scholarly journals Effects of Capping Strategy and Water Balance on Salt Movement in Oil Sands Reclamation Soils

Water ◽  
2020 ◽  
Vol 12 (2) ◽  
pp. 512
Author(s):  
Xiaopeng Li ◽  
Bin Ma ◽  
Bonnie Drozdowski ◽  
Francis Salifu ◽  
Scott X. Chang

The success of oil sands reclamation can be impacted by soil salinity depending on the materials used for soil reconstruction and the capping strategies applied. Using both a greenhouse-based column experiment and numerical modeling, we examined the potential pathways of salt migration from saline groundwater into the rooting zone under different capping strategies (the type and the thickness of the barrier layer) and water balance scenarios. The experimental results showed that there would be salinity issues in the cover soil within several growing seasons if there was a shallow saline groundwater table and if the soil was not properly reconstructed. The thickness of the barrier layer was the most significant factor affecting the upward movement of saline groundwater and salt accumulation in the cover soil. The suitable thickness of the barrier layer for preventing the upward movement of saline groundwater and salt accumulation in the cover soil for each material varied. A numerical simulation for a 15-year period further indicates that, when the cover soil was 50 cm of peat-mineral soil mix and when wet, dry, or normal climatic conditions were considered, the minimum barrier thickness to restrain salt intrusion into the cover soil in the long term was about 75 or 200 cm for coarse tailings sand or overburden barrier material, respectively. In view of the above, to minimize salt migration into the rooting zone and ensure normal plant growth, oil sands reclamation should consider salt migration when designing soil capping strategies.

2019 ◽  
Author(s):  
Md. Shahabul Alam ◽  
S. Lee Barbour ◽  
Mingbin Huang

Abstract. One technique to evaluate the performance of oil sands reclamation covers is through the simulation of long-term water balance using calibrated soil–vegetation–atmosphere–transfer models. Conventional practice has been to derive a single set of optimized hydraulic parameters through inverse modelling (IM) based on short-term (


2016 ◽  
Vol 2016 (1) ◽  
pp. 28-44 ◽  
Author(s):  
Bradley D. Pinno ◽  
◽  
Ira Sherr ◽  
Ruth C. Errington ◽  
Krista Shea

1963 ◽  
Vol 43 (1) ◽  
pp. 135-140 ◽  
Author(s):  
J. C. van Schaik ◽  
R. A. Milne

Considerable salt accumulation occurred in a grass-covered soil in southern Alberta where the saline groundwater was maintained at a depth of 3 feet. The SAR values of the saturation extract increased significantly under grass, and indications are that this increase was mainly due to precipitation of calcium. A fallow soil did not show a significant salt accumulation above the water table.It is suggested that a leaching program is necessary to maintain low salinity where shallow water tables are present and shallow tile drains are used.


2020 ◽  
Vol 22 (7) ◽  
pp. 703-712
Author(s):  
Eduardo K. Mitter ◽  
J. Renato de Freitas ◽  
James J. Germida

1999 ◽  
Vol 39 (8) ◽  
pp. 949 ◽  
Author(s):  
E. G. Barrett-Lennard ◽  
C. V. Malcolm

Summary. This paper examines the accumulation of soil chloride and the increase in electrical conductivity of the groundwater beneath stands of saltbushes (Atriplex species) in a plant spacing trial conducted near Kellerberrin in Western Australia. The trial had a randomised block design with 5 plant spacings (1 by 1 m, 1 by 2 m, 2 by 2 m, 2 by 3 m, and 3 by 3 m), 5 saltbush species (Atriplex undulata D. Dietr., A. amnicola Paul G. Wilson, A. vesicaria Heward ex Benth., A. paludosa R. Br. and A. bunburyana F. Muell.) and 3 replicate plots (each consisting of 25 plants in 5 by 5 array). The saline groundwater at the site was between 0.5 and 1.2 m below the surface for the duration of the experiment. Over a 2-year period there was a substantial increase in soil chloride concentration beneath the saltbushes. These increases were proportional to saltbush ‘leaf density’ (weight per unit soil surface area) and inversely proportional to the initial concentration of chloride in the soil. There was a substantial increase in the electrical conductivity of the groundwater which was also proportional to ‘leaf density’. It is argued that the increases in soil salinity and groundwater electrical conductivity were primarily due to the use of groundwater by the saltbush stands. Salt accumulation data suggest that about 60–100 mm of groundwater was used (transpiration and evaporation) over the 2 years. These results are discussed in terms of the ability of saltbushes to lower local watertables, thereby making saline soils better suited to the growth of superior annual pasture species.


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