Mitigation of low stream pH and its effects on salmonids

Crushed limestone (200 tonnes) was spread in bars on the bed of an acidic brook (mean pH 5.0) in Nova Scotia, Canada. A seasonally variable but significant increase in pH of running water resulted, and a longitudinal pH gradient over the limed section extended to the mouth of the brook. The effectiveness persisted after 3 years, during which pH downstream of the limestone increased an average of 0.4 pH units (range < 0.1-1.3 pH units) along with significantly increased Ca, Mg and acid neutralizing capacity. Total and exchangeable Al were not altered by the limestone and non-exchangeable forms dominated. The interstitial water was nearly neutral (mean pH 7.1) in limestone beds but it was acidic (mean pH 5.4) in gravel beds of the control section upstream. Spawning Atlantic salmon (Salmo salar) dug three times more redds in gravel of the limed section than in the control. Salmon fry survived and they were significantly more abundant in the limed section than in the control. The density of juvenile salmon increased over time, indicating a recovery of the population. The density of brook trout (Salvelinus fontinalis) also increased and trout fry were usually more abundant in the limed section than in the control. The observed benefits for salmonids suggest that small-scale application of limestone to stream beds and spawning sites can be used to mitigate the effects of low stream pH.