Air-surface exchange of mercury (Hg) was measured from soil low in Hg (0.013 mg/kg) amended with four different ash materials: a wood ash containing ϳ10% coal ash (0.070 mg/kg Hg), a mixture of two subbituminous coal fly ashes (0.075 mg/kg Hg), a subbituminous coal ash containing ϳ10% petroleum coke ash (1.2 mg/kg Hg), and an ash from incinerated municipal sewage sludge (4.3 mg/kg Hg) using a dynamic flux chamber. Ash was added to soil to simulate agricultural supplements, soil stabilization, and pad layers used in livestock areas. For the agricultural amendment, ϳ0.4% ash was well mixed into the soil. To make the stabilized soil that could be used for construction purposes, ϳ20% ash was mixed into soil with water. The pad layer consisted of a wetted 1-cm layer of ash material on the soil surface. Diel trends of Hg flux were observed for all of the substrates with significantly higher Hg emissions during the day and negligible flux or deposition of Hg during the night. Hg fluxes, which were measured in the summer months, were best correlated with solar radiation, temperature, and air O 3 concentrations. Mean Hg fluxes measured outdoors for unamended soils ranged from 19 to 140 ng/m 2 day, whereas those for soil amended with ash to simulate an agricultural application ranged from 7.2 to 230 ng/m 2 day. Fluxes for soil stabilized with ash ranged from 77 to 530 ng/m 2 day and for soil with pads constructed of ash ranged from Ϫ50 to 90 ng/m 2 day. Simple analytical tests (i.e., total Hg content, synthetic precipitation leaching procedure, heating, and indoor gas-exchange experiments) were performed to assess whether algorithms based on these tests could be used to predict Hg fluxes observed outdoors using the flux chamber. Based on this study, no consistent relationships could be developed. More work is needed to assess longterm and seasonal variations in Hg flux from (intact and disturbed) substrates before annual estimates of emissions can be developed.