Presentation on groundwater management in Saudi Arabia by Dr. Ali Saad Al-Tokhais at the International Annual UN-Water Zaragoza Conference 2012/2013. Preparing for the 2013 International Year. Water Cooperation: Making it Happen! 8-10 January 2013.
2. Water consumption for Saudi Arabia
Sector 2005 2006 2007 2008 2009 2010
Domestic 1,748 1,848 1,977 2,006 2,123 2,283
Industrial 654 668 683 698 714 753
Agricultural 18,586 17,003 15,420 15,083 14,747 14,410
Total 20,988 19,519 18,080 17,787 17,584 17,446
Unit is MCM/year
3. Background: How much groundwater is available?
First assessment of water resources:
•1963-1983: Exploration and identification of groundwater resources
•1979: British Arabian Advisory Company (BAAC)
•1980: Groundwater Development Consultants (GDC)
•1983: German Agency for Technical Cooperation (GTZ)
•1985: Bureau de Recherches Géologiques et Minièrs (BRGM)
Groundwater reserve: Estimation of groundwater in storage is 428,400 MCM
Groundwater abstraction: Total groundwater abstraction of 462,300 MCM (1975 – 2005)
Results:
1.Drying up of natural springs
2.Declining groundwater levels of all aquifers
3.Deterioration of water quality
What is next: The Ministry of Water & Electricity (MoWE) is working on the reassessment
of the water resources since 2003
9. Major water provinces in Saudi Arabia
Red Sea Coast
The water resources of
this area are made up by
desalinated seawater,
renewable water
resources, and treated
waste water
10. Major water provinces in Saudi Arabia
Northern
Arabian Shield
Desalinated seawater,
renewable water
resources, and treated
waste water are the only
water resource in this
area. However, the
amount of renewable
resources is low compared
to the Southern Shield,
because the rainfall is
lower.
11. Major water provinces in Saudi Arabia
Southern
Arabian Shield
Significant amounts of
rainfall (up to 400 mm/a)
enable a water supply that
is based solely on
renewable water
resources. This is the only
area in Saudi Arabia,
where a sustainable use of
the water is possible.
Desalinated seawater and
treated waste water are
among the water
resources
12. Major water provinces in Saudi Arabia
Arabian Platform
In this area, only non-
renewable ground-water
resources exist. Some
remote supply from
desalinated seawater
from the East Coast takes
place.
13. Major water provinces in Saudi Arabia
East Coast
Desalinated seawater and,
to much lesser extent,
non-renewable
groundwater resources as
well as treated waste
water make up the water
resources of this area.
14. Extent of principal aquifers on the Arabian Platform
Umm Er Radhuma & overlying aquifers
Wasia-Biyadh-Aruma
Khuff-Jilh-Minjur
Wajid & Saq
15. Major aquifer types on the Arabian Platform
Bedrock aquifers
Sandstone aquifers Karst aquifers
Fractures with permeable matrix Conduit system with a karstified rock matrix
Examples: Examples:
Wajid, Saq, Dhruma, Minjur, Wasia, Biyadh Aruma, Umm Er Radhuma, Dammam
16. Objectives of reassessment of the water resources studies
Assessment of groundwater budget
What are the in- and outflows to the aquifer system?
Assessment of groundwater resources
How much groundwater is (still) available?
Managing of groundwater resources
How can we make best use of the groundwater resource?
Is sustainable non-renewable groundwater management
possible in arid countries?
