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排序方式: 共有77条查询结果,搜索用时 14 毫秒
1.
在分析研究青岛市黄岛区潮河流域水文地质条件基础上,建立了水文地质概念模型和地下水流数值模拟模型,利用地下水水位动态监测资料对模型进行了识别,并预测了三枯一丰一平条件下地下水最大开采量以及水位、降深分布情况。结果表明,模型验证拟合结果较好,地下水最大开采量为2.4万m3/d,地下水开采不会引起地面沉降、海水入侵等问题。  相似文献   
2.
Abstract

Papadopulos and Cooper's (PC) solution can be used to describe the drawdown resulting from pumping with a constant rate at a large-diameter well. However, this solution is too complicated to be accurately evaluated due to the oscillatory nature of the Bessel functions. The PC approach resulted in tabulated values of dimensionless drawdown at the well with an accuracy of four or fewer digits for selected values of dimensionless storage coefficient versus dimensionless time. Some researchers have fitted the tabulated values with interpolation formulas that are easy to use in engineering applications. Those formulas may be more accurate if the tabulated values are computed with greater accuracy. In this study, we propose an efficient numerical procedure, including a root search scheme, to find the roots of the integrand, Gaussian quadrature for numerical integration, and Shanks transform to accelerate convergence of infinite series. The proposed procedure can evaluate the dimensionless drawdown with greater accuracy and is useful in practice if there is a need for high accuracy for the observation either at the well or in the aquifer at some distance from the pumping well

