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931.
湘西金矿尾矿—水相互作用:1.环境地球化学效应   总被引:8,自引:2,他引:8  
湘西金矿在生产过程中产生了大量的尾矿。该区尾矿-水相互作用强烈,并引起了尾矿中重金属元素的释放、迁移和对水体-土壤、蔬菜等表生环境的重金属污染。污染程度较大的元素均为Au、Sb、As、Cd、Hg、W等,与尾矿中元素的富集特征相一致。尾矿中重金属元素的水迁移能力由大到小顺序为Au、Cd、W、Sb、Pb、As、Zn、Cu。元素的生物吸收系数由大至小顺序为Cd、Au、Zn、Hg、Sb、Cu、Pb、As、W。植物中金属元素浓度主要受土壤中的浓度、植物种类和吸收的影响。  相似文献   
932.
Identification of system parameters with the help of records made on base-isolated bridge during earthquakes provides an excellent opportunity to study the performance of the various components of such bridge systems. Using a two-stage system identification methodology for non-classically damped systems, modal and structural parameters of four base-isolated bridges are reliably identified using acceleration data recorded during 18 earthquakes. Physical stiffness of reinforced concrete columns, dynamic properties of soil and foundation impedance are found by available theoretical models in conjunction with pertinent information from the recorded accelerographs. Soil–structure interaction (SSI) effect in these bridges is examined by comparing the identified and physical stiffness of the sub-structure components. It is found that SSI is relatively pronounced in bridges founded in weaker soils and is more strongly related to the ratio of pier flexural stiffness and horizontal foundation stiffness than soil shear modulus, Gs, alone. However, substantial reduction in Gs is observed for moderate seismic excitation and this effect should be taken into account while computing foundation impedance.  相似文献   
933.
Hydrobiogeochemical processes controlling stream water chemistry were examined in four small (<5 km2) catchments having contrasting bedrock lithologies in the western Sierra Nevada foothills of California. The Mediterranean climate with its cool/wet and hot/dry cycle produces strong seasonal patterns in hydrological, biological and geochemical processes. Stream water solutes fall into three general groups according to seasonal fluctuation in concentration: strong, rainy season minimum–dry season maximum (Cl, SO42−, base cations); weak, rainy season minimum–dry season maximum (Si); and rainy season maximum–dry season minimum (NO3 and K+). Solute dynamics in soil solutions and stream water suggest that mixing of drainage waters from bedrock and soil sources regulate stream water solute concentrations. Patterns are further altered by the leaching of solutes accumulated in the soil over the summer period of desiccation and the temporal discoupling of nutrient cycles that occurs due to differences in the timing between vegetation growth (late spring) and leaching (early winter). Solute concentrations are remarkably similar between watersheds with varying bedrock types, with the exception of nitrate, sulfate and bicarbonate. Three watersheds have nitrogen-bearing metasedimentary bedrock that contributes to elevated nitrate concentrations in stream waters. Watersheds whose bedrock includes mineralized veins of sulfide and carbonate minerals similarly have greater sulfate and bicarbonate concentrations in stream water. Hydrobiogeochemical processes are highly dynamic at the seasonal and storm-event temporal scales and spatially complex at the watershed scale making management of stream water chemical composition, such as nitrate concentrations, very challenging.  相似文献   
934.
Much of the development literature and the theory of urban transition have been based on an arbitrary division of production space into city and countryside. Despite growing recognition of the need for an integrated approach to urban‐rural relations, controversial issues related to the definition and measurement of the phenomenon remain unresolved. This case study of spatial transformation in China's Pearl River Delta analyzes with greater precision the geographic extent and functional attributes of a zone of urban‐rural interaction located outside and between major metropolitan centers. This zone has been the spatial focus of industrial and commercial development, although most of its population remains officially classified as “agricultural.” The peri‐urban zone was initially left behind by the central cities in terms of its contribution to the regional economy. After a decade of postreform development, this zone has moved ahead of the central cities and become the region's main destination for in‐migrants and foreign investment. The growth of the zone of urban‐rural interaction outside the central cities has absorbed a significant amount of the increased urban population, but it has not brought about a reduction of regional economic inequality because of the persistence of a backward economy in the periphery. Theoretical questions are raised concerning the validity of several fundamental assumptions underlying the conventional model of urban transition.  相似文献   
935.
离散气候系统中的周期与混沌   总被引:1,自引:0,他引:1       下载免费PDF全文
从零维气候模式导出了一个非线性映象公式,对由该公式表征的气候系统的平衡态和稳定域进行了研究。通过迭代计算揭露海洋热贮存C对气候系统的调控作用。计算结果表明,存在一个控制气候系统行为的很窄的C值敏感区;当C值大于敏感区上界时,气候系统趋向平衡态,即现代气候;当C值小于敏感区下界时,系统失稳。在敏感区内则呈现出周期与混沌行为,且随着C的增加,勾画出通过周期倍分岔通向混沌的道路。  相似文献   
936.
