simulation of potentially toxic elements (ptes) transport in stormwater management ... ·...
TRANSCRIPT
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Simulation of potentially toxic elements (PTEs) transport in stormwater management
practices (SMPs)
October 2019
Ali Behbahani, Robert Ryan, Erica McKenzie
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INTRODUCTION
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• Rainfall surface runoff water resource quantity (flooding, erosion)
• Control stormwaterquality (hazards to water resources and media)
• Stormwater management practice (SMP); infiltration into soil, vegetative cover
- design parameters: hydrological data, loading ratio, soil type (Kd), vegetative cover
PTEs ; daily usage, non-degradable
https://stormwater.pca.state.mn.us/index.php?title=File:Sand_filter_credit_article.jpg
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LOADING RATIO (LR)
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• 𝐥𝐥𝐥𝐥𝐥𝐥𝐥𝐥𝐥𝐥𝐥𝐥𝐥𝐥 𝐫𝐫𝐥𝐥𝐫𝐫𝐥𝐥𝐥𝐥 = 𝐥𝐥𝐫𝐫𝐥𝐥𝐥𝐥𝐥𝐥𝐥𝐥𝐥𝐥𝐝𝐝 𝐥𝐥𝐫𝐫𝐝𝐝𝐥𝐥𝐥𝐥𝐥𝐥𝐢𝐢𝐥𝐥𝐥𝐥𝐫𝐫𝐫𝐫𝐥𝐥𝐫𝐫𝐥𝐥𝐥𝐥𝐥𝐥 𝐥𝐥𝐫𝐫𝐝𝐝𝐥𝐥
• Maximum LRs of 8, 8, and 5 are recommended in Pennsylvania, Delaware, and Michigan, respectively.
• LR effect on water quality is rarely studied as a designing parameter
Caplan et al., 2018
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ADSORPTION COEFFICIENT
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• 𝑲𝑲𝒅𝒅 𝒂𝒂𝒂𝒂 𝒂𝒂𝒅𝒅𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂 𝒄𝒄𝒂𝒂𝒄𝒄𝒄𝒄𝒄𝒄𝒂𝒂𝒄𝒄𝒂𝒂𝒄𝒄𝒂𝒂𝒂𝒂(PTEs partitioning between aqueous and solid phases)
• Highly case-dependent
• PTE adsorption coefficient in soil depends mostly on
- pH- organic matter content- metal type- PTE concentration - type of soil- Cationic exchange capacity http://www.personal.psu.edu/faculty/a/s/asm4/turfgrass/education/turge
on/lessons/lesson13/corefiles/links/pestdanger/ad1.html
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OBJECTIVES
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• Assessing breakthrough and accumulation of PTEs in SMPs and how various LR and Kd impact the performance of SMP
• Estimating contamination indices in the porous media (soil) and porewater
• Determining which PTEs have higher priority in terms of imposing contamination
A cluster of metals (Cr, Fe, Cu, Zn, As, Cd, and Pb) and Cl- will be studied.
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METHOD
6
Simulation schematic
inputRainfall record(KPNE weather
station)
Surface contamination
(I95 samples and lognormal
distribution)
Soil characteristics
output
PTE Conc in porewater
PTE Conc in soil
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METHOD
7
