Spatial and temporal variations in surface water nitrate concentrations in a mixed land use catchment under humid temperate climatic conditions

Y. Van Herpe, Peter A Troch

Research output: Contribution to journalArticle

38 Citations (Scopus)

Abstract

Streamwater nitrate (NO3-) concentrations along the main stream and at the outlet of several subcatchments within the 114.3 km2 Zwalm watershed in Flanders, Belgium, have been monitored regularly since 1991. Land use within the Zwalm catchment is predominantly agricultural, with forested regions in the south and urban concentrations in the north-east of the catchment. Streamwater NO3- concentrations increased with increases in stream discharge rates, but in general, discharge rate explained only about 30% of the variation in NO3- concentrations. The low R2 values were attributed to the observed anticlockwise hysteresis in the NO3- concentration-discharge relationship and to differences in NO3- concentrations between both seasonal flow and various flow regimes, with winter flow explaining 51% of the variation in NO3- concentrations, whereas summer flow explained only 28% of the variation. A hypothesis was formulated in which flow regime accounts for the seasonal variation in NO3- export, postulating that the catchment seasonally alternates between two hydrological stages. The first stage occurs during wet winter periods, when the catchment drains as a single source area, whereas the second stage occurs during dry summer periods, when the groundwater store disconnects into separate subcatchments. This causes NO3- concentration peaks to be more delayed during summer storm events compared with winter storm events. Regarding flow regimes, differences between high and low flow conditions and between increasing and stable/decreasing flow eere not as pronounced a differences between seasons. In contrast to the estimation of NO3- concentrations, discharge was a strong predictor (R2 = 0.71) of the NO3- flux within the tributaries of the Zwalm catchment. The NO3- concentrations in the main stream increased with decreasing elevation, whereas the seasonal concentration patterns along the main channel were similar to those observed at the outlet. NO3- concentrations varied considerably among catchments and showed a high variability over time, although in general, the variation in NO3- concentration was higher between catchments than within catchments. The impact of land use is clearly reflected in the streamwater NO3- concentrations, although NO3- concentration patterns were also affected by topography and, to a lesser extent, by soil type. A gradual increase in NO3- concentrations at the outlet of the Zwalm catchment could be observed throughout the 1991 - 1998 study period, providing evidence for the general trends of increase in Flanders, which are attributed to the intensification of agricultural activities. Copyright (C) 2000 John Wiley and Sons, Ltd.

Original languageEnglish (US)
Pages (from-to)2439-2455
Number of pages17
JournalHydrological Processes
Volume14
Issue number14
DOIs
StatePublished - Oct 2000
Externally publishedYes

Fingerprint

temporal variation
spatial variation
catchment
nitrate
surface water
land use
streamwater
winter
summer
hysteresis
low flow
drain
soil type
tributary
seasonal variation
topography
watershed
groundwater

Keywords

  • Land-use impact assessment
  • Nitrate
  • Seasonality
  • Streamflow
  • Trend analysis

ASJC Scopus subject areas

  • Water Science and Technology

Cite this

@article{edaadde41b034fbd8d4f3905f32cf763,
title = "Spatial and temporal variations in surface water nitrate concentrations in a mixed land use catchment under humid temperate climatic conditions",
abstract = "Streamwater nitrate (NO3-) concentrations along the main stream and at the outlet of several subcatchments within the 114.3 km2 Zwalm watershed in Flanders, Belgium, have been monitored regularly since 1991. Land use within the Zwalm catchment is predominantly agricultural, with forested regions in the south and urban concentrations in the north-east of the catchment. Streamwater NO3- concentrations increased with increases in stream discharge rates, but in general, discharge rate explained only about 30{\%} of the variation in NO3- concentrations. The low R2 values were attributed to the observed anticlockwise hysteresis in the NO3- concentration-discharge relationship and to differences in NO3- concentrations between both seasonal flow and various flow regimes, with winter flow explaining 51{\%} of the variation in NO3- concentrations, whereas summer flow explained only 28{\%} of the variation. A hypothesis was formulated in which flow regime accounts for the seasonal variation in NO3- export, postulating that the catchment seasonally alternates between two hydrological stages. The first stage occurs during wet winter periods, when the catchment drains as a single source area, whereas the second stage occurs during dry summer periods, when the groundwater store disconnects into separate subcatchments. This causes NO3- concentration peaks to be more delayed during summer storm events compared with winter storm events. Regarding flow regimes, differences between high and low flow conditions and between increasing and stable/decreasing flow eere not as pronounced a differences between seasons. In contrast to the estimation of NO3- concentrations, discharge was a strong predictor (R2 = 0.71) of the NO3- flux within the tributaries of the Zwalm catchment. The NO3- concentrations in the main stream increased with decreasing elevation, whereas the seasonal concentration patterns along the main channel were similar to those observed at the outlet. NO3- concentrations varied considerably among catchments and showed a high variability over time, although in general, the variation in NO3- concentration was higher between catchments than within catchments. The impact of land use is clearly reflected in the streamwater NO3- concentrations, although NO3- concentration patterns were also affected by topography and, to a lesser extent, by soil type. A gradual increase in NO3- concentrations at the outlet of the Zwalm catchment could be observed throughout the 1991 - 1998 study period, providing evidence for the general trends of increase in Flanders, which are attributed to the intensification of agricultural activities. Copyright (C) 2000 John Wiley and Sons, Ltd.",
keywords = "Land-use impact assessment, Nitrate, Seasonality, Streamflow, Trend analysis",
author = "{Van Herpe}, Y. and Troch, {Peter A}",
year = "2000",
month = "10",
doi = "10.1002/1099-1085(20001015)14:14<2439::AID-HYP105>3.0.CO;2-H",
language = "English (US)",
volume = "14",
pages = "2439--2455",
journal = "Hydrological Processes",
issn = "0885-6087",
publisher = "John Wiley and Sons Ltd",
number = "14",

}

TY - JOUR

T1 - Spatial and temporal variations in surface water nitrate concentrations in a mixed land use catchment under humid temperate climatic conditions

AU - Van Herpe, Y.

