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Resource Manual on Integrated Production and Pest ... - julitoaligaen

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<str<strong>on</strong>g>Resource</str<strong>on</strong>g> <str<strong>on</strong>g>Manual</str<strong>on</strong>g> <strong>on</strong> IPPM in Rice<br />

World Educati<strong>on</strong> Philippines, Inc.<br />

Minimize disturbance of the soil, which would reduce biological diversity <strong>and</strong><br />

accelerate the destructi<strong>on</strong> of soil structure <strong>and</strong> organic matter.<br />

H. What is Soil pH?<br />

The pH of a soil refers literally to the Potential Hydrogen <strong>and</strong> is a measure of the soil<br />

acidity. Technically, pH refers to the amount of hydrogen i<strong>on</strong> (H+) present in the soil<br />

water (or any kind of liquid), measured <strong>on</strong> a logarithmic mathematical scale. In rice<br />

producti<strong>on</strong>, knowledge of soil pH, particularly how to measure <strong>and</strong> manage it, is very<br />

important especially since pH affects soil chemistry <strong>and</strong> plant nutriti<strong>on</strong>.<br />

The pH is a scale of measuring acidity that ranges from 0 to 14. A low pH (0-5) is<br />

acidic, <strong>and</strong> a high pH (9-14) is basic (lacking H+). A pH level that ranges from 6 to 8 is<br />

c<strong>on</strong>sidered neutral pH.<br />

In many areas of the tropics soils are generally acidic. Some soils have a pH level of as<br />

low as 4.0 <strong>and</strong> some even have as low as 3.0 pH. Soil acidity does not directly hurt the<br />

plants, but rather, it affects the availability of nutrients for the plant. The same is also<br />

true for soils that are too basic (lacking in H+).<br />

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