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Delineation of management regions for South African rivers based
on water chemistry
J. A. Day, H. F. Dallas, A. Wackernagel
Freshwater Research Unit, Zoology Department, University
of Cape Town, 7701 Rhodes Gift, Western Cape, South Africa |
Abstract
The rivers of South
Africa differ in water chemistry because of differences in geology
and climate, and in the nature of the terrestrial vegetation. Thus
the riverine biotas also differ in their water quality requirements.
This paper describes the use of multivariate analytical techniques
on a large inorganic chemical database as a means of dividing the
country's rivers into regions of like water chemistry for the purposes
of water quality management of aquatic ecosystems. Data were used
from about 500 usable sites for the three earliest hydrological
years (October 1980-September 1983 inclusive) for which information
is available for most of the sites. In some cases separate winter
(May-September) and summer (November-March) analyses were performed.
Those observations in which orthophosphate-phosphorus (PO3-4-P)
was greater than 0.1 mg -1> and/or nitrate- plus nitrite-nitrogen
(NO-2+3-N) was greater than 0.5 mg-1
and/or conductivity > 500 mS m-1, were excluded. Some
of the analyses were run on the subset of records for which the
reading of weir height (as a surrogate for discharge) was within
10% of the mean. Chemical variables comprised conductivity and pH,
and the concentrations of chloride, total alkalinity (TAL), sodium,
calcium, potassium, magnesium, chloride, sulphate, fluoride, silicate,
nitrate- plus nitrite-nitrogen, ammonium nitrogen and orthophosphate-phosphorus,
as well as the ratios Cl-:(Cl- + TAL), Cl-:(Cl-
+ SO24+) and Na+:(Na++
Ca2+). Multivariate techniques included principal components
analysis, detrended correspondence analysis and cluster analysis.
Eigenvalues are low ( < 0.05) for detrended correspondence analyses
but high ( > 0.7) for principal components analyses. In all cases,
[silicate] correlates most strongly with the first axis, and conductivity,
[K+] and/or [SO2-4] with the second.
Alkalinity correlates inversely with [H+], while [Ca2+]
and [Mg2+] are closely correlated with each other and
with alkalinity. [Na+] and [Cl-] are correlated
with each other and weakly with conductivity. Cluster analysis of
secondary drainage regions is used together with biogeographic and
physiographic information to produce a map of South Africa divided
into five major regions for the management of water quality for
riverine ecosystems. © 1998 Elsevier Science Ltd and AEHMS.
All rights reserved.
Keywords: Water quality management
regions; Multivariate analytical techniques; Cluster analysis; Physiographic;
Water chemistry
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