Computational process
A) water transport
• To determine the water content at each time and depthinfiltration rate is assumed equal to saturated hydraulic conductivity
f infiltration rate (L/T), K is saturated hydraulic conductivity (L/T)
Insignificant impact owing to equilibrium adsorption model (independent of contact time)
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METHOD
8
𝑪𝑪𝑺𝑺 = 𝑲𝑲𝒅𝒅𝑪𝑪𝑾𝑾
𝒎𝒎𝒂𝒂𝒂𝒂𝒂𝒂 𝒄𝒄𝒂𝒂𝒂𝒂𝒄𝒄𝒂𝒂𝒂𝒂𝒂𝒂𝒆𝒆 𝒂𝒂𝒕𝒕𝒄𝒄 𝒄𝒄𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒄𝒄 𝒖𝒖𝒂𝒂𝒂𝒂𝒂𝒂 = [𝑪𝑪𝑾𝑾𝑾𝑾× 𝑽𝑽] + [𝑪𝑪𝑺𝑺𝑾𝑾 × 𝑴𝑴𝒂𝒂]𝒎𝒎𝒂𝒂𝒂𝒂𝒂𝒂 𝒄𝒄𝒆𝒆𝒂𝒂𝒂𝒂𝒂𝒂𝒆𝒆 𝒂𝒂𝒕𝒕𝒄𝒄 𝒄𝒄𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒄𝒄 𝒖𝒖𝒂𝒂𝒂𝒂𝒂𝒂 = [𝑪𝑪𝑾𝑾𝒄𝒄× 𝑽𝑽] + [𝑪𝑪𝑺𝑺𝒄𝒄 × 𝑴𝑴𝒂𝒂]
Mass balance: 𝑪𝑪𝑾𝑾𝑾𝑾 × 𝑽𝑽 + 𝑪𝑪𝑺𝑺𝑾𝑾 × 𝑴𝑴𝒂𝒂 = 𝑪𝑪𝑾𝑾𝒄𝒄 × 𝑽𝑽 + 𝑲𝑲𝒅𝒅𝑪𝑪𝑾𝑾𝒄𝒄𝑴𝑴𝒂𝒂
𝑪𝑪𝑾𝑾𝒄𝒄 =𝑪𝑪𝑾𝑾𝑾𝑾 × 𝑽𝑽 + 𝑪𝑪𝑺𝑺𝑾𝑾 × 𝑴𝑴𝒂𝒂
𝑲𝑲𝒅𝒅𝑴𝑴𝒂𝒂 + 𝑽𝑽& 𝑪𝑪𝑺𝑺𝒄𝒄 = 𝑲𝑲𝒅𝒅𝑪𝑪𝑾𝑾𝒄𝒄
𝐶𝐶𝑊𝑊𝑊𝑊 :𝑃𝑃𝑃𝑃𝑃𝑃 𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐 𝑐𝑐𝑐𝑐 𝑝𝑝𝑐𝑐𝑐𝑐𝑐𝑐 𝑤𝑤𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑚𝑚𝑚𝑚𝐿𝐿 𝑐𝑐𝑐𝑐 𝑐𝑐𝑡𝑐𝑐 𝑐𝑐𝑐𝑐𝑒𝑒 𝑐𝑐𝑜𝑜 𝑐𝑐𝑐𝑐𝑚𝑚𝑐𝑐𝑡𝑡: 𝑠𝑠𝑐𝑐𝑐𝑐𝑐𝑐𝑚𝑚𝑤𝑤𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐 𝑐𝑐𝑟𝑟𝑐𝑐𝑐𝑐𝑜𝑜𝑜𝑜 𝑣𝑣𝑐𝑐𝑣𝑣𝑟𝑟𝑚𝑚𝑐𝑐 𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑚𝑚 𝑐𝑐𝑡𝑐𝑐 𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑐𝑣𝑣 𝑣𝑣𝑐𝑐𝑣𝑣𝑟𝑟𝑚𝑚𝑐𝑐 𝑒𝑒𝑟𝑟𝑐𝑐𝑐𝑐𝑐𝑐𝑚𝑚 𝑐𝑐𝑐𝑐𝑚𝑚𝑐𝑐 𝑠𝑠𝑐𝑐𝑐𝑐𝑝𝑝 (𝐿𝐿)
𝑪𝑪𝑺𝑺𝑾𝑾:𝑷𝑷𝑷𝑷𝑷𝑷 𝒄𝒄𝒂𝒂𝒂𝒂𝒄𝒄𝒄𝒄𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂 𝒂𝒂𝒂𝒂 𝒂𝒂𝒕𝒕𝒄𝒄 𝒂𝒂𝒂𝒂𝒂𝒂𝒄𝒄𝒎𝒎𝒆𝒆𝑲𝑲𝒆𝒆 𝒂𝒂𝒂𝒂 𝒂𝒂𝒕𝒕𝒄𝒄 𝒂𝒂𝒂𝒂𝒂𝒂 𝒂𝒂𝒄𝒄 𝒄𝒄𝒂𝒂𝒍𝒍𝒄𝒄𝒂𝒂
𝑪𝑪𝑺𝑺𝒄𝒄:𝑷𝑷𝑷𝑷𝑷𝑷 𝒄𝒄𝒂𝒂𝒂𝒂𝒄𝒄𝒄𝒄𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂 𝒂𝒂𝒂𝒂 𝒂𝒂𝒕𝒕𝒄𝒄 𝒂𝒂𝒂𝒂𝒂𝒂𝒄𝒄𝒎𝒎𝒆𝒆𝑲𝑲𝒆𝒆 𝒂𝒂𝒂𝒂 𝒂𝒂𝒕𝒕𝒄𝒄 𝒃𝒃𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒎𝒎 𝒂𝒂𝒄𝒄 𝒂𝒂𝒕𝒕𝒄𝒄 𝒄𝒄𝒂𝒂𝒍𝒍𝒄𝒄𝒂𝒂
𝑪𝑪𝑾𝑾𝑾𝑾:𝑷𝑷𝑷𝑷𝑷𝑷 𝒄𝒄𝒂𝒂𝒂𝒂𝒄𝒄𝒄𝒄𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂 𝒂𝒂𝒂𝒂 𝒂𝒂𝒂𝒂𝒂𝒂𝒄𝒄 𝒘𝒘𝒂𝒂𝒂𝒂𝒄𝒄𝒂𝒂𝒎𝒎𝒆𝒆𝑳𝑳 𝒂𝒂𝒂𝒂 𝒂𝒂𝒕𝒕𝒄𝒄 𝒂𝒂𝒂𝒂𝒂𝒂 𝒂𝒂𝒄𝒄 𝒄𝒄𝒂𝒂𝒍𝒍𝒄𝒄𝒂𝒂
𝑪𝑪𝑾𝑾𝒄𝒄:𝑷𝑷𝑷𝑷𝑷𝑷 𝒄𝒄𝒂𝒂𝒂𝒂𝒄𝒄𝒄𝒄𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂 𝒂𝒂𝒂𝒂 𝒂𝒂𝒂𝒂𝒂𝒂𝒄𝒄 𝒘𝒘𝒂𝒂𝒂𝒂𝒄𝒄𝒂𝒂𝒎𝒎𝒆𝒆𝑳𝑳 𝒂𝒂𝒂𝒂 𝒃𝒃𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒎𝒎 𝒂𝒂𝒄𝒄 𝒂𝒂𝒕𝒕𝒄𝒄 𝒄𝒄𝒂𝒂𝒍𝒍𝒄𝒄𝒂𝒂
𝑲𝑲𝒅𝒅:𝒂𝒂𝒅𝒅𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂 𝒄𝒄𝒂𝒂𝒄𝒄𝒄𝒄𝒄𝒄𝒂𝒂𝒄𝒄𝒂𝒂𝒄𝒄𝒂𝒂𝒂𝒂𝑳𝑳𝑲𝑲𝒆𝒆
𝑴𝑴𝑺𝑺: 𝒂𝒂𝒂𝒂𝒂𝒂𝒄𝒄 𝒄𝒄𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒄𝒄 𝒖𝒖𝒂𝒂𝒂𝒂𝒂𝒂 𝒎𝒎𝒂𝒂𝒂𝒂𝒂𝒂 𝑲𝑲𝒆𝒆
𝑽𝑽: 𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒎𝒎𝒘𝒘𝒂𝒂𝒂𝒂𝒄𝒄𝒂𝒂 𝒂𝒂𝒖𝒖𝒂𝒂𝒂𝒂𝒄𝒄𝒄𝒄 𝒗𝒗𝒂𝒂𝒄𝒄𝒖𝒖𝒎𝒎𝒄𝒄 𝒄𝒄𝒂𝒂𝒂𝒂𝒄𝒄𝒂𝒂𝒂𝒂𝒂𝒂𝒆𝒆 𝒂𝒂𝒕𝒕𝒄𝒄 𝒄𝒄𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒂𝒄𝒄 𝒗𝒗𝒂𝒂𝒄𝒄𝒖𝒖𝒎𝒎𝒄𝒄 𝒅𝒅𝒖𝒖𝒂𝒂𝒂𝒂𝒂𝒂𝒆𝒆 𝒂𝒂𝒂𝒂𝒎𝒎𝒄𝒄 𝒂𝒂𝒂𝒂𝒄𝒄𝒂𝒂 (𝑳𝑳)
Computational process
B) adsorption
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METHOD
9
Computational process
C) contamination evaluation
