Hydrosalinity fluxes in a small scale catchment of the berg river (Western Cape)

dc.contributor.advisor	Jovanovic, N.Z
dc.contributor.advisor	de Clercq, W.P
dc.contributor.author	Bugan, Richard
dc.date.accessioned	2014-10-14T11:17:59Z
dc.date.available	2014-10-14T11:17:59Z
dc.date.issued	2008
dc.identifier.uri	http://hdl.handle.net/11394/3772
dc.description	>Magister Scientiae - MSc	en_US
dc.description.abstract	The objective of this study was to determine the hydrosalinity fluxes associated with overland and subsurface (vadose zone) flow for different soils and land uses. For this purpose, the following data were collected during 2005 and 2006 in a typical small scale catchment located near the town of Riebeeck-Wes: weather data, hydrological and water quality measurements, soil water contents and chemistry, and vegetation growth. The area is characterized by a Mediterranean climate receiving winter rainfall of approximately 300 mm a catchment is conservative, with Na + and Cl- being the dominant ions.	en_US
dc.language.iso	en	en_US
dc.subject	Sources of salts	en_US
dc.subject	Soil salinity	en_US
dc.subject	Types of salinity	en_US
dc.subject	Berg river catchment	en_US
dc.title	Hydrosalinity fluxes in a small scale catchment of the berg river (Western Cape)	en_US
dc.rights.holder	uwc	en_US