Experimental investigation of short-term warming on arsenic flux from contaminated sediments of two well-oxygenated subarctic lakes
Fig 5
Experimental sediment metal(loid) fluxes in relation to temperature.
Metal(loid) fluxes from sediment to overlying water of Lower Martin Lake and Yellowknife Bay cores incubated at different temperatures. There are two points for each temperature which are measured fluxes of duplicate cores for each temperature treatment. Coefficients of determination are provided for statistically significant regressions.