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排序方式: 共有41条查询结果,搜索用时 31 毫秒
1.
汾河口傍河水源地激发补给量研究   总被引:2,自引:0,他引:2  
该文阐述傍河水源地地下水资源构成和补给特性。利用野外试验与室内数值模拟相结合方法,分析汾河口傍河水源地可采水资源量,数值模型刻画黄河实际摆动边界,考虑潜水延迟给水和极端干旱气候条件等多种方案;利用环境同位素技术追踪傍河水源地开采条件下的河水激发补给过程和补给强度。研究表明,在渗透性较好的常年性河流旁建立的水源地,具有抵御极端气象、水文环境以丰补歉的能力,枯水年动用的含水层储存量。丰水年恢复性强。  相似文献   
2.
The Vinalhaven intrusive complex consists mainly of coarse-grainedgranite, inward-dipping gabbro–diorite sheets, and a fine-grainedgranite core. Small bodies of porphyry occur throughout thecoarse-grained granite. The largest porphyry body (roughly 0·5km by 2·5 km) occurs with coeval gabbro, hybrid rocks,and minor fine-grained granite in the Vinal Cove complex, whichformed during the waning stages of solidification of the coarse-grainedVinalhaven granite. Porphyry contacts with surrounding coarse-grainedgranite are irregular and gradational. Compositions of wholerocks and minerals in the porphyry and the coarse-grained graniteare nearly identical. Neighboring phenocrysts in the porphyryvary greatly in degree of corrosion and reaction, indicatingthat the porphyry was well stirred. Thermal rejuvenation ofa silicic crystal mush by a basaltic influx can explain thecomposition and texture of the porphyry. Comparable rejuvenationevents have been recognized in recent studies of erupted rocks.Weakly corroded biotite phenocrysts in the porphyry requirethat hydrous interstitial melt existed in the granite duringremelting. Field relations, along with thermal calculations,suggest that cooling and crystallization of coeval mafic magmacould have generated the porphyry by thermal rejuvenation ofgranite crystal-mush containing about 20% melt. Field relationsalso suggest that some of the porphyry matrix may representnew felsic magma that was emplaced during remelting. KEY WORDS: granite; magma chamber; mafic replenishment; rejuvenation  相似文献   
3.
环境同位素法在西北地区地下水资源评价中的应用   总被引:6,自引:0,他引:6  
高志发 《甘肃地质》1995,4(1):62-72
应用环境同位素方法测定了不同类型地下水的年龄,识别了西北干旱、半干旱地区地下水的补给源,进行了补给量的计算,建立了地下水流系统,并取得了新的成果。  相似文献   
4.
浅谈地下水流模拟中河流的处理方法   总被引:3,自引:0,他引:3  
谭杰  王杰  杨操静 《地下水》2006,28(4):28-30
本文分析了河水与地下水不同作用形式下的补排关系,给出了河流在地下水流模拟中的两种处理方法.根据河流与地下水的相互作用规律将其概化为四种边界条件,并给出了在不同边界条件中河水与地下水交换量的计算公式,初步建立了河水与地下水的解析耦合模型.  相似文献   
5.
S. Lallahem  J. Mania 《水文研究》2006,20(7):1585-1595
Chalk crops out from a wide belt around the Paris basin, France, covering an area of about 70 000 km2. In this region, the chalk presents the most important unconfined aquifer because of its extent and the size of its resources ((11–12) × 109 m3 year?1). The assessment of underground outflow depends on the vertical feeding, the infiltration and the hydrometry. This paper analyses the regional structural map, interprets the groundwater reaction under rainfall, explains the water circulation in such media where the reservoir geometry plays an essential role on aquifer response, and determines different aquifer physical parameters. Attempts are made to identify the rapid transfer of groundwater at the level of faults and their important fissures. Based on a quantitative study of the seasonal and interannual piezometry fluctuations, it is noted that the mode and the piezometric chronology events are controlled by major parameters of geological and hydrogeologic contexts, aquifer hydraulic characteristics, the position of upstream and downstream basin limits, groundwater depth and replenishment time. This paper ends with determination of groundwater physical parameters of the diffusivity (T/S, T and S) values by examination of the groundwater replenishments periods. Copyright © 2005 John Wiley & Sons, Ltd.  相似文献   
6.
