HIGHLY WEATHERED VOLCANIC SOIL

Kula Series
   Photo by Tai McClellan
The Hana Series is a characteristic highly weathered, infertile volcanic soil.
  • Location: The Hana Series is located on the windward side of East Maui, and it occupies a land area of approximately 8,000 acres. The elevation at which you will find this soil is between sea level and in the uplands of 1,200 ft.
  • Texture: Silty clay loam
  • Rainfall and Temperature: The average annual rainfall is between 80 and 150 inches, and the average temperature is 73 degrees F.
  • Slope: Gently to moderately steep
  • Parent Material: The Hana Series was derived from volcanic ash that was deposited over cinders and `a`a lava flows. The depth of the soil profile may extend from 27 to 40 inches.
  • Depth: While the surface soil is typically 12 inches, the subsoil extends 22 inches.
  • Physical Traits: The surface may be very rocky depending upon the location. The soil has good drainage, with moderately rapid permeability and medium runoff.
  • Color of surface horizon: Dark brown/dark grayish brown
  • Fertility: The Hana Series is typically deficient in nutrients such as phosphorus.
  • Acidity: Strongly to medium acidity
  • Natural vegetation: Grasses and tree species.
  • Agriculture: Pasture.
  • Related Soil Series: Honomanu Series

HIGHLY WEATHERED VOLCANIC SOIL VS. MODERATELY WEATHERED VOLCANIC SOIL

The major differences between a highly weathered soil, such as the Honomanu Series (Hana’s sister series) and a moderately weathered soil, such as the Kula Series is highlighted in the following table. The Honomanu Series is acidic and depleted in plant nutrients such as calcium, whereas the Kula Series is slightly acidic and rich in calcium

Related Posts:

  • Highly Weathered Tropical Soils (Oxisol) Highly Weathered Tropical Soils (Oxisol) Typical Characteristics Climate: Oxisols are the most highly weathered soil order. These soils form under year-round hot, tropical climates. Although climatic pattern may have chan… Read More
  • Nutrient Mobility Nutrient Mobility WITHIN PLANT An important characteristic of some nutrients is the ability to move within the plant tissue. In general, when certain nutrients are deficient in the plant tissue, that nutrient is able tran… Read More
  • Terminology of relative nutrient status of soil The relative nutrient status of a plant may be easily described using the following terms: Deficiency rangeNutrient deficiencies occur in plants when an essential element is not taken up by the plant in sufficient amounts.… Read More
  • Buffering capacity of soil The quantity of aluminum and hydrogen in each of the 3 pools of acidity is not permanently fixed. Instead, the relative amounts of aluminum and hydrogen can change, as aluminum and hydrogen moves from pool to pool. Thus, … Read More
  • soil acidity Origins of acidity There are a multiple origins of soil acidity. The following is a list of causes which are common in Hawaii: Release of hydrogen atoms under natural chemical processes in the soil Atmospheric carbon diox… Read More

0 Comments:

Powered by Blogger.

Visitors

199263
Print Friendly Version of this pagePrint Get a PDF version of this webpagePDF


 download University Notes apps for android

Popular Posts

Flag Counter