17. Flow chart: aquifers studies
Collection and
interpretation of data
Development of aquifer
model
Application of aquifer
model as a
management tool
20. Groundwater budget: predevelopment state (before
1965)
Inflow: Outflow:
• groundwater recharge • spring discharge
• inflow through wadi channels • inland and coastal sabkhas
• Arabian Gulf
21. Groundwater budget: present state
Inflow: Outflow:
• groundwater recharge • agricultural water use
• inflow through wadi channels • industrial water use
• domestic water use
23. Consequences of high groundwater abstractions
1. Declining groundwater levels / large groundwater drawdown
2. Increase in production costs due to high pumping lifts
3. Destruction of the environment and increasing desertification zones
4. Deterioration of groundwater quality / salt water intrusion
5. Conflict between water users:
• agriculture, industry, domestic water use
• present generation / future generation
6. Possible land subsidence
24. Umm Er Radhuma aquifer: Al Hassa
Drying up of springs
Declining groundwater levels
Large scale groundwater drawdown
Deterioration of groundwater quality
25. Drawdown in Saq and Wasia Biyadh aquifer
Saq: Hail-Buraydah- Wasia-Biyadh:
Tabuk region Al Kharj region
26. Location of main consumers
Conflict in supply between:
- Urban centers
- Agriculture
27. Indicators for change in water strategy
• 2003: Establishment of the Ministry of Water & Electricity
(MoWE). Separation of the agricultural sector from the water
sector.
• 2003: Launch of reassessment of the water resources. Studies will
be finished by 2014.
• 2008: Establishment of National Water Company (NWC).
• 2008: Phasing out wheat production until 2016 (Royal Decree
335).
• 2010: Intensive development of groundwater resources for
municipal water supply.
• 2010: Preparation of comprehensive water law.
29. Irrigation efficiency
Crop consumptive
use and
groundwater
abstraction in Saudi
Arabia
Irrigation efficiency must be increased. Comparing crop consumptive use to
groundwater abstraction shows that irrigation efficiency is below 50%. Further
efforts are required by the Ministry of Agriculture in order to increase irrigation
efficiency to reach minimally 70%.
30. Question and challenges
Question:
Should non-renewable groundwater be pumped for maximum benefit
of the present generation without a concern about over drafting the
aquifers?
or
Should the present groundwater withdrawal be limited to preserve
the resource for the future generations?
Challenges in managing non-renewable groundwater
1.Rapid aquifer depletion
2.Rapid increase in urban water demand
3.High agricultural water demand
31. Solutions
1. Improve IWRM to achieve groundwater sustainability
2. Decrease non-renewable groundwater abstraction
3. Increase irrigation efficiency
4. Implementation of virtual water program for agricultural
production
5. Make groundwater protection everybody's responsibility
Presentation: Dr. Ali Al Tokhais - 4 – 5 September 2012
Overview of geology and aquifers. Simplified geological map of the Arabian Peninsula. Geological units: Arabian Shield (including Harrats) Arabian Platform Zagros fold belt Red Sea basin Ophiolites in Oman (Semail-ophioltes, oduction of ocean floor)
Arabian Shield. Comprises of igneous and metamorphic rocks of Precambrian age + volcanic rocks of Tertiary and younger age. Secondary aquifers. In general low yield. Exception alluvial wadi fillings.
Arabian Platform. The geology of the Arabian Platform is characterised by a thick pile of sedimentary formations that are lying on top of the basement rocks. Water-bearing sandstone and limestone layers (aquifers) alternate with low permeability shale layers Thick sedimentary sequence, ranging from Cambrian (540 Ma) to Recent. The sequence is resting on the flanks of the Arabian Shield. The Arabian Shield is a tectonically stable region. The base of the sequence is made of igneous and metamorphic rocks. The sedimentary succession consists of carbonates, sulphates, shales, marls and sandstones. The succession was deposited during several transgressive and regressive cycles. In the lower part clastic sediments (sandstones etc.) prevail. In the upper part limestones, dolomites and sulphates prevail.
Geological cross section through the Arabian Platform (Riyadh – Qatar). Notes: Tectonics (faults and horst structures) + oil traps + occurrence of oil and gas resources.
Rainfall distribution
The Kingdom of Saudi Arabia disposes of three major types of water resources. These are: non-renewable groundwater resources, renewable groundwater and surface water resources, and desalinated seawater. The availability of these resources varies throughout the country, and accordingly five different areas are distinguished. Red Sea Coast: The water resources of this area are made up by desalinated seawater and renewable water resources.
The Kingdom of Saudi Arabia disposes of three major types of water resources. These are: non-renewable groundwater resources, renewable groundwater and surface water resources, and desalinated seawater. The availability of these resources varies throughout the country, and accordingly five different areas are distinguished. Northern Arabian Shield: Renewable water resources are the only water resource in this area. However, the amount of renewable resources is low compared to the Southern Shield, because the rainfall is lower.
