Kyrgyzstan

Tajikistan

Kazakhstan

GROUNDWATER MANAGEMENT IN THE SYR
DARYA TRANSBOUNDARY BASIN

REPUBLIC OF TAJIKISTAN
NATIONAL BASIC SITUATIONAL ANALYSIS OF
Groundwater IN THE BASIN OF THE SYR DARYA RIVER.

PROJECT PREPARATION PHASE
INCEPTION MEETING
Paris – February 3-4, 2014
Groundwater Resources
Groundwater in the country are extremely diverse in
their chemical composition and the taste, mode of
occurrence, movement and flowing. Two hydrodynamic
zones are identified in the vertical geological layer.
1. The upper one is characterised with relatively low (up to
200-300 m) capacity, active water exchange and
preferential development of fresh Groundwater of a good
quality.
2. The lower layer, covering deep horizons of artesian basins,
with complicated water exchange. On this level salty and
brine Groundwater with mineralization up to 400 g/dm3
are common. The capacity of the zone is up to several
kilometers.
Groundwater Resources
Under geo-morphological features the Syr Darya
basin includes two broad areas - mountains and
plains.
•There are fracture and fissure-poral freshwaters
everywhere in mountainous areas. The chemical
composition of Groundwater makes hydro
carbonate and calcium with mineralization up to 1
g/dm3.
•Plain areas are characterised with quite diverse
hydro-geological conditions.
Scheme of the Fresh Groundwater
resources locations in SyrDarya Basin
Groundwater Resources,
thousand м3/days
River basin

Projected

Proven reserves

Syr Darya

9806 (19,1%)

3401,1 (41,3%)

Total in RT

51226

8236,2
Use of Groundwater,
mln.м3/year
River basins

Groundwater

Mining water

Syr Darya

241,95

3,21

Total

793,63

3,24
Mineral healing waters
Tajikistan is rich with various mineral healing waters
which are divided into seven main balneological groups:
•Waters without “specific” components and qualities
•Carbon dioxide
•sulphuorus
•Chalybeate
•Iodide and bromine
•Radon
•Siliceous therms.
Mineral healing waters
Within the basin of the Syr Darya river only
three types of mineral healing waters are
represented:
•Waters without “specific” components and
qualities (Kansai, Shurab, Havatag)
•Sulphurous (Obishifo)
•Radon (Taboshar, Adrasman, Kaftarhon,
Chashma)
Thermal waters
• In Tajikistan 35 deposits and occurrences of
thermal waters are identified, and only one is
within the Syr Darya river basin:
• Havatag with water temperature 41°С
Industrial waters
Depending on a set of industrial micro components eight
associations are identified:
•Iodine
•Bromine
•Lithia carrying
•Iodine - Bromine
•Iodine-bromine – Lithium carrying
•Iodine – Lithium – Rubidium carrying
•Iodine – Lithium – Rubidium – Caesium carrying
•Iodine – Lithium – Rubidium – Caesium - Strontium
carrying
Industrial waters
Within the Sogd oblast in Tajikistan one iodine
Industry association is identified.
Quality of Groundwater
Depth, m
Name of the
deposit

Testing

Increased content
of ingredients

Golodnostepskoe

128

Up to 26

Lyakkatskoe

154

Up to 30

Nauskoe

122

Up to 78

Kanibadamskoe

100

Ispharinskoe

100

Shahristanskoe

85

Up to 20
Up to 36
Up to 46
Up to 60
Up to 7
Up to 10
Up to 25
Up to 31
Up to 48
Up to 96
Not marked

Name of
ingredients with
recorded increased
content
Mineralization,
stiffness, sulphates
Mineralization,
stiffness, sulphates
Mineralization,
stiffness, sulphates
Mineralization,
stiffness, sulphates,
chlorides
Mineralization,
stiffness, sulphates

