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Sediment quality assessment criteria:
new approaches and views
M. Sprovieri, N. Sabatino, M.C. Lombardo, M. Sammartino, D. Valenti
IAS-CNR, Italy ([email protected]) University of Palermo, Italy
11th International SedNet Conference, 3-5 April 2019 Dubrovnik, Croatia
ENVIRONMENTAL RISK ASSESSMENT
Environmental Risk Assessment (ERA), including sediment assessment, is a COMPREHENSIVE approach to support decision making in the regulatory context, and covers a wide spatial set of situations under very different regulatory contexts
MY TODAY’S JOB…
It is a question of interfaces
Where the EqP model coupled to BLM, WHAM and speciation models fail
A quick glance on the complexity of the environment
Ecotoxicology under pressure
Dynamics vs thermodynamics vs kinetics
Proposal of a systemic approach: toxicity as an emergent property
PROCESSES AT THE INTERFACE
A GIANT PROBLEM OF CHEMISTRY AT THE INTERFACES
ECOTOXICOLOGY AND CHEMICAL SPECIATION: A GLANCE AT THE BOUNDARY
THE SEDIMENT PUZZLE
Porewater – Org
Partitioning to pore water
MnO2 – M = POC – Corg FeOOH – M
Binding to sediment phases
Ξ POC – M
H2S/FeS/FeS2 (sulfides)
Porewater – Mn+
Partitioning to pore water
MnO2
Fe3+/Fe(OH)3/FeOOH
Mn2+
FeS + M2+ MS + Fe2+
Reaction with AVS
Oxic
Sub-oxic
Anoxic
SEDIMENT
BIOAVAILABILITY…A CHALLANGE IN ITSELF
Equilibrium Partitioning [EqP] model (Di Toro et al., 2005) for metals Simultaneously Extracted Metals [SEM] (Di Toro et al., 2005) Acid Volatile Sulphide [AVS] Organic Carbon Fe,Mn hydroxide Grain Size
Equilibrium Partitioning [EqP] model (Di Toro et al., 2005) for POPs Grain size Organic Carbon Black carbon Aging
SEM = AVS + FOCKOCCW + Kd(a+b[FeOx+MnOx])
EqP-MODEL FOR METALS
AN OPERATIONAL APPROACH
SEM = AVS + FOCKOCCW
AVS, SEM… DEFINITIONS AT WORK
AVS= FeSmackinawite+FeSgreigite+FeSaquo+FeSclusters + …
FOCKOCCW
Kd(a+b[FeOx+MnOx])
SEM= [Ni]+[Cd]+[Zn]+[Sn]+[Ag]+[Hg]; Ksp>Ksp, Pyrite
FeS and Fe3S4 minerals have rarely been reported from marine sediments
The measurement of AVS-S cannot be related directly to any particular sulfide component in a sediment
Analytical protocols for AVS-S vary considerably and are entirely empirical. Different protocols leach different amount of AVS materials
AVS-S is not equivalent to FeS-S Pore water analyses will include filter-passing,
nanoparticulate solids as well as clusters and complexes Pyrite-S contributes to AVS-S and analytical protocols
cannot be assumed to separate S(-II) components from pyrite-S
The effects of sample handling on measurements of AVS-S have not been quantified
A DEEP GLANCE TO THE AVS PROBLEM
SEM = FeS + FOCKOCCW + Kd(a+b[FeOx+MnOx])
BIOAVAIL. = SEM + Σi fOC Ki,OC FCVi + EXTRA-M
POPs [MeHg] N-SEM EXTRA-M
Sediment Transport
Biotic Ligand Model
Toxicity Production
HydrodinamicTransport
O Carbon Production
Water Effects Ratio
Food Chain
Chemicals Fate and Transport
Biotic Sediments Accumulation
