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1.
Sedat Türkmen 《Environmental Earth Sciences》2010,61(2):419-427
This study covers the investigations of the reasons of deformations and leakages in the energy tunnels of Gezende Dam constructed
in 1990 for hydroelectric energy and the recommendations for treatments of the problems. Gezende Dam is located 30 km southwest
of Mut county/Mersin in southern Turkey. The dam is concrete arch type with a height of 72 m. The energy tunnel with an approximate
length of 9 km passes through six different geological units in age of Mesozoic to Cenozoic. After a short period of time
of the operation of the tunnel, leakage has started from the section of gypsum, which is intercalated with dolomitic limestone
between chainage from 5,970 to 6,840 m. The deformations have occurred in the concrete tunnel and springs have been detected
at different places and times through the Ermenek Canyon since 1996. The preventive precautions of the water effect caused
by groundwater effect on gypsum are as follows: (1) contact and consolidation grouting in the tunnel between chainage from
5,910 to 6,840 m, (2) removal of damage on the tunnel line, (3) reinforcement of the tunnel again, and (4) application of
new concrete lining. Besides, a drainage gallery of 320 m was excavated in the 23 m lower and 15 m left part of tunnel base
elevation in order to diminish the effect of groundwater in the section where the deformation occurred. 相似文献
2.
针对深埋岩溶隧道衬砌外水压力展开研究,根据隧道排水量和衬砌水压力模型的理论推导,结合试验进行分析。结果表明,衬砌上水压在采取排水措施后随排水量的增加而减小;但是当注浆材料渗透系数降低到1.65×10-6 m/s、注浆厚度到55 cm后,衬砌上水压随注浆范围的增大变化已经不太明显,说明注浆半径的选取有一个合理范围。注浆圈可以起到控制排水的作用,当给定了隧道某一段的合理排放量以后,就可以确定注浆的范围和注浆水平。 相似文献
3.
Aysan Gürer Tunç Bahadır Varlı Osman Metin İlkışık Ömer Feyzi Gürer 《Environmental Earth Sciences》2016,75(23):1480
Subsurface structures from two different districts of Istanbul, hosting waste and freshwater transmission lines, were imaged by geoelectrical method. The environmental impact on Ka??thane-Terkos freshwater transmission line is one of the issues. That waterline underwent a substantial landslide damage. The previous site selection of Ka??thane-Terkos line was only based on surface geological observations. Even though the pipeline was positioned away from the surface scarps of landslides, the pipes were damaged. To find out the reason, we made some vertical electrical sounding measurements using Schlumberger array in the region. We inverted the electrical sounding data using 2D inversion technique. The final geoelectrical images show main landslide failures, at about 10–30 m depth, which are overlain by debris with a resistivity value of with <6 Ω m. The geoelectrical findings reveal that a buried major failure surrounds the surface landslides behind. Consequently, the water infrastructure remains under the influence of landslide. Our second application site was the area of the Sazl?dere tunnel, which will transfer wastewater, polluting Sazl?dere dam, to the treatment plant. The geoelectrical images along Sazl?dere tunnel route show resistive (<100 Ω m) and moderately conductive (≤50 Ω m) structures along the tunnel axis, representing unaltered to highly weathered rocks, respectively. Furthermore, consecutive hidden fault zones which severely affect the construction process of the tunnel are detected and located. 相似文献
4.