• PTE concentration in aqueous and solid phases will be expressed as a ratio of published values• Geometric mean represents the simultaneous consideration of both phases• It is important to decide at what depth / depths, we are interested in evaluations
SCI(soil contamination index) =CsSx
PWCI(porewater contamination index) =CwLx
TCI(total contamination index) = 𝑆𝑆𝐶𝐶𝑆𝑆 × 𝑃𝑃𝑃𝑃𝐶𝐶𝑆𝑆
Porewater contamination index at groundwater table; soil contamination index at soil top layers
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R E S U LT S - P T E T R A N S P O R T
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Complete breakthrough when CwC0
= 1
Assessment of PTE transport using a fixed precipitation and load
Normalized Cl- (representing mobile PTE) porewater concentrations at various depths below the surface for constant precipitation, C0 = 1600 mg/L, LR=8, and Kd = 1 and 10 L/kg
Chloride is highly mobile and readily reaches groundwater (after 1.1 years)
Complete breakthrough after 1.6 years
A higher adsorption coefficient (higher loam or amended soil) resulted in more delay in breakthrough __ complete breakthrough after 14.8 years
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R E S U LT S - P T E T R A N S P O R T
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Normalized porewater concentrations of marginally mobile and significantly immobile PTEs at 5 cm below the surface for LR=8 and the case of constant C0 and precipitation
Metals reach layers lower than 60 cm in trace concentrations
Adsorption coefficient determinative in breakthrough
High accumulation of metals at media top layers
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R E S U LT S – P T E P R I O R I T I Z AT I O N
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PTE Cl- Cr Fe Cu Zn As Cd Pb
PWCI* 4.19 0.41 1.50 17.80 2.21 0.24 0.41 5.28
SCI** 1.15 14.78 0.26 0.01 0.003 1.18 0.18 0.10
TCI*** 2.20 2.46 0.62 0.44 0.08 0.53 0.27 0.73
PTE contamination indices at the top layer (1 to 5 cm below surface) of the basin after 20 years; * porewater contamination index; ** soil contamination index; *** total contamination index
Concern-worthy PTEs : Cr, As, and Cl-
PTE Cl- Cr Fe Cu Zn As Cd PbPWCI* 6.10 4E-6 4.E-22 2.7E-45 4E-20 2E-26 1E-13 1E-68
SCI** 1.62 13.25 0.24 4.6E-3 1.2E-3 1.08 0.08 4.6E-2
TCI*** 3.14 7.5E-3 1E-11 4E-24 7E-12 2E-12 1E-7 2E-35
PTE contamination indices at the groundwater table (i.e., 500 cm below surface) after 20 years; * porewater contamination index; ** soil contamination index; *** total contamination index
Concern-worthy PTE : Cl-
Prioritization: Cl- > Cr > As > Pb > Fe > Cu > Cd > ZnOther PTEs based on TCI at top layers
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R E S U LT S – C H L O R I D E I N T H E M E D I A
