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how do freezing, thawing, wetting, and drying contribute to soil creep?

How do freezing, thawing, wetting, and drying contribute to soil creep? ANSWER: –The soil expands and contracts, lifting particles and dropping them a slight distance downslope.

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    What processes are responsible for soil creep?

    The most important process producing creep, aside from direct gravitational influences, is frost heaving: as interstitial water freezes, surface particles are forced up and out perpendicular to the slope; when let down by melting, these particles are drawn directly downward by gravity and are thereby gradually moved …

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    How does water contribute to soil creep?

    2. Adding water increases slope instability. It lubricates rock fragments so that they slide down slope more easily.

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    What factors facilitate soil creep?

    Creep can be facilitated by freezing and thawing because, as shown in Figure 15.12, particles are lifted perpendicular to the surface by the growth of ice crystals within the soil, and then let down vertically by gravity when the ice melts. The same effect can be produced by frequent wetting and drying of the soil.

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    Can repeated freezing and thawing be important in soil creep movements?

    Repeated freezing and thawing can be important in soil creep movements. Lahars are essentially mudflows associated with volcanoes and volcanism. Solifluction is an important mass wasting process in areas of permafrost.

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    What factors influence soil creep?

    The results of graphical and statistical analysis showed that rates of creep are controlled by a number of ‘force’ factors, chiefly soil moisture, field capacity and plasticity index, together with ‘resistance’ factors, particularly bulk density and a number of shear stress measures.

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    What can facilitate soil creep?

    Creep can be facilitated by freezing and thawing because, as shown in Figure 15.12, particles are lifted perpendicular to the surface by the growth of ice crystals within the soil, and then let down vertically by gravity when the ice melts. The same effect can be produced by frequent wetting and drying of the soil.

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    What is soil creep and what contributes to it?

    Soil creep is a process operating at the granular scale. It happens on gentle slopes and is noticeable from the wavy surface it produces. Damp soil moves very slowly down the slope as the weight of water pushes it forwards. Rain splash may release soil grains that fall further downslope.

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    What can cause a creep?

    In materials science, creep (sometimes called cold flow) is the tendency of a solid material to undergo slow deformation while subject to persistent mechanical stresses. It can occur as a result of long-term exposure to high levels of stress that are still below the yield strength of the material.

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    What factors cause soil creep?

    Soil creep is determined and modified by climate (temperature and soil moisture conditions), biota, topography, rock weathering processes, and soil production rates [6, 26].

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    What is the process of soil creep?

    Soil creep is a process operating at the granular scale. It happens on gentle slopes and is noticeable from the wavy surface it produces. Damp soil moves very slowly down the slope as the weight of water pushes it forwards. Rain splash may release soil grains that fall further downslope.

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    Is frost important in soil creep?

    Frost action is shown to be the dominant factor causing soil creep.

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    What are the two main factors that contribute to creep in a soil?

    The seasonal soil creep is driven particularly by moisture and temperature fluctuations (e.g., frost heaving) and the activity of living organisms (Kirkby, 1967; Pawlik and Š amonil, 2018) The maximum soil creep rate is usually found at the top of the topsoil and occasionally at great depths (Clarke et al., 1999).

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    What conditions are needed for soil creep to occur?

    Soil creep occurs in moist soils where the water acts as a lubricant. It is more likely to occur on steeper slopes and in areas where the soil is thick. It may also be caused by the alternate wetting and drying or alternate freezing and thawing of the soil.

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    Which type of mass movement is caused by freeze and thaw?

    Creep is slow moving caused by seasonal freezing and thawing and causes fences and other structures to tilt downhill.

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    What contributes to soil creep?

    They defined soil creep caused by burrowing agents (e.g., worms, ants, and moles) and tree throw as the main factor for creeping soil.

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    How does water contribute to mass wasting?

    Adding water increases slope instability. It lubricates rock fragments so that they slide down slope more easily. Mass wasting occurs more readily in rainy seasons for this reason.

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    Is soil creep wet or dry?

    They can occur after periods of heavy rain, when the water saturates overlying rock, making it heavy and liable to slide. Soil creep is a very slow movement, occurring on very gentle slopes because of the way soil particles repeatedly expand and contract in wet and dry periods.

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