Irrigated agriculture is a clear source of non-point pollution by salts and nitrogen species. The impact of such pollution should be quantified according to specific cases. The case of the Malfarás creek basin, a sprinkler irrigation district located in the semiarid Ebro valley in northeast Spain, has been evaluated. The main crops in the district were corn, barley and alfalfa, occupying 93 % of the irrigated area. The fate of water, salts and nutrients was evaluated by a daily water balance developed at a field scale for the natural year 2010. The yearly data of the whole set of 101 irrigated fields plus the non-irrigated area compared to the measured drainage produced a basin water balance with a low degree of error. The basin consumed 90 % of the total water input of which 68 % was used for crop evapotranspiration and the rest was lost due to non-productive uses. 16 % of the incoming water left the irrigation area as drainage water. The irrigated area was responsible for 87 % of the drainage. The average volume of drained water was 152 mm year?1 for the whole basin area. The irrigated area drained 183 mm year?1. The basin exported 473 kg of salt per hectare during 2010. This value was the lowest of the sprinkler irrigation areas in the Ebro valley, mainly due to the lower soil salinity. All the crops except barley received a nitrogen surplus of 10–50 % above their needs. The extra nitrogen entered the water cycle increasing the nitrate concentration in the aquifer water (150 mg L?1) and drainage water (98 mg L?1). In 2010 the mass of nitrogen exported by drainage was 49 kg per irrigated hectare. This value is too high for this type of irrigation system and implies that 17 % of nitrogen applied as a fertilizer was lost to drainage water. The key to decreasing the nitrogen leaching and pollution that it causes could be appropriate time-controlled fertigation along with better irrigation scheduling. 相似文献
5.
为了能够较快速、较准确地估计出穿越活断层城市地铁隧道的抗震薄弱部位,基于拟静力弹塑性有限元方法,以北京地铁7号线工程的区间隧道作为研究对象,采用数值模拟的方法研究了在走滑断层位错作用下地铁隧道的非线性反应。通过在数值计算模型中嵌入合理的损伤塑性本构模型,利用损伤指标研究了走滑断层下衬砌结构的破坏形式,重点分析了结构损伤的开始部位、发展过程以及最终的损伤程度,并建立了能够估计结构损伤范围及破坏最严重位置的统计关系式。结果表明,在走滑断层作用下衬砌结构出现损伤的区域主要发生在活断层附近一定范围内,拱腰部位的损伤最为严重;增加基岩上覆土层厚度能够减轻衬砌结构的破坏程度,当基岩上覆土层厚度大于等于临界覆盖土层厚度时可以不考虑走滑断层断裂对于浅埋隧道的影响。衬砌结构损伤区域长度与震级的大小和土层厚度有关,损伤最严重的位置随土层厚度的变化而改变。研究成果为穿越活断层地铁隧道的抗震设计和安全性评价提供了参考依据。 相似文献
6.
A. K. Verma Manish Kumar Jha Srinivas Mantrala T. G. Sitharam 《Geotechnical and Geological Engineering》2017,35(5):1953-1966
Rapid growth of urban population in Indian cities have led traffic congestion leading to demand for scientific utilization of underground space. Immediate underground level and deep level underground below the major arterial roads are the sustainable spaces available for meeting the demand of the future traffic/transport. Due to recent increased transit activities it has become one of the soft targets by terrorists or prone to catastrophic accidents in recent years which have increased the importance of rock structures study under explosive loading. In this paper, the response of a underground metro tunnel subjected dynamic loads have been investigated including explosive capacity (30 kg TNT), ground characteristics, liner thickness and blast pressure characteristics. Blast pressure representing CONWEP air blast loading model with positive over pressure phase was applied to lining of tunnel. A three dimensional explicit finite element method was used to analyze dynamic response and damage in twin tunnels of underground metro. It is found that liner of thickness 28 cm will start deforming at the explosive loading of more than 65 kg TNT. 相似文献
7.
Assessment of tunnel instability—a numerical approach 总被引：2，自引：1，他引：1
This paper outlines the application of numerical modeling to predict deformation and stability of tunnel to be excavated in Bansagar, M.P., India. To meet the ever-increasing demand of transportation, energy, and other infrastructure projects, a large volume of rock tunneling is being carried out throughout the world. The geotechnical properties along the route of the 1,800-m long tunnel in the Bansagar region of India have been studied. The rock mass rating and rock mass quality systems were employed for empirical rock mass quality determination. Numerical analysis for the stress–strain distribution of the tunnel excavation and support systems was also carried out. In order to simulate the excavation of tunnel (NATM) at a depth of 150 m below the ground , a series of finite element analyses using Mohr-coulomb elasto-plastic constitutive model has been carried out using PLAXIS 2D. The stability of tunnel has been analyzed, and stress pattern have been discussed. 相似文献
8.