13
Chloride concentration in the media during 20 years for LR=8, Kd = 1 L/kg, and for the case of variable C0 and precipitation
Exceedance from screening standard
Attenuation of variations over depth
50 100 250 500
Depth below surface (cm)
0
500
1000
1500
2000
2500
3000
3500
4000
Cl c
once
ntra
tion
in th
e so
il (m
g/kg
)
published screening standard
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R E S U LT S – C H R O M I U M A N D A R S E N I C I N T H E M E D I A
14
Accumulation at top layers
Trace amount reaching layers lower than 60 cm
Underlying water protection
Chromium concentration in the media after 20 years for LR=8, Kd = 200 L/kg, and for the case of variable C0 and precipitation
Arsenic concentration in the media after 20 years for LR=8, Kd = 500 L/kg, and for the case of variable C0 and precipitation
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RESULTS –
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- Decrease in porewater concentration with increase in Kd for LR 8 and relative high Kds (breakthrough has occurred)- Drop in soil concentrations when there is not high load and Kd is relatively high
Effects of varying LR and Kd on the performance of infiltration basins
Chloride concentration at 100 cm below the surface after 20 years for the case of variable C0 and precipitation (a) in the porewater (b) in the soil
(a) (b)
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RESULTS –
16
Effects of varying LR and Kd on the performance of infiltration basins
Chloride porewater contamination index at 500 cm below the surface after 20 years for the case of variable C0 and precipitation
Imaginary line dividing PWCI
Combination of LR=8 and Kd > 6.5 L/kg results in PWCI < 1
Combination of LR=8 and Kd < 6.5 L/kg results in PWCI > 1
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SUMMARY
17
A contaminant transport simulation model was developed by combining various fields,including hydrology, geology, statistics, chemistry, and computer modeling. Importance of factors such as total incoming load, precipitation, soil background concentration , loading ratio, and
particularly adsorption coefficient in PTE transport
Chloride is highly mobile in the soil and readily reaches groundwater.
Among the suite of select environmentally relevant metals (Cr, As, Pb, Fe, Cu, Cd andZn), Cr and Zn showed the highest and lowest potential of contamination, respectively.
The breakthrough of high priority metals in the soil is a slow process and majority ofcontaminant loads is intercepted by the top 60 cm of the media within the 20 years ofsimulation.
