When.com Web Search

Search results

  1. Results From The WOW.Com Content Network
  2. Dryland salinity - Wikipedia

    en.wikipedia.org/wiki/Dryland_salinity

    Soil is considered in two contexts when it comes to dryland salinity: Recharge and discharge. Soils in groundwater recharge areas. Soils absorb and store water according to their water holding or field capacity and how dry they are to start with. In much of Victoria, under typical rainfall and natural vegetation cover, soils take on water ...

  3. Shrink–swell capacity - Wikipedia

    en.wikipedia.org/wiki/Shrink–swell_capacity

    Soils with this shrink-swell capacity fall under the soil order of Vertisols. [6] As these soils dry, deep cracks can form on the surface, which then allows water to penetrate to deeper levels of the soil. [7] This can cause the swelling of these soils to become cyclical, with periods of both shrinking and swelling.

  4. Badlands - Wikipedia

    en.wikipedia.org/wiki/Badlands

    Badlands are a type of dry terrain where softer sedimentary rocks and clay-rich soils have been extensively eroded. [1] They are characterized by steep slopes, minimal vegetation, lack of a substantial regolith, and high drainage density. [2] Ravines, gullies, buttes, hoodoos and other such geologic forms are common in badlands.

  5. Desertification - Wikipedia

    en.wikipedia.org/wiki/Desertification

    Unprotected, dry soil surfaces blow away with the wind or are washed away by flash floods, leaving infertile lower soil layers that bake in the sun and become an unproductive hardpan. This spread of arid areas is caused by a variety of factors, such as overexploitation of soil as a result of human activity and the effects of climate change. [3] [4]

  6. Aridisol - Wikipedia

    en.wikipedia.org/wiki/Aridisol

    Aridisols (from the Latin aridus, for "dry", and solum) form in an arid or semi-arid climate. Aridisols dominate the deserts and xeric shrublands, which occupy about one-third of the Earth's land surface. Aridisols have a very low concentration of organic matter, reflecting the paucity of vegetative production on these dry soils. Water ...

  7. A dry, warmer winter means more snirt. What is it and why is ...

    www.aol.com/dry-warmer-winter-means-more...

    The nutrient-rich dirt can build high yields and enrich the soil for generations of future farmers. But in dry years, when harvested corn and soybean fields remain uncovered by snow, that dirt can ...

  8. Why You Shouldn't Repot Houseplants in Winter (Plus 6 Times ...

    www.aol.com/lifestyle/why-shouldnt-repot...

    Backfill the pot with more soil until the soil line is about 1 inch below the pot’s rim. Firm the soil around the base of your plant to keep the stems upright and add a supporting stake if your ...

  9. Soil salinity - Wikipedia

    en.wikipedia.org/wiki/Soil_salinity

    Salts dissolved from the soil accumulate at the soil surface and are deposited on the ground and at the base of the fence post. Saline incrustation in a PVC irrigation pipe from Brazil. Soil salinity is the salt content in the soil; the process of increasing the salt content is known as salinization. [1] Salts occur naturally within soils and ...