外水压下隧道衬砌的力学响应及结构对策研究 总被引：5，自引：1，他引：4
随着控制排放的隧道防排水技术的广泛应用,外水压力作用下隧道衬砌的一些设计技术问题也愈发突出。基于对外水压力下隧道衬砌的力学响应分析,以龙潭隧道和白云隧道为依托,通过数值仿真,研究了公路隧道抗水压衬砌的结构优化对策。研究结果表明：由于外水压力的作用,衬砌的边墙、仰拱隅角和仰拱处存在明显的应（内）力集中和突变现象,安全度大大降低;通过引入下半断面矢跨比的新概念,从技术和经济的双重角度,指出增大该指标是抗水压衬砌结构优化的首要对策;可依次或组合采用通过增大仰拱隅角处半径、减小仰拱处半径、增大仰拱拱圈厚度、增大衬砌全断面厚度等措施来作为抗水压衬砌的结构优化对策。 相似文献
9.
10.
A geomorphologic and morphometric analysis was performed to determine the characteristics of the de La Flecha river basin, located in the southwest of San Juan province (31°50′S, 68°57′W), Precordillera of San Juan. The drainage networks were derived from shuttle radar topographic mission (SRTM), satellite imageries (Landsat TM and Spot image) and field works. The paper also addresses a preliminary evaluation of the flood hazard responsible for severe damage to people and infrastructure in the downstream region. The study area covers about 300 km2, comprising of six sub-watersheds, ranging from 31.7 to 81.8 km2. The irregular morphology of the basin and the diversity of alluvial deposits found along the de La Flecha river allow the authors to infer that it is in an active tectonic environment with strong lithological and structural controls. One feature common to all analyzed sub-basins is their elongated shape, which allows for a rapid concentration of water that intensifies the power of the flash floods. The drainage network in the different sub-basins has, in general, two predominant patterns; one is parallel to sub-parallel to the headers and foothill areas; and the other, in the alluvial zone, is divergent. Los Berros, Cañada Honda and Media Agua towns, located downstream of the basin, are the most affected by flash floods coming from the mountainous area. 相似文献
11.
Pierpaolo Oreste Giovanni Spagnoli Cesar Alejandro Luna Ramos Lisa Sebille 《Geotechnical and Geological Engineering》2018,36(4):2143-2169
Hyperstatic Reaction Method considers the interaction between the shotcrete lining and the rock mass modelling half tunnel section by beam elements connected by nodes, which can develop bending moments, axial forces and shear forces. The interaction between ground and support is represented by Winkler type springs in the nodes of the numerical model, in the normal and tangential direction. 1944 analyses were developed considering three different tunnel radius values (2.0, 4.5 and 7.0 m), three different rock types (RMR = 40, RMR = 60 and RMR = 80), three different stress ratios acting on the linings (\(K = 1, \,K = 0.5\) and \(K = 0\)), three different lining thickness values (0.1, 0.2 and 0.3 m) and three values of the average elastic modulus of the shotcrete (6000, 9000 and 12,000 MPa). Besides, also two different stiffness values of the tangential springs at nodes were considered. Results show that the lining thickness and the elastic modulus of the shotcrete have a strong influence on the bending moment values which develop inside. The maximum axial force is not practically influenced by the lining elastic modulus and thickness. Both maximum bending moments and maximum axial forces increase in a linear way with the vertical load value; tunnel radius, \(K\) and RMR values of the rock mass have also a great influence on the maximum bending moment and axial force. Besides, it is possible to note how the absence of shear interaction between the lining and the rock mass causes bending moment values in the lining higher with respect to the case where the stiffness of the tangential springs at nodes equals to half the stiffness of the normal springs. For this reason, the neglectance of the shear interaction between the lining and the tunnel wall leads to an overdesign of the SC lining. 相似文献
12.