Editor D. Koutsoyiannis

Citation Chang, Y.C., Yeh, H.D., and Wang, C.T., 2013. Improvement on the estimation of constant-rate drawdown in large-diameter wells. Hydrological Sciences Journal, 58 (3), 716–727.  相似文献   
3.
在鄂尔多斯盆地都思兔河流域供水水文地质详查的基础上,通过水文地质钻探、抽水试验、样品分析等手段,查明了流域含水层的结构、埋深以及含水层和隔水层在水平和垂直方向上的变化规律,探讨了各含水层之间的水力联系,并求取了含水层的水文地质参数;对比圈定了包乐浩晓、巴彦布拉格、好勒包勒吉3处富水区;采用地下水流数值模拟方法对上述3处富水区地下水开采量进行计算,提出了27种地下水开采方案,并经过对比得到地下水开采推荐方案。结果表明:包乐浩晓、巴彦布拉格、好勒包勒吉3处富水区主要补给为侧向径流及大气降水入渗补给,排泄方式以潜水面蒸发及向河流排泄为主;在地下水浅埋区,结合含水层单井涌水量的大小,确定采用管井开采方式、中段悬挂式非完整井结构,平均布井,井深300m,单一开采白垩系环河组的地下水,最大限度夺取潜水蒸发排泄量;根据推荐方案,上述3个富水区总开采量达到123 500m3/d,可为该地区地下水资源开发与利用提供技术保障。  相似文献   
4.
This study examines the effect of drawdown on the timing and magnitude of suspended solids and associated phosphorus export from a 12 ha reservoir located in an urbanized watershed in southern Ontario, Canada. Water level in Columbia Lake was lowered by 1·15 m over a 2‐week period in November 2001. The total phosphorus (TP) concentrations ranged from 63 to 486 µg L?1 in Columbia Lake and 71 to 373 µg L?1 at its outflow. All samples exceeded the Provincial Water Quality Objective of 30 µg TP L?1. Outflow concentrations of suspended solids and TP increased significantly with decreasing lake level and were attributed to the resuspension of cohesive bottom sediments that occurred at a critical threshold lake level (0·65 m below summer level). Suspended solids at the outflow consisted of flocculated cohesive materials with a median diameter (D50) of c. 5 µm. Particulate organic carbon accounted for 8·5% of the suspended solids export by mass. A total mass of 18·5 t of suspended solids and 62·6 kg TP was exported from Columbia Lake, which represents a significant pulse of sediment‐associated P to downstream environments each autumn during drawdown. The downstream impacts of this release can be minimized if the water level in Columbia Lake is lowered no more than 0·5 m below summer levels. Copyright © 2004 John Wiley & Sons, Ltd.  相似文献   
5.
本文着重探讨管井井点降水的计算方法,并结合工程实例分析管井降水设计和施工中需要注意的一些问题.  相似文献   
6.
ZHANG Wen-hua 《岩土力学》2006,27(Z1):1149-1152
By using the uniform hydraulic gradient and variable hydraulic gradient principle, a computational formula of permeability coefficient of the single well(drillhole) steady flow confined fully penetrating well is derived, in which the effect of noneffective drawdown on permeability coefficient is considered, and the most of water level recovery data in computational process are used, while some interference factors effect is excluded in the water level recovery. Therefore, the parameter calculation will still approximate to the fact.  相似文献   
7.
文章以漯河市为例说明了城市地下水最大可采资源的确定和开发管理中遵循不断变化着的实际情况,走科研与生产相结合道路的必要性。全文分3个方面介绍了开采条件下的人工串层补给,随机边界条件及地下水管理模拟中常见的几个核心问题的处理。文章最后强调,地下水数值模拟中辅以同位素年龄研究的重要性。  相似文献   
8.
地下水水位预测在深基坑工程中的应用   总被引:1,自引:0,他引:1  
通过地下水水位预测,能够确定从降水井合笼到基坑开挖时的日期、开挖速度,可调整降水井的布局,确定最佳降水方案。结合工程实例,阐述地下水水位预测在深基坑降水方案设计中的应用,具有较好的实用价值。  相似文献   
9.
The Toarcian Oceanic Anoxic Event (T-OAE, ~183 Ma) was characterized by enhanced carbon burial, a prominent negative carbon-isotope excursion (CIE) in marine carbonate and organic matter, and numerous geochemical anomalies. A precursor excursion has also been documented at the Pliensbachian/Toarcian boundary, but its possible causes are less constrained. The T-OAE is intensively studied in the Cleveland Basin, Yorkshire, UK, whose sedimentary deposits have been litho-, bio- and chemostratigraphically characterised. Here, we present new elemental data produced by hand-held X-ray fluorescence analysis to test the expression of redox-sensitive trace metals and detrital elements across the upper Pliensbachian to mid-Toarcian of the Cleveland Basin. Detrital elemental concentrations (Al, Si, Ti, Zr) are used as proxies for siliciclastic grain content and thus, sea-level change, which match previous sequence stratigraphic interpretations from the Cleveland Basin. The timescale of the event is debated, though our new elemental proxies of relative sea level change show evidence for a cyclicity of 350 cm that may be indicative of ~405 kyr eccentricity cycles in Yorkshire. Trends in total organic carbon and redox-sensitive elements (S, Fe, Mo, As) confirm scenarios of widespread ocean deoxygenation across the T-OAE. The correlation of comparable trends in Mo across the T-OAE in Yorkshire and the Paris Basin suggests a similar oceanic drawdown of this element accompanying widespread anoxia in the two basins. Data from Yorkshire point to a transgressive trend at the time of the Mo drawdown, which contradicts the “basin restriction” model for the euxinic conditions that characterise the CIE interval.  相似文献   
10.
不同出露时间下洞庭湖洲滩土壤及生态系统呼吸特征   总被引:1,自引:0,他引:1  
周延  靖磊  杨萌  史林鹭  吕偲  雷光春 《湖泊科学》2018,30(6):1664-1671
于2015年1月洞庭湖枯水期,针对不同出露时间下的洲滩,调查其土壤理化性质,并利用LI-8100便携式二氧化碳气体分析仪监测其生态系统呼吸.结果表明:在洞庭湖枯水期,洲滩出露后,洲滩土壤有机质、硝态氮、铵态氮和全氮含量随出露时间增长而先升高后降低.土壤溶解性有机碳含量是影响洞庭湖枯水期洲滩生态系统呼吸强度的最重要影响因子.溶解性有机碳含量随出露时间增长而提高,洲滩生态系统呼吸强度随之提高,并在洲滩出露约60天后达到最高值.出露洲滩生态系统呼吸通量均值为0.72±0.55 μmol/(m2·s),超过杨树林地、芦苇地和农田地,成为洞庭湖区冬季CO2排放最活跃的区域.  相似文献   
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