Startseite Limit Support Pressure of Tunnel Face in Multi-Layer Soils Below River Considering Water Pressure
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Limit Support Pressure of Tunnel Face in Multi-Layer Soils Below River Considering Water Pressure

  • Weiping Liu EMAIL logo , Lina Hu , Yongxuan Yang und Mingfu Fu
Veröffentlicht/Copyright: 31. Dezember 2018
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Abstract

This paper presents a method to determine the limit support pressure of tunnel face in multi-layer soils below river considering the water pressure. The proposed method is based on the 3D Terzaghi earth pressure theory and the wedge theory considering the water pressure. The limit support pressures are investigated using the limit equilibrium method and compared to those calculated using a numerical method, such as FLAC3D. Four cases focusing different combinations of three layers are analyzed. The results obtained by the numerical method agree well with the predictions of the proposed limit equilibrium method. The limit support pressure obtained using the limit equilibrium method is greater than that obtained by the numerical method. The limit equilibrium method is safe and conservative in obtaining the limit support pressure. The proposed limit equilibrium method is expected to be easily adaptable and to enhance the reliability of tunnel design and construction in multi-layer soils below river.

1 Introduction

With a rapid increase in the construction of subways, shield tunnel technology has been widely used in the construction of tunnels [1, 2, 3]. Tunnel face stability is a key construction consideration in shield tunnel projects. Complex geological conditions can pose serious technical challenges to shield tunnel excavation [4]. The support pressure counteracts the effective earth and water pressure. In order to ensure safety against the collapse of the tunnel face, it is essential to have a reliable analysis of tunnel face stability and predictions of the limit support pressure.

The limit support pressure of the tunnel face is the primary concern in stability analysis [5, 6]. The limit equilibrium method [7], numerical method [8, 9], and experimental method [10] are used to analyze the stability of the tunnel face and support pressure. For the experimental aspects on the stability of the tunnel face, Zhou et al. [11] used the in situ method to analyze the deformation that takes place close to the tunnel face. Messerli et al. [12] investigated the limit support pressure of the tunnel face in sand using experiments. Idinger et al. [13] used centrifuge model tests to investigate face stability on a small scale tunnel in cohesion-less soil, with the slip surface arising from a tunnel invert propagated at an angle of approximately 45∘ + φ/2 to the horizontal. Chambon et al. [14] also studied tunnel face stability using a centrifuge test, and analyzed the effect of tunnel depths on the collapse forms of tunnel faces.

Numerical models are increasingly being used to assess the stability of tunnel faces. Zhang et al. [15] used a 2D numerical approach to study face stability during the slurry shield tunneling process. Chen et al. [16] constructed a 3D discrete element method to analyze the face stability of shallow shield tunnels in dry sand. Zhang et al. [17] adopted 3D numerical simulations to analyze the effects of diameter-to-depth ratios and soil properties on the tunnel face stability. Hasanpour et al. [18] simulated the single shield, double shield, and universal double shield for excavation of deep long tunnels. Graziani et al. [19] considered the creep effects for the Brenner Base Tunnel. Liu et al. [20] conducted a numerical analysis to investigate the influence of different construction schemes on the tunnel heave.

The wedge limit equilibrium model has become very popular in calculating the stability of the tunnel face [21, 22, 23, 24]. Lee et al. [25] revealed the influence of steel pipe-reinforced multi-step grouting on tunnel face stability using the limit equilibrium method. Xu et al. [26] calculated support pressure using the nonlinear Mohr-Coulomb failure criterion. Broere et al. [27] calculated the required limit support pressure using a time-dependent groundwater flow water model and the limit equilibrium wedge model. Leca et al. [28] assumed that the failure zone consisted of a series of conical bodies and derived the limit support pressure. Several researchers [29, 30, 31] derived the limit support pressure for tunnel face failure by assuming that the failure zone is a different shape. Zhang developed a horizontal slice method based on the limit equilibrium analysis theory to analyze tunnel face stability in soft surrounding rocks [32].

When the shield tunnel excavates below the river bed, high water pressure is encountered in the site [33]. Water pressure plays an important role in stability of tunnel excavation, and it may cause the stability of the tunnel face to become difficult to control [34]. If the applied face pressure is less than the limit support pressure, the tunnel face will collapse. The shield tunnel is inevitably constructed below the river, so the research on the stability of the tunnel face in multi-layer soils below river is significant. In this paper, the limit equilibrium method which takes water pressure into account is proposed for the calculation of the limit support pressure, and the solutions are compared with the numerical results for verification. The numerical analysis is carried out using FLAC3D [35].

