Articles | Volume 4, issue 1
https://doi.org/10.5194/soil-4-63-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/soil-4-63-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Saturated and unsaturated salt transport in peat from a constructed fen
Reuven B. Simhayov
CORRESPONDING AUTHOR
Department of Geography, University of Waterloo, Waterloo,
Ontario, N2L 3G1, Canada
Tobias K. D. Weber
Department of Geography, University of Waterloo, Waterloo,
Ontario, N2L 3G1, Canada
Soil Science and Soil Physics Division, Institute of
Geoecology, TU Braunschweig, Langer Kamp 19c, 38106 Braunschweig,
Germany
now at: Institute for Soil Science and Land Evaluation, Biogeophysics, University of Hohenheim, Emil-Wolff-Straße 27, 70599 Stuttgart, Germany
Jonathan S. Price
Department of Geography, University of Waterloo, Waterloo,
Ontario, N2L 3G1, Canada
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26 citations as recorded by crossref.
- Cadmium and copper transport in alluvial soils in the Brazilian semiarid region: column percolation and modeling V. Barros et al. 10.36783/18069657rbcs20220153
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- Non-Fickian dispersivity investigation from numerical simulations of tracer transport in a model double-porosity medium at different saturations T. Tran Ngoc et al. 10.1016/j.jconhyd.2020.103678
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- The influences of vegetation and peat properties on the hydrodynamic variability of a constructed fen, Fort McMurray, Alberta S. Scarlett & J. Price 10.1016/j.ecoleng.2019.08.005
- Methane emissions from fens in Alberta’s boreal region: reference data for functional evaluation of restoration outcomes A. Bienida et al. 10.1007/s11273-020-09715-2
- Wetlands in the Athabasca Oil Sands Region: the nexus between wetland hydrological function and resource extraction O. Volik et al. 10.1139/er-2019-0040
- Modelling the hydrologic effects of vegetation growth on the long-term trajectory of a reclamation watershed O. Sutton & J. Price 10.1016/j.scitotenv.2020.139323
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- Effects of different biomass materials as a salt-isolation layer on water and salt migration in coastal saline soil M. Yang et al. 10.7717/peerj.11766
- Competitive transport processes of chloride, sodium, potassium, and ammonium in fen peat C. McCarter et al. 10.1016/j.jconhyd.2018.08.004
- Microtopographical and hydrophysical controls on subsurface flow and solute transport: A continuous solute release experiment in a subarctic bog N. Balliston et al. 10.1002/hyp.13236
- Effect of anisotropy on solute transport in degraded fen peat soils M. Wang et al. 10.1002/hyp.13717
- Preferential recharge in a reclaimed tailings sand upland: Implications on solute flushing E. Kessel et al. 10.1016/j.ejrh.2021.100953
- The distribution and migration of sodium from a reclaimed upland to a constructed fen peatland in a post-mined oil sands landscape E. Kessel et al. 10.1016/j.scitotenv.2018.02.253
- Heterogeneity of the peat profile and its role in unsaturated sodium chloride rise at field and laboratory scales N. Balliston & J. Price 10.1002/vzj2.20015
- Remote Sensing, Geophysics, and Modeling to Support Precision Agriculture—Part 1: Soil Applications A. Pradipta et al. 10.3390/w14071158
- Modelling the potential for peat-block transplants to restore industrially contaminated Sphagnum peatlands C. McCarter et al. 10.1016/j.ecoleng.2022.106874
- Attenuation of Zn(II) and Cu(II) by low-alkali activated clay-fly ash liners A. Fashtali et al. 10.1016/j.clay.2024.107298
- Hydraulic and Physical Properties of Managed and Intact Peatlands: Application of the Van Genuchten‐Mualem Models to Peat Soils M. Menberu et al. 10.1029/2020WR028624
26 citations as recorded by crossref.