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IMPLICATIONS
18
operative agencies
• Timetable for maintenance or soil replacement in the basins
designers• Pick LR and soil type (Kd) as
designing factor and assess the impacts
academia• Impacts of the Kd on the
accumulation of contaminants at different layers
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ACKNOWLEDGEMENTS
19
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T H A N K S F O R Y O U R A T T E N T I O N
C O M M E N T S
20
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APPENDIXA D SORPTION C O EFFICIENT
21
metal paper 1 paper 2 paper 3 paper 4 paper 5 paper 6 paper 7 paper 8 paper 9 paper 10Cr 22 532 140 16700Fe 25000 124000Co 5000 1300Cu 1310 1697 1700 450 483 616 900 797Zn 85 315 1980 10 2170 140 1100 467As 34 5740 4000Cd 16 188 616 73 691 274 630Pb 1215 1398 925 6000 19100 32000
paper 1
paper 2
paper 3
paper 4
paper 5
paper 6
paper 7
paper 8
paper 9
paper 10
field samples - loamy sand soil - heavy metal concentration 1000 mg/l - Freundlich isotherm OM of soil : 0.8 % , soil CEC= 2.3 meq/100gr, soil pH = 7field samples - loamy sand soil - heavy metal concentration is high- Freundlich isotherm OM of soil : low , soil CEC: high, soil pH = 7
field samples - clayey silty soil - heavy metal concentration 1000 mg/l - Freundlich isotherm TOC of soil : 0.3 % , soil CEC= ? cmol/gr, soil pH = 6.5field samples - sandy soil - heavy metal concentration ? mg/l - Freundlich isotherm TOC of soil : 2.4 % , soil CEC= ? cmol/gr, soil pH = 5.7field samples - sandy soil - heavy metal concentration ? mg/l - Freundlich isotherm DOC of soil : 20 mg/l , soil CEC= ? cmol/gr, soil pH = 5uniform soil sampl - heavy metal concentration ? mg/l - Freundlich isotherm DOM of soil : 50 mg/l , soil CEC= ? cmol/gr, soil pH = 7field samples - silty clay soil - heavy metal concentration between 25 to 1000 mg/l - Freundlich isotherm DOC of soil : ? mg/l , soil CEC= ? cmol/gr, soil pH = 6.4
Kd values in L/kg
Conditions
field samples - calcareous soil - heavy metal concentration between 10 to 200 mg/l - Freundlich isotherm OM of soil : 2.5 % , soil CEC= 24 cmol/gr, soil pH = 7.5 field samples - mineral soil - heavy metal concentration between 0.1 to10 meq/l - Freundlich isotherm OC of soil : 16 g/kg , soil CEC= 33.6 cmol/gr, soil pH = 8.3field samples - sandy loam soil - heavy metal concentration between 0 to50 mg/l - Freundlich isotherm TOC of soil : 1.1 % , soil CEC= 13.5 cmol/gr, soil pH = 6
Kd
Kd values in L/kg
metalpaper 1paper 2paper 3paper 4paper 5paper 6paper 7paper 8paper 9paper 10
Cr22532140167004348.58237.2183613968
Fe250001240007450070003.5713374682
Co5000130031502616.2950903902
Cu131016971700450483616900797994.125512.7080588126
Zn8531519801021701401100467783.375868.0131561709
As345740400032582924.4712342576
Cd1618861673691274630355.4285714286284.4690124559
Pb121513989256000191003200010106.333333333312777.076452251
Conditions
paper 1field samples - calcareous soil - heavy metal concentration between 10 to 200 mg/l - Freundlich isotherm OM of soil : 2.5 % , soil CEC= 24 cmol/gr, soil pH = 7.5
paper 2field samples - mineral soil - heavy metal concentration between 0.1 to10 meq/l - Freundlich isotherm OC of soil : 16 g/kg , soil CEC= 33.6 cmol/gr, soil pH = 8.3
paper 3field samples - sandy loam soil - heavy metal concentration between 0 to50 mg/l - Freundlich isotherm TOC of soil : 1.1 % , soil CEC= 13.5 cmol/gr, soil pH = 6
paper 4field samples - clayey silty soil - heavy metal concentration 1000 mg/l - Freundlich isotherm TOC of soil : 0.3 % , soil CEC= ? cmol/gr, soil pH = 6.5
paper 5field samples - sandy soil - heavy metal concentration ? mg/l - Freundlich isotherm TOC of soil : 2.4 % , soil CEC= ? cmol/gr, soil pH = 5.7
paper 6field samples - sandy soil - heavy metal concentration ? mg/l - Freundlich isotherm DOC of soil : 20 mg/l , soil CEC= ? cmol/gr, soil pH = 5
paper 7uniform soil sampl - heavy metal concentration ? mg/l - Freundlich isotherm DOM of soil : 50 mg/l , soil CEC= ? cmol/gr, soil pH = 7
