北京市阳光广场降水与锚拉护坡桩工程施工设计及工艺     

曹新明  王建珍 《地质与勘探》1995,31(2):51-54

阐述了深基坑大面积基础工程的降水与护坡的设计原理，成井灌注桩施工工艺及实际应用效果，为深基坑大面积降水和锚拉护坡桩工程的进行提供了参考依据。  相似文献   

三明移动通讯大楼基坑降水设计方案比较分析   总被引：1，自引：0，他引：1  

吴开化 《福建地质》2006,25(2):102-106

通过对两种不同基坑降水的设计方案进行分析对比,阐述了降水技术要求,预防周边建筑物不均匀沉降的防治措施,从而提高工程设计的经济效益和社会效益。  相似文献   

Groundwater flow modeling in the Zhangye Basin,Northwestern China   总被引：1，自引：0，他引：1  

X. H. Wen  Y. Q. Wu  L. J. E. Lee  J. P. Su  J. Wu 《Environmental Geology》2007,53(1):77-84

The Zhangye basin is in the middle reaches of the Heihe River, northwestern China. Heavy abstraction of groundwater since the 1970s in the area is for agricultural, industrial and drinking water supplies and has led to a substantial decline in the potentiometric surface. A three-dimensional regional numerical groundwater flow model, calibrated under transient conditions, has been developed and used to predict the drawdown for the period from 2000 to 2030 under two different groundwater management scenarios.  相似文献   

三峡库区提升库水位下降速率条件下沟边上滑坡稳定性评价     

陈欢 《探矿工程》2018,45(9):60-65

三峡库区对非汛期库水位下降速率（0.6 m/d）的严格控制,预防了近千处涉水库岸滑坡大规模下滑入江,但控制消落期库水位下降速率在某种程度上却限制了防洪和蓄水发电效益的发挥,本文主要通过研究在非汛期时候,增加库水位下落速率是否具有可行性,使用Geo-studio中的SEEP/W、SLOPE两个模块对沟边上滑坡进行渗流分析和稳定性分析评价,以计算结果来确定库水位消落期的水位下降速率,对库区调控水位下降速率的调整有重大现实意义和科学价值。  相似文献   

层状孔隙裂隙热储最大允许水位降深研究——以德州市城区为例          下载免费PDF全文

杨询昌 《山东国土资源》2016,32(7)

当前,地热水最大降深如何确定方法很多,各地区因开采条件不同其最大允许降深也不完全相同。在基于地面沉降防控基础上以德州市城区为例,通过对地面沉降与深层地下地热水分析,建立起了地热水最大允许水位降深数值模型,并计算出新近纪明化镇组、馆陶组和古近纪东营组地热水开采最大允许水位降深值,确定了相似区域最大允许水位降深范围,这对层状孔隙裂隙热储地区热储最大允许水位降深确定和地热资源的可持续开发利用具有重要现实意义和理论参考价值。  相似文献   

Environmental impact assessment using FORM and groundwater system reliability concept: case study Jining, China   总被引：2，自引：0，他引：2  

Long Cang Shu  Pei Gui Liu  Basil T. Iro Ongor 《Environmental Geology》2008,55(3):661-667

In this paper, fist-order reliability method (FORM) is used to evaluate the impacts of uncertainties posed by traditional deterministic models on the environment in Jining, China. Because of groundwater contamination in shallow aquifer, and an increase in water demand, the new wells target the confined aquifer with constant pumping rate of 5,000 m³/d. Using Theis equation, the groundwater drawdown is analyzed to determine whether the confined aquifer will be contaminated. Although the piezometric level is higher than the phreatic level by 11.0 m, the risk of drawdown is still 19.49% when the pumping rate of 5,000 m³/d is maintained for 2 years. The deterministic model indicates a drawdown of 8.94 m which is lower than the maximum tolerance drawdown of 11.0 m. The sensitivity and uncertainty analysis reveal that the model result is more sensitive to transmissivity than specific yield, while the reliability analysis offers significant information for the decision makers. This approach exposes and minimizes the risk of undesirable consequences such as groundwater contamination.  相似文献   