Sum of
concentration ratio

Index of
contamination

3,4-3,5

2

4,4-4,5

2

2,3-2,5

2

12,1-14,1
6,4-6,6
5,7
4,3
12,4
6,9-7,5
1,3-2,7
3,7-4,7
1,1
1,4

3
2
2
2
3
2
1
2
1
1
Quality of Groundwater
Depth, m

Name of
ingredients
with increased
content

Sum of
concentration
ratio

Index of
contamination

Name of the
deposit

Testing

Increased
content of
ingredients

Dalverzin

164

Not marked

206

Up to 23
Up to 62

Mineralization,
stiffness,
sulphates

2,2
4,7-5,8

1
2

68

Up to 32
Up to 41
Up to 68

Mineralization,
stiffness,
sulphates

1,4-4,1
6,2-8,0
3,3-3,6

1-2
2
2

74

Up to 25
Up to 30

Mineralization,
stiffness,
sulphates

3,4
9,7-10,0

2
2

Up to 22
Up to 56

Mineralization,
stiffness,
sulphates,
chlorides

11,0-11,5
3,2-3,4

3
2

Mirzaravat

Syrdariya

Samgar

Kamyshkurgan

120
Reasons for Groundwater contamination
• Deterioration of the quality of surface waters used for
irrigation, as a result water mineralization of Syr
Darya, increased from 0.7 to 1.4-1.6 g/dm3;
• Lack of reliable isolation of an upper water carrying
horizon
• Fertilisation and processing of crops with pesticides;
• Numerous defects of the canalization network and its
full absence in settlements
• Untreated waste water discharge to fields under
irrigation
• Lack of the zone under sanitary protection
Legislative framework
Groundwater are managed based on the
following legislative acts:
•Water code
•The Law “On Nature Protection”
•The Law on Subsurface Resources
•Tax Code
Legislative framework (continued)
1. Regulation on delimitation of authorities of
specially designated state bodies on
controlling the use and protection of waters
2. On the procedure for state water cadastre
maintenance
3. The procedure for execution, registration
and issuance of permissions for water use on
special conditions
Legislative framework (continued)
4. The procedure for encouraging water users,
performing socially useful measures for the
rational use and protection of waters
5. The procedure for recognition of water units
as monuments of nature and culture
6. The procedure for use of Groundwater, not
attributed to drinking or healing waters
Legislative framework (continued)
7. The procedure for identification of water
ways as a category of navigable waters and
the rules for their operation
8. The procedure for use of water units for
fishery
9. The rules for use of water units for power
industry
Legislative framework (continued)
10. The regulation on the procedure for state
recording and state registration of works on
subsurface geology research for extraction of
natural resources and for the purposes not
related to their extraction.
11. The procedure for submission of reports to
the government by enterprises, which
explore natural resource fields and extract
them.
Legislative framework (continued)
12. The procedure for signing subsurface use contracts
13. The procedure for determination of royalty rates in
signing mining contracts, the procedure for bonus
calculation, the procedure for determining an
internal rate of return, and the procedure for the tax
expertise of subsurface use contracts.
14. The procedure for specific terms of licensing of
certain types of activities
Transboundary aspects of management
and use of Groundwater
Number in
the scheme
1
2
3
4
5

Name of the transboundary Direction of flow of
site
Groundwater
Zafarobod
TJ-UZ-TJ-UZ
Dalverzin
TJ-UZ
Nau-Kostakoz
KG-TJ
Isfara-Lyakkan
KG-TJ-UZ
Kanibadam
UZ-TJ
Scheme of Transboundary areas where
connection of Groundwater in the SyrDarya Basin

2
5
3

1

Name of potential transboundary sites
1. Zafarobod
2. Dalverzin
3. Nau-Kostakoz
4. Isfara-Lyakkan
5. Kanibadam

