Hydrological Connectivity Dominates NO3‐N Cycling in Complex Landscapes – Insights From Integration of Isotopes and Water Quality Modeling

Distributed water quality modeling often involves considerable uncertainty due to complexity and spatial heterogeneity of hydrological and biogeochemical processes. To address this, stable water isotopes were coupled into a water quality modeling framework (EcH2O‐iso‐nitrate) for 30‐year hydrological and NO3‐N simulations in a mixed‐land‐use catchment (Demnitz Mill Creek, DMC, Germany). The isotope‐aided model effectively simulated the (dis)connection of different flow paths and related biogeochemical transformations. Results highlight the role of transient hydrological states in NO3‐N cycling in addition to static landscape characteristics. First, hydrological connectivity controls N transformations by regulating soil moisture and available NO3‐N for processing from upstream inflows, which was demonstrated by the spatially‐explicit estimates of water ages and Damköhler number. Second, hydrological pathways determine where, when, and which NO3‐N storages were connected, thereby dictating NO3‐N concentrations in different flow paths. In DMC, subsurface flows were the primary pathway, but transition to near‐surface flow occurred in specific riparian “hot‐spots” due to the development of soil saturation along flow paths. Such transition was transient but exerted disproportional impacts on NO3‐N dynamics by creating a preferential “fast‐track” toward channel network. This explains why DMC, as a groundwater‐dominated catchment, has flashy NO3‐N peaks in stream flow. To further unveil the role of hydrological connectivity in management planning, scenario analysis was conducted to identify optimal locations for wetland construction, showing riparian hotspots with better connectivity had the greatest potential for NO3‐N removal. These findings underscore the necessity of considering hydrological heterogeneity in modeling and management planning, which can be revealed by tracer‐aided modeling.

Publication Details

Journal
edoc Publication server (Humboldt University of Berlin)
Published
2025-07-12
DOI
https://doi.org/10.18452/34292
Primary Topic
Hydrology and Watershed Management Studies
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Hydrological Connectivity Dominates NO3‐N Cycling in Complex Landscapes – Insights From Integration of Isotopes and Water Quality Modeling

edoc Publication server (Humboldt University of Berlin)
Hydrology and Watershed Management Studies
article

Hydrological Connectivity Dominates NO3‐N Cycling in Complex Landscapes – Insights From Integration of Isotopes and Water Quality Modeling

article en

Abstract

Distributed water quality modeling often involves considerable uncertainty due to complexity and spatial heterogeneity of hydrological and biogeochemical processes. To address this, stable water isotopes were coupled into a water quality modeling framework (EcH2O‐iso‐nitrate) for 30‐year hydrological and NO3‐N simulations in a mixed‐land‐use catchment (Demnitz Mill Creek, DMC, Germany). The isotope‐aided model effectively simulated the (dis)connection of different flow paths and related biogeochemical transformations. Results highlight the role of transient hydrological states in NO3‐N cycling in addition to static landscape characteristics. First, hydrological connectivity controls N transformations by regulating soil moisture and available NO3‐N for processing from upstream inflows, which was demonstrated by the spatially‐explicit estimates of water ages and Damköhler number. Second, hydrological pathways determine where, when, and which NO3‐N storages were connected, thereby dictating NO3‐N concentrations in different flow paths. In DMC, subsurface flows were the primary pathway, but transition to near‐surface flow occurred in specific riparian “hot‐spots” due to the development of soil saturation along flow paths. Such transition was transient but exerted disproportional impacts on NO3‐N dynamics by creating a preferential “fast‐track” toward channel network. This explains why DMC, as a groundwater‐dominated catchment, has flashy NO3‐N peaks in stream flow. To further unveil the role of hydrological connectivity in management planning, scenario analysis was conducted to identify optimal locations for wetland construction, showing riparian hotspots with better connectivity had the greatest potential for NO3‐N removal. These findings underscore the necessity of considering hydrological heterogeneity in modeling and management planning, which can be revealed by tracer‐aided modeling.

edoc Publication server (Humboldt University of Berlin)
Openalex Percentile: Top 62%
Hydrology and Watershed Management Studies
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.