Rehabilitation studies on saline land caused by potash mining activity

<p>The salinity at the waste management areas at potash mines is extreme. Saturated brine seeps from the tailings pile and contaminates the surrounding land killing vegetation and affecting soil structure. Conventional saline land reclamation practices cannot be applied directly because of the...

Full description

Bibliographic Details
Main Author: Thorpe, Mark Bramley
Other Authors: Neal, Dick
Format: Others
Language:en
Published: University of Saskatchewan 2012
Online Access:http://library.usask.ca/theses/available/etd-06012012-114706/
id ndltd-USASK-oai-usask.ca-etd-06012012-114706
record_format oai_dc
spelling ndltd-USASK-oai-usask.ca-etd-06012012-1147062013-01-08T16:35:21Z Rehabilitation studies on saline land caused by potash mining activity Thorpe, Mark Bramley <p>The salinity at the waste management areas at potash mines is extreme. Saturated brine seeps from the tailings pile and contaminates the surrounding land killing vegetation and affecting soil structure. Conventional saline land reclamation practices cannot be applied directly because of the high salt concentrations and the continued inputs. Some major modifications of saline land reclamation practices are, therefore, required.</p> <p>Some of the factors affecting the movement of NaCl into areas of comparatively low salinity surrounded by extreme salinity were investigated. Methods of rehabilitating extremely saline areas with high NaCl inputs, by applying amendments and using salt tolerant vegetation, were investigated using field plots, a greenhouse column study, laboratory testing of the salinity tolerance of vegetation and the Trasee /Tracon computer model.</p> <p>The movement of Na upwards in the profile of an area of low salinity was affected by the [Na] in the base of the profile and climate, in the form of evapotranspirational losses. The vegetation cover did not affect the movement of Na. To maintain low [Na] in the soil profiles, the [Na] in the saline base must be kept low and, where possible, the water table kept low.</p> <p>In the revegetation trials, the movement of Na into the sewage sludge amendments was slower than into the topsoil amendments. This affected the vegetation which became established on the two amendments. The vegetation on the topsoil amendment was all killed after 3 months but the vegetation on the sewage sludge amendment remained for the 3 years of the field trial. Of the five species of grass planted, <u>Agropyron trachycaulum</u> and <u>Elymus junceus</u> proved to be best suited to the saline conditions on the sewage sludge amendment. These species also showed considerable salt tolerance at germination and at the mature stage in the laboratory.</p> <p>The greenhouse column study also showed that the movement of Na in to the topsoil was faster than into the sewage sludge amendment. The surface of the sewage sludge amendment dried out, reducing evaporation from that amendment, indicating that evaporation driving the mass flow of water and Na into the amendment might be the key factor affecting the movement of Na in to the two materials.</p> <p>The Trasee /Tracon computer model indicated that the surface evaporation from the sewage sludge was less than from the topsoil. The model accurately simulated Na movement in both the field and column studies. Potential revegetation scenarios are also discussed.</p> Neal, Dick Redmann, R.E. DeJong, E. Randell, R. Ripley, E. Steeves, T. University of Saskatchewan 2012-06-01 text application/pdf http://library.usask.ca/theses/available/etd-06012012-114706/ http://library.usask.ca/theses/available/etd-06012012-114706/ en unrestricted I hereby certify that, if appropriate, I have obtained and attached hereto a written permission statement from the owner(s) of each third party copyrighted matter to be included in my thesis, dissertation, or project report, allowing distribution as specified below. I certify that the version I submitted is the same as that approved by my advisory committee. I hereby grant to University of Saskatchewan or its agents the non-exclusive license to archive and make accessible, under the conditions specified below, my thesis, dissertation, or project report in whole or in part in all forms of media, now or hereafter known. I retain all other ownership rights to the copyright of the thesis, dissertation or project report. I also retain the right to use in future works (such as articles or books) all or part of this thesis, dissertation, or project report.
collection NDLTD
language en
format Others
sources NDLTD
description <p>The salinity at the waste management areas at potash mines is extreme. Saturated brine seeps from the tailings pile and contaminates the surrounding land killing vegetation and affecting soil structure. Conventional saline land reclamation practices cannot be applied directly because of the high salt concentrations and the continued inputs. Some major modifications of saline land reclamation practices are, therefore, required.</p> <p>Some of the factors affecting the movement of NaCl into areas of comparatively low salinity surrounded by extreme salinity were investigated. Methods of rehabilitating extremely saline areas with high NaCl inputs, by applying amendments and using salt tolerant vegetation, were investigated using field plots, a greenhouse column study, laboratory testing of the salinity tolerance of vegetation and the Trasee /Tracon computer model.</p> <p>The movement of Na upwards in the profile of an area of low salinity was affected by the [Na] in the base of the profile and climate, in the form of evapotranspirational losses. The vegetation cover did not affect the movement of Na. To maintain low [Na] in the soil profiles, the [Na] in the saline base must be kept low and, where possible, the water table kept low.</p> <p>In the revegetation trials, the movement of Na into the sewage sludge amendments was slower than into the topsoil amendments. This affected the vegetation which became established on the two amendments. The vegetation on the topsoil amendment was all killed after 3 months but the vegetation on the sewage sludge amendment remained for the 3 years of the field trial. Of the five species of grass planted, <u>Agropyron trachycaulum</u> and <u>Elymus junceus</u> proved to be best suited to the saline conditions on the sewage sludge amendment. These species also showed considerable salt tolerance at germination and at the mature stage in the laboratory.</p> <p>The greenhouse column study also showed that the movement of Na in to the topsoil was faster than into the sewage sludge amendment. The surface of the sewage sludge amendment dried out, reducing evaporation from that amendment, indicating that evaporation driving the mass flow of water and Na into the amendment might be the key factor affecting the movement of Na in to the two materials.</p> <p>The Trasee /Tracon computer model indicated that the surface evaporation from the sewage sludge was less than from the topsoil. The model accurately simulated Na movement in both the field and column studies. Potential revegetation scenarios are also discussed.</p>
author2 Neal, Dick
author_facet Neal, Dick
Thorpe, Mark Bramley
author Thorpe, Mark Bramley
spellingShingle Thorpe, Mark Bramley
Rehabilitation studies on saline land caused by potash mining activity
author_sort Thorpe, Mark Bramley
title Rehabilitation studies on saline land caused by potash mining activity
title_short Rehabilitation studies on saline land caused by potash mining activity
title_full Rehabilitation studies on saline land caused by potash mining activity
title_fullStr Rehabilitation studies on saline land caused by potash mining activity
title_full_unstemmed Rehabilitation studies on saline land caused by potash mining activity
title_sort rehabilitation studies on saline land caused by potash mining activity
publisher University of Saskatchewan
publishDate 2012
url http://library.usask.ca/theses/available/etd-06012012-114706/
work_keys_str_mv AT thorpemarkbramley rehabilitationstudiesonsalinelandcausedbypotashminingactivity
_version_ 1716532838642221056