Given time-independent monthly mean sea temperature,numerical simulation was done of the path of the tropicalcy clone Forrest and its related physical quantity field in terms of the improved version of the σ-coordinate 10-level primitive equation model for tropical cyclones developed by the Guangzhou Institute of Marine Meteorology.Result ssuggest the similarity between the simulated and observed physical quantity fields except that the simulated path was to the right of the observed,with the deviation increasing with time.Sea and tropical cyclone,in effect,interact mutually.In an attempt to compare the results from coupling and uncoupling experiments,an oceanic mixed layer model was formulated based on experiments with sea response to cyclone and integrated in synchronous coupling with the aforementioned version of tropical cyclones,the computational domain covering the western North Pacific with the coastal configuration involved.The coupling experiment shows that the negative feedback of the interaction between sea and mature cyclone leads to weaker sea response as compared to the uncoupling case.Except for the location of the divergence core of oceanic current,the mixed layer depth and inhomogeneous distribution of sea surface temperature (SST) caused by the cyclone-core position and intensity,the values of the maximum oceanic current,departure of the mixed layer depth and SST drop were smaller in the coupling than in the uncoupling case,and so was the maximum wind near the cyclone core.The path from the coupling run is to the left of the course in the uncoupling experiment but closer to the observed one though remaining somewhat leftward.Even on a scale of less than 3 days,the effects of sea and sea-cyclone interaction on the cyclone were by no means negli-gible.  相似文献   
937.
天津局地气候的反演建模及其研究   总被引:25,自引:1,他引:25  
林振山  史芳斌  王辉 《气象学报》1995,53(1):115-121
利用天津月平均温度T、气压P和雨量R的时间序列反演出一组近似描写天津(T-P-R)局地气候的动力方程,并对其演化特性及内部相互作用机制进行了研究。  相似文献   
938.
In this paper the relationships between the sea surface temperature (SST) of Xisha and that in the northern Indianand northern Pacific Oceans,the geopotential height at 500 hPa level of the Northern Hemisphere,and rainfall in Chinaare studied statistically using data in the period of 1961—1992.Results show that in winter,the interannual variation inSST of Xisha describes that for a large oceanic region off the East Asia coast,and is closely related to the activity of EastAsia winter monsoon.On the other hand,there exist very high values of auto-correlation of Xisha SST anomaly fromDecember through the following July,but the anomalous condition is hardly correlated to that in the preceding autumn.The winter monsoon related anomalous SST condition in Xisha has a strong tendency to persist through the succeedingsummer monsoon season with the same sign.In addition,correlation maps of monthly mean rainfall in China with re-spect to Xisha SST of the same month show positive correlations with confidence level above 95% to the east of 110°Eand to the south of Changjiang (Yangtze) River during the months of October through April;the region becomes smal-ler in May and changes correlation sign in June;the positive correlation region is located in the middle and lower reachesof Changjiang River from July to September.The air-sea interaction plays an important role in these processes.  相似文献   
939.
In this paper, the coupling equations describing nonlinear three-wave interaction among Rossby waves including the forcing of an external vorticity source are obtained. Under certain conditions, the coupling equations with a constant amplitude forcing, the stability analysis indi-cates that when the amplitude of the external forcing increases to a certain extent, a pitchfork bifurcation occurs. Also, it is shown from numerical results that the bifurcation can lead to chaotic behavior of “strange” attractor. For the obtained three-variable equation, when the amplitude of modulated external forcing gradually increases, a period-doubling bifurcation is found to lead to chaotic behavior. Thus, in a nonlinear three-wave coupling model in the large-scale forced barotropic atmospheric flow, chaotic behavior can be observed. This chaotic behavior can explain in part 30-60-day low-frequency oscillations observed in mid-high latitudes.  相似文献   
940.
The Singular Cross Spectrum Analysis(SCSA) method was employed to investigate the coupled-periods of air-sea/mid-low circulation interaction using 1951-1993 500-hpa geopotential heights and the sea surface temperature(SST)in the Northern Hemisphere. Results show that air-sea correlation is noticeable on the 3-7 year scale which is similar to ENSO circle. In this sense, ENSO is a Strong signal. Quasi-ten/quasi-four year periods are prominent in the mid-low interaction, and quasi-if our year oscillation is uniform with the ENSO circle.Studies indicate that the mid-low interaction possess quasi-ten year oscillation beside being affected by ENSO.  相似文献   
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