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OPTICAL CHARACTERISTICS OF NEW ZEALAND RIVERS IN RELATION TO FLOW 1
Author(s) -
Smith David G.,
DaviesColley Robert J.,
Knoef Jeroen,
Slot Gerritdina W. J.
Publication year - 1997
Publication title -
jawra journal of the american water resources association
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.957
H-Index - 105
eISSN - 1752-1688
pISSN - 1093-474X
DOI - 10.1111/j.1752-1688.1997.tb03511.x
Subject(s) - turbidity , visibility , colored dissolved organic matter , environmental science , hydrology (agriculture) , water quality , flow (mathematics) , water flow , turbidite , geology , soil science , chemistry , ecology , geography , meteorology , nutrient , geomorphology , mathematics , structural basin , oceanography , organic chemistry , biology , geometry , geotechnical engineering , phytoplankton
Six years (1989–1994) of data from New Zealand's National Rivers Water Quality Network were used to characterize the optical water quality regime of river waters as regards: visual clarity (black disc visibility), turbidity, and light‐absorbing aquatic humic material (referred to as ‘yellow substance,’ measured as light absorption at 440 nm). Quantitative relationships between optical water quality variables and flow in rivers are well‐described by power law expressions. Visual clarity usually decreases strongly with increasing flow in individual rivers. There is a strong, inverse relationship between turbidity and visibility, but, because of differences between sites, turbidity is not a good general predictor of visual clarity (the attribute of real interest) in rivers. Yellow substance tends to increase with increasing flow, probably because during rainstorms, soil water high in yellow‐colored humic material, rather than rain water or ground water, dominates discharge. Therefore, rivers are typically clear and low in humic matter at low flow, and turbid and yellow‐colored at high flow.