2 Methods

The limit equilibrium method first proposed by Horn [36] is used to analyze the tunnel face stability. The tunnel face is supposed to be three-dimensional failure mode. The simple mechanism model of face stability is illustrated in Figure 1. The tunnel face mechanism approximates the circular face by means of a square and consists of a wedge and a right-angled prism. The wedge is assumed as a rigid body. B,L,H are the width, length, and height of the prism, respectively. The soil is assumed to obey the Mohr-Coulomb failure condition with cohesion represented as c and friction angle represented as φ.

Figure 1 Wedge stability model
Figure 1

Wedge stability model

The side length B of the square is approximated by setting its area equal to that of the circular tunnel face [36, 37].

(1)B2=14πD2

where D is the tunnel diameter.

The inclination of wedge α is

(2)α=45+φ2

The other side length of prism is

(3)L=Btanα

Consider an element having a dimension dz within a prism of height H as shown in Figure 1. The upper and lower vertical force of element are, respectively,

(4)P1=Aσv
(5)P2=Aσv+dσv

where σv is the effective earth pressure from the overlying prism, A is the cross-sectional area of prism.

The vertical friction applied to the lateral side of the element is

(6)f=k0Uσvtanφdz+Ucdz

where U is the girth of prism, k0 is coefficient of earth pressure at rest, and k0 = 1 − sin φ.

The vertical equilibrium equation of dz reads as follows

(7)k0Uσvtanφdz+Ucdz+Aσv+dσvAσv=γAdz

where γ is the gravity of the soil.

From the equilibrium equation of the forces acting on the wedge Eq. (7), with boundary conditionsz = 0, σv = p0, p0 is the surcharge on the surface. The effective earth pressure acting upon the wedge can be calculated using the following equation.

(8)σv=AγUcUk0tanφ1ezUk0tanφA+p0ezUk0tanφA

In practical engineering, the overburden layer of a tunnel is often the composite layers. In this paper, the effect of a multi-layered overburden on the overlying earth pressure also can be taken into account. A model of earth pressure calculation is shown in Figure 2.

Figure 2 Model of earth pressure calculation
Figure 2

Model of earth pressure calculation

It is assumed that there are n layers in the composite soils. σv1 and σvi are the earth pressures acting upon the wedge of the first and i-th layer, respectively. They can be respectively expressed as

(9)σv1=Aγ1Uc1Uk01tanφ11ez1Uk01tanφ1A+p0ez1Uk01tanφ1A
(10)σvi=AγiUciUk0itanφi1eziUk0itanφiA+σvi1eziUk0itanφiA

The earth pressure of the No. n layer can be obtained using a layer to layer method.

(11)σvn=i=2nAγiUciUk0itanφi1eziUk0itanφiAi=1i1eziUk0itanφiA+AγnUcnUk0ntanφn1eznUk0ntanφnA+p0i=1neziUk0itanφiA

Wedge analysis based on the limit equilibrium theory is adopted to obtain the support pressure for the tunnel face stability. Assuming the failure criterion holds along the failure face, a static equilibrium equation can be set up. When a shield tunnel is located below the river, the stability analyses of the shield tunnels face needs to consider the influence of water pressure. Water pressure is usually considered an external force [33], and the forces acting upon the wedge at the face are illustrated in Figure 3. A hydrostatic distribution of water pressures along the slip surface is assumed. There is an effective earth stress σv at the wedge-prism-interface, the self-weight of wedge G, the support force P at the tunnel face, the normal force Non the inclined sliding surface, the shear forces T on the inclined as well as on the sliding surface, the symmetric normal force N' and the shear force T'on the two lateral surfaces of the wedge.

Figure 3 Forces acting upon the wedge
Figure 3

Forces acting upon the wedge

The self-weight of the wedge G

(12)G=γB32tanα

where Bis the height of the wedge.

