Results 51 to 60 of about 906 (240)
The water content of the foundation soil will change dynamically as a result of rainfall, snowfall, and ground surface evaporation, leading to a significant change in frost heave properties of the foundation soil in cold regions. One-dimensional freezing
Yongtao Wang +5 more
doaj +1 more source
Artificial freezing of water-bearing soil layers composing a sedimentary deposit can induce frost heave and water migration that affect the natural stress–strain state of the soil layers and freezing process.
M. Zhelnin +5 more
doaj +1 more source
Stability of the Foundation of Buried Energy Pipeline in Permafrost Region
During operation, a buried pipeline is threatened by a variety of geological hazards, particularly in permafrost regions, where freezing-thawing disasters have a significant influence on the integrity and safety of the buried pipelines. The topographical
Yan Li +4 more
doaj +1 more source
Study on Frost Heaving Characteristics of Sulfate-Bearing Sand in Seasonally Frozen Regions
With the Longzhong Water Conservation and Ecological Water Supply and Storage Reservoir Project (Upper Yellow River) as the engineering background, this study selected sulfate sandy soil from Jingtai County (Baiyin City, Gansu Province, the project area)
Kaixiang Yang +3 more
doaj +1 more source
The initiation and reception of shields are major risk events for shield construction in water-rich and weak strata. Although the freezing method and the steel sleeve method receiving-shield tunneling technologies both have engineering applications, the ...
Y. Mei +4 more
doaj +1 more source
The evolution of the temperature field and frozen wall under different fracture conditions was examined by an artificial ground freezing‐based thermal‐hydraulic coupled model. It was observed that fracture inclination affects the interaction extent of freezing pipes and fracture, while phase transition extent is the dominant factor for heat transfer in
Chenyi Zhang +9 more
wiley +1 more source
Measurement of Suction Pressure Generated in the Process of Frost Heaving in Rock
Recently it has been found that frost heave phenomena can be seen not also in soil but also in rock. It is obvious, however, that the number of researches on frost heaving in rock is much less than that of researches on frost heaving in soil.
Dai NAKAMURA +5 more
doaj +1 more source
B1 is bord width 1, B2 is bord width 2, L is the pillar length, W is the pillar width, red color and letter A represent the pillars, and white color and number 1 represent excavated areas. Pstress is the average pillar stress; σv is the vertical component of the virgin stress, MPa; and e is the areal extraction ratio. e = B o B o + B P ${\rm{e}}=\frac{{
Tawanda Zvarivadza +4 more
wiley +1 more source
Frost heave tests on tills with an apparatus for constant heat flow
Paper presented at the 2nd International Symposium on Ground Freezing, Norwegian Institute of Technology, Trondheim, Norway, June 24—26 ...
Sven Freden, L Stenberg
openalex +2 more sources
Field frost heave predictions using the segregation potential concept
The Konrad–Morgenstern theory of frost heave using the segregation potential concept is briefly outlined, and the method of predicting frost heave under field conditions is reviewed. A recent paper by Nixon et al.
John F. Nixon
core +1 more source

