Danny Reible y The University of Texas at Austin Biogeochemistry - - PowerPoint PPT Presentation
Danny Reible y The University of Texas at Austin Biogeochemistry - - PowerPoint PPT Presentation
Danny Reible y The University of Texas at Austin Biogeochemistry beneath the cap Active Capping Permeable adsorptive barrier A ti C i P bl d ti b i Material Options Management of upwelling water /gas/NAPL M t f lli t
Biogeochemistry beneath the cap
A ti C i P bl d ti b i
Active Capping‐ Permeable adsorptive barrier
Material Options M t f lli t / /NAPL Management of upwelling water /gas/NAPL Effectiveness of materials Placement of materials Placement of materials Capping design‐ modeling
Monitoring Cap Performance
Monitoring Cap Performance
Definition of Cap Objectives
M t l ft ff ti l t i d b ti l
Metals often effectively contained by a conventional cap AVS vs. SEM‐ Capping will enhance reducing conditions
SEM
>
AVS
‐1 10 20 30 40
Salt Zn2+(ppb)
Metals will not be toxic M2+ + FeS(s) → MS(s) + Fe2+
1 2 3 Depth (cm)
SEM
<
AVS
Divalent metals may be
3 4 5 6 Sediment D
3
Divalent metals may be toxic
7 8
Conceptual Model
Pre-Cap Post-Cap
F OOH O2 O2 O2 FeOOH FeOOH FeOOH SO4
2-
Methyl mercury
SO4
2-
Methyl mercury
Mobility and toxicity generally not redox sensitive
D d ti i d iti
Degradation is redox sensitive
Hydrocarbon degradation facilitated aerobically Chl i t d i d ti l d hl i t b t Chlorinated organics reductively dechlorinate but many sediment contaminants refractory
Dynamics controlled by sorption in cap and Dynamics controlled by sorption in cap and
groundwater upwelling
Potentially greater effectiveness than with sand can
be achieved with “active” or amended caps
Encourage fate processes such as sequestration or degradation of contaminants beneath cap Discourage recontamination of cap g p
Feasible if high value components are placed in thin
layer in a controllable manner
Effective if time/capacity of active cap sufficient to Effective if time/capacity of active cap sufficient to
manage finite mass of contaminants
Significant stakeholder acceptance advantage
g p g
Permeability Control
Discourage upwelling through contaminated sediment b di i d fl by diverting groundwater flow
Contaminant Migration Control
Sl t i t i ti t i ll th h Slow contaminant migration, typically through sorption related retardation
Contaminant Degradation Aid Contaminant Degradation Aid
Less well developed, contaminant specific but designed to encourage contaminant fate processes
Clays for permeability control
Demonstrated
Clays for permeability control Activated Carbon or other carbon sequestration agent Organoclays for NAPL control & some dissolved control
Significant swelling and permeability reduction with NAPL Significant swelling and permeability reduction with NAPL
Clay and sequestration agent mixtures Phosphate additives for metals
k h h d d Rock phosphate (i.e. apatite) demonstrated
Iron Sulfide for Hg and MeHg control Siderite (FeCO3) for pH control Zero valent iron Oxygen or hydrogen release compounds/technologies Biopolymers Biopolymers Electrochemical controls on redox conditions
Speculative
C i ll il bl
Commercially available
AquaBlok B t t Bentomat HDPE
C f ll di t d t lli
Can successfully divert groundwater upwelling
Where will the groundwater go? Pl f l i d l Plan for gas accumulation and release Long term effectiveness in the face of gas/tidal dynamics? dynamics?