paper 8field samples - silty clay soil - heavy metal concentration between 25 to 1000 mg/l - Freundlich isotherm DOC of soil : ? mg/l , soil CEC= ? cmol/gr, soil pH = 6.4
paper 9field samples - loamy sand soil - heavy metal concentration 1000 mg/l - Freundlich isotherm OM of soil : 0.8 % , soil CEC= 2.3 meq/100gr, soil pH = 7
paper 10field samples - loamy sand soil - heavy metal concentration is high- Freundlich isotherm OM of soil : low , soil CEC: high, soil pH = 7
Ln (Kd)
Kd values in L/kg
metalpaper 1paper 2paper 3paper 4paper 5paper 6paper 7paper 8paper 9paper 10
Cr3.09104245346.27664348934.94164242269.72316399846.00812309092.8000221791
Fe10.126631103911.728036844610.92733397421.1323648587
Co8.51719319147.17011954347.84365636740.9525249112
Cu7.17778241627.43661726527.438383536.10924758286.18001665376.42324696356.80239476336.68085467886.78106798170.5305428085
Zn4.44265125655.75257263887.59085212372.3025850937.68248244654.94164242267.00306545886.14632925775.73277258721.8164085236
As3.52636052468.65521448938.29404964016.8252082182.8625874817
Cd2.77258872225.23644196286.42324696354.29045944116.53813982385.61312810646.44571981945.33138926281.3910139953
Pb7.10249935587.24279792286.82979373758.69951474829.85744361410.37349118188.35092342671.5219881493
Conditions
paper 1field samples - calcareous soil - heavy metal concentration between 10 to 200 mg/l - Freundlich isotherm OM of soil : 2.5 % , soil CEC= 24 cmol/gr, soil pH = 7.5
paper 2field samples - mineral soil - heavy metal concentration between 0.1 to10 meq/l - Freundlich isotherm OC of soil : 16 g/kg , soil CEC= 33.6 cmol/gr, soil pH = 8.3
paper 3field samples - sandy loam soil - heavy metal concentration between 0 to50 mg/l - Freundlich isotherm TOC of soil : 1.1 % , soil CEC= 13.5 cmol/gr, soil pH = 6
paper 4field samples - clayey silty soil - heavy metal concentration 1000 mg/l - Freundlich isotherm TOC of soil : 0.3 % , soil CEC= ? cmol/gr, soil pH = 6.5
paper 5field samples - sandy soil - heavy metal concentration ? mg/l - Freundlich isotherm TOC of soil : 2.4 % , soil CEC= ? cmol/gr, soil pH = 5.7
paper 6field samples - sandy soil - heavy metal concentration ? mg/l - Freundlich isotherm DOC of soil : 20 mg/l , soil CEC= ? cmol/gr, soil pH = 5
paper 7uniform soil sampl - heavy metal concentration ? mg/l - Freundlich isotherm DOM of soil : 50 mg/l , soil CEC= ? cmol/gr, soil pH = 7
paper 8field samples - silty clay soil - heavy metal concentration between 25 to 1000 mg/l - Freundlich isotherm DOC of soil : ? mg/l , soil CEC= ? cmol/gr, soil pH = 6.4
paper 9field samples - loamy sand soil - heavy metal concentration 1000 mg/l - Freundlich isotherm OM of soil : 0.8 % , soil CEC= 2.3 meq/100gr, soil pH = 7
paper 10field samples - loamy sand soil - heavy metal concentration is high- Freundlich isotherm OM of soil : low , soil CEC: high, soil pH = 7
papers list
1Majid Baghenejad, Fatemeh Javaheri & Ali Akbar Moosavi (2016) Adsorptionisotherms of some heavy metals under conditions of their competitive adsorption onto highlycalcareous soils of southern Iran, Archives of Agronomy and Soil Science, 62:10, 1462-1473, DOI:10.1080/03650340.2016.1147647
2Modeling competitive metal sorption in a mineral soilMiquel Vidal a,⁎, Maria Josefa Santos b, Taufik Abrão c, Jordi Rodríguez a, Anna Rigol a
3Adsorption-desorption Study of Heavy Metals on Sandy-loam Soilof Sapele MetropolisChokor, Augustine A.
4Solid/liquid partition coefficients(Kd) for selected soils andsediments at Forsmark andLaxemar-SimpevarpSteve Sheppard, Jeff Long, Barb SanipelliECOMatters Inc, Canada
5de Groot, A.C., Peijnenburg, W.J.G.M., van den Hoop, M.A.G.T., Ritsema, R. & van Veen, R.P.M.1998. Heavy metals in Dutch field soils: an experimental and theoretical study on equilibriumpartitioning. National Institute of Public Health and the Environment (RIVM), TheNetherlands.
6Weng, L.P., Temminghoff, E.J.M., Lofts, S., Tipping, E. & van Riemsdijk, W.H. 2002.Complexation with dissolved organic matter and solubility control of heavy metals in a sandysoil. Environmental Science & Technology, 36, 4804–4810.