ratio
Ecological Risk Assessment
…BY THE WAY, THE SYSTEM IS COMPLEX AND HIGHLY DYNAMIC
Ecotoxicology (mainly bioassays) under pressure…
An integrated view of processes…no system understanding
A static view of sediments: (thermo)dynamics vs kinetics
A black-box of responses: limited understanding of dynamic chemical processes at the sediment interfaces
Only a “linear” exploration of COMPLEXITY
False positives and negatives obscure/hide complexity
NEED OF A MUCH MORE DEEPER LEARNING
Improved biogeochemistry and system non-linear responses
Dynamics vs Stable conditions
Improved scientific handling of environmental variables
An integrated view of processes
Complexity vs linearity
From a linear and/or combined view of pollutants behaviour, multiple physical parameters of sediments and aquatic/biotic interfaces to… a systemic approach
Analysis of emergent properties of the whole chemical-physical and ecological system rather than of any or a simple addition of its components
COMPLEX SYSTEM AND EMERGENT PROPERTIES
Properties of the system as a whole rather than properties that can be derived from the properties of components of a system
Emergent properties are a consequence of the relationships between system components
They can therefore only be assessed and measured once the components have been integrated into a system
EMERGENT PROPERTIES
Properties of the Whole vs. Properties of the Parts
Sum of the Actions Product of Interactions
BIOAVAILABILITY/TOXICITY EMERGENT PROPERTY OF A COMPLEX SYSTEM
MINERALOGY AND DYNAMICS OF PHYSICAL AND CHEMICAL
PARAMETERS
GEOCHEMISTRY AT WORK
A FIRST EXAMPLE OF AN APPROACH IN TERMS OF A COMPLEX/DYNAMIC SYSTEM
Fe(OH)3 + 3H+ = Fe2+ + 3H2O Fe2+ + ¼ O2 +2OH- + 1/2 H2O = Fe(OH)3 FeS + H2S = FeS2 + H2 FeS2 + H+ = Fe2+ +HS- +S0 FeS2 + 8H2O + 14Fe3+ = 15Fe2+ + 2SO4
2- + 16H+ FeS2 + H2O + 7/2O2 = Fe2+ + 2SO4
2- + 4H+ Fe2+ + HS- = FeSH+ Fe2+ + H2S = FeS + 2H+ FeS + 2 H+ = Fe2+ + H2S FeS +H+ = Fe2+ + HS-
BASIC SYSTEM OF EQUATIONS
BASIC SYSTEM OF EQUATIONS
SO42− + 10H+ ka
−−! H2S+ 4H2O
SO42− + 9H+ kb
−−! HS− + 4H2O
HS− + H+ kc−−! H2S
Fe2+ + 14O2 + 2OH− + 1
2H2O
k1−−! Fe(OH)3
FeS+ H2Sk2
−−! FeS2 + H2
FeS2 + H+ k3 −− Fe2+ + HS− + S0
FeS2 + H2O + 72O2
k4−−! Fe2+ + 2SO4
2− + 4H+
Fe2+ H2Sk5
−−*) −−k− 5
FeS+ 2H+
SO42− + 10H+ ka
−−! H2S+ 4H2O
SO42− + 9H+ kb
−−! HS− + 4H2O
HS− + H+ kc−−! H2S
Fe2+ + 14O2 + 2OH− + 1
2H2O
k1−−! Fe(OH)3
FeS+ H2Sk2
−−! FeS2 + H2
FeS2 + H+ k3 −− Fe2+ + HS− + S0
FeS2 + H2O + 72O2
k4−−! Fe2+ + 2SO4
2− + 4H+
Fe2+ H2Sk5
−−*) −−k− 5
FeS+ 2H+
SO42− + 10H+ ka
−−! H2S+ 4H2O
SO42− + 9H+ kb
−−! HS− + 4H2O
HS− + H+ kc−−! H2S
Fe2+ + 14O2 + 2OH− + 1
2H2O
k1−−! Fe(OH)3
FeS+ H2Sk2
−−! FeS2 + H2
FeS2 + H+ k3 −− Fe2+ + HS− + S0
FeS2 + H2O + 72O2
k4−−! Fe2+ + 2SO4
2− + 4H+
Fe2+ H2Sk5
−−*) −−k− 5
FeS+ 2H+
SO42− + 10H+ ka
−−! H2S+ 4H2O
SO42− + 9H+ kb
−−! HS− + 4H2O
HS− + H+ kc−−! H2S
Fe2+ + 14O2 + 2OH− + 1
2H2O
k1−−! Fe(OH)3
FeS+ H2Sk2
−−! FeS2 + H2
