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81.
Modeling soil collapse by artificial neural networks 总被引:1,自引:0,他引:1
The feasibility of using neural networks to model the complex relationship between soil parameters, loading conditions, and
the collapse potential is investigated in this paper. A back propagation neural network process was used in this study. The
neural network was trained using experimental data. The experimental program involved the assessment of the collapse potential
using the one-dimensional oedometer apparatus. To cover the broadest possible scope of data, a total of eight types of soils
were selected covering a wide range of gradation. Various conditions of water content, unit weights and applied pressures
were imposed on the soils. For each placement condition, three samples were prepared and tested with the measured collapse
potential values averaged to obtain a representative data point. This resulted in 414 collapse tests with 138 average test
values, which were divided into two groups. Group I, consisting of 82 data points, was used to train the neural networks for
a specific paradigm. Training was carried out until the mean sum squared error (MSSE) was minimized. The model consisting
of eight hidden nodes and six variables was the most successful. These variables were: soil coefficient of uniformity, initial
water content, compaction unit weight, applied pressure at wetting, percent sand and percent clay. Once the neural networks
have been deemed fully trained its accuracy in predicting collapse potential was tested using group II of the experimental
data. The model was further validated using information available in the literature. The data used in both the testing and
validation phases were not included in the training phase. The results proved that neural networks are very efficient in assessing
the complex behavior of collapsible soils using minimal processing of data.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
82.
A design of a dewatering system is necessary for site improvement prior to the construction of some structures. The design
of an efficient dewatering system requires estimating the value of the in-situ coefficient of permeability. The available
relationships for estimating the permeability coefficient were developed based on limited field measurements and conditions,
and their predictions vary by several orders of magnitudes. Therefore, it was necessary to conduct field measurements of permeability
and determine the relationship that best fits these measurements prior to the design of a dewatering system for specific geological
and site conditions.
This paper presents field measurements of permeability in complex chaotic and diagenetic limestone strata. It also offers
comparative analysis of several relationships available in the literature for predicting the in-situ coefficient of permeability.
The analysis is conducted for both steady and nonsteady conditions. The results show that the coefficient of permeability
value is dependent on the water table level, which is affected by the tidal condition. The US Navy equation is shown to give
the best correlation with field measurements.
Electronic Publication 相似文献
83.
In this study, the changes in the chemical composition of the groundwater along a flow path were examined by using the water
samples collected from unconfined, semi-confined and confined parts of the Karasu karstic aquifer. It was determined that
transport of bicarbonate, calcium, and magnesium was dominant in unconfined and semi-confined parts of the aquifer, whereas
calcite and dolomite precipitate in the confined parts. On the other hand, gypsum dissolution is present in all parts of the
aquifer. In addition, the computed saturation indices explain the occurrences and precipitation of travertines in the Goksu
Valley, which is the discharge area for the aquifer.
Electronic Publication 相似文献
84.
A geotechnical investigation of the retrogressive Yaka Landslide and the debris flow threatening the town of Yaka (Isparta,SW Turkey) 总被引:2,自引:1,他引:1
In this study the factors affecting the retrogressive Yaka Landslide, its mechanism and the hazard of debris flow on the town of Yaka are investigated. In the landslide area, the first landslide was small and occurred in March 2006 on the lower part of the Alaard?ç Slope near the Gelendost District town of Yaka (Isparta, SW Turkey). The second, the Yaka Landslide, was large and occurred on 19 February 2007 in the soil-like marl on the central part of Alaard?ç Slope. The geometry of the failure surface was circular and the depth of the failure surface was about 3 m. Following the landslide, a 85,800 m3 of displaced material transformed to a debris flow. Then, the debris flow moved down the Eglence Valley, traveling a total distance of about 750 m. The town of Yaka is located 1,600 m downstream of Eglence Creek and hence poses a considerable risk of debris flow, should the creek be temporarily dammed as a result of further mass movement. Material from the debris accumulation has been deposited on the base of Eglence Valley and has formed a debris-dam lake behind a debris dam. Trees, agricultural areas, and weirs in the Eglence Creek have seen serious damage resulting from the debris flow. The slope angle, slope aspect and elevation of the area in this study were generated using a GIS-based digital elevation model (DEM). The stability of the Alaard?ç Slope was assessed using limit equilibrium analysis with undrained peak and residual shear strength parameters. In the stability analyses, laboratory test results performed on the soil-like marls were used. It was determined that the Alaard?ç Slope is found to be stable under dry conditions and unstable under completely saturated conditions. The Alaard?ç Slope and its vicinity is a paleolandslide area, and there the factor of safety for sliding was found to be about 1.0 under saturated conditions. The Alaard?ç Slope and the deposited earthen materials in Eglence Creek could easily be triggered into movement by any factors or combination of factors, such as prolonged or heavy rainfall, snowmelt or an earthquake. It was established that the depth of the debris flow initiated on the Yaka Landslide reached up to 8 m in Eglence Creek at the point it is 20 m wide. If this deposited material in Eglence Creek is set into motion, the canal that passes through Yaka, with its respective width and depth of 7 and 1.45 m, could not possibly discharge the flow. The destruction or spillover of this canal in Yaka could bring catastrophic loss to residents which are located within 3–5 m of the bank of the canal. Furthermore, if material present in the landslide source area slides and this displaced material puts pressure on the unstable deposited material in Eglence Creek, even more catastrophic loss would occur to the town of Yaka. In this study, it was determined that debris flows are still a major hazard to Yaka and its population of 3,000. The results provided in this study could help citizens, planners, and engineers to reduce losses caused by existing and future landslides and debris flow in rainfall and snowmelt conditions by means of prevention and mitigation. 相似文献
85.