AU - Troch, Peter A

PY - 2000/10

Y1 - 2000/10

N2 - Streamwater nitrate (NO3-) concentrations along the main stream and at the outlet of several subcatchments within the 114.3 km2 Zwalm watershed in Flanders, Belgium, have been monitored regularly since 1991. Land use within the Zwalm catchment is predominantly agricultural, with forested regions in the south and urban concentrations in the north-east of the catchment. Streamwater NO3- concentrations increased with increases in stream discharge rates, but in general, discharge rate explained only about 30% of the variation in NO3- concentrations. The low R2 values were attributed to the observed anticlockwise hysteresis in the NO3- concentration-discharge relationship and to differences in NO3- concentrations between both seasonal flow and various flow regimes, with winter flow explaining 51% of the variation in NO3- concentrations, whereas summer flow explained only 28% of the variation. A hypothesis was formulated in which flow regime accounts for the seasonal variation in NO3- export, postulating that the catchment seasonally alternates between two hydrological stages. The first stage occurs during wet winter periods, when the catchment drains as a single source area, whereas the second stage occurs during dry summer periods, when the groundwater store disconnects into separate subcatchments. This causes NO3- concentration peaks to be more delayed during summer storm events compared with winter storm events. Regarding flow regimes, differences between high and low flow conditions and between increasing and stable/decreasing flow eere not as pronounced a differences between seasons. In contrast to the estimation of NO3- concentrations, discharge was a strong predictor (R2 = 0.71) of the NO3- flux within the tributaries of the Zwalm catchment. The NO3- concentrations in the main stream increased with decreasing elevation, whereas the seasonal concentration patterns along the main channel were similar to those observed at the outlet. NO3- concentrations varied considerably among catchments and showed a high variability over time, although in general, the variation in NO3- concentration was higher between catchments than within catchments. The impact of land use is clearly reflected in the streamwater NO3- concentrations, although NO3- concentration patterns were also affected by topography and, to a lesser extent, by soil type. A gradual increase in NO3- concentrations at the outlet of the Zwalm catchment could be observed throughout the 1991 - 1998 study period, providing evidence for the general trends of increase in Flanders, which are attributed to the intensification of agricultural activities. Copyright (C) 2000 John Wiley and Sons, Ltd.

AB - Streamwater nitrate (NO3-) concentrations along the main stream and at the outlet of several subcatchments within the 114.3 km2 Zwalm watershed in Flanders, Belgium, have been monitored regularly since 1991. Land use within the Zwalm catchment is predominantly agricultural, with forested regions in the south and urban concentrations in the north-east of the catchment. Streamwater NO3- concentrations increased with increases in stream discharge rates, but in general, discharge rate explained only about 30% of the variation in NO3- concentrations. The low R2 values were attributed to the observed anticlockwise hysteresis in the NO3- concentration-discharge relationship and to differences in NO3- concentrations between both seasonal flow and various flow regimes, with winter flow explaining 51% of the variation in NO3- concentrations, whereas summer flow explained only 28% of the variation. A hypothesis was formulated in which flow regime accounts for the seasonal variation in NO3- export, postulating that the catchment seasonally alternates between two hydrological stages. The first stage occurs during wet winter periods, when the catchment drains as a single source area, whereas the second stage occurs during dry summer periods, when the groundwater store disconnects into separate subcatchments. This causes NO3- concentration peaks to be more delayed during summer storm events compared with winter storm events. Regarding flow regimes, differences between high and low flow conditions and between increasing and stable/decreasing flow eere not as pronounced a differences between seasons. In contrast to the estimation of NO3- concentrations, discharge was a strong predictor (R2 = 0.71) of the NO3- flux within the tributaries of the Zwalm catchment. The NO3- concentrations in the main stream increased with decreasing elevation, whereas the seasonal concentration patterns along the main channel were similar to those observed at the outlet. NO3- concentrations varied considerably among catchments and showed a high variability over time, although in general, the variation in NO3- concentration was higher between catchments than within catchments. The impact of land use is clearly reflected in the streamwater NO3- concentrations, although NO3- concentration patterns were also affected by topography and, to a lesser extent, by soil type. A gradual increase in NO3- concentrations at the outlet of the Zwalm catchment could be observed throughout the 1991 - 1998 study period, providing evidence for the general trends of increase in Flanders, which are attributed to the intensification of agricultural activities. Copyright (C) 2000 John Wiley and Sons, Ltd.

KW - Land-use impact assessment

KW - Nitrate

KW - Seasonality

KW - Streamflow

KW - Trend analysis

UR - http://www.scopus.com/inward/record.url?scp=0034298237&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0034298237&partnerID=8YFLogxK

U2 - 10.1002/1099-1085(20001015)14:14<2439::AID-HYP105>3.0.CO;2-H

DO - 10.1002/1099-1085(20001015)14:14<2439::AID-HYP105>3.0.CO;2-H

M3 - Article

VL - 14

SP - 2439

EP - 2455

JO - Hydrological Processes

JF - Hydrological Processes

SN - 0885-6087

IS - 14

ER -