Changing the soil

Soil Modification for Growers

Acidifying Soil


pH Ranges for Selected Trees and Shrubs:


Forms of lime


Signs of Lime Deficiency


Signs of Over-Liming


Cation exchange and soil pH

Cation exchange capacity (CEC) is a key indicator of soil fertility and its ability to absorb and retain cations, including biocides and radioisotopes. CEC is measured in milliequivalents, representing the amount of matter that can replace or combine with 1 mg of hydrogen per 100 g of dry soil. Most exchangeable cations are absorbed on the negatively charged surfaces of clay particles, with varying CECs among different clay minerals. For example, Kaolinite has a low CEC of 3-15 me/100g, while montmorillonite has a high CEC of 70-100 me/100g. Humus also plays a significant role in cation support, with very high CEC values ranging from 150-400 me/100g.



Common pH preferences for various plants