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  2. Soil thermal properties - Wikipedia

    en.wikipedia.org/wiki/Soil_thermal_properties

    Apart from the basic soil composition, which is constant at one location, soil thermal properties are strongly influenced by the soil volumetric water content, volume fraction of solids and volume fraction of air. Air is a poor thermal conductor and reduces the effectiveness of the solid and liquid phases to conduct heat.

  3. Weathering - Wikipedia

    en.wikipedia.org/wiki/Weathering

    Mineral weathering can also be initiated or accelerated by soil microorganisms. Soil organisms make up about 10 mg/cm 3 of typical soils, and laboratory experiments have demonstrated that albite and muscovite weather twice as fast in live versus sterile soil. Lichens on rocks are among the most effective biological agents of chemical weathering ...

  4. Frost heaving - Wikipedia

    en.wikipedia.org/wiki/Frost_heaving

    Photograph taken 21 March 2010 in Norwich, Vermont. Frost heaving (or a frost heave) is an upwards swelling of soil during freezing conditions caused by an increasing presence of ice as it grows towards the surface, upwards from the depth in the soil where freezing temperatures have penetrated into the soil (the freezing front or freezing boundary).

  5. Soil formation - Wikipedia

    en.wikipedia.org/wiki/Soil_formation

    Very intense chemical weathering, leaching, and erosion in warm and humid regions where soil does not freeze; Climate directly affects the rate of weathering and leaching. Wind moves sand and smaller particles (dust), especially in arid regions where there is little plant cover, depositing it close to [55] or far from the entrainment source. [56]

  6. Ready to start your spring planting? 5 things to know about ...

    www.aol.com/ready-start-spring-planting-5...

    It's almost Derby, which means it's almost peak gardening season. But before starting any planting, it’s best to look at the dirt under your feet.

  7. Active layer - Wikipedia

    en.wikipedia.org/wiki/Active_layer

    Cryoturbation is the dominant force operating in the active layer, and tends to make it generally uniform in composition throughout. However, variation in the composition of soils due to differences in parent rock are very marked in permafrost regions due to the low rate of weathering in the very cold climate.

  8. Physical properties of soil - Wikipedia

    en.wikipedia.org/wiki/Physical_properties_of_soil

    Soil bulk density, when determined at standardized moisture conditions, is an estimate of soil compaction. [3] Soil porosity consists of the void part of the soil volume and is occupied by gases or water. Soil consistency is the ability of soil materials to stick together. Soil temperature and colour are self-defining.

  9. Why is it warm in November? How climate change has ... - AOL

    www.aol.com/why-warm-november-climate-change...

    Voters in New York City saw the warmest weather on a presidential Election Day since the 1930s. High temperatures, drought, and wind have created the perfect fire conditions in the area.