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Soil Types - Soil Quality AnalysisSoil Acidity (pH) - Soil Fertility and Organic Matter
For example, the largest particles, sand, determine aeration and drainage characteristics, while the tiniest, sub-microscopic clay particles, are chemically active, binding with water and plant nutrients. The ratio of these sizes determines soil type: clay, loam, clay-loam, silt-loam, and so on. Soil Acidity or pH readingThe pH is a measure of the acidity or alkalinity of soil in a solution. An acid solution has a pH value less than 7. While a basic solution always has a pH larger than 7, an alkaline solution (i.e. a solution with positive acid neutralizing capacity) does not necessarily have a pH larger than 7. Soil pH is an important consideration for gardeners for several reasons; as many plants and soil life forms prefer either alkaline or acidic conditions, some diseases tend to thrive when the soil is alkaline or acidic or the pH can affect the availability of nutrients in the soil. In addition to the pH the mineral composition of soil; Soil Fertility and Organic Matter, known as humus also plays a crucial role in soil characteristics and soil fertility for plant life. Soil may be mixed with larger aggregate, such as pebbles or gravel. Not all Soil Types are permeable, such as pure clay, which can be used for lining ponds. There are many recognized soil classifications, both international and national.
Sponsored Links:Soil Analysis Soil pH Soil Types Soil Acidity Soil Fertility
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