In aqueous solution, an acid dissociates according to the following reaction:
#HA(aq) + H_2O(l) rightleftharpoonsH_3O^+ + A^-#
We can usually measure the extent of this equilibrium by some some means, and thus:
#K_a=([H_3O^+][A^-])/([HA])#
Here, #K_a# is a numerical constant that might be large or small. Strong mineral acids such as #HX, X=Cl, Br, I; H_2SO_4; HClO_4#, have very large acid dissociation constants, and the equilibrium lies strongly to the right. For weaker acids the equilibrium lies to the LEFT. In your text you will probably find a list of weak acids, whose #pK_a# values (#pK_a=-log_10K_a#) have been reported.