The vertical mean stress σ'z on the inclined sliding surface

(13)σz=2σvn3+Bγ3

The shear forces T on the inclined sliding surface

(14)T=cB2sinα+Ntanφ

The shear force T' on the two sides of the wedge

(15)T=B22tanαc+k0σztanφ

The vertical earth pressure Pv acting on the top of wedge is presented as

(16)Pv=Aσv=BLσv

When not taking the infiltration in the excavation face into account, the overburden strata are assumed to be permeable with high permeability, such as sand. Thus, a complete hydraulic connection exists between the river water and the groundwater [38]. The water table can be assumed to be at the surface of the river water for the computation of water pressure acting on the tunnel. In this sense, the water pressure generated by river water can be expressed as

(17)Pw=B2γwzi+γwh

where γw is the unit weight of water, zi is the thickness of the i-th stratum, which is located above the center point of the tunnel face.

According to the limit equilibrium principles, force equilibrium is realized horizontally and vertically. By considering the water pressure and equating force in the vertical and horizontal directions, the equations of equilibrium in the horizontal and vertical dimensions are obtained as

(18)PPw+Tcosα+2Tcosα=Nsinα
(19)Pv+G=Tsinα+2Tsinα+Ncosα

By solving the equilibrium Equations (18) and (19), the limit support force on the tunnel face is calculated as

(20)P=εσvBL+GcB2sinα+2Tεsinα+cosα+Pw

where ε=sinαtanφcosαcosα+tanφsinα.

The face stability analysis relevant to a circular rigid tunnel could be idealized. The support pressure is simplified to be uniform [17]. The minimal support pressure termed as the limit support pressure σT can be calculated with consideration of water pressure in river and is given as

(21)σT=PB2

3 Results

3.1 Results using the numerical method

The validity of the proposed method is evaluated in this section through a comparison with the numerical model using FLAC3D. The FLAC3D is adopted to predict the limit state and the development of deformation. An explicit Lagrangian calculation scheme is used in the FLAC3D. This is a forward scheme for a nonlinear problem which does not require iteration [18]. This code can deal with the large deformation problem very well and can avoid the problem of numerical instabilities during analysis [39, 40, 41]. Therefore, the FLAC3D is adopted to simulate the limit support pressure. The FLAC3D model is shown in Figure 4. The three-dimensional numerical model is 40 m long, 21 m wide, and 30 m high. A circular tunnel under the three layers soils is considered in evaluating the limit support pressure on the tunnel face. The tunnel support parameters are as follows: the segment is C50 concrete, the segment thickness is 30 cm, the Young modulus of the concrete segment is 34.5 GPa, Poisson’ ratio of the concrete segment is 0.2, and the density is 2.45 g/cm3. The parameters of the tunnel and soils are selected from the case of subway Line No.1 across the Ganjiang River. A circular tunnel with a diameter D of 6 m, a tunnel depth H of 12 m, and a water depth h of 10 m in river is assumed. The analysis is conducted using a linear Mohr-Coulomb yield criterion. Analyses are performed for the four cases, and the mechanical parameters of friction angle φ and cohesion c of the soil stratum are summarized in Table 1. The four cases are used to analyze the situations with the excavation layer as cohesive soil or cohesive soil, and the cases of overlying soil as cohesive soil or cohesive soil. The soil thicknesses of 1-1, 1-2, 1-3 are 6 m, 6 m, 18 m, respectively. For stratum 1-1, 1-2, 1-3, an elastic modulus Eo f 40 MPa, Poisson’ ratio ν of 0.33, and gravity γ of 20 kN/m3 of are selected.

Figure 4 Numerical model of calculation
Figure 4

Numerical model of calculation

Table 1

Mechanical parameters of soil

soilCase ACase BCase CCase D
c /kPaφ /∘c /kPaφ /∘c /kPaφ /∘c /kPaφ /∘
1-1025535025535 s
1-2535025535025
1-3025025535535

The analyses of tunnel face stability and supporting pressure are performed with FLAC3D. The applied support pressure can be normalized by the initial earth pressure [42]. The support pressure ratiois equal to the applied support pressure divided by the initial horizontal earth stress at the center of the tunnel face. The initial support pressure on the face is set as the initial horizontal earth pressure, and is gradually reduced until the tunnel face collapses. The displacements in the surrounding ground have been highlighted. Displacement contoursaround tunnel face and the displacement fields for case A, case B, case C, and case D are plotted in Figure 5. The monitoring displacements in Figure 5 are in the horizontal direction (excavation direction), and the unit of the displacement is in meters. The displacements of the tunnel face are calculated according to the different cases with a variation in soil layers. For case A and case B, the tunnel faces are in cohesionless soils. Case C and case D are in cohesivefrictional soils.

