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Then, using the initial soil pH and the aluminium content, the amount of lime needed to raise the pH to a desired level can be calculated. [68] Amendments other than agricultural lime that can be used to increase the pH of soil include wood ash, industrial calcium oxide , magnesium oxide, basic slag (calcium silicate), and oyster shells.
Effect of soil pH on cation-exchange capacity. The amount of negative charge from deprotonation of clay hydroxy groups or organic matter depends on the pH of the surrounding solution. Increasing the pH (i.e. decreasing the concentration of H + cations) increases this variable charge, and therefore also increases the cation-exchange capacity.
Soil acidification naturally occurs as lichens and algae begin to break down rock surfaces. Acids continue with this dissolution as soil develops. With time and weathering, soils become more acidic in natural ecosystems. Soil acidification rates can vary, and increase with certain factors such as acid rain, agriculture, and pollution. [1]
Soil pH Test: For a very low price, your local Extension office will test your soil pH. To have a test completed, simply collect one cup’s worth of soil and remove all debris, such as sticks ...
Soil pH is a function of many soil forming factors, and is generally lower (more acidic) where weathering is more advanced. [ 43 ] Most plant nutrients, with the exception of nitrogen , originate from the minerals that make up the soil parent material.
It is of use in distinguishing boundaries of horizons within a soil profile, [110] determining the origin of a soil's parent material, [111] as an indication of wetness and waterlogged conditions, [112] and as a qualitative means of measuring organic, [113] iron oxide [114] and clay contents of soils. [111]