估计方法:根据大气水分含量或地表附近空气湿度来估计大气透射率;通过分析标准大气剖面资料,尤其是大气水分和气温随高程的变化规律,根据地表温度推算大气平均作用温度. 相似文献
4.
We developed kinetic theory for the charging processes of small dust grains near the lunar surface due to interaction with the anisotropic solar wind plasma. Once charged, these dust grains, which are exposed to the electric field in the sheath region near the lunar surface, could loft and distribute around such heights off the surface where they reach equilibrium with the local gravitational force. Analytical solutions were derived for the charging time, grain floating potential, and grain charge, characterizing the charging processes of small dust grains in a two-component and in a multi-component solar wind plasma, and further highlighting the unique features presented by the high streaming plasma velocity. We have also formulated a novel kinetic theory of sheath formation around an absorbing planar surface immersed in the anisotropic solar wind plasma in the case of a negligible photoelectric effect and presented solutions for the sheath structure. In this study we combined the results from these analyses and provided estimates for the size distribution function of dust that is expected to be lofted in regions dominated by the solar wind plasma, such as near the terminator and in nearby shadowed craters. Corresponding to the two dominant streaming velocity peaks of 300 and 800 km/s, mean dust diameters of 500 and 350 nm, respectively, are expected to be found at equilibrium at heights of relevance to exploration operations, e.g., around 1.5 m height off the lunar surface. In shadowed craters near the terminator region, where isotropic plasma should be dominating, we estimate mean lofted dust diameter of 800 nm around the same 1.5 m height off the lunar surface. The generally applicable solutions could be used to readily calculate the expected lofted size distribution near the lunar surface as a function of plasma parameters, dust grain composition, and other parameters of interest. 相似文献
5.
Arnon ARAD 《水文科学杂志》2013,58(1):122-146
ABSTRACT The regional groundwater groups of central Israel include:
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bicarbonate waters representing the replenishment areas;
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chloride waters representing the confined and the base-level zones;
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sulfate waters of the intermediate zones (fig. 2).
6.
Monitoring desertification by remote sensing using the Tasselled Cap transform for long-term change detection 总被引：2，自引：0，他引：2
Sensitive areas like oases are threatened by climatic variations and human activities that can catalyze desertification processes. Remote sensing the Earth surface from satellites is a good tool to monitor such types of change through several techniques. In this paper a remote sensing method that has been widely used for vegetated areas is adapted to study dry regions. The method consists of a combination of the Change Vector Analysis and the Tasselled Cap (TC) transform. To adapt it to dryland conditions a new set of parameters for the TC transform is hereby calculated for the Landsat 8 OLI system. The new TC parameters are tested in the analysis of the surface change in Azraq Oasis, Jordan, over a time span of 30 years (1984–2013) for Landsat satellites images. Azraq is considered a good testing site since in the early 1990s it has been subject to a complete drying up of the superficial springs, mainly due to over-exploitation of the groundwater basin. Results show that the chosen technique is able to detect the expected change on the surface, consistent with photo-interpretation and historical information available. 相似文献
7.
用陆地卫星TM6数据演算地表温度的单窗算法 总被引：263，自引：3，他引：263
陆地卫星 TM数据 (TM6)热波段表示地表热辐射和地表温度变化。长期以来 ,从 TM6数据中演算地表温度通常是通过所谓大气校正法。这一方法需要估计大气热辐射和大气对地表热辐射传导的影响 ,计算过程很复杂 ,误差也较大 ,在实际中应用不多。根据地表热辐射传导方程 ,推导出一个简单易行并且精度较高的演算方法 ,把大气和地表的影响直接包括在演算公式中。该算法需要用地表辐射率、大气透射率和大气平均温度 3个参数进行地表温度的演算。验证表明 ,该方法的地表温度演算较高。当参数估计没有误差时 ,该方法的地表温度演算精度达到 <0 .4℃ ,在参数估计有适度误差时 ,演算精度仍达 <1 .1℃。因该方法适用于仅有一个热波段的遥感数据 ,故称为单窗算法。 相似文献
8.
Arnon Golan 《Urban geography》2013,34(5):721-734
In this article, I analyze Tel Aviv’s Rothschild Boulevard as an example of an urban symbol and suggest that while main streets, avenues and boulevards are usually perceived as integral parts of the urban symbolic ecology, they are rarely considered as exclusive urban icons in their own right. Although prestige of “privileged” streets influences reputations of cities and constitutes an important part of their imaginary, their complicated physical structure and multifunctional character conflict with their iconic status. The physical nature of streets resists configuration and articulation as exclusive, durable urban icons because symbols are generally conspicuous physical objects that can be directly interpreted and rendered as iconic. 相似文献
9.
M. Sprintsin A. Karnieli S. Sprintsin S. Cohen P. Berliner 《Journal of Arid Environments》2009,73(10):955-962
This paper describes evaluation of forest stand density combining satellite imagery with forest inventory data set. The degree of canopy cover is described in terms of fractional vegetation cover (FVC) obtained by a linear mixture model applied on multi-spectral IKONOS image and canopy cover (CC). CC was calculated from field measurements of crown width of 646 standing trees sited within 72 circular (200 m2) plots. A comparison between CC and FVC shows that the former can be accurately represented by the latter linking in-situ measured forest characteristics with surface reflectance measured by a satellite.Stand density expressed as an absolute term (number of trees per unit area) showed high and significant positive correlation to FVC (R2 = 0.96) and to relative density measure (Crown Competition Factor; R2 = 0.89).In order to show the applicability of the presented approach for managerial practices, a map of the spatial distribution of stand density within the forest was produced using the above-mentioned correlations. Its quality was verified against an independent data set of ground measurements. The correlation between field- and map-based number of trees per unit area was found to be satisfactory (R2 = 0.4; p < 0.05), even though a slight lack of sensitivity was evident for low-density stands. 相似文献
10.