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A  Challenge  with  Groundwater Management A  Challenge  with  Groundwater Management

A Challenge with Groundwater Management - PowerPoint Presentation

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Uploaded On 2023-10-04

A Challenge with Groundwater Management - PPT Presentation

Preserving Water Quality Arsenic and Chromium Threats Scott Fendorf Stanford University Surface WaterSediment Ratio 10001 GroundwaterSediment Ratio 11000 Water Quality Problems ID: 1021788

aquifer arsenic pnas pumping arsenic aquifer pumping pnas water release groundwater iii compression 2mn2 erban 2018 2007 deep 2mno2

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1. A Challenge with Groundwater ManagementPreserving Water Quality: Arsenic and Chromium ThreatsScott FendorfStanford University

2. Surface Water:Sediment Ratio, 1000:1Groundwater:Sediment Ratio, 1:1000  Water Quality ProblemsGroundwater Quality Challenge

3. Appreciating Geogenic ThreatsFeCr2O4(s)UO2(s)As2S3(s)MnO2(s)

4. Arsenic Mobilization ProcessesPersistence of anaerobic conditionsAlkaline pH (greater than 8.5)Competing anions (e.g., phosphateKnown processesEmerging processesChange in ionic composition Aquifer compression with pumping

5. Orange County Water DistrictNon-oxidative Release of Low-Arsenic Strata

6. Modes of Recharge

7. Post-Treatment Infiltration

8. YearMonitoring Well Arsenic

9. Cation bridging is key to arsenic retentionCa2+HAsO42-

10. Destabilized Arsenic with Purified WaterFakhreddine et al., EST 2015

11. Direct Injection to Confined AquifersFakhreddine, 2018

12.

13. Direct Injection to Confined AquifersFakhreddine, 2018

14. Pumping and Aquifer Compression

15. Arsenic Release From Clay Pore-Water with Aquifer Compression

16. Tulare Basin SubsidenceSmith, Knight, Fendorf, Nature Com. 2018

17. As (mg/L)10>100Arsenic Release with Groundwater Pumping

18. Groundwater Cr(VI) Concentrations

19. Industrial SourcedGroundwaterCr(VI)Geogenic Cr(VI)Cr(VI) Contamination of California Groundwater

20. 50 micronschromite grains(Fe0.46Mg0.52)(Cr0.61Al0.29Fe0.10)2O4FeCr2O4(s) + 7/2MnO2(s) + 5H+ = 2HCrO4-(aq) + Fe(OH)3(am) + 7/2Mn2+(aq)  Chromite OxidationOze et al., PNAS 2007

21. CONTRIBUTORS and COLLABORATORS Sarah Fakhreddine Debra Hausladen Ryan Smith Chris Oze Laura Erban Jason Dadakis, OCWD Steve Gorelick Rosemary Knight

22.

23. Cr(VI) Generation from Native Cr(III) Minerals

24.

25. 50 micronschromite grains(Fe0.46Mg0.52)(Cr0.61Al0.29Fe0.10)2O4FeCr2O4(s) + 7/2MnO2(s) + 5H+ = 2HCrO4-(aq) + Fe(OH)3(am) + 7/2Mn2+(aq)  Chromite OxidationOze et al., PNAS 2007

26.

27. Cr(OH)3MnO2Cr – Mn Separation Distance is Key to Cr(VI)

28. Deposition of MnO2 Proximal to Cr(OH)3

29.

30.

31. Cr(III) Oxidation: Mn-oxide DependentCr(OH)3 (s)+ 2H+ Cr(OH)2+ + 2H2O DissolutionOxidationCr(OH)2+ + 2MnO2 + 3H+ HCrO4- + 2Mn2++ 2H2O Oze et al., PNAS 2007

32. California Groundwater Chromium(VI)

33. Arsenic in Lower Mekong Delta -- VietnamErban et al. PNAS 2013

34. Shallow vs Deep Aquifer Arsenic

35. Erban et al. EST 2014Shallow vs Deep Aquifer Arsenic

36. Deep Aquifer Arsenic and Pumping Erban et al., PNAS 2013

37. Pumping Induced Land Subsidence

38. Release PathwaysOxidation-ReductionCr(III) (s)  Cr(VI) (aq)Se(0)/S(-II) (s)  Se(VI) (aq)U(IV) (s)  U(VI) (aq)Oxidative (Aerobic) ReleaseAs(V) (s)  As(III) (aq)Reductive (Anaerobic) Release