Figure 5 Displacement contours around the tunnel face
Figure 5

Displacement contours around the tunnel face

The failure zones in case A and case B are obviously larger than that in case C and case D, and mainly concentrate in the upper region of tunnel face. By comparing Figure 5(a) and Figure 5(b), it is evident that the case A has the larger zone of sliding, but is blocked by the cohesive soil layer 1-2 and is mainly concentrate in the soil layer 1-3. The sliding zone in case B extends gradually to the river bed surface, the displacement decreases drastically. For case C and case D, when the tunnel excavates in the cohesive soil layer, the sliding zone shrinks and concentrates in front of the tunnel face. It is obvious that cohesion has an important influence on the failure form.

Tunnel face stability and the behavior of surrounding soils are analyzed with varying support pressure ratios at the tunnel face. Evaluating the relationship between the displacement of a control point (the face center) and the applied support pressure ratio (normalized by initial stress) is a common way to analyze the tunnel face stability [43]. Figure 6(a) and Figure 6(b) show horizontal and vertical displacement of the face center with a variation of support pressure ratios for the case A, case B, case C, and case D, respectively. Large displacement is expected to occur when there is small support pressure ratio. The displacement increases significantly when the support pressure ratio decreases to a certain value. This value is the limit support pressure ratio. From the results of the FLAC3D analysis for the four cases previously mentioned, the calculation results of the limit support pressure on the tunnel face are shown in Table 2.

Figure 6 Displacement of the central point of face
Figure 6

Displacement of the central point of face

Table 2

Results with the FLAC3D

CaseInitial earth pressure /kPaLimit support pressure ratioLimit support pressure /kPa
A2750.755207.63
B2750.78214.50
C2750.715196.63
D2750.720198.00

3.2 Results using the limit equilibrium method

Comparative calculations are carried out. The same cases are analyzed using the proposed limit equilibrium method and numerical method using FLAC3D. The analyses of the tunnel face supporting pressure with the proposed limit equilibrium method are preformed. Table 3 compares the limit support pressure obtained using the limit equilibrium method with that obtained from the numerical method.

Table 3

Results of limit support pressure

ABCD
numerical method207.63214.50196.63198.00
limit equilibrium method219.01229.27197.72204.39
error5.19%6.44%0.55%3.12%

4 Discussion

The results of case A and case B, which were excavated in cohesionless soil, are different. The error of them is nearly 10%, although the tunnel excavates at the same soil layer. The reason is that the upper soil layer 1-2 in case A is comprised of cohesive soils, which are conducive to the stability of the tunnel face and prevent the development of a failure zone. Thus, the required limit support pressure to keep the tunnel face stable in case A is small compared to that in case B. When the excavation is in the cohesive soil for case C and case D, their required limit support pressures are similar, although the cover soil layers are different. The limit support pressure in case A and case B are obviously greater than that in case C and case D. The main reason is that the excavation stratum of case A and case B is cohesionless soil.

The limit support pressures calculated by limit equilibrium method are 219.01 kPa, 229.27 kPa, 197.72 kPa, 204.39 kPa for the cases A, B, C, and D, respectively. The results of the limit equilibrium method agree well with numerical calculations with respect to the limit support pressure, as shown in Table 3. The obtained results suggest that the approach proposed herein could be applied for fast estimations of the pressure needed for face support in multilayer soils below river, with consideration to water pressure. These values are about 5%higher than the prediction from the numerical method. Mollon et al. [44] got a similar result for a 2D stability analysis of a pressurized tunnel face in sand. The proposed limit equilibrium method is also an effective method to calculate the limit support pressure on the tunnel face for permeable overburden strata that has a high permeability. It cannot be used for impermeable overburden strata that has a low permeability. The proposed method is suitable for cohesionless soil. The proposed method is reliable and effective when it is used to design the tunnel excavation process.

5 Conclusions

Managing suitable support pressures acting on a tunnel face is very important in stabilizing the tunnel face. In this paper, a limit equilibrium method with considerations for water pressure is proposed to determine the limit support pressure of tunnel faces in multi-layer soils below river. Based on the proposed limit equilibrium methods, the limit support pressures required for tunnel face stability below the river bed are estimated on variable ground. The face stability is also investigated using the FLAC3D. The limit support pressures have been calculated to compare the results of the limit equilibrium method with those from a three-dimension numerical method FLAC3D. There is good agreement between the limit equilibrium results and the numerical results. The limit support pressure using the limit equilibrium method is greater than that obtained by the numerical method. It is safe and efficient when the limit equilibrium method is used to design the support pressure on tunnel face with permeable overburden strata that has a high permeability. This research can provide a theoretical foundation for tunnel engineering practices in multi-layer soils below the river bed. The next stage of the work is studying the limit support pressure for impermeable overburden strata that has a low permeability.