7Partitioning of metals (Cd, Co, Cu, Ni, Pb, Zn) insoils: concepts, methodologies, prediction andapplications – a review F. DEGRYSE, E. SMOLDERS & D. R. PARKER
8Adsorption Behavior of Heavy Metalson Various SoilsNoppadol Sangiumsak1, Pongsakorn Punrattanasin2
9http://www.state.nj.us/dep/dsr/publications/sorption-desorption-yr3-part2.pdf
10Adsorption of heavy metal ions on soils and soils constituents, Heike B. Bradl
http://www.state.nj.us/dep/dsr/publications/sorption-desorption-yr3-part2.pdf
Cr - Kds
11059.5569086995avestd
11809.7059753258697.70571757172446.5920904303
5394.5181347778
11872.1763726824
9557.3811937561
5151.9616150005
6642.5506419575
8853.2824912869
12235.6928856224
12296.4975584619
5646.7933703281
12343.4846829726
12232.8931606091
8346.6452056421
10940.5849722805
5517.2487537152
7822.6397812081
11891.6134819074
10874.0847607667
12252.0486319241
9749.9793271476
4642.6648944534
11342.9635091655
12042.0063294785
9939.3896798506
10590.1709164664
10469.8444110938
7579.3596069872
9747.8145122001
5758.6021280002
10164.3557999473
4610.714106663
6629.5750963028
4728.8238266599
5148.5956918326
11131.5019430068
10071.9550909247
6960.5176594209
12175.6865077183
4632.239886783
7962.5330951469
7491.4803285614
10654.2289429947
10898.7352263116
5887.8104494032
8382.7962735509
8018.890833904
9672.3213938417
10191.6930093918
10565.0189936273
6622.1788323491
9947.3593697999
9744.6853065878
5687.9683708593
5328.7098874491
8453.6335194497
12254.1205569475
7152.3315575166
9169.4782644718
6192.0878173874
10536.850814927
6449.7741688625
8516.1787158535
10106.9476156154
11687.0646296625
12250.3929412521
8856.0338108422
5490.3798057518
5578.2673237783
6469.6517189771
11273.6716173982
6443.0778334994
11055.9419203777
6354.4683437434
12003.0473791272
7231.392703222
5967.8980065373
6416.7325650709
9422.9945175514
8247.0835962381
7245.1961483995
11192.2168285518
9169.4481176772
8876.693399691
11903.6244882918
6703.0184141174
10585.7236301842
10557.1311346107
7482.3155160716
9025.7708447549
4973.3283467495
4792.8989080587
8720.7953496194
10766.6706140858
12042.1499575028
5418.5658056477
9034.0247035077
8214.9732070062
4446.5399454295
7125.4528363513
Fe - Kds
112138.619960389avestd
202878.50044856483116.413204659681372.0759209428
-83627.3473804039
134855.211539834
96814.7052091804
-17042.8509408893
44147.0099340692
98484.9362861678
325000.56545293
268370.482693184
-19996.9067161813
286955.481386802
125280.886411352
70085.9336863332
124534.555857749
60151.6439155331
65809.4522631816
178784.152761637
173137.446427268
173708.530216027
121507.197497139
-10028.3969342991
124709.267096104
188622.292366029
108724.309927703
146932.205934784
125384.555290779
53258.0515742666
95072.0522116914
19387.392082327
136690.86698589
-5799.0040651963
-324.7493715843
17832.2003951914
-131610.406379442
175191.757442132
97264.499127915
21652.3215524174
170425.791608654
-45312.2617268062
67342.6636314782
57597.8447980074
96845.611737381
96401.2190890405
13955.3170070441
72396.301942865
62957.8798163309
118441.751883155
151032.501256178
152153.092425107
14041.2180629207
79915.4126547463
-10492.5290778412
-3449.0285938116
74020.5225714862
181789.595123858
20620.6372985779
100497.843213213
58708.2862024132
152718.920175685
-1738.390072536
76779.1387653222
113178.864739707
151546.645904956
182600.347590987
80515.4862115729
-29916.6487207726
22536.2203795666
185.4873982935
239040.399962045
31405.669773694
126868.04649582
61030.017066898
136705.903309407
20957.8219035763
-23663.8358329741
-25071.3945444411
108675.317196634
62083.1055696904
60775.5556798236
173856.779384092
94911.947525831
88347.4801930329
185644.606511452
18184.5100340832
123266.196992114
132959.153938855
57439.0697839139
89597.6762794685
-7113.2388288097
-5860.794252579
81841.6046644229
125060.361670466
255493.621351467
27815.2713575751
87613.8407433071
68725.095608392
-60818.5077316365
43770.8015271817
-51133.9283101923
Co - Kds
4556.6958972488avestd
7947.98435930973472.02756415493041.1785944615
-2759.8099515058
5405.6998248081
3983.9839319057
-271.298468874
2015.5953209785
4046.4067095189