4
Monitoring of Groundwater
The following organizations carry out
monitoring of Groundwater:
•Chief directorate on geology
•Melioration and irrigation agency
•Environment Protection Committee
Current problems
• Potential threat to purity of Groundwater and
environment resulted from filtration of
irrigation and drainage discharges.
• De-scoping of groundwater monitoring due to
economic difficulties. Therefore, it is very
difficult to assess the use of Groundwater and
factors of pressure on transboundary
aquifers.
Current problems (continued)
• Lack of the single monitoring methodology for
Groundwater, absence of information
exchange.
• The Water code and the Law “On subsurface"
are not sufficiently interlinked in terms of
distribution of authorities, management,
research, use and protection of Groundwater.
• No comments to the Water Code.
Current problems (continued)
• Lack of qualified personnel
• Lack of target financing of activities relating to
maintenance of the state water cadaster
• Lack of modern distance methods on
monitoring of Groundwater
Recommended activities
• Development of the general scheme of using fresh drinking,
mineral, healing waters along with setting up an appropriate
infrastructure and taking measures for environment
protection.
• Development, approval and issuance of the state standard
norm (GOST) "Geology. Basic terms and definitions”, that will
help better understand legislation on natural resources and
environment protection.
• Development of the national strategy of the use and
protection of Groundwater.
• Arranging researches of all complex issues of formation and
use of Groundwater, including cross-border outstretch.
Recommended activities (continued)
• Improving statutory regulation in the sphere of
Groundwater.
• Development of provisions on the procedure for the
state monitoring of subsurface in RT, including the
subsystem - “monitoring of Groundwater”.
• Refining of the state system of prevention and
elimination of emergencies with the functional
subsystem of the state monitoring of subsurface
resources, taking into account Groundwater.
Recommended activities (continued)
• Re-valuation of operating reserves of Groundwater
– Why it is recommended to revaluate reserves of
Groundwater

• Contamination of Groundwater on mineralization,
stiffness, content of sulphates and chlorides.
• Expiry of the period of the exploitation of
Groundwater
• Increasing the depth of the operated aquifer up to
150-200 m.
Kyrgyzstan

Tajikistan

Kazakhstan

GROUNDWATER MANAGEMENT IN THE SYR DARYA TRANSBOUNDARY BASIN

THANK YOU FOR ATTENTION!

PROJECT PREPARATION PHASE
INCEPTION MEETING
Paris – February 3-4, 2014

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Situational analysis republic of tajikistan eng

