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Investigating the spatio‐temporal variations of nitrate leaching on a tea garden hillslope by combining HYDRUS‐3D and DNDC models
Journal of Plant Nutrition and Soil Science ( IF 2.6 ) Pub Date : 2019-10-29 , DOI: 10.1002/jpln.201900087
Xiaoming Lai 1, 2 , Ya Liu 1, 2 , Zhiwen Zhou 1, 2 , Qing Zhu 1, 2 , Kaihua Liao 1, 2
Affiliation  

Spatio‐temporal variations of nitrate‐nitrogen ( NO 3 - ‐N) leaching is driven by both soil hydrology and biogeochemistry. However, the widely used soil hydrology and biogeochemistry models have their weaknesses in simulating soil N cycling and soil water movement processes, respectively. In this study, we proposed an alternative approach by simply combining the HYDRUS‐3D and DNDC models to investigate the spatio‐temporal variations of NO 3 - ‐N leaching on a representative tea garden hillslope in Taihu Lake Basin, China. Results showed that the soil hydrology and N cycle were well simulated by HYDRUS‐3D and DNDC models, respectively. Based on the leaching equation, the soil water flux simulated by HYDRUS‐3D and soil NO 3 - ‐N content simulated by DNDC were combined to calculate the leachate NO 3 - ‐N concentrations with good accuracy. The accumulative NO 3 - ‐N leaching flux during the simulation year was 71.7 kg N ha−1, with remarkable spatio‐temporal variations on this hillslope. Hot spots of NO 3 - ‐N leaching were observed in blocks 24, 27, 31, 34, 37, and 40 with accumulative leaching fluxes > 82.0 kg N ha−1 y−1. The spatial variation of NO 3 - ‐N leaching was mainly controlled by soil texture and soil hydraulic properties. Hot moments of NO 3 - ‐N leaching were observed after the applications of spring fertilizer (16 March) and basal fertilizer (30 October). The temporal variation of NO 3 - ‐N leaching was mainly controlled by precipitation and the spring fertilization. Methods and findings of this study will be benefit for the risk assessment of non‐point source N loss and the precise agricultural management.
更新日期:2019-10-29
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