e isotopic studies on major k aquifer in lake van basin … aydin... · 2011-05-11 ·...
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ENVIRONMENTAL ISOTOPIC STUDIES ON MAJOR KARST AQUIFER IN LAKE VAN BASIN (TURKEY)
Harun AYDIN(a)
Erkan DİŞLİ(a), Mehmet EKMEKÇİ(b), Levent TEZCAN(b), Nevin AKSOY(c) (a) Department of Environmental Engineering, Yüzüncü Yıl University, Van, Turkey
(b) International Research Center for Karst Water Resources (UKAM), Hacettepe University, Beytepe, Ankara, Turkey (c) 17th Regional Directory of State Hydraulic Works, Van, Turkey
27 March – 1 April 2011, Monaco
INTERNATIONAL SYMPOSIUM ON ISOTOPES IN HYDROLOGY, MARINE ECOSYSTEMS, AND CLIMATE CHANGE STUDIES OCEANOGRAPHIC MUSEUM OF MONACO
Recharge Flow
Storage Discharge
Requires Special Studies
Conceptual
Hydrogeological Model
Granular Karstic
Recharge Climate Morphology + Climate
Flow media Porosity Fractured systems + Karstic channels
Storage Saturated Zone Vadose + Saturated zone
Discharge Low High
Flow type Laminar Laminar – Turbulence
Hydraulic head Low High
Chemical composition Low High
Groundwater velocity < 10-3 m/s > 10-3 m/s
Granular Environment isotropic/homogen hydrodynamic properties
Karstic Environment anisotropic/heterogen hydrodynamic properties ?
Sudy Objective
to use physical, chemical and
isotopic techniques to evaluate
the hydrodynamic properties of
the major karst aquifer in the
Lake Van basin.
Lake Van Level 1648 m Depth 451 m Area 3577 × 106 km2
Volume 568 × 109 km3
Study Area Area 2530 km2
Min 1648 m Max 3680 m Mean 2353 m
Karst Springs
Akpınar
Dönemeç
Sakalar Gündoğan Springs
Soğuksu
Karst Springs
Şamran
Şamran Şamran
3.0
3.5
4.0
4.5
5.0
5.5
6.0
6.5
7.0
Feb 07 Jul 07 Nov 07 Apr 08 Sep 08 Feb 09 Jul 09 Dec 09 May 10 Oct 10 Mar 11
Dis
ch
arg
e (m
3/s
)
Daily
Monthly
Parametres Şamran Akpınar Gündoğan Sakalar
Sum (SAM) (CAM) (GND) (GUN) (SAK)
n 265 6 4 4 4 -
Average (m3/s) 4.739 0.195 0.164 0.180 0.167 5.445
Min (m3/s) 3.497 0.147 0.125 0.152 0.138 4.059
Max (m3/s) 6.669 0.233 0.188 0.226 0.223 7.549
February 7, 2007 to February 24, 2011
End of recession
period
0
10
20
30
40
50
60
70
80
90
100
0 50 100 150 200 250 300 350 400 450 500 550 600
Vo
lum
e (%
)
t (day - after July 17, 2007)
Discharged water volume
Remain water volume
2007 2008
(day-1) 0.002 0.0015
t (day) 242 243
Vt (*106 m3) 242.61 289.38
Vd (*106 m3) 98.1 86.43
(%) 40.42 29.9
Vr (*106 m3-%) 144.5 202.95
(%) 59.58 70.10
Recession Period
July 17, 2007 to March 15, 2008
July 3, 2008 to March 3, 2009
Maillet Equation
K T S Fractured Systems
Field measurements YSI 556 MP (T, pH, EC, TDS, etc.) Major ions Hacettepe University Trace elements Ankara, TURKEY 3H Stable isotopes Perdue University (18O ve D ) Indiana, USA
Hydrochemistry (Data Logger and Field Measurements)
February 07, 2007
Hidro
geoc
hemistr
y (Field M
easu
rement
s)
n
18577 pH T (C) ECA (mS/cm) EC25 (mS/cm)
Min 6.27 10.17 464.00 647.37
Max 7.34 10.61 685.00 944.63
Ave 6.76 10.37 593.60 823.74
SD 0.14 0.11 22.25 27.6
CV 2.02 1.06 3.75 3.3
Hidro
geoc
hemistr
y
Isotopic Studies – Local Meteoric Water Line
Sampling
nameSampling time d
2H d18O d ‰
Elevation
(m)
Snow1 26.02.2009 -143.7 -19.5 12.3 2350
Snow2 26.02.2009 -115.6 -17.1 20.9 2226
Snow3 26.02.2009 -98.9 -14.6 17.7 2120
Snow4 26.02.2009 -93.1 -13.2 12.1 2030
Snow5 26.02.2009 -88.7 -12.8 13.6 1923
Snow6 26.02.2009 -84.4 -12.9 18.5 1913
Snow7 26.02.2009 -72.3 -11.6 20.1 1823
Snow8 26.02.2009 -75.2 -11.1 13.9 1744
-72.3 -11.1 20.9
-143.7 -19.5 12.1
-96.5 -14.1 16.1
Maximum
Minimum
Average
GMVL
dD = 8 d18O + 10
MMWL
dD = 8 d18O + 22
-150
-140
-130
-120
-110
-100
-90
-80
-70
-60
-20 -19 -18 -17 -16 -15 -14 -13 -12 -11 -10 -9
dD
(‰ S
MO
W)
d18O (‰ SMOW)
LMWL
dD=8xd18O+16.5
GMWL
dD = 8 d18O + 10
MMWL
dD = 8 d18O + 22
-90
-85
-80
-75
-70
-65
-60
-55
-14 -13 -12 -11 -10 -9
dD(‰
SM
OW
)
d18O (‰ SMOW)
Gürpınar Marbel Aquifer (GND, GUN,SAK, SAM)
Gürpınar Marble Aquifer (ARK, CAM, DON)
Lake Van
Zernek Dam
Isotopic Studies – Spring Waters
Isotopic Studies – Spring Waters
0.0
2.0
4.0
6.0
8.0
10.0
12.0
14.0
0.0 2.0 4.0 6.0 8.0 10.0 12.0 14.0 16.0 18.0 20.0
Tri
tyu
m (T
U)
Cl (ppm)
Gürpınar Marble Aquifer (GND, GUN, SAK ve SAM)
Gürpınar Marble Aquifer (ARK, DON, CAM)
SnowYoung Waters
Old WatersDeep Circulation
Isotopic Studies Recharge Altitude
dD = -0.1239 H + 155.59
-160
-140
-120
-100
-80
-60
-40
-20
0
1500 1700 1900 2100 2300 2500
Elevation (m, asl)
dD
%oAverage recharge
altitudes calculated as
approximately 2200 m.
Conclusions
This study was supported by The Scientific and Technological Research Council of Turkey (TÜBİTAK)
with Project No: 106Y040.
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Lake Van, Akdamar Church and Mt. Artos