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Remco van [email protected]
Saltwater intrusion in the Netherlands in relation to the WFD
Seminar on Ground- and surface water monitoring Smardzewice, 9-12 July 2007 - INFRA 24055
Deltares (in formation)
2
Content
1. Introduction
2. Origin of saline groundwater
3. Impact analysis
4. Implications for WFD implementation
5. Conclusions
3
1. Introduction
According to WFD Annex II – GWB status
Alterations to flow direction resulting from level changes may occur temporarily, or continuously in a spatially limited area ….
but such reversals do not cause saltwater or other intrusion, and do not indicate a sustained and clearly identified anthropogenic induced trend in flow direction likely to result in such intrusions.
4
1. Introduction
WGC-2 Groundwater “Status compliance and trends”
Types of intrusion
5
1. Introduction
WGC-2 Groundwater “Status compliance and trends”
Groundwater good status is not met if
•Relevant TVs are exceeded and there is either a significant and sustained upward trend in one or more key parameters at relevant monitoring points
•or there is an existing significant impact on a point of abstraction as a consequence of an intrusion.
6
1. Introduction
Threshold values (Stuyfzand, 1993)
Main class Subdivided mg Cl / l
Fresh Oligohaline 0-5
Oligohaline-fresh 5-30
Fresh 30-150
Fresh-brackish 150-300
Brackish Brackish 300-1000
Brackish-salt 1000-10.000
Salt Salt 10.000-20.000
Hypersaline Hypersaline > 20.0000
Fresh - Brackish: 150 mg Cl / l
Brackish – Salt: 1000 mg Cl / l
7
1. Introduction
WGC-2 Groundwater “Status compliance and trends”
• Identify areas with natural high saline concentrations
• Identify areas where there is risk of intrusion (pressure due to pumping)
• Identify monitoring points which exceed relevant GW-QS and TVs
• Integrate the data mentioned above
• Calculate trends in Electrical Conductivity (EC) and other relevant substances concentrations indicating an expansion of intrusion
• Is there a significant impact on any point of abstraction due to intrusion?
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2. Origin of saline groundwater
NL has been part of the North sea in the pastDevelopment of brackish aquifers
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7100 ADHolocene
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Holocene3150 AD
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2. Origin of saline groundwaterDistribution of fresh water aquifers
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2. Origin of saline groundwaterDistribution of fresh water aquifers
Depth [m] relative to sea level< 100100 - 200200 - 300300 - 400400 - 500≥ 500Areas with inversion(e.g. saltwater above fresh water)
Source: REGIS (TNO)
13
2. Origin of saline groundwater
(Stuyfzand & Stuurman, 1994)
Sea water or saline water pollution?
12 sources
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3. Impact analysis
Mining of fresh groundwater in the Dune region
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3. Impact analysis
Mining of fresh groundwater in the Dune region
(Stuyfzand, 1994)
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3. Impact analysis
Large scale intrusion in Polder areas
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3. Impact analysis
Large scale intrusion in Polder areas (Oude Essink, 1996)
Distance [m]
Dep
th [
m]
SeaDunearea
Haarlemmermeerpolder
1902
Distance [m]
Dep
th [
m]
SeaDunearea
Haarlemmermeerpolder
1854
Distance [m]
Dep
th [
m]
SeaDunearea
Haarlemmermeerpolder
1957
Distance [m]
Dep
th [
m]
SeaDunearea
Haarlemmermeerpolder
2006
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3. Impact analysis
Saltwater wells (de Louw, 2006)
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3. Impact analysis
Saltwater wells (Oude Essink, TNO)
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3. Impact analysis
Impact on pumping stations: upconing of saltwater
n > 200
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3. Impact analysis
(n = 16)
Impact on pumping stations: upconing of saltwater
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3. Impact analysis
Sea level rise
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3. Impact analysis
Sea level rise
Affected zone (λ) equals (kDc)
• For x=3λ, ΔΦ(x) = Φ0*e-3 = Φ0*0.05
• So for x=3λ only 5% of Φ0 remains
Affected zone (λ) equals (kDc)
• For x=3λ, ΔΦ(x) = Φ0*e-3 = Φ0*0.05
• So for x=3λ only 5% of Φ0 remains
x/0e
(x) x/0e
(x)
kDc
Noordzee/Nieuwe Waterweg North sea
Low polder area
Mazure equation
24
3. Impact analysis
Sea level riseAffected zone due to sea level rise and land subsidence in the Province Zuid-Holland
Difference in hydraulic head (m) at -12.5 below sea levelbetween 2000 and 2050
Source: TNO, Oude Essink, 2004
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3. Impact analysis
Sea level rise: saltwater intrusion through rivers
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4. Implications for WFD implementation
• Large database (> 60.000 bore holes) but only 10% deeper than 70 m
Based on these measurements a 3D model of salinity in groundwater was created
A good estimate of theinitial Cl-distributionis vital for modelling
(TNO, 2004)
60764 chloride concentrations in NL
Modelling
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Modelling
NAGROM (MLAEM-VD)• National scale • Saltwater distribution (3D) is fixed
MODFLOW (MOCDENS3D)• Regional scale• Saltwater distribution is not fixed
Chloride distribution (Cl mg l-1) Salt load in kg/ha/yr during an extreme dry year
4. Implications for WFD implementation
28
Monitoring: Distribution salt water in groundwaterDepth [m] of Cl concentration 1000 mg/l
4. Implications for WFD implementation
29
Horizontal intrusion
Vertical intrusion
Area vulnerable for upconing
Main salt water border for WFD
Area vulnerable for lateralIntrusion from the Peelhorst aquifer
Depth [m] of Cl concentration 1000 mg/l
4. Implications for WFD implementation
Monitoring: Distribution salt water in groundwater
30
Monitoring: LocationsDepth [m] of Cl concentration 1000 mg/l
Outside DWPA (drinking water protection area)
Inside DWPA (drinking water protection area)
Filter in brackish zoneFilter below salt borderSalt ‘gard’
Filter in brackish zoneFilter below salt borderSalt ‘gard’
4. Implications for WFD implementation
31
Present monitoring locations for WFD
Possible extension of monitoring locations
Salt water intrusion in groundwater
4. Implications for WFD implementation
Monitoring frequency
- Regional (vertical) 1/6yr- Dunes 1/2yr- Peel border 1/2yr- Dunes with abs. 1/yr- GW abs. 1-2/yr
32
5. Conclusions
1. Saltwater is abundantly present in the groundwaterbodies of NL (especially in the western and northern part). Mostly it is ‘old’ marine water.
2. Most important cause of saltwater intrusion is due to the deep polder areas. It is a slow process and considered to be irreversible (exemption).
3. Saltwater intrusion due to groundwater abstraction can occur on a small scale. It is considered as reversible.
4. Monitoring system is available and operational, but some modifications may be needed.