数次大地震震害调查表明,隧道穿越断层处是受地震破坏较为严重的区域。为此,基于地震动能量的传播与释放特征,建立了一种穿越断层隧道结构抗减震的设计理念,并提出了一种穿越断层隧道节段接头形式。以跨断层龙溪隧道为依托,采用振动台模型试验研究了单一错动方式与断层错动-震动综合加载方式下带有接头的衬砌结构响应。研究结果证明：强震作用下,地震波对穿越断层隧道的影响是不可忽略的,断层错动-震动综合加载方式是合理的;新型接头能够自身适应性变形协调减轻隧道结构震害,节段间接头的设置改变了隧道的变形形态,提高隧道整体抗震能力;同时减小了衬砌的环向破坏,消弱了节段间地震力的传递,实现了衬砌震害的局部化。由于接头的设置,上盘隧道结构震害集中在距断层1.8倍洞径的范围内,下盘处隧道衬砌震害集中在距断层1.2倍洞径范围内;上盘的衬砌震害主要是由错动-震动联合作用造成的,而下盘衬砌震害主要受地震动的影响。 相似文献
13.
Excavation of the Aica-Mules pilot tunnel for the Brenner base tunnel: information gained on water inflows in tunnels in granitic massifs 总被引：1，自引：1，他引：0
Paolo Perello Alessandro Baietto Ulrich Burger Stefan Skuk 《Rock Mechanics and Rock Engineering》2014,47(3):1049-1071
The construction of the Aica-Mules tunnel, completed in 2010, provides a relevant case history for improving the knowledge of hydrogeological issues related to the excavation of deep tunnels in granitic massifs. The Aica-Mules tunnel is a 10 km-long structure, forming part of the high-speed railway connection between Austria and Italy across the Alpine chain, located at an average depth of 500–1,000 m below the surface. Prior to and during the construction, intense hydrogeological monitoring was set up, allowing the collection of abundant data concerning: (1) the evolution of water inflows into the tunnel; (2) the chemistry and temperature of drained groundwater; and (3) the influence of tunnel drainage on springs. Based on detailed analysis of geological/hydrogeological data, this article provides an insight into the permeability distribution in granitic rocks affected by relevant brittle tectonic deformation, and the consequences of water inflow during excavation. The available time series from the principal water discharges in the tunnel have been used in order to test the reliability of some of the most commonly applied analytical methods for the forecast of water inflows into tunnels. 相似文献
14.
Hydraulic conductivity distribution in crystalline rocks, derived from inflows to tunnels and galleries in the Central Alps, Switzerland 总被引：4，自引：3，他引：1
Inflow data from 23 tunnels and galleries, 136 km in length and located in the Aar and Gotthard massifs of the Swiss Alps, have been analyzed with the objective (1) to understand the 3-dimensional spatial distribution of groundwater flow in crystalline basement rocks, (2) to assess the dependency of tunnel inflow rate on depth, tectonic overprint, and lithology, and (3) to derive the distribution of fracture transmissivity and effective hydraulic conductivity at the 100-m scale. Brittle tectonic overprint is shown to be the principal parameter regulating inflow rate and dominates over depth and lithology. The highest early time inflow rate is 1,300 l/s and has been reported from a shallow hydropower gallery intersecting a 200-m wide cataclastic fault zone. The derived lognormal transmissivity distribution is based on 1,361 tunnel intervals with a length of 100 m. Such interval transmissivities range between 10?9 and 10?1 m2/s within the first 200–400 m of depth and between 10?9 and 10?4 m2/s in the depth interval of 400–1,500 m below ground surface. Outside brittle fault zones, a trend of decreasing transmissivity/hydraulic conductivity with increasing depth is observed for some schistous and gneissic geological units, whereas no trend is identified for the granitic units. 相似文献
15.
