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TransboundaryNisavaRiver catchment in the Morava River ... · Neogene aquifers are in the Leskovac...

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Transboundary Nisava River catchment in the Morava River Basin in Serbia Dragana Ninković, Dipl.-Ing. Dušan Dobričić, Dipl.-Ing. UNECE Workshop on Integrated Transboundary Water Resources Management in SEE, Sarajevo, 18-20 May, 2009
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Page 1: TransboundaryNisavaRiver catchment in the Morava River ... · Neogene aquifers are in the Leskovac and Jagodina-Paraćin basins. The extent of the karsticaquifers is limited. Eastern

Transboundary Nisava River catchmentin the Morava River Basin in Serbia

Dragana Ninković, Dipl.-Ing.

Dušan Dobričić, Dipl.-Ing.

UNECE Workshop on Integrated Transboundary Water ResourcesManagement in SEE,

Sarajevo, 18-20 May, 2009

Page 2: TransboundaryNisavaRiver catchment in the Morava River ... · Neogene aquifers are in the Leskovac and Jagodina-Paraćin basins. The extent of the karsticaquifers is limited. Eastern

Content

1. Institutional and legal framework

2. Location of the Morava RB and the Nisavatransboundary catchment

3. General characteristics of the Nisava catchment

4. Hydrology, hydrogeology, aquifers

5. WFD implementation - Surface waters

6. Main pressures

7. Status, measures

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Institutional andlegal framework

• Legal framework:

– Law on Water, Law on Ministries

• Water management responsible institution:

– Ministry of Agriculture, Forestry and Water Management, Directorate for Water

• Water management policy

• Multipurpose water usage

• Water regime

• Protection from water

• Water protection measures

• International cooperation

• Other activities according to the Law on Water

• Other Ministries responsible for certain aspects of water management:

– Ministry for Environment and Spatial Planning

– Ministry of Health

– Ministry for Governance and Local Governance

– Ministry for infrastructure

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Institutional andlegal frameworkWater management organization

Goverment of Republic of Serbia

MAFWM -DIRECTORATE FOR WATER

Public Water CompanyVODE VOJVODINE

Water CenterMORAVA

Water CenterSAVA - DUNAV

RepublicHydro-meteorological

Service

Public Water CompanySRBIJAVODE

Danube-Tisza-Dunavsystem

Water Companies

Page 5: TransboundaryNisavaRiver catchment in the Morava River ... · Neogene aquifers are in the Leskovac and Jagodina-Paraćin basins. The extent of the karsticaquifers is limited. Eastern

Institutional andlegal frameworkInternational cooperation

Bilateral agreementsBilateral agreements• Existing (Hungary, Romania, Bulgaria – all from mid. 50’s); should be adopted in accordance with EU legislation

• Planned (Croatia, Bosnia&Herzegovina, Macedonia, Montenegro)

Multilateral agreementsMultilateral agreements• Danube River:

• ICPDR (The Convention on Cooperation for the Protection andSustainable Use of the River Danube, Sofia, 1994)

•DANUBE COMMISSION (1948, Belgrade Convention)

• Sava River:• INTERNATIONAL SAVA RIVER BASIN COMMISSION (FrameworkAgreement on the Sava River Basin, Kranjska Gora 2002)

Page 6: TransboundaryNisavaRiver catchment in the Morava River ... · Neogene aquifers are in the Leskovac and Jagodina-Paraćin basins. The extent of the karsticaquifers is limited. Eastern

-- New Water Law, due to:New Water Law, due to:

-- Lack of harmony between the current Water Law and Lack of harmony between the current Water Law and other laws and regulationsother laws and regulations

-- Unresolved territorial and other forms of jurisdiction Unresolved territorial and other forms of jurisdiction -- Inability to implement transformation of ownership in Inability to implement transformation of ownership in

the manner set out in the current Lawthe manner set out in the current Law-- Harmonization with the EU WFDHarmonization with the EU WFD

-- FinancingFinancing-- CCapacity buildingapacity building-- InvestmentsInvestments-- MMaintanaaintananncece-- IInternational cooperationnternational cooperation

Institutional andlegal frameworkThe most important water issuesto be solved

Page 7: TransboundaryNisavaRiver catchment in the Morava River ... · Neogene aquifers are in the Leskovac and Jagodina-Paraćin basins. The extent of the karsticaquifers is limited. Eastern

Location of the Morava RB andthe Nisava transboundary catchment

The Morava sub basin36640 km2

The Nisava transboundarycatchment:

11 % of the Morava RB areapart in BG: 3% of Morava

Page 8: TransboundaryNisavaRiver catchment in the Morava River ... · Neogene aquifers are in the Leskovac and Jagodina-Paraćin basins. The extent of the karsticaquifers is limited. Eastern