- Cadmium and copper transport in alluvial soils in the Brazilian semiarid region: column percolation and modeling V. Barros et al. 10.36783/18069657rbcs20220153
- Multiphase flow behavior of diesel in bog, fen, and swamp peats P. Gupta et al. 10.1016/j.jconhyd.2023.104162
- Comparison of soil hydraulic properties estimated from steady-state experiments and transient field observations through simulating soil moisture in regenerated Sphagnum moss J. Elliott & J. Price 10.1016/j.jhydrol.2019.124489
- Transport of chloride and deuterated water in peat: The role of anion exclusion, diffusion, and anion adsorption in a dual porosity organic media C. McCarter et al. 10.1016/j.jconhyd.2019.103497
- Non-Fickian dispersivity investigation from numerical simulations of tracer transport in a model double-porosity medium at different saturations T. Tran Ngoc et al. 10.1016/j.jconhyd.2020.103678
- Hydrologic‐based modelling of burn depth potentials in degraded peat soils N. Link et al. 10.1002/hyp.14808
- Pore-scale controls on hydrological and geochemical processes in peat: Implications on interacting processes C. McCarter et al. 10.1016/j.earscirev.2020.103227
- Effects of Different Peat Application Methods on Water and Salt Migration in a Coastal Saline Soil M. Yang et al. 10.1007/s42729-021-00691-x
- Wetlands as integral parts of surface water–groundwater interactions in the Athabasca Oil Sands Area: Review and synthesis O. Volik et al. 10.1139/er-2023-0064
- The influences of vegetation and peat properties on the hydrodynamic variability of a constructed fen, Fort McMurray, Alberta S. Scarlett & J. Price 10.1016/j.ecoleng.2019.08.005
- Methane emissions from fens in Alberta’s boreal region: reference data for functional evaluation of restoration outcomes A. Bienida et al. 10.1007/s11273-020-09715-2
- Wetlands in the Athabasca Oil Sands Region: the nexus between wetland hydrological function and resource extraction O. Volik et al. 10.1139/er-2019-0040
- Modelling the hydrologic effects of vegetation growth on the long-term trajectory of a reclamation watershed O. Sutton & J. Price 10.1016/j.scitotenv.2020.139323
- Advances in wetland hydrology: the Canadian contribution over 75 years J. Price et al. 10.1080/07011784.2023.2269137
- Projecting the hydrochemical trajectory of a constructed fen watershed: Implications for long-term wetland function O. Sutton & J. Price 10.1016/j.scitotenv.2022.157543
- Effects of different biomass materials as a salt-isolation layer on water and salt migration in coastal saline soil M. Yang et al. 10.7717/peerj.11766
- Competitive transport processes of chloride, sodium, potassium, and ammonium in fen peat C. McCarter et al. 10.1016/j.jconhyd.2018.08.004
- Microtopographical and hydrophysical controls on subsurface flow and solute transport: A continuous solute release experiment in a subarctic bog N. Balliston et al. 10.1002/hyp.13236
- Effect of anisotropy on solute transport in degraded fen peat soils M. Wang et al. 10.1002/hyp.13717
- Preferential recharge in a reclaimed tailings sand upland: Implications on solute flushing E. Kessel et al. 10.1016/j.ejrh.2021.100953
- The distribution and migration of sodium from a reclaimed upland to a constructed fen peatland in a post-mined oil sands landscape E. Kessel et al. 10.1016/j.scitotenv.2018.02.253
- Heterogeneity of the peat profile and its role in unsaturated sodium chloride rise at field and laboratory scales N. Balliston & J. Price 10.1002/vzj2.20015
- Remote Sensing, Geophysics, and Modeling to Support Precision Agriculture—Part 1: Soil Applications A. Pradipta et al. 10.3390/w14071158
- Modelling the potential for peat-block transplants to restore industrially contaminated Sphagnum peatlands C. McCarter et al. 10.1016/j.ecoleng.2022.106874
- Attenuation of Zn(II) and Cu(II) by low-alkali activated clay-fly ash liners A. Fashtali et al. 10.1016/j.clay.2024.107298
- Hydraulic and Physical Properties of Managed and Intact Peatlands: Application of the Van Genuchten‐Mualem Models to Peat Soils M. Menberu et al. 10.1029/2020WR028624
Latest update: 03 Nov 2024
Short summary
Lab experiments were performed to understand solute transport in peat from an experimental fen. Transport was analyzed under saturated and unsaturated conditions using NaCl (salt). We tested the applicability of a physical-based model which finds a wide consensus vs. alternative models. Evidence indicated that Cl transport can be explained using a simple transport model. Hence, use of the physical transport mechanism in peat should be evidence based and not automatically assumed.
Lab experiments were performed to understand solute transport in peat from an experimental fen....