can we explain the so4 concentration by the observed ... · esf project „establishment of...
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![Page 1: Can we explain the SO4 concentration by the observed ... · ESF Project „Establishment of interdisciplinary scientist group and modelling system for groundwater research” Project](https://reader034.vdocument.in/reader034/viewer/2022051605/6011350cd5b802352d5e5af0/html5/thumbnails/1.jpg)
ESF Project „Establishment of interdisciplinary scientist group and modelling system for groundwater research”
Project Nr. 2009/0212/1DP/1.1.1.2.0/09/APIA/VIAA/060
INVESTING IN YOUR FUTURE
Can we explain the SO42-
concentration by the observed occurrence of
gypsum and modelled groundwater flow?
Andis Kalvāns
![Page 2: Can we explain the SO4 concentration by the observed ... · ESF Project „Establishment of interdisciplinary scientist group and modelling system for groundwater research” Project](https://reader034.vdocument.in/reader034/viewer/2022051605/6011350cd5b802352d5e5af0/html5/thumbnails/2.jpg)
ESF Project „Establishment of interdisciplinary scientist group and modelling system for groundwater research”Project number 2009/0212/1DP/1.1.1.2.0/09/APIA/VIAA/060
Problem definition
• May it be that the high [SO42-] in the SW
part of Latvia is a relict from geological past when groundwater flow patterns were different?
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ESF Project „Establishment of interdisciplinary scientist group and modelling system for groundwater research”Project number 2009/0212/1DP/1.1.1.2.0/09/APIA/VIAA/060
Method
• Interpolation with radius 20 km (2E4 m)• [SO4
2-] – the maximum value observed in the sampling point for each strat of V0
• Gypsum – a thickness normalised index for each strat of V0: – If gyps as primary mineral, score: 3– If gyps as secondary mineral, score: 2– No gypsum, score: 1
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Gyps in D3 st-el formations
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Gyps in D3 og-kt formations
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Gyps in D2 nr formation
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Gypsum, D3 pl-dgSO42- in D3 pl-dgSO4
2-, D3 gj-am
D3 pl-dg formations
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The SO42- in D3 gj-am formations
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ESF Project „Establishment of interdisciplinary scientist group and modelling system for groundwater research”Project number 2009/0212/1DP/1.1.1.2.0/09/APIA/VIAA/060
W-E section along y = 6 280 km
D3 pl-dg
D3 gj-am
D2-3 ar-br
D2 nr*
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SO42-
Gypsum
D3 pl-dg
D3 gj-am
D2-3 ar-br
D2 nr*
D3 pl-dg
D3 gj-am
D2-3 ar-br
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ESF Project „Establishment of interdisciplinary scientist group and modelling system for groundwater research”Project number 2009/0212/1DP/1.1.1.2.0/09/APIA/VIAA/060
X=415+/-45km
Y=6285+/-10
D3st-el
D3 og-kt
D3 pl-dg
D3 gj-am
D2-3 ar-br
D2 nr*
SO42-, D3 gj-am
D3 pl-dg
D3 gj-am
D2-3 ar-br
Gyps
SO42-
![Page 12: Can we explain the SO4 concentration by the observed ... · ESF Project „Establishment of interdisciplinary scientist group and modelling system for groundwater research” Project](https://reader034.vdocument.in/reader034/viewer/2022051605/6011350cd5b802352d5e5af0/html5/thumbnails/12.jpg)
ESF Project „Establishment of interdisciplinary scientist group and modelling system for groundwater research”Project number 2009/0212/1DP/1.1.1.2.0/09/APIA/VIAA/060
So what?
• Generally the observed SO42-
concentration in the groundwater can be well explained by the V0 model
• There is some water that seems to be formed at a time when different flow pattern persisted
• Tracer tests with score counting could provide some interesting statistics
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ESF Project „Establishment of interdisciplinary scientist group and modelling system for groundwater research”Project number 2009/0212/1DP/1.1.1.2.0/09/APIA/VIAA/060
Thanks for Your attention!