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Based on hydrogeological data and groundwater chemical analysis data and the theory and methodologies of groundwater chemical dynamics in combination with limited pumping test data, some groundwater chemical index such as activity of component、mineral saturation index are calculated and some hydrogeological parameters such as hydraulic conductively,transmissibility,artual speed of groundwater、specific velocity and groundwater age are also calculated zonally.The above calculation results are beneficial to quantificationally recognize the local hydrogeological conditions and to attest that the confined aquifer of Taconic formation has good permeability and transmissibility and t good renewal ability because of the active groundwater movement.

依据已有水文地质和水质分析资料,运用地下水化学动力学理论和方法,通过水化学指标(组分活度α、矿物饱和指数β)的计算分析,结合有限的抽水试验资料,分区计算出渗透系数K、导水系数T、地下水实际流速U、渗透速度V和地下水年龄t等5项水文地质参数,定量的认识水文地质条件,认证了水源地泰康组承压含水层具有渗透性强、导水性强、地下水循环交替快、可更新能力强等特点。

The relation between the coseismic changes of water level and water temperature of artesion well has been analyzed by use of the coseismic data of Ms8.7 Sumatera earthquake and the structure information of well-aquifer system in the studied area. The physical model is established by simulating the changes of water temperature and water level of the well. The mechanism of coseismic response to distant earthquake in such artesian well is also revealed.

利用本溪自流井水位及水温对苏门答腊Ms8.7大震的同震响应资料,通过分析水位变化与水温变化的相互关系和研究区的井-含水层系统结构,建立了不同层位地下水混合的物理模型,并根据水位变化数据模拟出水温变化曲线,同时也揭示了同类型观测井水位与水温对远场大震的同震响应机理。

In order to solve the problems of dewatering and hydraulic connection among the multi-aquifer system in the excavation of the pits of the Dasi deep well gate and the lock gate,pumping tests were conducted in the field and the characteristics of groundwater transport in the ③_2 and ⑤ find sands were analyzed.

为了解决大寺深孔闸、船闸基坑开挖时的降排水工作及多层含水层的相互联通关系,我们进行了现场抽水试验,查明了拟建场地地基土③2层极细砂和⑤层极细砂的地下水运移特征,提出了基坑开挖应采取的排水措施。

In order to analyze the influence and damage of the top and bottom of rock mass in floor water-resisting layers due to water pressure in water bearing layer and mining pressure, this paper applies the methods of similar material simulation test and mechanical analysis of floor water invasion in the near of faultage to further comprehend the mechanism of floor water invasion.

为了分析底板含水层水压及采动矿压对底板隔水层岩体上部与下部的影响与破坏,应用了相似材料模拟试验以及断层附近底板突水的力学分析方法,对底板突水机理有了进一步的认识;同时,由断层附近底板突水的力学分析方法所得到的理论计算结果,也可以作为判别类似条件下遇断层时承压水体上采煤是否安全的依据。

The method of determination of hydrographical and geological parameters in water bearing layer of site by pumping test adopted for car dumper shed of Phase One Project of Huanghua Port was introduced in the paper.

介绍黄骅港一期工程翻车机房采用抽水试验确定场地含水层水文地质参数的方法,并对地基处理所造成的影响进行了初步探

Base on the GIS technology, PI and COP methods are applied to the frangibility assessment research of Jinan karstic aquifer.

本论文基于GIS技术,应用了欧洲方法中的PI方法和COP方法对济南泉域岩溶含水层的脆弱性进行了评价研究。

The research aim is to make certain relatively class and area of jinan karstic aquifer to the pollution of human being activity, to provide technical sustain to the protection of the karstic water resources, soil and resources exploritation in reason and layout of city construction.

本次研究的主要目的就是通过评价,确定济南泉域含水层容易受到人类活动污染的相对级别及范围,为济南泉域岩溶水资源的保护、国土资源的合理开发与城市建设的规划提供技术上的支持。

In order to know the characteristics of water-rock interaction and the sources of the contaminants in the ground water system of the karstic area,we carry out a study on the water geochemistry of the surface and ground water in Guiyang,the capital city of Guizhou Province,China.

为了解喀斯特地区水-岩相互作用特征和辨别地下水污染物的来源,为揭示人类活动对喀斯特地下水文地球化学环境的影响,研究了贵州省贵阳市不同岩性含水层地下水和地表水的化学特征。

The solution analysis indicates that both the silt layer and the leakance of the semi-permeable layer influence significantly the hydraulic head fluctuation in the confined aquifer.

分析表明弱透水层的越流和淤泥层的存在均对承压含水层水头波动有显著影响。

These colorless crustaceans are among the few creatures that have adapted to the lightless world at the bottom of the region's aquifers, springs, and sinkholes.

在这个无光的世界中,只有深海含水层与落水洞,犹如坠入淡水迷宫一般。

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