Fiorucci M. Iannucci R. Lenti L. Martino S. Paciello A. Prestininzi A. Rivellino S. 《Natural Hazards》2016,86(2):345-362
A monitoring system is operative in the Peschiera Springs slope (Central Apennines, Italy) to mitigate the landslide risk related to the hosted main drainage plant of Rome aqueducts by providing alert warning. Such a strategy allows to avoid out-of-service episodes so reducing extra-costs of water distribution management. The Peschiera Springs slope is involved in a rock mass creep characterized by an average steady strain rate of 1 mm year−1 and responsible for several landforms including sinkholes, subvertical scarps and trenches. Moreover, an average aquifer discharge of 19 m3 s−1 causes an intense limestone dissolution concentrated in correspondence with release bands and discontinuities that dislodge the jointed rock mass. Since 2008, an accelerometric network has been operating within the slope; about 1300 microseismic local events were recorded up to now, distinguished in failures and collapses. A control index, based on frequency of occurrence and cumulative energy of the recorded microseismic events was defined to provide three levels of alert. In 2013, a temporary nanoseismic Seismic Navigation System (SNS) array was installed inside a tunnel of the drainage plant to integrate the pre-existent seismic monitoring system. This array allowed to record 37 microseismic events, which locations are in good agreement with the evolutionary geological model of the ongoing gravitational slope deformation. In 2014, a permanent nanoseismic SNS array was installed in the plant and allowed to record several sequences of underground collapses including more than 500 events. The nanoseismic monitoring system is allowing to: (1) increase the detection level of the monitoring system; (2) locate hypocentres of the events; and (3) detect precursors of the strongest events.
相似文献16.
M. Fiorucci R. Iannucci L. Lenti S. Martino A. Paciello A. Prestininzi S. Rivellino 《Natural Hazards》2017,86(2):345-362
A monitoring system is operative in the Peschiera Springs slope (Central Apennines, Italy) to mitigate the landslide risk related to the hosted main drainage plant of Rome aqueducts by providing alert warning. Such a strategy allows to avoid out-of-service episodes so reducing extra-costs of water distribution management. The Peschiera Springs slope is involved in a rock mass creep characterized by an average steady strain rate of 1 mm year?1 and responsible for several landforms including sinkholes, subvertical scarps and trenches. Moreover, an average aquifer discharge of 19 m3 s?1 causes an intense limestone dissolution concentrated in correspondence with release bands and discontinuities that dislodge the jointed rock mass. Since 2008, an accelerometric network has been operating within the slope; about 1300 microseismic local events were recorded up to now, distinguished in failures and collapses. A control index, based on frequency of occurrence and cumulative energy of the recorded microseismic events was defined to provide three levels of alert. In 2013, a temporary nanoseismic Seismic Navigation System (SNS) array was installed inside a tunnel of the drainage plant to integrate the pre-existent seismic monitoring system. This array allowed to record 37 microseismic events, which locations are in good agreement with the evolutionary geological model of the ongoing gravitational slope deformation. In 2014, a permanent nanoseismic SNS array was installed in the plant and allowed to record several sequences of underground collapses including more than 500 events. The nanoseismic monitoring system is allowing to: (1) increase the detection level of the monitoring system; (2) locate hypocentres of the events; and (3) detect precursors of the strongest events. 相似文献
17.
在模型试验中,锚杆一般尺寸较小,应变监测较为困难,可将光纤Bragg传感技术（FBG）应用于隧道模型试验中解决该问题。基于西安地铁二号线4个典型断面实际工况进行隧道模型试验,将自行设计封装的光纤Bragg光栅传感器粘贴在锚杆模型表面,监测其在不同应力状态下的应变。根据隧道开挖前、隧道开挖后、衬砌支护后、抗裂极限状态和极限破坏状态5个应力状态的实测数据,得到锚杆轴力在隧道受力过程中的变化规律。试验结果表明,锚杆受力大小在隧道开挖前后有一定变化。衬砌支护后,随围岩压力增加,锚杆轴力基本呈增加趋势,拱顶附近锚杆承受压力,支护后压力变化不大;拱肩到墙角的锚杆承受拉力,衬砌支护后受力开始增加;锚杆在含水率大的黄土隧道中受力较大,更能发挥其作用。文中方法在模型试验中的应变监测方面提出新的可靠途径。 相似文献
18.