12512.1423434755
10395.664503352
-381.7025735866
11090.2553634898
5047.8715119917
2985.0298448733
5019.9783498926
2613.7483080536
2825.2017513104
7047.4885368339
6836.4500173057
6857.7935528411
4906.8346536079
-9.1421070601
5026.5079618299
7415.1765825864
4429.0903707983
5857.0622415054
5051.7460054646
2356.1089983773
3918.8544764561
1090.2358660848
5474.305129345
148.9261112508
353.5194684489
1032.1125404148
-4553.116196592
6913.2272976449
4000.7944116937
1174.8847452544
6735.1053422853
-1327.8320031013
2882.5035903169
2518.3032905476
3985.1390243736
3968.5304102468
887.2189188644
3071.3769413136
2718.6278315994
4792.2674943186
6010.3056019736
6052.1862820167
890.4293623663
3352.3942102914
-26.4884598963
236.7534773368
3132.0801365134
7159.8131503506
1136.3268489059
4121.6365643542
2559.8046359571
6073.3333797616
300.6864321605
3235.1799336377
4595.5737324282
6029.5211090455
7190.1140001266
3374.821201805
-752.4404060128
1207.9193478791
372.5889234812
9299.4896944116
1539.4038201234
5107.1896161477
2646.5763955228
5474.867092951
1148.9286977772
-518.7494193404
-571.3551489511
4427.2593293345
2685.9342486502
2637.0662224723
6863.3341783133
3912.8707659755
3667.5320879265
7303.8893334966
1045.2796683305
4972.5750387614
5334.8370659968
2512.3692748705
3714.256588118
99.8082463572
146.6167810158
3424.3832045791
5039.629678243
9914.4080694578
1405.2172126772
3640.1132398106
2934.1702399496
-1907.358368831
2001.5350067843
-1545.4094410259
-
APPENDIXA D SORPTION C O EFFICIENT
22
1Majid Baghenejad, Fatemeh Javaheri & Ali Akbar Moosavi (2016) Adsorptionisotherms of some heavy metals under conditions of their competitive adsorption onto highlycalcareous soils of southern Iran, Archives of Agronomy and Soil Science, 62:10, 1462-1473, DOI:10.1080/03650340.2016.1147647
2 Modeling competitive metal sorption in a mineral soilMiquel Vidal a,⁎, Maria Josefa Santos b, Taufik Abrão c, Jordi Rodríguez a, Anna Rigol a
3Adsorption-desorption Study of Heavy Metals on Sandy-loam Soilof Sapele MetropolisChokor, Augustine A.
4
Solid/liquid partition coefficients(Kd) for selected soils andsediments at Forsmark andLaxemar-SimpevarpSteve Sheppard, Jeff Long, Barb SanipelliECOMatters Inc, Canada
5de Groot, A.C., Peijnenburg, W.J.G.M., van den Hoop, M.A.G.T., Ritsema, R. & van Veen, R.P.M.1998. Heavy metals in Dutch field soils: an experimental and theoretical study on equilibriumpartitioning. National Institute of Public Health and the Environment (RIVM), TheNetherlands.
6Weng, L.P., Temminghoff, E.J.M., Lofts, S., Tipping, E. & van Riemsdijk, W.H. 2002.Complexation with dissolved organic matter and solubility control of heavy metals in a sandysoil. Environmental Science & Technology, 36, 4804–4810.
7Partitioning of metals (Cd, Co, Cu, Ni, Pb, Zn) insoils: concepts, methodologies, prediction andapplications – a review F. DEGRYSE, E. SMOLDERS & D. R. PARKER
8Adsorption Behavior of Heavy Metalson Various SoilsNoppadol Sangiumsak1, Pongsakorn Punrattanasin2
9 http://www.state.nj.us/dep/dsr/publications/sorption-desorption-yr3-part2.pdf
10 Adsorption of heavy metal ions on soils and soils constituents, Heike B. Bradl
http://www.state.nj.us/dep/dsr/publications/sorption-desorption-yr3-part2.pdf
-
APPENDIXP E NNSYLVANIA B A CKGROUND A ND S TA NDARD VA L UES
23
PTE porewater standard (ug/L)* soil screening (mg/kg)**
Cl-
CrFeCuZn
250,00074
3003
120
1,0004
150,0008,10066,000
As 10 12CdPb
12.5
1.2500
PTE Cl- Cr Fe Cu Zn As Cd Pb
Mean C0 (ug/L) 1.61x106 33.89 1,410 67.53 239.89 2.34 0.36 14.56
Std C0 (ug/L) 2.99x106 52.36 1,457 33.10 233.05 3.44 0.66 13.27
Soil background concentration
(mg/kg)100 53 36,000 37 81 13 0.10 23
Slide Number 1IntroductionLoading Ratio (LR)Adsorption coefficient ObjectivesmethodmethodmethodmethodResults-PTE transportResults-PTE transportResults – PTE prioritization Results – chloride in the mediaResults – chromium and arsenic in the mediaResults –�Results –�summaryimplicationsAcknowledgementsThanks for your attention���CommentsAppendix�Adsorption coefficient Appendix�Adsorption coefficient Appendix�Pennsylvania background and standard values