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《四川建筑》2021,41(4)
济枣高铁济泰段通过济南南部的千佛山、慧佛山,其为济南泉群的重要补给区,铁路建设对济南泉群或多或少产生一定影响。文章基于研究区区域地质、水文地质及地下水的补给、径流和排泄、测区地下水动态变化特征等研究,分析评价拟建济枣高铁济泰段对济南泉群的影响,并探讨其防治对策。主要结论有:(1)拟建济枣高铁济泰段主要处于济南单斜地质单元,地层岩性以寒武系-奥陶系的碎屑岩和碳酸盐岩为主,中强富水性;(2)济南泉群主要以其南部的千佛山、慧佛山降水补给为主,其次为河床渗落、孔隙水补给;(3)拟建铁路推荐线位对济南四大泉群的补给、径流影响较小;比选线位对趵突泉和涌泉泉域影响较小,对白泉泉域无影响;(4)工程防治对策首先应遵循铁路轨面标高处于泉群补给区垂直渗流带的地质选线原则,其次隧道设计施工中坚持以堵为主、疏排为辅的综合治理措施。研究成果可为测区类似工程提供借鉴指导。 相似文献
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晋陕峡谷地区岩溶地下水的同位素及水化学分析 总被引:1,自引:0,他引:1
本文研究采用同位素和水化学分析的方法对本地区 2个泉域即天桥和柳林泉域的地下水系统进行分析。研究发现 :(1)天桥泉域北部大部分地区岩溶地下水主要接受了大气降水的补给 ,同时在局部地区也接受了地表水的补给 ;天桥泉域南部岩溶地下水接受了不同高程的大气降水的补给 ,迳流较为活跃。 (2 )柳林泉域岩溶水系统存在浅部和深部 2个子系统 ,来自这 2个系统的地下水互相混合 ,形成了排泄区较为复杂的地下水化学类型 相似文献
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宜万铁路马鹿箐隧道途经岩溶强烈发育、水文地质条件复杂的灰岩地层,地下暗河管道错综复杂。为了确定马鹿箐隧道区小马滩地下暗河系统与突水溶洞之间的水力联系及暗河系统的补给、径流和排泄条件,采用工业盐(NaCl)作为示踪剂的地下水单元(单一示踪剂)示踪试验方法进行探测。本次试验发现小马滩地下暗河是单一管道流地下暗河,以大气降雨、小马滩上游地表水及地下水为补给源,以蝌蚂口泉群为集中排泄点,龙潭是该暗河系统的天窗。小马滩地下暗河系统地下水流速快,地表水与地下水交替转化迅速,隧道岩溶突水与小马滩伏流的水力联系较弱。 相似文献
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广州市水文地质特征分析 总被引:4,自引:0,他引:4
综合分析了广州市地下水形成的自然条件、地下水的类型、分布状况、水文地质特征和补给径流排泄条件。为有效管理广州市地下水资源,实施地下水资源的监测与保护提供了详实的依据。 相似文献
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数学(物理)模拟计算中的降雨补给处理 总被引:2,自引:0,他引:2
在地下水和地表水的数学(物理)模拟计算中,降雨补给量的计算是非常重要的内容。本文讨论了有效降雨和无效降雨、降雨的滞后作用、降雨强度及降雨的均匀性对补给的作用,进而给出以月降雨量为单位的补给函数和以日降雨量为单位的补给参数,对水资源评价等涉及到大气降雨补给的计算有重要意义。 相似文献
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当场地存在多层层间有一定水力联系的承压含水层时,基坑内降水可引发基坑止水帷幕墙底以下的承压含水层的水头下降,并相应引起坑外多个含水层水位降低,若对所有层进行回灌则将导致成本大幅提高,此时可对某一层回灌,通过越流对其他含水层进行水位补给。通过在天津地铁某车站基坑所在场地开展抽水试验、单井回灌试验、先抽后灌试验对基坑内外的水力联系、不同含水层间的水力联系和隔层回灌的效果进行了研究。结果表明,由于各含水层间之间有一定水力联系导致竖向越流补给较强,基坑内疏干降水可引起坑外承压含水层水头下降并引起坑外地层沉降。对基坑外第Ⅰ微承压含水层进行回灌可有效对其上部潜水层和下部第Ⅱ-1承压层的水头起到抬升作用,通过隔层回灌从而控制其水位下降导致的坑外沉降。对第Ⅰ承压含水层进行回灌对基坑外第Ⅱ-2承压层水位抬升也有一定的作用,但是尚不足以使其因基坑内降水引起的坑外水位下降值完全恢复,建议结合设置此层的备用回灌井以控制其水位下降。 相似文献
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This paper reviews methods of estimating recharge for a wide variety of aquifers in Britain. A soil moisture balance technique is used with direct representation of relevant soil and crop properties. Recharge contributions due to rainfall, runoff from impervious areas and leaking water mains and sewers are considered. In many field situations low permeability strata, which overlie the main aquifer, modify the timing and magnitude of the actual recharge. Runoff from less permeable strata can become runoff-recharge at the aquifer outcrop. Reference is made to several case studies. 相似文献
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《Water research》1986,20(9):1119-1127
Results of a pilot plant study on the influence of the composition of sandy soil on water quality changes during groundwater recharge of pretreated Rhine water are presented. It is confirmed that content and nature of the soil organic matter substantially affect the quality of the percolating water. Recharge in the sand with a higher content of unstable organic matter (0.76% OC), under anaerobic conditions (Eh ∼ + 100 mV) resulted in an increase of COD, DOC, colour, NH4+, PO43−, Fe, Mn, SiO2 and As content. On the other hand the concentration of trihalomethanes, tetrachloromethane, 1,1,1-trichloroethane, tetrachloroethene, haloacetonitriles, nitro-aromatics and the mutagenic activity decreased during the recharge. Passage through the sand with lower content of stabilized organic matter (0.22% OC), under anaerobic conditions (Eh ∼ + 200 mV), showed a similar but less pronounced effect. In the sand with very low content organic matter (0.04% OC) under aerobic conditions, a moderate improvement of macroconstituents and trace elements was observed. From the organic micropollutants studied only brominated trihalomethanes were transformed here to a degree increasing with the bromine content. Adsorbable and extractable halogenated organic compounds formed by the chlorination of the recharge water, characterized with the group parameters (AOX and EOX), were largely removed during the percolation in all sands examined. 相似文献
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《Urban Water Journal》2013,10(2):161-171
