Essay On Types Of Soil

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Types of Soils
Soil is defined as the earth surface that serves as a natural medium for plants growth. “Soil is a combination of organic materials, mineral grains, water, and gas” (Thompson & Turk, 1993, p.253). It is very important to the environments as it produced essential products and provide critical ecosystem for life. In general soils are classified into three major categories. Which are Histosols, Oxisols and Ultisols (Refer to figure 1 in appendix 1).

The first type of soil is Histosols. Histosols are formed in Topical Wetland climate with a weathered and thick organic soils (more than 20% organic materials by mass) or peat soils (Bouwman, 1990). According to Histosol (n.d.), organic soils are formed by the accumulation of partially decomposed organic matter under waterlogged conditions of peat bogs, moors, and swamps. Thus the accumulated of plants residues and animals and their decomposition products are preserved, resulting in high organic content in soils. They are light in weight, with extremely high water holding capacities (WHC) and have high cation exchange capacity (CEC), it also appeared dark in color (University of Hawai‘i, 2014). Based on Grozav & Rogobete (2010) who studied soil on Romania said that histosols have high compressibility, low bulk density, and high rate of decay upon drainage. According to Kim (2000), in a water-saturated environment, where conditions are good, thick and much deposit are usually formed. There are problem of dropping in the level of soils surface causes by the natural drainage, where “continuous decomposition of the organic matter brought about by the better aeration” (Kim, 2000, pp. 23-24). Since Histosols exhibit very low bulk density values, it may need to be compacted in o...

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... that resulting in yellow to red colour of soils (University of Hawai‘i, 2014). Ultisols is considered to be low activity, or low fertility because of its acidic condition and low base status. However, it usually contain clay that is non-sticky and very workable (University of Hawai‘i, 2014). Bouwman (1990) stated that ultisols are frequently high in aluminium saturation and the cation exchange capacities (CEC) are saturated with less than 35 % base-cations. Although they are low availability of nutrient, with adequate liming, the addition of organic matter, fertilizer application, and with proper management, these soils can be agriculturally productive soils of Malaysia (Kim, 2000).
In conclusion, there are three major type of soil and they are differentiated by the region where they are formed and its soil structure associated with the environments of the soils.

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