JEQ Journal of Natural Resources and Life Sciences Education
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Fig. 2. Changes in alkalinity with detention time of mine drainage within limestone drains at Howe Bridge, Morrison, and Buck Mountain sites. Detention time (td) computed as product of porosity ({phi}), downflow distance (L), and cross-sectional area (A) divided by flow rate (Q): td = {phi}LA/Q, assuming {phi} = 0.49.





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