Difference between revisions of "PH"
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== Why soils become acidic == | == Why soils become acidic == | ||
+ | While the pH of a soil is measured based on how many H<sup>+</sup> a soil contains, Aluminium ions (Al<sup>3+<sup>) are also important. In acidic soils Al<sup>3+<sup> reacts with water and releases extra H<sup>+</sup> ions. | ||
=== Rainfall and leaching === | === Rainfall and leaching === | ||
+ | Acidic soils are most often found in areas of high rainfall. In time, excessive rainfall leaches the soil profile's basic elements (calcium, magnesium, sodium, and potassium) that prevent soil acidity. Additionally, rainwater has a slightly acidic pH of 5.7 due to a reaction with CO<sub>2</sub> in the atmosphere that forms carbonic acid. | ||
=== Acidic parent material === | === Acidic parent material === |
Revision as of 08:26, 15 January 2012
- Topic in Gardening courses
Soil pH is a measure for how many H+ ions a soil contains. pH is a measure of how acidic or basic things are.
pH is defined as the negative logarithm (base 10) of the activity of hydrogen ions (H+) in solution. It ranges from 0 to 14, with 7 being neutral. A pH below 7 is acidic and above 7 is basic.[1] A pH of 6 means that there are 10 times more H+ ions in the soil compared to pH 7, while, for example, a pH of 3 means that there are 10,000(104) times more H+ ions in solution compared to pH 7.
Substances such as lemon juice and battery acid are acidic and fall in the 0-7 range, whereas seawater and bleach are basic (also called "alkaline") and fall in the 7-14 pH range. Pure water is neutral, or 7 on the pH scale.
Soil pH controls many chemical processes that take place in the soil. It specifically affects plant nutrient availability by changing the chemical form in which these nutrients are available. The optimum pH range for most plants is between 6 and 7.5, but many plants have adapted to pH values outside this range.
Classification of soil pH ranges
A peaty soil is acid. Some clay soils are neutral. Chalky soils are alkaline or basic or limey.
Denomination | pH range |
---|---|
Ultra acid | <3.5 |
Extreme acid | 3.5 - 4.4 |
Very strong acid | 4.5 - 5.0 |
Strong acid | 5.1 - 5.5 |
Moderate acid | 5.6 -6.0 |
Slight acid | 6.1 -6.5 |
Neutral | 6.6 - 7.3 |
Slightly alkaline | 7.4 - 7.8 |
Moderately alkaline | 7.9 - 8.4 |
Strongly alkaline | 8.5 -9.0 |
Very strongly alkaline | >9.0 |
Source: The United States Department of Agriculture Natural Resources Conservation Service
Why soils become acidic
While the pH of a soil is measured based on how many H+ a soil contains, Aluminium ions (Al3+) are also important. In acidic soils Al3+ reacts with water and releases extra H+ ions.
Rainfall and leaching
Acidic soils are most often found in areas of high rainfall. In time, excessive rainfall leaches the soil profile's basic elements (calcium, magnesium, sodium, and potassium) that prevent soil acidity. Additionally, rainwater has a slightly acidic pH of 5.7 due to a reaction with CO2 in the atmosphere that forms carbonic acid.
Acidic parent material
Organic matter decay
High-yielding crops
Plant pH preferences
- This list is still under construction and needs to be checked with various sources
- pH 4.5-5.0 Blueberry, Bilberry, Heather, Cranberry, Orchid, Azalea
- pH 5.0 - 5.5 Parsley, Potato, Heather, Pine, Maize, Radish, Ferns, Iris, Rhododendron
- pH 5.5 - 6.0 Bean, Brussels Sprouts, Carrot, Endive, Rhubarb, Soybean, Aster, Begonia, Daffodil, Zucchini, most bulbs
- pH 6.0 - 6.5 Broccoli, Cauliflower, Cucumber, Egg Plant, Hemp, Pea, Pumpkin, Tomato, Turnip, Clover, Gladiolus, Poppy, Rose, Viola, Wallflower, Zinnea, Strawberry
- pH 6.5 - 7.0 Asparagus, Beetroot , Cabbage, Celery, Lettuce, Melons, Onion, Parsnip, Spinach, Alfalfa, Chrysanthemum, Dahlia, Sweet Pea and Tulip.
- pH 7.1 - 8.0 Lilac, brassica
See also
References
External links
- Soil pH Wikipedia
- Understanding and Correcting Soil Acidity by Jeff Ball, The Samuel Roberts Noble Foundation