Narva va ri river nutrie trient t input: t: divi vision betw tween countrie ies Alt lternativ ive ways s to def efin ine contrib ibutio ions
Natalia Oblomkova Water Management of the Narva River: harmonization and sustention (NarvaWatMan Project)
Alt lternativ ive ways s to def efin ine contrib ibutio ions - - PowerPoint PPT Presentation
Narva va ri river nutrie trient t input: t: divi vision betw tween countrie ies Alt lternativ ive ways s to def efin ine contrib ibutio ions Water Management of the Narva River: harmonization and sustention ( NarvaWatMan Project)
Narva va ri river nutrie trient t input: t: divi vision betw tween countrie ies Alt lternativ ive ways s to def efin ine contrib ibutio ions
Natalia Oblomkova Water Management of the Narva River: harmonization and sustention (NarvaWatMan Project)
– November 2021)
Technology
Institute”, SC "Mineral“ – Saint-Petersburg, Russia
Government, Administration of municipal formation «City Ivangorod Kingisepp municipal district of Leningrad Region»
river nutrient input defined based on application of the MONERIS
Republic, and Germany has modeled their inputs to Oder taking
moment German share was assumed to be constant (5.5% for TN and 3.1% for TP according to PLC Guideline ). Poland reports the total input figures.
provided necessary information to Swedish experts, who modelled nutrient loads from the whole catchment area considering retention (communication with Lars Sonesten). Contributions have been assessed based on the 2006 data. Since that time total input has been divided based on that constant
55 % of the load. Total input estimated according to the monitoring data collected by countries. Average is computed of Finnish and Swedish data (Presentation by BNI). Values are almost similar.
Picrure: Ibragimow, Aleksandra & Albrecht, Eerika & Albrecht, Moritz. (2019). The transboundary water management - Comparing policy translations of the Water Framework Directive in the international basin districts of the Oder River and the Torne River. Quaestiones Geographicae. 38. 29-39. 10.2478/quageo- 2019-0006.
1 – capitols, 2 – state borders, 3 – the Baltic Sea, 4 – the International Oder River Basin District, 5 – the International Torne River Basin District.
0,00 200,00 400,00 600,00 800,00 1000,00 1200,00 2017 2010-2013 2017 2009 2006-2010 2011-2015 2005 2006-2010 2011-2015 EST_Narva_tot RUS_Narva_tot EST_Peipsi RUS_Peipsi
Ntot loss, kg/sq. km
0,00 5,00 10,00 15,00 20,00 25,00 2017 2010-2013 2017 2009 2006-20102011-2015 2005 2006-20102011-2015 EST_Narva_tot RUS_Narva_tot EST_Peipsi RUS_Peipsi
Ptot loss, kg/sq.km
Nutrient losses per square kilometer of the catchment according to the different modelling activities in Peipsi Lake and whole Nerva river catchment Area specific loss of N and P, calculated based on results from previous modelling, showed that loads from Estonian side are higher than Russian ones for corresponding period (especially for nitrogen) and that there is decreasing dynamics in inputs to the Peipsi Lake during recent
and consider only current share of load when calibrating the models. Thus, current approach to allocate loads according to the catchment area seems to be rather rough.
estimates diffuse losses as the remaining part of the monitored load after subtracting input from point source and considering retention in inland surface waters , while Russia use reservoir retention for the same purpose;
assume zero load compared to Estonian estimates which coincide 440 kg per square kilometer;
source included in runoff from urban areas;
similar equation only for riverine part prior big reservoirs, the remaining retention calculated by subtracting total load from sum of diffuse and point sources load.
agricultural area within the catchment or use per capita estimates According to per capita approach Russian contribution should be 59% (based on 2002 data) and Estonian is 41% (2011 data). Agricultural areas were in proportion: 53% in Russia and 47% in Estonia [Frumin, 2013].
anthropogenic loads based on fulfillment of the HELCOM Recommendations, BAT, BEP etc.
is
the most complicated issues to consider due to specific features of the Narva river lake system and unevenly distributed anthropogenic pressures.
Source Ntot retention, % Ptot retention, % Area
Nõges et al., 2003
50-70
Peipsi Lake Lozovik, 2018
53 52
Peipsi Lake RusNIP II report, 2015
56 37
Entire Narva river catchment
56
Peipsi Lake Frumin, 2013
53 46
Entire Narva river catchment Stålnacke et al., 2015
56
Entire Narva river catchment
49
Peipsi Lake
To increase reliability of the estimates the spatial distribution of the sources as minimum should be considered. It would be beneficial to reduce possible mistakes related with retention when defining shares in nutrient input as far as it has no influence for planning measures at local level.
Approach Input data demand Approbation Advantages Disadvantages MESAW model Rather high (but low compared to semi-physical models) Good for Baltic Sea catchment area
in accordance with monitoring data;
sources
ESTMODEL Good for Estonian part ILLM based approach Good for Russian part Per agricultural area approach Low
1. Doesn’t consider spatial distribution
aspects (water treatment quality etc.) Per capita approach Low
Potential reduction approach Moderate Low (only in several Russian studies)
and possibility to reduce it
to source and elaborate corresponding measures;
need to define natural background load
still rather uncertain;
KEY POINTS:
e.g. not enough monitoring data).
AGREED APPROACH: 1) To consider only pilot area – Narva river immediate catchment (There are several monitoring stations along the river); 2) To use balance method (point sources; diffuse sources (emission coefficients-based method); calculate riverine retention (for e.g Behrendt method) and to compare with load between two hydrochemical stations (outlet from Peipsi Lake and in the Narva river mouth); 3) Before step 2. - to test Estonian and Russian coefficients by calculation emissions using both values and follow-up comparing of the results of the balance calculation FOLLOW-UP: To collect data for pilot area starting from 2006 (tbc) to 2019 during summer 2020