The qanat water supply technology, by which gravity drains mountain aquifers into valleys, is considered as a culturally appropriate and ecological sustainable design to meet freshwater development needs in northern Cyprus. This work provides a first-order analysis of the surface water budget to estimate qanat feasibility. The proposed qanat recharge area of 370 km2 is in the upper elevations of the limestone dominated Five Finger Mountain Range, is analysed using technical data reports, field visits, and satellite elevation data. Satellite based tropical rainfall measuring mission (TRMM) monthly rainfall totals at a 0.25° grid were tested for complementing sparse precipitation gauge data, but TRMM underestimated gauge observations by 43% in narrow zones of high rainfall during the wet winter months. A water budget for qanat supply used 30-year average gauge records within the qanat recharge region, which set annual precipitation at 529 mm year?1. A calibrated complementary relationship areal evapotranspiration model established atmospheric outputs at 222 mm year?1, slightly below the island-average of 280 mm year?1 estimated by the Cyprus Water Department. Recharge to the qanat aquifer was determined by subtracting evaporation from precipitation, and then allocating 50% of the remainder to environmental services. In the proposed qanat recharge region, this water budget yields an estimated recharge volume of 57 mm3 year?1. At less than 25% development, this volume satisfies the 13 mm3 annual deficit in northern Cyprus and protects against saltwater intrusion. Additional freshwater conservation measures in northern Cyprus are needed to ensure ecological sustainability in northern Cyprus. 相似文献
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A GIS-based DRASTIC model for assessing aquifer vulnerability in Kakamigahara Heights, Gifu Prefecture, central Japan 总被引:14,自引:0,他引:14
Vulnerability assessment to delineate areas that are more susceptible to contamination from anthropogenic sources has become an important element for sensible resource management and land use planning. This contribution aims at estimating aquifer vulnerability by applying the DRASTIC model as well as utilizing sensitivity analyses to evaluate the relative importance of the model parameters for aquifer vulnerability in Kakamigahara Heights, Gifu Prefecture central Japan. An additional objective is to demonstrate the combined use of the DRASTIC and geographical information system (GIS) as an effective method for groundwater pollution risk assessment. The DRASTIC model uses seven environmental parameters (Depth to water, net Recharge, Aquifer media, Soil media, Topography, Impact of vadose zone, and hydraulic Conductivity) to characterize the hydrogeological setting and evaluate aquifer vulnerability. The western part of the Kakamigahara aquifer was dominated by "High" vulnerability classes while the eastern part was characterized by "Moderate" vulnerability classes. The elevated north-eastern part of the study area displayed "Low" aquifer vulnerability. The integrated vulnerability map shows the high risk imposed on the eastern part of the Kakamigahara aquifer due to the high pollution potential of intensive vegetable cultivation. The more vulnerable western part of the aquifer is, however, under a lower contamination risk. In Kakamigahara Heights, land use seems to be a better predictor of groundwater contamination by nitrate. Net recharge parameter inflicted the largest impact on the intrinsic vulnerability of the aquifer followed by soil media, topography, vadose zone media, and hydraulic conductivity. Sensitivity analyses indicated that the removal of net recharge, soil media and topography causes large variation in vulnerability index. Moreover, net recharge and hydraulic conductivity were found to be more effective in assessing aquifer vulnerability than assumed by the DRASTIC model. The GIS technique has provided efficient environment for analyses and high capabilities of handling large spatial data. 相似文献
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Within the scope of the Sub-GATE-project (Submarine Groundwater Fluxes and Transport Processes from Methane Rich Coastal Sedimentary Environments), hydrogeology of the catchment area of the Eckernfoerde Bay within gehe whole Pleistocene succession down to the up-permost continous Tertiary aquitard was studied. This aquitard usually consists of clays of the Miocene Vierland-Stufe, which occur at 160 to 190 m bsl. Regional catchment areas of the most important aquifers and their main characteristics were estimated by evaluation of hydraulic and hydrochemical data from wells in this region. Groundwater in the Miocene aquifer in general is more reduced than groundwater in the Pleistocene aquifer, mainly due to the advanced activity of microorganisms. Recharge areas of the Pleistocene aquifer occur NW and S of Eckernfoerde, while recharge areas of the Miocene aquifer are situated in the SW of the study area and at the southern coast of the Eckernfoerde Bay. Some uncertainty arising from data aquisation at different times used in geostatistical regionalisation was accounted for by application of a fuzzy-kriging-procedure. 相似文献
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珠三角城边工业旧村在行政上是一种城市社区,但与普通城市社区的社区发展目标不同,它需要通过社区发展加快社区的城市化进程.城边工业旧村具有边缘优势、相对优势和后发优势三大潜在优势,逐一实现这些优势就是其社区发展路线,当前应结合更新改造变"边缘效应"为边缘优势,避免演变为成熟的城中村. 相似文献