Item talk:Q238781
From geokb
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"name": "Water-quality response to a high-elevation wildfire in the Colorado Front Range",
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"abstract": "Water quality of the Big Thompson River in the Front Range of Colorado was studied for 2\u2009years following a high\u2010elevation wildfire that started in October 2012 and burned 15% of the watershed. A combination of fixed\u2010interval sampling and continuous water\u2010quality monitors was used to examine the timing and magnitude of water\u2010quality changes caused by the wildfire. Prefire water quality was well characterized because the site has been monitored at least monthly since the early 2000s. Major ions and nitrate showed the largest changes in concentrations; major ion increases were greatest in the first postfire snowmelt period, but nitrate increases were greatest in the second snowmelt period. The delay in nitrate release until the second snowmelt season likely reflected a combination of factors including fire timing, hydrologic regime, and rates of nitrogen transformations. Despite the small size of the fire, annual yields of dissolved constituents from the watershed increased 20\u201352% in the first 2\u2009years following the fire. Turbidity data from the continuous sensor indicated high\u2010intensity summer rain storms had a much greater effect on sediment transport compared to snowmelt. High\u2010frequency sensor data also revealed that weekly sampling missed the concentration peak during snowmelt and short\u2010duration spikes during rain events, underscoring the challenge of characterizing postfire water\u2010quality response with fixed\u2010interval sampling.",
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