A series of studies on the performance of Hg0 removal from simulated flue gas were carried out in a wet Hg0 bubbling reactor using a visible-light-responsive Ag/AgCl photocatalyst prepared by a precipitation-photoreduction method. The effects of SO2, NO, and reaction temperature were also investigated in detail. The properties of fresh and used photocatalysts were characterized by N2 adsorption/desorption, scanning electron microscope and energy dispersive X-ray spectroscopy (SEM-EDS), X-ray diffraction (XRD), UV-visible diffuse reflectance spectroscopy (DRS), X-ray photoelectron spectroscopy (XPS) and electron spin resonance (ESR) techniques. The results showed that compared with the Hg0 removal efficiencies of only visible light irradiation and only Ag/AgCl, Hg0 removal efficiency was greatly enhanced when visible light and Ag/AgCl were employed simultaneously. Due to large amounts of reactive species consumption, the presences of SO2 and NO would inhibit the performance of Hg0 removal. The activity of Hg0 removal could be restored to their initial values when SO2 and NO were turned off. The reactive species, such as hydroxyl radicals (·OH), superoxide radicals (·O2-), were produced in the Ag/AgCl solution under visible light. The ·OH, holes (h+), and Cl2, were reactive species responsible for removing Hg0, and in particular the ·O2- played a key role in Hg0 removal.
Understanding the spatial distribution of phosphorus (P) loss is of value to identify the critical source areas (CSAs) for diffuse pollution control, but little is known about difference between the emission amount thatemitted to the reach and export amount that exported out from reach. Taking Fengyu River watershed, a typical sub-basin of Erhai Lake basin in Yunnan plateau lake area, as the case study area, this work studied on the spatial distribution of the emission and export of P loss using SWAT, furthermore, evaluated the role of P delivery through the reaches in the spatial distribution of P loss. High emission intensity of total Ploss was mostly located in the hydrological sensitive areas or soil erosion sensitive areas with slope arable lands. The highest emission intensity of total Ploss was 1.52~1.82kg/hm2. Moreover, the delivery process of emitted P toreaches decreased the distribution area of the highest export intensity of total P. The highest export intensity of total Ploss reduced to bethe soil erosion sensitive area. The retention coefficients of reaches in different sub-watersheds ranged from -25.6% to 21.6% because of the variation of transporting processes between sub-watersheds, which changed the spatial features of P loss.