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Limnological studies on the Pretoria Salt Pan, a hypersaline maar lake

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dc.contributor.author Ashton, PJ
dc.contributor.author Schoeman, FR
dc.date.accessioned 2011-02-11T13:55:09Z
dc.date.available 2011-02-11T13:55:09Z
dc.date.issued 1983
dc.identifier.citation Limnological studies on the Pretoria Salt Pan, a hypersaline maar lake. Hydrobiologia, Vol 99, pp 61-73 en_US
dc.identifier.uri http://hdl.handle.net/10204/4856
dc.description.abstract The Pretoria Salt pan is shallow and alkaline with pronounced mesothermy at a depth of between 0.55 and 0.7 metres. Secchi disc transparencies ranged from 7 to 19 cm. Endorheic or closed drainage basins are widely distributed in many climate conditions. Where evaporation exceeds precipitation, close lakes within the basins become saline, particularly if they receive inflows sufficient to maintain standing body water. en_US
dc.language.iso en en_US
dc.relation.ispartofseries Journal Article;
dc.subject Diatoms en_US
dc.subject Pretoria salt pan en_US
dc.subject Limnology en_US
dc.subject Morphometric en_US
dc.subject Marine diatoms en_US
dc.subject Hydro biology en_US
dc.title Limnological studies on the Pretoria Salt Pan, a hypersaline maar lake en_US
dc.type Article en_US
dc.identifier.apacitation Ashton, P., & Schoeman, F. (1983). Limnological studies on the Pretoria Salt Pan, a hypersaline maar lake. http://hdl.handle.net/10204/4856 en_ZA
dc.identifier.chicagocitation Ashton, PJ, and FR Schoeman "Limnological studies on the Pretoria Salt Pan, a hypersaline maar lake." (1983) http://hdl.handle.net/10204/4856 en_ZA
dc.identifier.vancouvercitation Ashton P, Schoeman F. Limnological studies on the Pretoria Salt Pan, a hypersaline maar lake. 1983; http://hdl.handle.net/10204/4856. en_ZA
dc.identifier.ris TY - Article AU - Ashton, PJ AU - Schoeman, FR AB - The Pretoria Salt pan is shallow and alkaline with pronounced mesothermy at a depth of between 0.55 and 0.7 metres. Secchi disc transparencies ranged from 7 to 19 cm. Endorheic or closed drainage basins are widely distributed in many climate conditions. Where evaporation exceeds precipitation, close lakes within the basins become saline, particularly if they receive inflows sufficient to maintain standing body water. DA - 1983 DB - ResearchSpace DP - CSIR KW - Diatoms KW - Pretoria salt pan KW - Limnology KW - Morphometric KW - Marine diatoms KW - Hydro biology LK - https://researchspace.csir.co.za PY - 1983 T1 - Limnological studies on the Pretoria Salt Pan, a hypersaline maar lake TI - Limnological studies on the Pretoria Salt Pan, a hypersaline maar lake UR - http://hdl.handle.net/10204/4856 ER - en_ZA


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