pH
Siderite
11 12 13
Vlassopoulos and Serrano, 2008
Siderite Ferrous Sulfate Alum
8 9 10
pH
Metals
Apatite
5 6 7
Available FeCO3 ~ 2 g/cm of layer thickness/cm2 2 cm/yr upwelling = 1000 years of pH protection
Iron Sulfide
Organics
.5 1 1.5 2 4 5
FeCO3 reacted (g/L) y p g y p p
Organoclay Activated carbon
NAPL present ‐ Organoclays
Capacity of O(1 g NAPL/g organoclay) Placement within a laminated mat for residual NAPL or to allow replacement if capacity exceeded Placement in bulk for significant NAPL volumes Placement in bulk for significant NAPL volumes Multiple organoclay layers or organoclay/activated carbon layer for both NAPL and dissolved contaminant control
l d l d b
Dissolved contaminants only ‐ Activated carbon
Placement in mat may be necessary to allow easy placement Placement as amendment also possible Placement as amendment also possible Activated carbon typically more subject to fouling than
- rganoclay
1.E+06
- n µg/kg
Hg (PM199)
y = 6920.9x0.7212 R² = 0.9516 1.E+04 1.E+06 Hg Concentratio Hg (PM199) 1.E+00 1.E+02 0.001 0.1 10 1000 Sorbed H Power (Hg (PM199))
Special Hg formulations exist
Hg Water Phase Concentration, µg/L
Spec a g o u a o s e s Conventional formulations may be similarly effective if Hg complexed with suspended
Hg (MRM)
Hg complexed with suspended
- rganic matter
y = 9417.7x0.6709 R² = 0.935 1 E+04 1.E+06 ation µg/kg 1.E+02 1.E+04 ed Hg concentra Hg (meas) Power (Hg (meas)) 1.E+00 0.001 0.1 10 1000 Sorb Hg concentration µg/L
100 mg/g 10 ncentration AC Site 1/10 1 ediment con AC Lab OC Site OC Lab 1/100 2 4 6 8 10 12 Se Water Concentration mg/L
50 60 70 n mg/g 30 40 50
- ncentration
AC Site
10 20 Sediment co
OC Site OC Lab
2 4 6 8 10 12 S Water Concentration mg/L Water Concentration mg/L
– Expect bioavailability reduction proportional to – Expect bioavailability reduction proportional to porewater concentration (inversely proportional to partition coefficient, Kd) – Equivalent sand cap thickness – diffusion/dispersion q p p dominated (u<<1 cm/day)
~
active
d active eff active active
K R L L L R K =
sand
ff sand d
R K
~ 10-4 Koc 0.01Koc focKoc ~ 100Koc Log Kd ~ 1-10Koc
f
16
foc ~ 0.01‐0.05
ACTIVE CAP DESIGN MODEL
To Appear Journal of Soil and Sediment Contamination – Summer 2009
including steady state design model from Lampert and Reible (2009)* Version 3.13 2/9/2008 Instructions: This spreadsheet determines concentrations and fluxes in a sediment cap at steady-state worksheet 1), unsteady state (worksheet 2), assuming advection, diffusion, dispersion, bioturbation, deposition/erosion, sorption onto ll id l i tt d b d l t f A ti l ith h d ti i id d b colloidal organic matter, and boundary layer mass transfer. An active cap layer with enhanced sorption is considered by converting to an equivalent conventional cap thickness. Depth is defined from the cap-water interface. A constant deposition rate can be entered but is not allowed to result in a net contaminant velocity <0 (relative to the changing cap-water interface) . The cells in blue are input cells; these can be changed for the design of interest. DO NOT CHANGE THE CELLS IN RED (or the spreadsheet will not function properly). A second worksheet calculates the transient profiles for a semi-infinite case. The third worksheet title "array" allows the user to create an array of outputs for a given input (e.g. to study different compounds for a given site) Contaminant Properties Contaminant Chlorobenzene Organic carbon partition coefficient, log K oc 2.52 log L/kg Colloidal organic carbon partition coefficient, log K DOC 2.15 log L/kg W t diff i it D 6 0E 06 cm2/s a given site).
0.00 10.00
Transient Concentration Profiles
Cap-Water Interface Bioturbation Layer Bioturbation Layer
Water diffusivity, D w 6.0E-06 cm /s Cap decay rate (porewater basis), λ 1 0.00 yr-1 Bioturbation layer decay rate (porewater basis), λ 2 0.00 yr-1 Sediment/Bioturbation Layer Properties Contaminant pore water concentration, C0 1 ug/L
20.00 30.00 40.00 50.00 Depth, cm
Series13 2 1.21E-11 1.0E+00 2.0E+00 3.0E+00 4.0E+00 5.0E+00 6 0E+00
Effective Cap Layer y Containment Layer
g Biological active zone fraction organic carbon, (f oc ) bio 0.05 Colloidal organic carbon concentration, ρ DOC 10 mg/L Darcy velocity, V 2 cm/yr Depositional velocity, V dep 0 cm/yr Bioturbation layer thickness, h bio 10 cm
60.00 70.00 0.00 0.20 0.40 0.60 0.80 1.00 Dimensionless Concentration
6.0E+00 7.0E+00 8.0E+00 9.0E+00 1.0E+01 Infinity
Underlying Sediment Underlying Sediment
Spreadsheet model
Transient model until penetration of chemical isolation layer Transient model until penetration of chemical isolation layer Steady state model (bioturbation &isolation layer) Variant for additional active cap layer‐ transient and ss p y
Numerical model
Matlab version Matlab version Multiple layers, nonlinear sorption, finite source
Available at http://www caee utexas edu/reiblegroup/ Available at http://www.caee.utexas.edu/reiblegroup/
|Performance Measures
Manag ing Co ntaminatio n
- I
so latio n o f c o ntaminate d se dime nt- Cap stability? E li i ti f di t i C
t bilit ?