  • 1. Kyrgyzstan Tajikistan Kazakhstan GROUNDWATER MANAGEMENT IN THE SYR DARYA TRANSBOUNDARY BASIN REPUBLIC OF TAJIKISTAN NATIONAL BASIC SITUATIONAL ANALYSIS OF Groundwater IN THE BASIN OF THE SYR DARYA RIVER. PROJECT PREPARATION PHASE INCEPTION MEETING Paris – February 3-4, 2014
  • 2. Groundwater Resources Groundwater in the country are extremely diverse in their chemical composition and the taste, mode of occurrence, movement and flowing. Two hydrodynamic zones are identified in the vertical geological layer. 1. The upper one is characterised with relatively low (up to 200-300 m) capacity, active water exchange and preferential development of fresh Groundwater of a good quality. 2. The lower layer, covering deep horizons of artesian basins, with complicated water exchange. On this level salty and brine Groundwater with mineralization up to 400 g/dm3 are common. The capacity of the zone is up to several kilometers.
  • 3. Groundwater Resources Under geo-morphological features the Syr Darya basin includes two broad areas - mountains and plains. •There are fracture and fissure-poral freshwaters everywhere in mountainous areas. The chemical composition of Groundwater makes hydro carbonate and calcium with mineralization up to 1 g/dm3. •Plain areas are characterised with quite diverse hydro-geological conditions.
  • 4. Scheme of the Fresh Groundwater resources locations in SyrDarya Basin
  • 5. Groundwater Resources, thousand м3/days River basin Projected Proven reserves Syr Darya 9806 (19,1%) 3401,1 (41,3%) Total in RT 51226 8236,2
  • 6. Use of Groundwater, mln.м3/year River basins Groundwater Mining water Syr Darya 241,95 3,21 Total 793,63 3,24
  • 7. Mineral healing waters Tajikistan is rich with various mineral healing waters which are divided into seven main balneological groups: •Waters without “specific” components and qualities •Carbon dioxide •sulphuorus •Chalybeate •Iodide and bromine •Radon •Siliceous therms.
  • 8. Mineral healing waters Within the basin of the Syr Darya river only three types of mineral healing waters are represented: •Waters without “specific” components and qualities (Kansai, Shurab, Havatag) •Sulphurous (Obishifo) •Radon (Taboshar, Adrasman, Kaftarhon, Chashma)
  • 9. Thermal waters • In Tajikistan 35 deposits and occurrences of thermal waters are identified, and only one is within the Syr Darya river basin: • Havatag with water temperature 41°С
  • 10. Industrial waters Depending on a set of industrial micro components eight associations are identified: •Iodine •Bromine •Lithia carrying •Iodine - Bromine •Iodine-bromine – Lithium carrying •Iodine – Lithium – Rubidium carrying •Iodine – Lithium – Rubidium – Caesium carrying •Iodine – Lithium – Rubidium – Caesium - Strontium carrying
  • 11. Industrial waters Within the Sogd oblast in Tajikistan one iodine Industry association is identified.
  • 12. Quality of Groundwater Depth, m Name of the deposit Testing Increased content of ingredients Golodnostepskoe 128 Up to 26 Lyakkatskoe 154 Up to 30 Nauskoe 122 Up to 78 Kanibadamskoe 100 Ispharinskoe 100 Shahristanskoe 85 Up to 20 Up to 36 Up to 46 Up to 60 Up to 7 Up to 10 Up to 25 Up to 31 Up to 48 Up to 96 Not marked Name of ingredients with recorded increased content Mineralization, stiffness, sulphates Mineralization, stiffness, sulphates Mineralization, stiffness, sulphates Mineralization, stiffness, sulphates, chlorides Mineralization, stiffness, sulphates Sum of concentration ratio Index of contamination 3,4-3,5 2 4,4-4,5 2 2,3-2,5 2 12,1-14,1 6,4-6,6 5,7 4,3 12,4 6,9-7,5 1,3-2,7 3,7-4,7 1,1 1,4 3 2 2 2 3 2 1 2 1 1
  • 13. Quality of Groundwater Depth, m Name of ingredients with increased content Sum of concentration ratio Index of contamination Name of the deposit Testing Increased content of ingredients Dalverzin 164 Not marked 206 Up to 23 Up to 62 Mineralization, stiffness, sulphates 2,2 4,7-5,8 1 2 68 Up to 32 Up to 41 Up to 68 Mineralization, stiffness, sulphates 1,4-4,1 6,2-8,0 3,3-3,6 1-2 2 2 74 Up to 25 Up to 30 Mineralization, stiffness, sulphates 3,4 9,7-10,0 2 2 Up to 22 Up to 56 Mineralization, stiffness, sulphates, chlorides 11,0-11,5 3,2-3,4 3 2 Mirzaravat Syrdariya Samgar Kamyshkurgan 120
  • 14. Reasons for Groundwater contamination • Deterioration of the quality of surface waters used for irrigation, as a result water mineralization of Syr Darya, increased from 0.7 to 1.4-1.6 g/dm3; • Lack of reliable isolation of an upper water carrying horizon • Fertilisation and processing of crops with pesticides; • Numerous defects of the canalization network and its full absence in settlements • Untreated waste water discharge to fields under irrigation • Lack of the zone under sanitary protection
  • 15. Legislative framework Groundwater are managed based on the following legislative acts: •Water code •The Law “On Nature Protection” •The Law on Subsurface Resources •Tax Code