The Kingdom of Saudi Arabia disposes of three major types of water resources. These are: non-renewable groundwater resources, renewable groundwater and surface water resources, and desalinated seawater. The availability of these resources varies throughout the country, and accordingly five different areas are distinguished. Southern Arabian Shield: Significant amounts of rainfall (up to 500 mm/a) enable a water supply that is based solely on renewable water resources, if good water management is implemented. This is the only area in Saudi Arabia, where a sustainable use of the water resources is possible.
The Kingdom of Saudi Arabia disposes of three major types of water resources. These are: non-renewable groundwater resources, renewable groundwater and surface water resources, and desalinated seawater. The availability of these resources varies throughout the country, and accordingly five different areas are distinguished. Arabian Platform: In this area, only non-renewable groundwater resources exist. Some remote supply from desalinated seawater from the East Coast takes place.
The Kingdom of Saudi Arabia disposes of three major types of water resources. These are: non-renewable groundwater resources, renewable groundwater and surface water resources, and desalinated seawater. The availability of these resources varies throughout the country, and accordingly five different areas are distinguished. East Coast: Desalinated seawater and, to much lesser extent, non-renewable groundwater resources make up the water resources of this area.
Geological column with principal and secondary aquifers on the Arabian Platform The map shows the location of the groundwater study areas on the Arabian Platform. The borders of the areas in KSA are defined by the extent of the aquifers (outcrop + sub crop). Location of the study areas: Wajid – Saq - Khuff-Jilh-Minjur - Wasia-Biyadh-Aruma - Umm Er Radhuma. Aquifer studies carried out by GTZ & DCo and BRGM since 2003. Ongoing until 2013
Major aquifer types on the Arabian Platform Groundwater is found in underground reservoirs or aquifers. Definition of the term aquifer: an aquifer is a geologic unit that can store and transmit enough water to be a significant water resource. Aquifer types. Porous media aquifers + bedrock aquifer. Description of vessels where groundwater is stored. Aquifer properties. Storativity + hydraulic conductivity.
Main objectives of aquifer studies
Flow chart of aquifer studies. Exploring, mapping and assessing of groundwater resources.
Presentation of results
Groundwater budget components in arid areas: predevelopment state The predevelopment state is defined by a site which is in its natural condition prior to any major human activity. Prior to the introduction of motor pumps Population in 1932: 2.4 Mio. Kingdom was founded Population in 1950: 3.2 Mio Population in 2010: 27 Mio. Population in 2050: 45 Mio.
Groundwater budget components in arid areas: present state
Global water budget for the Kingdom of Saudi Arabia
Consequences of overexploitation. Same problem in the USA: Ogallala Aquifer, also known as the High Plains Aquifer. Fluviatile sediments of Miocene and Pliocene age.
Examples for long-term decline in groundwater levels for selected observation wells of the Umm Er Radhuma, Dammam, and Neogene aquifer in the region of Al Hassa due to non sustainable groundwater abstraction. In some areas groundwater levels are declining by meters per year. These are alarming rates. Spatial extent of the cones of depression in the Umm Er Radhuma, Dammam, and Neogene aquifer for 2004. Groundwater depletion in some high-abstraction areas attracts saline waters from nearby wadi beds or underlying aquifers, and seawater intrusion.
Examples for long-term decline in groundwater levels for selected observation wells of the Umm Er Radhuma, Dammam, and Neogene aquifer in the region of Al Hassa due to non sustainable groundwater abstraction. In some areas groundwater levels are declining by meters per year. These are alarming rates. Spatial extent of the cones of depression in the Umm Er Radhuma, Dammam, and Neogene aquifer for 2004. Groundwater depletion in some high-abstraction areas attracts saline waters from nearby wadi beds or underlying aquifers, and seawater intrusion.
Location of main consumers on the Arabian Platform. Conflict in supply. Competition between domestic, industrial, and agricultural users. The nearst is the cheapiest! Transmission costs are high. Consequence: conserve the groundwater for domestic (municipal) use next to urban centers.