Manag ing Co ntaminatio n
- E
liminatio n o f se dime nt re suspe nsio n – Cap stability?
- Re duc tio n in c o ntaminant flux to wate r – F
lux?
- Re duc tio n in c o ntaminant ac c umulatio n in be nthic
- Re duc tio n in c o ntaminant ac c umulatio n in be nthic
- rg anisms- F
lux? Co ntaminant iso latio n? Bio ac c umulatio n?
Thi L C i Thi k L C i Thin Layer Capping Thick Layer Capping vs.
T hin L aye r Cap T hic k L aye r Cap
Percent Sediment and Phen C/C
0versus Depth
15 17 Cap sediment Intermixing Zone 19 21
(cm)
Phenanthrene % Sediment
Clean Sand Cap Cap-sediment Intermixing Zone 23 25
Depth
Sediment 27 29 29 0% 50% 100% 150%
C/C0 and Percent Passing
lk d l f l d f
Bulk sediment concentration is less useful as indicator of
exposure‐risk i b d
Porewater concentration is better indicator
(even for active benthic uptake by ingestion) ff
Porewater is difficult to measure, but possible with solid
phase micro extraction (SPME)
21
Field deployable SPME, capable of measuring porewater with vertical resolution
PAH B(b)F B(k)F B P i M li t
35
PAH Tissue Correlation with Pore Water Concentration (0-7 cm)
35
PAH Tissue Correlation with TOC NormalizedSediment Concentration
PAHs – B(b)F, B(k)F, BaP in Muscalista
R² = 0.8723
10 15 20 25 30
entration (ug/kg)
R² = 0.2703
10 15 20 25 30
entration (ug/kg)
5 10 0.0 1.0 2.0 3.0 4.0
Tissue Conce Pore Water Concentration (ng/L)
5 10 5000 10000 15000 20000 25000 30000
Tissue Conce Sediment Concentration (ng/g)
Single correlation with porewater concentrations works well for all three compounds Single correlation with porewater concentrations works well for all three compounds
|T hin L aye r Capping |
4-c m Sand Cap 4-c m Sand Cap
Day 28 Day 0
|L abo rato ry Studie s o f T hin L aye r Capping
4-c m Sand Cap
Day 28 Day
Capping Performance Capping Performance
B[a]A Pore Water Concentrations
Capping Performance Capping Performance
- 4
Pore Water Concentration (ng/L)
Overlying Water
- 2
0.00 1.00 2.00 3.00 4.00 5.00 6.00 7.00 8.00 9.00 10.00 2 Depth (cm) ACS 0cm 2cm 4cm 4 D 6cm 6 8
25
Thin Layer Capping to Manage Thin Layer Capping to Manage Residuals Residuals Residuals Residuals
Pyrene Concentrations in Worm Tissue Overlying Water
12000 14000 8000 10000 12000
g)
4000 6000
C (ng/
2000
All Contaminated Sediment 0cm 2cm 4cm 6cm 10cm Sediment Depth of Cap
26
9000 7000 8000 9000 4000 5000 6000 /f l (ppb) Phenanthrene Chrysene B(a)A B(b)F 2000 3000 4000 C t / (b) B(k)F B(a)P 1 1.04 1 1000 1000 2000 3000 4000 5000 6000 7000 CpwKow (ppb)
Unit slope is BSF estimated by Kow
27
Conventional sand caps easy to place and effective
Conventional sand caps easy to place and effective
Contain sediment Retard contaminant migration g Physically separate organisms from contamination
There are existing and developing alternatives when a
conventional cap is not sufficiently protective
Permeability Control Adsorptive Caps
Porewater concentrations /profiles can be an effective