2012
DOI: 10.1016/j.envsci.2012.08.009
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Changes in nitrogen loads to estuaries following implementation of governmental action plans in Denmark: A paired catchment and estuary approach for analysing regional responses

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Cited by 64 publications
(57 citation statements)
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“…At the agricultural field level, the nitrogen surplus was halved from levels >400,000 t N year −1 in the early 1990s (Windolf et al 2012;Blicher-Mathiesen et al 2014). This reduction was achieved through APAE requirements for manure storage capacity, rules for timing and application technique of manure, maximum limits to the amount of N which may be applied to different crops, and wetland restoration increasing the N retention in surface waters.…”
Section: Trends In Nutrient Inputsmentioning
confidence: 99%
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“…At the agricultural field level, the nitrogen surplus was halved from levels >400,000 t N year −1 in the early 1990s (Windolf et al 2012;Blicher-Mathiesen et al 2014). This reduction was achieved through APAE requirements for manure storage capacity, rules for timing and application technique of manure, maximum limits to the amount of N which may be applied to different crops, and wetland restoration increasing the N retention in surface waters.…”
Section: Trends In Nutrient Inputsmentioning
confidence: 99%
“…Gross outlets of TN and TP from diffuse sources were calculated by combining monthly modeled freshwater discharge and discharge weighted monthly concentrations of TN and TP from empirical models derived on measured data from 83 (N) and 24 (P) gauging stations with no significant sewage outlets (Windolf et al 2011;Andersen et al 2005). Adding the outlets of nutrients with sewage in the ungauged catchments and subtracting estimated nutrient retention in streams and lakes then provided the total monthly nutrient load from ungauged catchments (Windolf et al 2011(Windolf et al , 2012.…”
Section: Nutrient Inputsmentioning
confidence: 99%
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“…as follows from a number of publications (e.g. schilling, Wolter, 2007;Meals et al, 2010;Windolf et al, 2012), time for responding groundwater body/zone to the effects of measures at restoring the groundwater quality varies from a few years to decades and consists of the time needed to create the necessary effect in practice, the time required for expression of the effect on the level of the ground water level and the time required for water body/zone in response to the effect of measures. amongst these, the last one is usually the longest.…”
Section: The Need To Take Effective Measuresmentioning
confidence: 99%
“…The starting point for solving this problem is to identify areas that significantly contribute to current water status. Environmental risk assessment, through which it is possible to identify these areas, is based on the concept of 'source of pollution → transport path → receptor (part of the environment and/or human health)' (Daly et al, 2002;Malík, Švasta, 2004;Windolf et al, 2012), which, given the particular type and origin of contamination, may be interpreted as nutrient load environment → transport nutrients in the environment → receptor. The specific vulnerability of groundwater in groundwater body (hydrogeological structure) represents a more 'environmentalist' thinking on groundwater protection, as it seeks to provide below-limit concentrations of specific substances across the aquifer.…”
mentioning
confidence: 99%