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首页> 外文期刊>Bulletin of engineering geology and the environment >Preliminary analysis of spatial development of karst using a geostatistical simulation approach
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Preliminary analysis of spatial development of karst using a geostatistical simulation approach

机译:地统计学模拟方法对喀斯特空间发育的初步分析

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Earth science phenomena are primarily spatially dependent with variations occurring on varying scales. Geostatistics is a well-known approach for the assessment of spatial models of regionalized variables, such as porosity. In this study, we used the results of 953 Lugeon tests (402 tests in exploratory wells and 550 tests in grouting wells) to assess effective porosity and karst development at the Tangab Dam site, Iran. Lugeon values were first normalized, following which the variogram method (i.e., range, sill, and nugget effect) was used to identify the spatial variability of Lugeon values. A high correlation range of 200 m was obtained along the grout curtain galleries, while the range was about 40 m in the vertical direction. The simple kriging method with Gaussian variograms was determined to be the best method for estimating the Lugeon values in the study area using cross validation-criteria (e.g., RMSE = 0.835 and ρ = 0.914). Spatial variation of Lugeon values was mapped using a simulated annealing approach. The analysis revealed: (1) a higher potential for karst development on the left abutment of the Tangab Dam site, (2) the average of simulated Lugeon values decreased from values of about 180 close to the ground surface at 1,440 m a.s.l. to lower values of about 50 at 1,260 m a.s.l., and (3) high Lugeon values in the abutments of the dam site approximately followed the 15° bedrock dip, which confirms the potential development of karst features in the Asmari limestone. A schematic model for development of karst at the Tangab Dam site is proposed based on hydrogeological data and results of simulated Lugeon values around the dam site.
机译:地球科学现象主要在空间上依赖,并且发生在不同的尺度上。地统计学是一种用于评估区域变量(例如孔隙度)的空间模型的众所周知的方法。在这项研究中,我们使用了953个Lugeon测试的结果(探井的402个测试和注浆井的550个测试)的结果来评估伊朗Tangab大坝现场的有效孔隙率和岩溶发育。首先对Lugeon值进行规范化,然后使用变异函数法(即范围,基石和块金效应)来确定Lugeon值的空间变异性。沿着灌浆帘幕的通道获得了200 m的高相关范围,而在垂直方向上的相关范围约为40 m。使用交叉验证标准(例如,RMSE = 0.835和ρ= 0.914),使用高斯变异函数的简单克里格方法被认为是估计研究区域中Lugeon值的最佳方法。使用模拟退火方法绘制了Lugeon值的空间变化。分析显示:(1)坦加布水坝遗址左岸的喀斯特发展潜力更大;(2)模拟Lugeon平均值从1,440 m a.s.l的接近地面的约180降低。降低至1,260 m a.s.l.处约50的较低值,以及(3)坝址附近的Lugeon值较高,大约跟随15°基岩倾角,这证实了Asmari石灰岩中岩溶特征的潜在发展。基于水文地质数据和坝址周围的Lugeon模拟结果,提出了坦ab坝坝址岩溶发育的示意图。

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