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Updated: Aug 6, 2026

Calibrated Passive Sampling - Multi-plot Field Measurements of NH3 Emissions with a Combination of Dynamic Tube Method and Passive Samplers
Published on: March 21, 2016
Modeling nitrogen deposition with an ultra-fine mesh: application in farmland with dense river network
Zaili Ling1, Jiayi Xin2, Tao Huang2
1College of Agricultural and Forestry Economics and Management, Lanzhou University of Finance and Economics, Lanzhou 730101, P. R. China.
None:
Ammonia (NH3) emissions from agriculture significantly impact aquatic ecosystems through the deposition of ammonia nitrogen (NHx-N). Models established on a gridded map provide a useful tool to investigate NH3 dispersion and deposition. However, coarse model grid cells in major atmospheric chemistry models often lead to large bias in modeled N burden due to NHx-N deposition in small household farms, which are typical in Southeastern China with dense farmland water networks. Here, we first simulated atmospheric concentrations of NH3 and NH4+ in 2020 in Changshu, a representative area with developed agriculture and dense river and farmland water networks attached to the Taihu Lake Basin in Southeast China, using the WRF-CMAQ model. To address the bias caused by coarse model grids, we employed a large leaf model to calculate dry deposition velocities for NH3 and NH4+ at a high resolution of 10 meters. This allowed for a more accurate estimation of the nitrogen load to surface waters from re-emitted farmland NH3. The results show that coarse particulate NH4+ (CNH4+) exhibited the largest dry deposition velocity, followed by gaseous NH3 and fine particulate NH4+ (FNH4+). The dry deposition velocities of NH3 and NH4+ were significantly influenced by land use type. Our results indicate that approximately 118.0 tons of nitrogen from ammonia reemission from farmlands entered surface water in 2020 in Changshu via atmospheric NHx-N deposition. The wet deposition of NH4+ was the largest contributor (49.8%), followed by dry deposition of gaseous NH3 (20.9%), CNH4+ (20.7%), and FNH4+ (8.6%), respectively.