用开尔文黏弹模型对实验蠕变曲线和冰后期地面抬升观测曲线进行反演,得到相关的黏弹参数,发现所有的黏弹参数都随实验(或观测)时间长度发生有规律的变化, 表明黏弹参数是实验(或观测)时间的函数.在此基础上提出非定常参数的黏弹模型,将通常采用的剪切模量μ2、弛豫时间τ 和黏度η 相应地从常数修正为时间的函数μ2(t)、τ(t) 和η(t),检验表明修正后的开尔文模型可以更好地符合实测蠕变曲线.用修正后的μ2(t)对软流层的黏度进行估算,其值约为4.6×1020 Pa·s. 相似文献
86.
Gilles Grandjean Céline Pennetier Adnan Bitri Ombeline Meric Jean-Philippe Malet 《Comptes Rendus Geoscience》2006,338(9):587-595
Geophysical methods such as seismic surveying and electrical resistivity imaging appear to be well-adapted to investigate and understand landslide mechanisms. They allow direct and non-intrusive measurement of acoustic velocity and electrical resistivity, two fundamental parameters used to define the physical properties of the reworked moving materials. Both methods were applied at the Super-Sauze site in the French South Alps, where a typical example of an intra-material earthflow-mudslide can be observed. Measurements were taken simultaneously along two orthogonal profiles: one 325 m in length is perpendicular to the axis of the earthflow; the other 235 m in length is located along the axis of the earthflow. The results show a correlation between the seismic and electrical resistivity data, confirming that the simultaneous use of both methods gives complementary information about landslide mechanisms. The seismic data provide information on fracture density variations, whereas the electrical resistivity data provide information on water content variations. To cite this article: G. Grandjean et al., C. R. Geoscience 338 (2006). 相似文献
87.
88.
The work attempts to assess the effects of global warming on the efficacy of current greenhouse cooling methods following a methodology previously proved for other agricultural buildings. The cooling potential of four greenhouse cooling techniques (natural ventilation, forced ventilation, fogging and shading) were simulated by computer modelling for five European locations, calculating the greenhouse internal air temperature from measured external climate data. Four 2080s scenarios were analysed in these five locations. They were constructed as a combination of General Circulation Models (Had CM3 and ECHAM4) downscaled for Europe with the HIRHAM and RCA3 regional models and driven by the A2 and B2 socio-economic scenarios. The crop considered as reference was tomato. The results showed that, in locations in southern Europe, adding evaporative cooling methods to ventilation and/or shading will be indispensable. In some areas of northern Europe, natural ventilation will no longer be sufficient, and shading or fogging will also be necessary. The economic consequences will be important, over all in the southern locations where water consumption, investment and working costs will be higher and necessary to ensure the crop production. 相似文献
89.
Hidden subvertical discontinuities oriented parallel to subparallel to the exposed faces of outcropping sandstone were effectively mapped at three different study sites in central Missouri using a ground-penetrating radar system (GPR) equipped with a 400-MHz monostatic antenna and a survey wheel. At each site, a suite of 2-D ground-penetrating radar profiles were acquired along multiple closely spaced traverses on relatively smooth exposed rock surfaces. Time-zero correction was applied to the raw GPR data which were then processed using band-pass filtering, range and display gain, color transformation, and deconvolution techniques. Pseudo 3D images of each identified discontinuity at each site were constructed based on the interpretation of the nonmigrated ground-penetrating radar profiles. These pseudo 3D images were hand-migrated and transformed into true 3D images which depict variable depths at “perpendicular horizontal distance” to each discontinuity relative to the exposed rock face. The results demonstrate that GPR can be used to detect and map hidden discontinuities. This information can then be used for rock slope stability analysis and rock engineering purposes. 相似文献
90.
Michael Fuchs Adnan A. Awan Sardar S. Akhtar Ijaz Ahmad Simon Sadiq Asif Razzak Naghmah Haider 《山地科学学报》2017,14(5):948-963
In the frame of landslide susceptibility assessment, a spectral library was created to support the identification of materials confined to a particular region using remote sensing images. This library, called Pakistan spectral library (pklib) version 0.1, contains the analysis data of sixty rock samples taken in the Balakot region in Northern Pakistan. The spectral library is implemented as SQLite database. Structure and naming are inspired by the convention system of the ASTER Spectral Library. Usability, application and benefit of the pklib were evaluated and depicted taking two approaches, the multivariate and the spectral based. The spectral information were used to create indices. The indices were applied to Landsat and ASTER data to support the spatial delineation of outcropping rock sequences in stratigraphic formations. The application of the indices introduced in this paper helps to identify spots where specific lithological characteristics occur. Especially in areas with sparse or missing detailed geological mapping, the spectral discrimination via remote sensing data can speed up the survey. The library can be used not only to support the improvement of factor maps for landslide susceptibility analysis, but also to provide a geoscientific basis to further analyze the lithological spot in numerous regions in the Hindu Kush. 相似文献