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首页> 外文期刊>Engineering Geology >Evaluation of rock-mass permeability tensor and prediction of tunnel inflows by means of geostructural surveys and finite element seepage analysis
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Evaluation of rock-mass permeability tensor and prediction of tunnel inflows by means of geostructural surveys and finite element seepage analysis

机译:岩体渗透率张量评估及隧道涌水量的地质调查与有限元渗流分析

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In this paper, a new practical technical approach for the evaluation of hydraulic conductivity and tunnel water inflow in complex fractured rock masses is presented. This study was performed in order to evaluate water flow into tunnels planned along the new highway project from Firenze Nord gate to Barberino di Mugello (Tuscany). The results are based on detailed and comprehensive geostructural characterization of rock masses, by means of field surveys, geological and hydrogeological studies. Starting from discontinuities properties surveyed in the field, the permeability K tensor was calculated using the Kiraly equation, integrated with the introduction of the effective hydraulic opening of fissures (e). Principal directions of tensor K were calculated for each geostructural survey station using an automated software script especially developed for this purpose. Available K data from Lugeon tests were also collected and analyzed with results that do not fully represent the rock mass due to its structural (hydraulic) variability. In order to evaluate water flow into tunnels planned for excavation under the water table (for a total number of eight), a finite elements seepage analysis was performed on 38 representative geological sections transverse to tunnel paths (alpha-planes). Each section referred to the nearest and geologically most compatible geostructural station. Principal directions of K tensors were projected on the alpha-planes by means of trigonometric transformations. Unitary water inflows were then evaluated for long-term steady-state, as well as for initial state immediately after tunnel excavation. Inflow values calculated for each unitary section were extended to geologically homogeneous lengths of the tunnel, according to the variability of the water head above excavation, and then summed up for the whole length of each tunnel. Inflow values obtained with FE seepage analysis were also compared to other inflow evaluation methods.
机译:本文提出了一种新的实用技术方法,用于评价复杂裂隙岩体的水力传导率和隧道入水量。进行这项研究的目的是评估从Firenze Nord门到Barberino di Mugello(托斯卡纳)的新高速公路项目规划的隧道中的水流量。结果是基于对岩体的详细全面的地质构造特征,通过现场调查,地质和水文地质研究得出的。从现场调查的不连续性属性开始,使用Kiraly方程计算渗透率K张量,并结合裂缝的有效水力开裂(e)进行计算。使用专门为此目的开发的自动化软件脚本,为每个岩土测量站计算了张量K的主要方向。还收集了来自Lugeon测试的可用K数据并进行了分析,结果由于结构(液压)变化而不能完全代表岩体。为了评估流向计划在地下水位以下开挖的隧道中的水流量(总共8个),对横穿隧道路径(α平面)的38个代表性地质断面进行了有限元渗流分析。每个部分都指最近的,地质上最兼容的地质构造台站。通过三角变换将K张量的主要方向投影在alpha平面上。然后评估整体入水的长期稳态以及隧道开挖后的初始状态。根据开挖上方水头的变化性,将每个整体断面计算的入流值扩展到隧道的地质上均匀的长度,然后对每个隧道的整个长度求和。通过FE渗流分析获得的入流值也与其他入流评估方法进行了比较。

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