库水位骤降时的滑坡稳定性评价方法研究   总被引：24，自引：5，他引：19  

刘新喜  夏元友  练操  张开鹏 《岩土力学》2005,26(9):1427-1431

三峡水库蓄水及水位波动,将极大地改变滑坡体内的水文地质条件,库水位骤降和暴雨入渗是导致滑坡的主要因素。库水位骤降时的滑坡稳定性评价是滑坡防治中的一个难题。根据三峡水库水位调控方案和库区滑坡地下水作用的力学模式,利用有限元模拟库水位从175 m骤降至145 m时的滑坡暂态渗流场。建立了渗透力作用下滑坡稳定性评价的不平衡推力法。研究表明：滑坡的渗透系数和库水位下降速度是影响滑坡稳定性的主要因素,当库区堆积层滑坡渗透系数小于0.864 m/d,库水位发生骤降为2 m/d。库水位骤降时滑坡稳定性降到最小的水位通常在175 m水位以下10～20 m处。其研究为库区 175 m水位滑坡治理提供了科学依据。  相似文献   

三峡澎溪河回水区高水位期间高阳平湖总磷模型   总被引：2，自引：1，他引：1  

赫斌  李哲  冯婧  肖艳  郭劲松 《湖泊科学》2016,28(2):295-302

三峡水库"蓄清排浑"的调度运行方式使得冬季高水位期间近岸消落带受淹.消落带氮、磷等营养物受淹后向水体中释放与积累对冬末初春的水华将可能具有重要贡献.构建高水位时期澎溪河高阳平湖总磷收支模型,定量分析高水位期间总磷的收支途径、累积量以及累积磷的主要来源.结果表明:蓄水期,由于蓄水水位升高和顶托而导致大量磷积累;稳定期,磷收支变幅较小,总体趋于平缓;水华期,前期积累的磷被大量消耗,形成水华.淹没消落带磷释放是冬季高水位时期高阳平湖总磷的主要来源,蓄水期所淹没大量消落带所释放的磷为冬季末水华暴发提供条件.研究结果为后续定量分析磷形态的转化和分配奠定重要基础.  相似文献   

Analytical approach for time‐dependent groundwater inflow into shield tunnel face in confined aquifer          下载免费PDF全文

Xiao‐Xue Liu  Shui‐Long Shen  Ye‐Shuang Xu  Zhen‐Yu Yin 《国际地质力学数值与分析法杂志》2018,42(4):655-673

Prediction of time‐dependent groundwater inflow into a shield tunnel is a significant task facing engineers. Published literature shows that there is no available method with which to predict time‐dependent groundwater inflow into a tunnel. This paper presents a prediction approach for time‐dependent groundwater inflow into a tunnel in both anisotropic and isotropic confined aquifers. The proposed solution can predict groundwater inrush from the tunnel cutting face. To obtain the time‐dependent groundwater flow quantity, the concept of a horizontal‐well pumping test based on the theory of a point source is adopted. Multiple factors, eg, drawdown, thickness of aquifer, conductivities, and specific storage, are taken into account. Both groundwater inflow to the cross section of a tunnel face in the y‐z plane and total tunnel inflow are obtained. Based on the proposed approach, the time‐dependent groundwater inflow to a tunnel can be classified as either a uniform or non‐uniform flow. The proposed approach is applied to analyse groundwater inflow of 2 field cases: (1) Metro line No. 7, Guangzhou City and (2) an underground tunnel in Huizhou, Guangdong Province. Results show that the proposed method can predict the measured values, and drawdown‐related curves are also derived. In addition, the calculated results also reveal that the effect of hydraulic conductivity k_z on the total groundwater inflow differs from that of hydraulic conductivities k_x and k_y and the thickness of the aquifer.  相似文献   

沈阳市阳光港湾建筑群基坑降水施工研究     

赵立杰  张东岳 《中国煤炭地质》2010,(9):32-34,75

沈阳市阳光港湾建筑群高层建筑采用筏板基础,多层建筑采用人工挖孔灌注桩基础,在基础施工时,均需进行相应的降水工作。采用了分期降水的施工方法,首期降水施工是在分析场地水文地质条件的基础上,利用稳定流"大井法"预算基坑的涌水量,布置了9口井,使基坑周边的1#、2#、3#、4#观测孔水位均下降至5.11m,基本上达到了首期的降水的目的;第二期降水是利用首期降水观测的水位资料,采用稳定流干扰井群计算公式对场区地下水位进行了预报,重新设计了3口井。12口井全部投放使用后,测得稳定排水量为43 000m3/d,并形成了以基坑为中心的地下水降落漏斗,降水效果明显。此经验值得同类工程借鉴。  相似文献