Karl Gunnar Holter 《Rock Mechanics and Rock Engineering》2014,47(3):1003-1020
A composite tunnel lining system based on a sprayed waterproofing membrane combined with sprayed concrete is currently being considered for future Norwegian rail and road tunnels. Possible loading of the tunnel linings caused by water pressure is being investigated. This tunnel lining system consists of a waterproof membrane which, during application on the sprayed concrete lining, bonds mechanically to the sprayed concrete on either side. Hence, a continuous, sealing, and non-draining structure from the rock mass to the interior tunnel surface is formed in the walls and crown. Experiences from some successful recent projects with this lining system in Europe are reviewed. However, these experiences are not directly comparable to the Scandinavian hard rock tunnel lining approach, which utilizes a relatively thin sprayed and irregular concrete layer for permanent lining. When considering the sprayed membrane and sprayed concrete composite lining concept, introducing a partially sealing and undrained element in the lining, the experiences with the traditionally used lining systems in Norway need to be reconsidered and fully understood. A review of several hard rock tunnels with adverse conditions, in which the tunnel lining has been subject to load monitoring, shows that only very small loads in the tunnel linings occur. Recent investigations with in situ water pressure testing, including two sites with the composite sprayed membrane in a partially drained waterproof tunnel lining, are discussed. In a case with a cavern located in a hydraulically saturated rock mass subjected to approximately 8 bar hydrostatic pressure, a negative pressure gradient towards the tunnel lining has been measured. The investigation results from the Norwegian test sites indicate that no significant loading of the tunnel lining takes place in a hydraulically saturated rock when applying this composite waterproof tunnel lining in parts of the tunnel perimeter. 相似文献
19.
Clast-supported boulder gravel in outwash-fans along the glacial-maximum margin of the Laurentide Ice Sheet in Wisconsin indicates the occurrence of outburst floods. These sediments, with clast intermediate axes of up to 2 m, are located downstream of tunnel channels and were deposited shortly before cessation of glaciofluvial activity on each fan. Since tunnel channels with fans are widespread along the ice-sheet margin in the western Great Lakes region, these outburst floods were probably common. Paleodischarge estimates derived from the boulder deposits are poorly constrained, but values of at least several hundred m3 s−1 are likely. Four potential water sources for the floods exist: an extreme surface-melt event, an extreme precipitation event, drainage of supraglacial lakes, or drainage of stored subglacial meltwater. We focus on the storage of subglacial meltwater behind the ice-sheet margin, as proglacial permafrost was present as ice advanced to its maximum extent, and a frozen-bed zone upstream from the margin probably impeded drainage through groundwater aquifers. Decay of this permafrost ‘seal’ would have eventually allowed trapped water to drain through the tunnel channels. We suggest that the 2-m boulders were entrained in an outburst of subglacial water that enlarged a pre-existing channel cut by ablation-derived flows. 相似文献
20.
Interaction of longitudinal surface settlements for twin tunnels in shallow and soft soils: the case of Istanbul Metro 总被引：1，自引：1，他引：0
Ibrahim Ocak 《Environmental Earth Sciences》2013,69(5):1673-1683
Increasing demands on infrastructures increases the attention on shallow soft ground tunneling methods in urbanized areas. Especially, in metro tunnel excavations, it is important to control the surface settlements observed before and after excavation, which may cause damage to surface structures. To solve this problem, earth pressure balance machines (EPBMs) have widely been used throughout the world. This study focuses on surface settlement measurements, the interaction of twin tunnel surface settlement, and the relationship between shield parameters and surface settlement for parallel tunnels using EPBM shields in clay and sand soils. In this study, the tunnels were excavated using two EPBMs. The tunnels were 6.5 m in diameter, as twin tubes with a 14 m distance from center to center. The EPBM in the first tube followed about 100 m behind the other tube. Segmental lining with 1.4 m of length was employed as a final support. The results from this study showed that (1) the most important parameters for the maximum surface settlements are the face pressure and backfill; (2) in twin tunnel excavation with EPBM for longitudinal profile, the settlement rate reached its peak value when the shield came to the monitoring section and this peak value continued until the shield passed the monitoring section; (3) every shield affected the other tunnel’s longitudinal surface settlement profile by approximately 35–36.8 %; (4) S A, S B and S C values were found to be 38.0, 35.8 and 26.2 %, respectively for an EPBM, and (5) ensuring good construction quality is a very effective way to control face stability and minimize surface settlement. 相似文献