Preprints
https://doi.org/10.5194/egusphere-2026-4671
https://doi.org/10.5194/egusphere-2026-4671
07 Aug 2026
 | 07 Aug 2026
Status: this preprint is open for discussion and under review for Hydrology and Earth System Sciences (HESS).

Unveiling the role of groundwater in hydrology and nitrate-N transport over agricultural watersheds in the U.S. Corn Belt: insights from model structure intercomparison

Yaji Wang, Bin Peng, Mengqi Jia, Zewei Ma, Qianyu Zhao, Ryan Bailey, Daniel Abrams, Jie Yang, Kaiyu Guan, Ming Pan, and Yuanxin Song

Abstract. Groundwater is an important component in water cycling across agricultural landscapes, but its role in regulating hydrology and nitrogen transport within agricultural watersheds remains highly uncertain, due to limited observations and the reliance on modeling approaches with different model structural representations. Here, we investigated groundwater’s role at the watershed scale in the Upper Sangamon River Basin over 20012020 by evaluating its annual and seasonal contributions to both hydrology and nitrogen transport using three validated models with different representations of groundwater-related processes, including (1) default SWAT+, (2) SWAT+gwflow, and (3) SWAT+MODFLOW+RT3D. These models represent increasing levels of groundwater-process complexity within the same model family, enabling us to isolate the effects of groundwater representation on hydrology and nitrogen transport while minimizing differences arising from other model components. We find that groundwater’s annual average net contribution to streamflow ranges from 24.0 % to 31.0 % across models, but its partitioning among contributing pathways varies across models, being dominated by groundwater discharge in the default SWAT+, and by tile flow in SWAT+gwflow and SWAT+MODFLOW+RT3D. The multi-year mean net groundwater contribution to nitrate-N export ranges from 16.0 % to 35.0 %. Seasonal analysis shows that groundwater is a year-round source of nitrate–N to the river system, and its contribution peaks after fertilization at more than 10 times that of the non-growing season. Model comparison shows that physically based groundwater models (SWAT+gwflow and SWAT+MODFLOW+RT3D) better capture surface-subsurface exchange processes, while the empirical groundwater model of default SWAT+ provides efficient flux estimates. Our results highlight the importance of groundwater representation in shaping watershed hydrologic and nitrogen dynamics and underscore the need to balance process realism with computational efficiency when selecting models for agricultural watershed management.

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Yaji Wang, Bin Peng, Mengqi Jia, Zewei Ma, Qianyu Zhao, Ryan Bailey, Daniel Abrams, Jie Yang, Kaiyu Guan, Ming Pan, and Yuanxin Song

Status: open (until 18 Sep 2026)

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Yaji Wang, Bin Peng, Mengqi Jia, Zewei Ma, Qianyu Zhao, Ryan Bailey, Daniel Abrams, Jie Yang, Kaiyu Guan, Ming Pan, and Yuanxin Song
Yaji Wang, Bin Peng, Mengqi Jia, Zewei Ma, Qianyu Zhao, Ryan Bailey, Daniel Abrams, Jie Yang, Kaiyu Guan, Ming Pan, and Yuanxin Song
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Latest update: 07 Aug 2026
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Short summary
Groundwater is critical for supplying rivers and transporting nitrogen, but watershed models describe these processes in different ways. We compared three watershed models with different groundwater detail levels. More detailed simulations better captured underground water movement and nitrogen transport, while simpler approaches provided reliable estimates of groundwater contributions to rivers. The results help researchers and water managers choose models that best fit different applications.
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