1. Transboundary Groundwater

2. The Hydrologic Cycle 2

3. Surface and Groundwater interrelationship
Groundwater is influenced by land-development patters
Overexploitation of water:
Discharge rate is more than recharge rate
Decreases water levels
Contamination 3

4. 4

5. Problems in Groundwater
Disperses beneath the surface, irrespective of state boundaries
Characteristics vary in each aquifer
Often deep or unevenly distributed geographically
An aquifer definition cannot provide concrete conclusion about ownership 5

6. Country A
Country B 6

7. While international boundaries may follow natural physical features as rivers, the aquifers underlying them do not 7

8. Definition of an aquifer
A saturated permeable geologic unit that can transmit significant quantities of water under ordinary hydrologic gradients
A geologic unit that can store and transmit water at rates fast enough to supply reasonable amounts to well 8

9. Transboundary Aquifers9

10. ‘Models’
An aquifer is entirely in one country 10

11. ‘Models’
An aquifer is divided by international boundary 11

12. ‘Models’
An aquifer is entirely in the territory of one country but is linked hydrologically to an international river 12

13. ‘Models’
An aquifer is entirely in the territory of one country but is linked hydrologically with another aquifer in a neighboring country 13

14. ‘Models’
An aquifer is entirely in the territory of one country but its recharge area is in a neighboring country 14

15. 15

16. Water Conventions 16

17. Helsinki Rules 1967 International Drainage Basin
An international drainage basin is a geographical area extending over two or more states determined by the watershed limits of the system of waters, including surface and underground water, flowing into a common terminus
Excluded confined aquifers which constitute a large portion of groundwater 17

18. Seoul Rules 1987
An aquifer that contributes waters to, receives water from, surface waters of an international basin constitutes part of an international basin for the purpose of the Helsinki Rules 18

19. Seoul Rules 1987
An aquifer intersected by the boundary between two or more States that does not contribute water to, or receive water from, surface waters of an international drainage basin constitutes an international drainage basin 19

20. Bellagio Draft Treaty 1989 Defines an aquifer to be:
a subsurface waterbearing geologic formation from which significant quantities of water may be extracted.
Groundwater:
The water in aquifers. 20

21. Bellagio Draft Treaty 1989
The overriding goal of the treaty is to achieve joint, optimum utilization of the available waters, facilitated by procedures for avoidances or resolution of differences over shared groundwaters in the face of the over increasing pressures on these priceless resources 21

22. The terminology used in international legal principles must coincide with that used by scientists to avoid any confusion 22

23. 1997 Convention:
"confined" to mean "unrelated to surface water“
Reflected the old interpretation of the term
Under current scientific terms, a confined aquifer refers to an aquifer in which the water is stored above atmospheric pressure; the term has no relation to an aquifer's hydrologic connections to surface waters; confined aquifers can be hydrologically connected to surface waters 23

24. Obligation not to cause significant harm
Human activities at the ground surface, e.g. landfill of waste, can result in aquifer pollution
The polluted groundwater from one side of an international boundary can travel to the other
Once polluted, aquifer cleanup is slow and expensive; the detection of its sub surface distribution can also be expensive 24

25. Obligation not to cause significant harm
The differences between surface and groundwater resources is the time needed to detect pollution
The aquifer systems impacts generated by the present generation may be detected by the future generations 25

26. Karstic aquifers
Characterized by the presence of preferred pathways (e.g., conduits) in which flow speeds are very much larger than average
Contaminants within these pathways travel much faster, and consequently have much shorter travel times, than predicted by standard models based on Darcy’s law and the advection-dispersion equation 26

27. Karstic aquifers
This is a dangerous situation; for example, conventional modeling may predict a water supply to be safe from contamination, when in fact it is not. The result of an inaccurate prediction of contaminant behavior can be a costly clean-up 27

28. International Shared Aquifer Resource Management (ISARM)
Supported by:
IAH: International Hydrological Program
UNESCO: United Nations Educational, Scientific and Cultural Organization.
FAO: Food and Agriculture Organization.
UNECE: United Nations Economic Commission for Europe 28

29. International Shared Aquifer Resource Management (ISARM)
In any legal agreement to be drawn up for the equitable share of transboundary resource, ISARM sees that the initial stage must be the correct identification of flow and movement of water followed by its quantification 29

30. International Shared Aquifer Resource Management (ISARM)
Knowledge of basic hydrological processes
Understanding of the extent and nature of the aquifer
How it relates to other aquifers and hydrogeologic features
How the recharge and discharge of water takes place within the aquifer
Where potential sources of contamination are located 30

31. International Shared Aquifer Resource Management (ISARM)
We need to know
Precipitation
Groundwater levels
Stream flow
Evaporation
Water use 31

32. Factors affecting the behavior and the development potential of aquifers
Hydraulic parameters
Rainfall and recharge zones
Confined and unconfined areas
Natural discharge zones
Present and planned groundwater development zones
Water quality, potential risks of its deterioration
Vulnerability to polluting agents 32

33. There are several examples of transboundary aquifers where recharge is received on one side while the natural discharges (and sometime better yields) are across the border
Examples of this condition are found in the Mountain Aquifer extending over Israel and Palestine 33

34. Example
The mountain aquifer lies primarily underneath the West Bank and consists of three basins:
The western
The northeastern
The Eastern
83% of the recharge areas for these basins lie within the West Bank 34

35. Example Eastern Aquifer: 172 MCM/year recharge
54 MCM/year was currently being pumped by the Palestinians
40 MCM/year by the Israelis
The remaining 78 MCM/year was available to be developed 35

36. Example Northeastern Aquifer: Yield 145 MCM/year
103 MCM/year being used by the Israelis
32 MCM/yr being used by the Palestinians 36

37. Example Western Aquifer: Estimated recharge of 362 MCM/year
340 MCM/year used by Israelis
20 MCM/year used by the Palestinians 37

38. Example
Several studies have questioned these estimates as overly optimistic, especially the estimated size of the eastern aquifer
Israel currently uses 93% of the annual recharge to the aquifer
Palestinians receive only about 17% of the water supply underlying West Bank territory and nothing from the Jordan River.
Israel supplies Palestinians with 63% of the total water consumed in the West Bank via Mekerot pipelines 38

39. The Inventory phase
ISARM Key Players