Nisava: general characteristics

NIŠAVA

GABERSKA

JERMA

TEMSKA

VISOCICA

Crvena reka

Koritnicka

Kutinska

Rogoz

jezera

državna granica

!. naseljena mesta

# hidrološke stanice

d hidroelektrane

±

0 40 80 12020Km

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d

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Južna Morava

Nišava Zavojsko jezero

Niš

Pirot

Sukovo

Mrtvine

Brajcevci

Stanicenje

Bela Palanka

Dimitrovgrad

Visocka Ržana

Radikine Bare

Strazimirovci

Trnski Odorovci

Niš

Pirot

Bela Palanka

Niška Banja

Dimitrovgrad

Area:2990 km2 in RS (73%)1096 km2 in BG (27%)

Main tributaries (figure)

Monitoring: RHMSS

quantity: 13 stationsquality: 7 stations

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Nisava: general characteristicsCLC land use

Page 10: TransboundaryNisavaRiver catchment in the Morava River ... · Neogene aquifers are in the Leskovac and Jagodina-Paraćin basins. The extent of the karsticaquifers is limited. Eastern

Nisava: Hydrology

±!(!(

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Južna Morava

Nišava Zavojsko jezero

Niš

Pirot

Sukovo

Mrtvine

Brajcevci

Stanicenje

Bela Palanka

Dimitrovgrad

Visocka Ržana

Radikine Bare

Strazimirovci

Trnski Odorovci

Niš

Pirot

Bela Palanka

Niška Banja

Dimitrovgrad

• developed river network• 13 monitoring stations• encompasses 25% of the Juzna Morava basin by area and 32 % by discharge (very rich with water)

• 2 m3/s < Qav < 31 m3/s from Dimitrovgrad (border monitoring site) to Nis (mouth to Juzna Morava)

• low flow: cca 6 m3/s• mean high flow: cca 200 m3/s (Q100 = 988 m

3/s)

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Nisava: Hydrogelogy

Velika Morava Basin comprise parts of the several Hydrogeological Units:

•Central Serbia: The most important are alluvial aquifers (exposed to highly intensive anthropogenic impacts) of the Velika, Južna and Zapadna Morava. The Velika Morava alluvium is the main water-bearing medium, comprised of 6-60 m thick sandy-gravelly sediments. The major Neogene aquifers are in the Leskovac and Jagodina-Paraćin basins. The extent of the karstic aquifers is limited.

Eastern Serbia: Large alluvial aquifers are rare (the Nišava and Timok basins). Most important is the artificially-recharged Mediana water source in the City of Niš, with yield of some 600 l/s.Thelarge number of karstic springs, 16 of which have a minimum Q > 100 l/s. Neogene aquifers in isolated lacustrine basins are less significant.

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Nisava: WFD implementationTransboundary GW bodies,GW use

In 2007 as a part of UN ECE “First Assesment of rivers , lakes and groundwaters”, possible TB GWs identified between Serbia and Bulgaria (No. 34 “Stara planina/Salasha Montana”Transboundary Groundwaters).

In the Velika Morava Basin, 3 GW bodies are part of this : Vidlič, Stara planina and Nišava 2.

No transboundary impact observed.

AGRIntergranular343,8RS_NI_GW_P_2Nišava 2

DW,AGRKarst337,5RS_NI_GW_K_2Stara planina

DW, AGR,INDKarst285,09RS_NI_GW_K_1Vidlič

GW useAquifer typeArea

(km2)

Nat. codeGW Body

Page 13: TransboundaryNisavaRiver catchment in the Morava River ... · Neogene aquifers are in the Leskovac and Jagodina-Paraćin basins. The extent of the karsticaquifers is limited. Eastern

Nisava: WFD implementationSurface waters

Activities performed so far

(rivers with catcment area > 100 km2)

•identification of surface waters categories

•river typology

•delineation of river water bodies

•provisional identification of HMWB

•identification of pressures

•risk assessment for large rivers (Nisava)

Page 14: TransboundaryNisavaRiver catchment in the Morava River ... · Neogene aquifers are in the Leskovac and Jagodina-Paraćin basins. The extent of the karsticaquifers is limited. Eastern

Nisava: WFD implementationSurface waters bodies

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Nisava: main pressures

HYMO:

• large dams (Zavoj , Sukovo)

• number of small HP plants

• flood protection structures and river training works (mainly on the Nisava River)

Point sources:

• municipal, industrial sources

Risk assessment (only for the Nisava river)

• 2 of 3 water bodies possibly at risk from organic pollution, hazardous substances and nutrients

Page 16: TransboundaryNisavaRiver catchment in the Morava River ... · Neogene aquifers are in the Leskovac and Jagodina-Paraćin basins. The extent of the karsticaquifers is limited. Eastern

Nisava: transboundaryimpact

• river engineering works in BG

• affected rivers: Nisava, Visocica

• pressure: water abstraction – diverting to another catcment

• impact: decrease of mean and low flows at entrance to RS

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Nisava: status, measures

• No status assessment so far in Serbia

• List of measures only at the Danube river basin level(in favorable conditions, improvement of the wastewater treatment issues in the city of Nis can be expected)

Page 18: TransboundaryNisavaRiver catchment in the Morava River ... · Neogene aquifers are in the Leskovac and Jagodina-Paraćin basins. The extent of the karsticaquifers is limited. Eastern

Thanks for your attention…

Visocica River


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