Acknowledgement

The authors gratefully acknowledge the financial support from the National Natural Sciences Foundation of China (Grant: 51468041) and Jiangxi Science Foundation (Grant: 20124ABE02106, 20161BAB203078).

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Received: 2017-12-20
Accepted: 2018-11-18
Published Online: 2018-12-31

© 2018 Weiping Liu et al., published by De Gruyter

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

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  9. Architecture and reservoir quality of low-permeable Eocene lacustrine turbidite sandstone from the Dongying Depression, East China
  10. Flow units classification for geostatisitical three-dimensional modeling of a non-marine sandstone reservoir: A case study from the Paleocene Funing Formation of the Gaoji Oilfield, east China
  11. Umbrisols at Lower Altitudes, Case Study from Borská lowland (Slovakia)
  12. Modelling habitats in karst landscape by integrating remote sensing and topography data
  13. Mineral Constituents and Kaolinite Crystallinity of the <2 μm Fraction of Cretaceous-Paleogene/Neogene Kaolins from Eastern Dahomey and Niger Delta Basins, Nigeria
  14. Construction of a dynamic arrival time coverage map for emergency medical services
  15. Characterizing Seismo-stratigraphic and Structural Framework of Late Cretaceous-Recent succession of offshore Indus Pakistan
  16. Geosite Assessment Using Three Different Methods; a Comparative Study of the Krupaja and the Žagubica Springs – Hydrological Heritage of Serbia
  17. Use of discriminated nondimensionalization in the search of universal solutions for 2-D rectangular and cylindrical consolidation problems
  18. Trying to underline geotourist profile of National park visitors: Case study of NP Fruška Gora, Serbia (Typology of potential geotourists at NP Fruška Gora)
  19. Fluid-rock interaction and dissolution of feldspar in the Upper Triassic Xujiahe tight sandstone, western Sichuan Basin, China
  20. Calcified microorganisms bloom in Furongian of the North China Platform: Evidence from Microbialitic-Bioherm in Qijiayu Section, Hebei
  21. Spatial predictive modeling of prehistoric sites in the Bohemian-Moravian Highlands based on graph similarity analysis
  22. Geotourism starts with accessible information: the Internet as a promotional tool for the georesources of Lower Silesia
  23. Models for evaluating craters morphology, relation of indentation hardness and uniaxial compressive strength via a flat-end indenter
  24. Geotourism in an urban space?
  25. The first loess map and related topics: contributions by twenty significant women loess scholars
  26. Modeling of stringer deformation and displacement in Ara salt after the end of salt tectonics
  27. A multi-criteria decision analysis with special reference to loess and archaeological sites in Serbia (Could geosciences and archaeology cohabitate?)
  28. Speleotourism in Slovenia: balancing between mass tourism and geoheritage protection
  29. Attractiveness of protected areas for geotourism purposes from the perspective of visitors: the example of Babiogórski National Park (Poland)
  30. Implementation of Heat Maps in Geographical Information System – Exploratory Study on Traffic Accident Data
  31. Mapping War Geoheritage: Recognising Geomorphological Traces of War
  32. Numerical limitations of the attainment of the orientation of geological planes
  33. Assessment of runoff nitrogen load reduction measures for agricultural catchments
  34. Awheel Along Europe’s Rivers: Geoarchaeological Trails for Cycling Geotourists
  35. Simulation of Carbon Isotope Excursion Events at the Permian-Triassic Boundary Based on GEOCARB
  36. Morphometry of lunette dunes in the Tirari Desert, South Australia
  37. Multi-spectral and Topographic Fusion for Automated Road Extraction
  38. Ground-motion prediction equation and site effect characterization for the central area of the Main Syncline, Upper Silesia Coal Basin, Poland
  39. Dilatancy as a measure of fracturing development in the process of rock damage
  40. Error-bounded and Number-bounded Approximate Spatial Query for Interactive Visualization
  41. The Significance of Megalithic Monuments in the Process of Place Identity Creation and in Tourism Development
  42. Analysis of landslide effects along a road located in the Carpathian flysch