FeS2 + H+ k3 −− Fe2+ + HS− + S0
FeS2 + H2O + 72
O2k4
−−! Fe2+ + 2SO42− + 4H+
Fe2+ H2Sk5
−−*) −−k− 5
FeS+ 2H+
SO42− + 10H+ ka
−−! H2S+ 4H2O
SO42− + 9H+ kb
−−! HS− + 4H2O
HS− + H+ kc−−! H2S
Fe2+ + 14O2 + 2OH− + 1
2H2O
k1−−! Fe(OH)3
FeS+ H2Sk2
−−! FeS2 + H2
FeS2 + H+ k3 −− Fe2+ + HS− + S0
FeS2 + H2O + 72
O2k4
−−! Fe2+ + 2SO42− + 4H+
Fe2+ H2Sk5
−−*) −−k− 5
FeS+ 2H+
SO42− + 10H+ ka
−−! H2S+ 4H2O
SO42− + 9H+ kb
−−! HS− + 4H2O
HS− + H+ kc−−! H2S
Fe2+ + 14
O2 + 2OH− + 12H2O
k1−−! Fe(OH)3
FeS+ H2Sk2
−−! FeS2 + H2
FeS2 + H+ k3 −− Fe2+ + HS− + S0
FeS2 + H2O + 72
O2k4
−−! Fe2+ + 2SO42− + 4H+
Fe2+ H2Sk5
−−*) −−k− 5
FeS+ 2H+
SO42− + 10H+ ka
−−! H2S+ 4H2O
SO42− + 9H+ kb
−−! HS− + 4H2O
HS− + H+ kc−−! H2S
Fe2+ + 14O2 + 2OH− + 1
2H2O
k1−−! Fe(OH)3
FeS+ H2Sk2
−−! FeS2 + H2
FeS2 + H+ k3 −− Fe2+ + HS− + S0
FeS2 + H2O + 72O2
k4−−! Fe2+ + 2SO4
2− + 4H+
Fe2+ H2Sk5
−−*) −−k− 5
FeS+ 2H+
SO42− + 10H+ ka
−−! H2S+ 4H2O
SO42− + 9H+ kb
−−! HS− + 4H2O
HS− + H+ kc−−! H2S
Fe2+ + 14O2 + 2OH− + 1
2H2O
k1−−! Fe(OH)3
FeS+ H2Sk2
−−! FeS2 + H2
FeS2 + H+ k3 −− Fe2+ + HS− + S0
FeS2 + H2O + 72
O2k4
−−! Fe2+ + 2SO42− + 4H+
Fe2+ H2Sk5
−−*) −−k− 5
FeS+ 2H+
1)
3)
4)
5)
8)
2)
6)
7)
k = 1040
k = 1033
k = 107
kcin = 1.5*1013 l2 mol-2 atm-1 min-1
k = 106.1 Kcin = 1.03 * 10-4 l mol-1s-1
Ksp = 10-16.4 Kcin = 1 * 10-7.52 mol m-2 s-1
kcin = 10-10 mol m-2 s-1
K =10– 3.7 kcin= 7 l mol-1 s-1
x1(t) = [F e2+ ] x2(t) = [F eS] x3(t) = [F eS2]
x4(t) = [H2S] x5(t) = [H S− ]
8>>>>>>>>>>>>>>>>>>>>>>>><
>>>>>>>>>>>>>>>>>>>>>>>>:
dx1
dt= C − k1
A
[H + ]2[O2]
1/ 4[H2O]1/ 2x1 + k− 5[H+ ]2x2 + k4[H2O][O2]
7/ 2x3
− k5x1x4 − k3[S0] x1x5,
dx2
dt= − k2x2x4 + k5x1x4 − k− 5[H
+ ]2 x2
dx3
dt= k2x2x4 + k3[S
0] x1x5 − k4[H2O][O2]7/ 2 x3
dx4
dt= − k2x2x4 − k5x1x4 + k− 5[H
+ ]2 x2 + kc[H+ ] x5 + ka[SO2−
4 ] [H + ]10
dx5
dt= − k3[S
0] x1x5 − kc[H+ ] x5 + kb[H
+ ]9 [SO2−4 ]
DYNAMICAL
SYSTEM
Non-linear system, continuous and converging towards attractors. System stable at various conditions
Trajectories of the different species in the Eh-pH stability field are well-described and quantified
We can calculate the buffer (complexing) capacity of the FexSy system
Need of field-tests to verify theory
SPECIFIC FEATURES OF THE SYSTEM
Eh(V
) [FexSy] (mmol)
Av. Metals
1x10-3 3x10-3 2x10-3 5x10-3 4x10-3 0 8x10-3 6x10-3 7x10-3
FEXSY NORMALIZATION
SEDIMENT AVAILABLE CADMIUM (mmol/mmol FeS)
MO
RTA
LITY
(%
)
Eh=-0,5V Eh=-0,2V
…MY TAKE HOME MESSAGE… We must re-think our approach to evaluation of
sediments bioavailability/toxicity in terms of complex system and biogeochemical dynamics. Non linear addition of “pieces” but approaches to emergent properties
Eh, pH, O2 (physics) dominate dynamics of [Fe, S, OC,FE/Mn hydroxides] chemistry in sediments: we need new and more “conservative” sampling methods
Dynamics dominate stable conditions…this is complexity at work
Ecotoxicity needs a deeper understanding of biogeochemical dynamics of pollutants in seds
Thanks for your attention!