Numerous studies indicate biochar's nitrogen (N) adsorption capacity plays a crucial role in soil N retention. However, there is limited understanding on inorganic N adsorption mechanisms in biochar derived from aquatic weeds such as water hyacinth (WH). This study investigated ammonium-N (NH4+-N) and nitrate-N (NO3--N) adsorption capacities and mechanisms of WH biochar pyrolyzed at different pyrolysis temperatures of 400°C, 600°C, and 800°C (BC400, BC600, and BC800, respectively). Results showed NH4+-N adsorption was maximized (1.07-1.09mgg-1) with BC400 at initial solution pH 7.0-9.0, while NO3--N adsorption peaked (0.80mgg-1) with BC800 at initial solution pH 5.0. Both NH4+-N and NO3--N followed well the Pseudo-second-order model in adsorption kinetics (R2 = 0.990-0.997 and 0.962-0.992, respectively). The Sips model accurately described the adsorption isotherms for NH4+-N (R2 = 0.994-0.999) and NO3--N (R2 = 0.992-0.999). The calculated maximum adsorption capacity for NH4+-N and NO3--N using Sips model was 11.2-16.8mgg-1 and 0.693-4.99mgg-1, respectively. Co-existing cations and anions reduced NH4+-N and NO3--N adsorption capacity, respectively, with other ions with higher valence exhibiting higher inhibition effects (43%-97% and 44%-73%, respectively). Primary adsorption mechanism for NH4+-N included cation exchange via oxygen-containing surface functional groups in BC400 and pore filling and surface struvite precipitation in BC800. Major adsorption mechanisms for NO3--N included electrostatic interactions in BC400 and pore filling in BC800. These findings suggested that biochar derived from aquatic weeds possessed the same potential usefulness for soil N retention as biochar from other feedstocks, and that it might assist for further detailed considerations in other studies for biochar soil application.
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