Acid mine drainage (AMD) is a common problem in southwestern Missouri
and is partly responsible for many contaminated water supplies. Missis
sippian-aged limestone layers act to buffer the hazardous AMD thus red
ucing the risk. Five such units were analyzed over a range of four agg
regate sizes (Very Fine Gravel, Fine Gravel, Coarse Gravel, and Very C
oarse Gravel). As the mean aggregate size decreases, the buffering pot
ential increases. The natural stratigraphy aids in neutralizing the AM
D, but natural ground-water flow rates may limit this effect. Neutrali
zation is also hampered by a finite reduction in buffering potential d
ue to repeat exposure. Also, limestone aggregate may be utilized as a
control measure for AMD produced in surficial settings such as spoil p
iles and tailings ponds.