  43. Lithological mapping of East Tianshan area using integrated data fused by Chinese GF-1 PAN and ASTER multi-spectral data
  44. Evaluating the CBM reservoirs using NMR logging data
  45. The trends in the main thalweg path of selected reaches of the Middle Vistula River, and their relationships to the geological structure of river channel zone
  46. Lithostratigraphic Classification Method Combining Optimal Texture Window Size Selection and Test Sample Purification Using Landsat 8 OLI Data
  47. Effect of the hydrothermal activity in the Lower Yangtze region on marine shale gas enrichment: A case study of Lower Cambrian and Upper Ordovician-Lower Silurian shales in Jiangye-1 well
  48. Modified flash flood potential index in order to estimate areas with predisposition to water accumulation
  49. Quantifying the scales of spatial variation in gravel beds using terrestrial and airborne laser scanning data
  50. The evaluation of geosites in the territory of National park „Kopaonik“(Serbia)
  51. Combining multi-proxy palaeoecology with natural and manipulative experiments — XLII International Moor Excursion to Northern Poland
  52. Dynamic Reclamation Methods for Subsidence Land in the Mining Area with High Underground Water Level
  53. Loess documentary sites and their potential for geotourism in Lower Silesia (Poland)
  54. Equipment selection based on two different fuzzy multi criteria decision making methods: Fuzzy TOPSIS and fuzzy VIKOR
  55. Land deformation associated with exploitation of groundwater in Changzhou City measured by COSMO-SkyMed and Sentinel-1A SAR data
  56. Gas Desorption of Low-Maturity Lacustrine Shales, Trassic Yanchang Formation, Ordos Basin, China
  57. Feasibility of applying viscous remanent magnetization (VRM) orientation in the study of palaeowind direction by loess magnetic fabric
  58. Sensitivity evaluation of Krakowiec clay based on time-dependent behavior
  59. Effect of limestone and dolomite tailings’ particle size on potentially toxic elements adsorption
  60. Diagenesis and rock properties of sandstones from the Stormberg Group, Karoo Supergroup in the Eastern Cape Province of South Africa
  61. Using cluster analysis methods for multivariate mapping of traffic accidents
  62. Geographic Process Modeling Based on Geographic Ontology
  63. Soil Disintegration Characteristics of Collapsed Walls and Influencing Factors in Southern China
  64. Evaluation of aquifer hydraulic characteristics using geoelectrical sounding, pumping and laboratory tests: A case study of Lokoja and Patti Formations, Southern Bida Basin, Nigeria
  65. Petrography, modal composition and tectonic provenance of some selected sandstones from the Molteno, Elliot and Clarens Formations, Karoo Supergroup, in the Eastern Cape Province, South Africa
  66. Deformation and Subsidence prediction on Surface of Yuzhou mined-out areas along Middle Route Project of South-to-North Water Diversion, China
  67. Abnormal open-hole natural gamma ray (GR) log in Baikouquan Formation of Xiazijie Fan-delta, Mahu Depression, Junggar Basin, China
  68. GIS based approach to analyze soil liquefaction and amplification: A case study in Eskisehir, Turkey
  69. Analysis of the Factors that Influence Diagenesis in the Terminal Fan Reservoir of Fuyu Oil Layer in the Southern Songliao Basin, Northeast China
  70. Gravity Structure around Mt. Pandan, Madiun, East Java, Indonesia and Its Relationship to 2016 Seismic Activity
  71. Simulation of cement raw material deposits using plurigaussian technique
  72. Application of the nanoindentation technique for the characterization of varved clay
  73. Verification of compressibility and consolidation parameters of varved clays from Radzymin (Central Poland) based on direct observations of settlements of road embankment
  74. An enthusiasm for loess: Leonard Horner in Bonn and Liu Tungsheng in Beijing
  75. Limit Support Pressure of Tunnel Face in Multi-Layer Soils Below River Considering Water Pressure
  76. Spatial-temporal variability of the fluctuation of water level in Poyang Lake basin, China
  77. Modeling of IDF curves for stormwater design in Makkah Al Mukarramah region, The Kingdom of Saudi Arabia
Heruntergeladen am 7.9.2025 von https://www.degruyterbrill.com/document/doi/10.1515/geo-2018-0074/html
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