  • 16. Legislative framework (continued) 1. Regulation on delimitation of authorities of specially designated state bodies on controlling the use and protection of waters 2. On the procedure for state water cadastre maintenance 3. The procedure for execution, registration and issuance of permissions for water use on special conditions
  • 17. Legislative framework (continued) 4. The procedure for encouraging water users, performing socially useful measures for the rational use and protection of waters 5. The procedure for recognition of water units as monuments of nature and culture 6. The procedure for use of Groundwater, not attributed to drinking or healing waters
  • 18. Legislative framework (continued) 7. The procedure for identification of water ways as a category of navigable waters and the rules for their operation 8. The procedure for use of water units for fishery 9. The rules for use of water units for power industry
  • 19. Legislative framework (continued) 10. The regulation on the procedure for state recording and state registration of works on subsurface geology research for extraction of natural resources and for the purposes not related to their extraction. 11. The procedure for submission of reports to the government by enterprises, which explore natural resource fields and extract them.
  • 20. Legislative framework (continued) 12. The procedure for signing subsurface use contracts 13. The procedure for determination of royalty rates in signing mining contracts, the procedure for bonus calculation, the procedure for determining an internal rate of return, and the procedure for the tax expertise of subsurface use contracts. 14. The procedure for specific terms of licensing of certain types of activities
  • 21. Transboundary aspects of management and use of Groundwater Number in the scheme 1 2 3 4 5 Name of the transboundary Direction of flow of site Groundwater Zafarobod TJ-UZ-TJ-UZ Dalverzin TJ-UZ Nau-Kostakoz KG-TJ Isfara-Lyakkan KG-TJ-UZ Kanibadam UZ-TJ
  • 22. Scheme of Transboundary areas where connection of Groundwater in the SyrDarya Basin 2 5 3 1 Name of potential transboundary sites 1. Zafarobod 2. Dalverzin 3. Nau-Kostakoz 4. Isfara-Lyakkan 5. Kanibadam 4
  • 23. Monitoring of Groundwater The following organizations carry out monitoring of Groundwater: •Chief directorate on geology •Melioration and irrigation agency •Environment Protection Committee
  • 24. Current problems • Potential threat to purity of Groundwater and environment resulted from filtration of irrigation and drainage discharges. • De-scoping of groundwater monitoring due to economic difficulties. Therefore, it is very difficult to assess the use of Groundwater and factors of pressure on transboundary aquifers.
  • 25. Current problems (continued) • Lack of the single monitoring methodology for Groundwater, absence of information exchange. • The Water code and the Law “On subsurface" are not sufficiently interlinked in terms of distribution of authorities, management, research, use and protection of Groundwater. • No comments to the Water Code.
  • 26. Current problems (continued) • Lack of qualified personnel • Lack of target financing of activities relating to maintenance of the state water cadaster • Lack of modern distance methods on monitoring of Groundwater
  • 27. Recommended activities • Development of the general scheme of using fresh drinking, mineral, healing waters along with setting up an appropriate infrastructure and taking measures for environment protection. • Development, approval and issuance of the state standard norm (GOST) "Geology. Basic terms and definitions”, that will help better understand legislation on natural resources and environment protection. • Development of the national strategy of the use and protection of Groundwater. • Arranging researches of all complex issues of formation and use of Groundwater, including cross-border outstretch.
  • 28. Recommended activities (continued) • Improving statutory regulation in the sphere of Groundwater. • Development of provisions on the procedure for the state monitoring of subsurface in RT, including the subsystem - “monitoring of Groundwater”. • Refining of the state system of prevention and elimination of emergencies with the functional subsystem of the state monitoring of subsurface resources, taking into account Groundwater.
  • 29. Recommended activities (continued) • Re-valuation of operating reserves of Groundwater – Why it is recommended to revaluate reserves of Groundwater • Contamination of Groundwater on mineralization, stiffness, content of sulphates and chlorides. • Expiry of the period of the exploitation of Groundwater • Increasing the depth of the operated aquifer up to 150-200 m.
  • 30. Kyrgyzstan Tajikistan Kazakhstan GROUNDWATER MANAGEMENT IN THE SYR DARYA TRANSBOUNDARY BASIN THANK YOU FOR ATTENTION! PROJECT PREPARATION PHASE INCEPTION MEETING Paris – February 3-4, 2014