陶芸  陈锁忠  都娥娥 《水文》2011,31(3):76-81
在分析研究区浅层地下水空间分布特征的基础上,采用同位素与化学分析相结合的方法研究苏锡常浅层地下水的补径排条件。利用氢氧同位素的分析结果,建立潜水与微承压水的δD-δ18O关系曲线,分析潜水含水层与河流、湖泊等地表水体关系以及微承水的蒸发程度;利用放射性同位素氚与14C研究微承水与现代水的补给关系;利用常规的水化学分析方法研究浅层地下水补给源的变化问题。结合研究区地下水水位、地层岩性、地形、地貌等多方面因素综合分析了浅层地下水的补径排条件,从而指导苏锡常地区浅层地下水合理开发利用。  相似文献   
7.
单轴压力下有补给水岩石电阻率变化各向异性研究   总被引:18,自引:1,他引:18  
安金珍  修济刚 《中国地震》1996,12(3):300-306
将两种规格的长方体水饱和花岗岩标本,以标本一个面的中心点为中心,对称布置成互成45°角的4条对称四极法电阻率测线。标本电极面和相邻面的一小部分用防水环氧胶密封,使标本在装有水的承压水箱中,沿标本长轴方向受压,观测标本视电阻率随压力的变化。实验结果为:(1)有补给水实验与无补给水实验,电阻率变化整体形态相似,即电阻率随压力的变化先上升,后下降,但有补给水实验的电阻率下降幅度要大一些。(2)电阻率变化出现明显的方向性,可以用电阻率变化最大的各向异性主轴方向表示;实验中,用4条测线、4种组合(每3条测线组合可以确定1个视电阻率变化各向异性主轴方向)方法确定的4个电阻率变化各向异性主轴方向基本一致。(3)加压期间,电阻率各向异性主轴方向随压力增加发生变化,这种变化不是渐变和乱变,而是有规律的跃变,即整个实验过程,多数标本只跃变1—3次,每次跃变形成一个主方向,在主方向内,角度变化不大。(4)有补给水岩石电阻率变化整体形态与美国Brace等(1968)所作的围压和孔隙压的岩石电阻率变化形态相似。  相似文献   
8.
The recovery capacity of shallow Posidonia oceanica meadows degraded by beach replenishment eighteen years before was assessed in two impacted meadows and compared with other two undisturbed localities. Inside each locality, we selected randomly three sites separated by 500–1000 m. At site level we study the vitality of P. oceanica meadow assessing the vegetative growth, leaf characteristics, and non-structural carbohydrates of the plants. Additionally, at locality level, silt-clay fraction, organic matter, pH and light intensity incident on the sea bottom were measured to evaluate the environmental conditions. Covering of P. oceanica was significantly lower at the impacted localities while amount of dead “matte” was higher. Leaf production of horizontal rhizomes (14.6 ± 1.11 vs 19.47 ± 1.45 leaves y−1), net total rhizomes recruitment (2.33 ± 0.17 vs 4.3 ± 0.33 branches y−1) and starch concentration (43.625 ± 0.67 vs 54.45 ± 0.74 mg per g of rhizome) at impacted meadows were significantly lower than controls. Leaf features, epiphytes biomass, colonization, elongation and horizontal and vertical rhizome production did not show significant differences. Sediments at impacted localities contained higher silt-clay fraction and higher organic matter load while pH was lower. Light intensity on the sea bottom measured at all localities was over the minimum light requirements estimated for P. oceanica. Our results show that the press impact produced by beach replenishment was enduring in the time slowing natural recovery by 45%. This impact may be related with changes in the sediment features.  相似文献   
9.
基于DEM的清水河分布式水文模型   总被引:1,自引:1,他引:1  
对于以冰雪融水和雨水混合补给为主的西北山区流域,需要结合山区特点建立分布式水文模型。通过取塔里木河流域中的清水河水系为研究区域,采用300 m×300 m DEM数据进行流域河网水系提取,同时用DEM数据对参数进行分布式异化,建立冰雪融水与降雨相结合的分布式水文模型。分析模拟结果表明:夏季模拟径流主峰值与实测径流值较为接近,而冬春季节两者之间的差别较大,反映了西北山区流域冰雪融水和雨水混合补给为主的特点;进而开拓塔里木河区域应用该类模型的可行性。  相似文献   
10.
高架索海上补给装置在小型船舶补给上的应用   总被引:9,自引:0,他引:9  
针对现有高架索补给系统,在补给方式、波浪补偿装置、吊钩和接受端方面进行改进,提出适合小型船舶补给作业的补给系统;并在此基础之上对补给中关键参数进行计算,计算结果表明,此系统可以保证补给过程顺利实施,适合小型船舶补给需求。  相似文献   
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