Horizontal levees are a nature-based
approach for removing nitrogen
from municipal wastewater effluent while simultaneously providing
additional benefits, such as flood control. To assess nitrogen removal
mechanisms and the efficacy of a horizontal levee, we monitored an
experimental system receiving nitrified municipal wastewater effluent
for 2 years. Based on mass balances and microbial gene abundance data,
we determined that much of the applied nitrogen was most likely removed
by heterotrophic denitrifiers that consumed labile organic carbon
from decaying plants and added wood chips. Fe(III) and sulfate reduction
driven by decay of labile organic carbon also produced Fe(II) sulfide
minerals. During winter months, when heterotrophic activity was lower,
strong correlations between sulfate release and nitrogen removal suggested
that autotrophic denitrifiers oxidized Fe(II) sulfides using nitrate
as an electron acceptor. These trends were seasonal, with Fe(II) sulfide
minerals formed during summer fueling denitrification during the subsequent
winter. Overall, around 30% of gaseous nitrogen losses in the winter
were attributable to autotrophic denitrifiers. To predict long-term
nitrogen removal, we developed an electron-transfer model that accounted
for the production and consumption of electron donors. The model indicated
that the labile organic carbon released from wood chips may be capable
of supporting nitrogen removal from wastewater effluent for several
decades with sulfide minerals, decaying vegetation, and root exudates
likely sustaining nitrogen removal over a longer timescale.