Abstract

Achievements of good chemical and ecological status of groundwater (GW) and surface water (SW) bodies are currently challenged mainly due to poor identification and quantification of pollution sources. A high spatio-temporal hydrological and water quality monitoring of SW and GW bodies is the basis for a reliable assessment of water quality in a catchment. However, high spatio-temporal hydrological and water quality monitoring is expensive, laborious, and hard to accomplish. This study uses spatio-temporally low resolved monitored water quality and river discharge data in combination with integrated hydrological modelling to estimate the governing pollution pathways and identify potential transformation processes. A key task at the regarded lowland river Augraben is (i) to understand the SW and GW interactions by estimating representative GW zones (GWZ) based on simulated GW flow directions and GW quality monitoring stations, (ii) to quantify GW flows to the Augraben River and its tributaries, and (iii) to simulate SW discharges at ungauged locations. Based on simulated GW flows and SW discharges, NO3-N, NO2-N, NH4-N, and P loads are calculated from each defined SW tributary outlet (SWTO) and respective GWZ by using low-frequency monitored SW and GW quality data. The magnitudes of NO3-N transformations and plant uptake rates are accessed by estimating a NO3-N balance at the catchment outlet. Based on sensitivity analysis results, Manning’s roughness, saturated hydraulic conductivity, and boundary conditions are mainly used for calibration. The water balance results show that 60–65% of total precipitation is lost via evapotranspiration (ET). A total of 85–95% of SW discharge in Augraben River and its tributaries is fed by GW via base flow. SW NO3-N loads are mainly dependent on GW flows and GW quality. Estimated SW NO3-N loads at SWTO_Ivenack and SWTO_Lindenberg show that these tributaries are heavily polluted and contribute mainly to the total SW NO3-N loads at Augraben River catchment outlet (SWO_Gehmkow). SWTO_Hasseldorf contributes least to the total SW NO3-N loads. SW quality of Augraben River catchment lies, on average, in the category of heavily polluted river with a maximum NO3-N load of 650 kg/d in 2017. Estimated GW loads in GWZ_Ivenack have contributed approximately 96% of the total GW loads and require maximum water quality improvement efforts to reduce high NO3-N levels. By focusing on the impacts of NO3-N reduction measures and best agricultural practices, further studies can enhance the better agricultural and water quality management in the study area.

Highlights

  • Lowland catchments are characterized by a high groundwater (GW) table, low flow velocity, flat topography, and a significant presence of organic soils [1,2,3,4]

  • The most sensitive parameters for the Augraben River catchment were assessed by sensitivity analysis

  • The coupled MIKE SHE and MIKE 11 model was used for generating discharges at ungauged locations

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Summary

Introduction

Lowland catchments are characterized by a high groundwater (GW) table, low flow velocity, flat topography, and a significant presence of organic soils [1,2,3,4]. Diffuse pollution from agriculture has increased considerably over the past few decades due to human activities related to the surplus use of both organic and synthetic fertilizers [7,8]. The EU nitrate directive was introduced in 1991 to identify and reduce the NO3-N pollution in water bodies (Directive 91/676/EEC), and it focuses on integrated management of water in river catchments to acquire, improve, or maintain a good chemical and ecological status. Due to deficiencies in implementing the ordinance of agriculture fertilizer application and surplus use of both synthetic and organic fertilizers, a rise in NO3-N concentrations in comparison to the reported NO3-N concentrations from 2004 to 2007 is observed [16,17]. In 2016, the European court of justice brought legal action against Germany due to deficiencies in implementing the ordinance of agriculture fertilizer applications [7,18]

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