Organic Soil (Histosol)

Typical Characteristics

  • Parent Material: Organic soils are formed by the accumulation of partially decomposed organic matter. These soils have undergone little profile development, due to the anaerobic environment (absent of oxygen) that persists. Organic soils contain more than one layer of organic soil material, typically in the upper 80 cm of the soil profile.
  • Climate and Distribution: Organic soils are most common in moist, cool areas, such as wetlands of Canada, but may be found in warm environments. Organic deposits in marshes, bogs, and swamps are common examples, but their formation is not strictly limited to wetlands.
  • Productivity: Many organic soils on the continental United States have been drained and mined for agricultural use. These soils can be very productive, but require very different nutrient management strategies than other soil orders.

Organic Soils of Maui:

Histosols of Maui
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WET/DRY ORGANIC SOILS WITH LEAF MAT ACCUMULATIONS (USTIFOLIST)

  • Kaimu Series

WET ORGANIC SOIL WITH LEAF MAT ACCUMULATIONS (UDIFOLIST)

  • Malama Series
  • Opihikao Series

Unique Characteristics of Organic Soils of Maui County:

Most of Maui’s organic soils are forested, wildlife habitats. Other organic soils are found in residential areas or used to supply water. However, the Malama Series is an organic soil that is has some agricultural significance.
  • Data for the Malama Series in Maui is not available. Location: The Malama series are upland organic soils located in East Maui at elevations between sea level and 1,000 ft.
  • Texture: Stony muck above `a`a lava flow
  • Rainfall and Temperature: The average annual rainfall is 60 to 90 inches, and the average annual temperature is 72 degrees F.
  • Slope: Gentle to moderate
  • Physical Traits: The surface layer is characterized as shallow, stony black muck. The soils have excessive drainage, very rapid permeability, and slow runoff.
  • Color of surface Horizon: Black muck
  • Agricultural Use: While mostly used to supply water, the Malama Series have been used in pasture and orchards.

Related Posts:

  • Histosol (Organic soil) Organic Soil (Histosol) Typical Characteristics Parent Material: Organic soils are formed by the accumulation of partially decomposed organic matter. These soils have undergone little profile development, due to the anaer… Read More
  • Volcanic materials of soil Volcanic materials Volcanic soils are developed from volcanic materials, which have a glassy, or non-crystalline, structure. As a result, volcanic soils largely consist of amorphous materials that lack a crystalline struct… Read More
  • Silicate clays of soila Layered Silicate clays Layered silicate clays are secondary minerals that have formed as the result of weathering of parent material. There are two major categories of layered silicate clays within the soil: high activity … Read More
  • What is soil WHAT IS SOIL? Soils are complex mixtures of minerals, water, air, organic matter, and countless organisms that are the decaying remains of once-living things. It forms at the surface of land – it is the “skin of the e… Read More
  • Arid Soils (Aridisol) Typical Characteristics Distribution: Arid soils are one of the most prevalent soil orders of the world. Climate: Arid soils are most characterized by their water deficiencies. Most arid soils contain sufficien… Read More

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