نتایج جستجو برای: soil freezing

تعداد نتایج: 197785  

2006
R. Cory Greer Joan Q. Wu Prabhakar Singh Donald K. McCool

The Palouse area of the Northwestern Wheat and Range Region suffers high erosion throughout the winter season. The excessive soil loss is a result of a combination of winter precipitation, intermittent freezing and thawing of soils, steep land slopes, and improper management practices. Soil strength is typically decreased by the cyclic freeze and thaw, particularly during the period of thawing....

2016
Mikhail Filimonov Nataliia Vaganova

A mathematical model, numerical algorithm and program code for simulation thermal changes in permafrost as a result of operation of a horizontal flare system in northern oil and gas field are presented. In the model the most significant climatic and physical factors are taken into account such as solar radiation, determined by specific geographical location, heterogeneous structure of frozen so...

Journal: :Fractal and fractional 2022

Freezing action always results in great damage to the pore structure and fractal characteristics of freezing–thawing soft soil. Nuclear magnetic resonance (NMR) can help collect data describe microstructure frozen–thawed This paper conducted a series nuclear tests interpret effect freezing duration, pressure temperature on soil’s micro-pore characteristics. The size distributions (PSDs) tested ...

2007
Zhen Li Chou Xie Xinwu Li

The surface displacement by seasonally freezing bulge and thawing subsidence are main hazards for engineering construction in permafrost regions, especially for the Qinghai-Tibet railway. For detecting the distortion at permafrost area, we try to study the interferometric method of monitoring the deformation at permafrost area with time-series EnviSat ASAR data. In this paper, the coherence cha...

2007
M. A. Kessler A. B. Murray B. T. Werner

Sorted circles emerge as self-organized patterns from a laterally uniform active layer that becomes laterally sorted as frost heave deforms the interface between a stone layer and an underlying soil layer. In a three-dimensional, cellular model of the active layer, cyclic freezing and thawing drives transport of stone and soil particles by (1) addition of ice particles representing soil expansi...

Journal: :IEEE Transactions on Geoscience and Remote Sensing 2004

Journal: :Journal of the Japanese Society of Snow and Ice 1997

2015
Nataliia Vaganova Mikhail Filimonov

A mathematical model, numerical algorithm and program code for simulation and long-term forecasting of changes in permafrost as a result of operation of a multiple well pad of northern oil and gas field are presented. In the model the most significant climatic and physical factors are taken into account such as solar radiation, determined by specific geographical location, heterogeneous structu...

Journal: :Proceedings. Biological sciences 2011
S K Schmidt R C Lynch A J King D Karki M S Robeson L Nagy M W Williams M S Mitter K R Freeman

High-elevation valleys in dry areas of the Himalayas are among the most extreme, yet least explored environments on Earth. These barren, rocky valleys are subjected to year-round temperature fluctuations across the freezing point and very low availability of water and nutrients, causing previous workers to hypothesize that no photoautotrophic life (primary producers) exists in these locations. ...

Journal: :SIAM Journal of Applied Mathematics 2011
Stephen Peppin Apala Majumdar Robert Style Graham Sander

We develop a mathematical model of frost heave in colloidal soils. The theory accounts for heave and consolidation, while not requiring a frozen fringe assumption. Two solidification regimes occur: a compaction regime in which the soil consolidates to accommodate the ice lenses, and a heave regime during which liquid is sucked into the consolidated soil from an external reservoir, and the added...

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