Translator Disclaimer
1 September 2013 In situ measurement of snowmelt infiltration under various topsoil cap thicknesses on a reclaimed site
Andre F. Christensen, Hailong He, Miles F. Dyck, E. Lenore Turner, David S. Chanasyk, M. Anne Naeth, Connie Nichol
Author Affiliations +
Abstract

Christensen, A. F., He, H., Dyck, M. F., Turner, L., Chanasyk, D. S., Naeth, M. A. and Nichol, C. 2013. In situ measurement of snowmelt infiltration under various topsoil cap thicknesses on a reclaimed site. Can. J. Soil Sci. 93: 497-510. Understanding the soil and climatic conditions affecting the partitioning of snowmelt to runoff and infiltration during spring snow ablation is a requisite for water resources management and environmental risk assessment in cold semi-arid regions. Soil freezing and thawing processes, snowmelt runoff or infiltration into seasonally frozen soils have been documented for natural, agricultural or forested systems but rarely studied in severely disturbed systems such as reclaimed lands. The objective of this study was to quantify the snowmelt infiltration/runoff on phosphogypsum (PG) tailings piles capped with varying thicknesses of topsoil (0.15, 0.3, and 0.46 m) at a phosphate fertilizer production facility in Alberta. There are currently no environmental regulations specifying topsoil capping thickness or characteristics for these types of tailings piles. Generally, the function of the topsoil cap is to facilitate plant growth and minimize the amount of drainage into the underlying PG. Experimental plots were established in 2006 to better understand the vegetation and water dynamics in this reconstructed soil. In 2011, time domain reflectometry (TDR) probes and temperature sensors were installed at various depths for continuous, simultaneous, and automated measurement of composite dielectric permittivity (εeff) and soil temperature, respectively. An on-site meteorological station was used to record routine weather data. Liquid water and ice content were calculated with TDR-measured effective permittivity (εeff) and a composite dielectric mixing model. Spatial and temporal change of total water content (ice and liquid) revealed that snowmelt infiltration into the topsoil cap increased with increasing topsoil depth and net soil water flux from the topsoil cap into the PG material was positive during the snowmelt period in the spring of 2011. Given the objective of the capping soil is to reduce drainage of water into the PG material it is recognized that a capping soil with a higher water-holding capacity could reduce the amount of meteoric water entering the tailings.

Andre F. Christensen, Hailong He, Miles F. Dyck, E. Lenore Turner, David S. Chanasyk, M. Anne Naeth, and Connie Nichol "In situ measurement of snowmelt infiltration under various topsoil cap thicknesses on a reclaimed site," Canadian Journal of Soil Science 93(4), 497-510, (1 September 2013). https://doi.org/10.1139/CJSS2012-048
Received: 1 May 2012; Accepted: 1 May 2013; Published: 1 September 2013
JOURNAL ARTICLE
14 PAGES


Share
SHARE
KEYWORDS
dynamique de l'eau et de la chaleur
Fort Saskatchewan
Fort Saskatchewan
ground thermal regime
infiltration de l'eau de fonte
phosphogypsum tailing
régime thermique du sol
ARTICLE IMPACT
RIGHTS & PERMISSIONS
Get copyright permission
Back to Top