Soil pH is a measure of the acidity or alkalinity of the soil. In an
acqueous solution, pH is defined to be the negative logarithm (base 10)
of the concentration of free hydrogen ions. In soil, the pH results
from the interaction of soil minerals, ions in solution, and cation
exchange.
Sand, Silt, Clay Fractions | Rock Fragment Class | Rock Fragment Volume
Bulk Density | Porosity | Permeability
Available Water Capacity | pH | Plasticity
K-Factor | Hydrologic Soil Groups | Curve Numbers
Soil Landscapes | Soil Climates | Soil Datasets | Personnel | Site Map
Comments and Questions
8/27/2001