Abstract
The Kromme is a permanently open estuary that receives little freshwater input because the capacity of the dams is equivalent to the mean annual runoff from the catchment. The estuary is marine dominated and phytoplankton chlorophyll a is low because of the low freshwater pulses that introduce nutrient-rich freshwater. Water released (2 x 106 m3) from the Mpofu Dam in 1998 produced little micro-algal response in the estuary. The study reported here addresses further runoff scenarios to see which might be beneficial in stimulating microalgal production. Recent surveys together with past research were used to describe the present state and reference condition of the estuary. Average intertidal chlorophyll a was 12.9 ± 2.5 μg·g-1 of sediment and 4.9 ± 0.4 μg·g-1 of sediment during November 2003 and July 2004. These concentrations are relatively low but comparable to those found in intertidal sediments in other South African estuaries and might indicate that intertidal microalgal biomass is not severely limited by low freshwater inputs. Average water column chlorophyll a concentrations have ranged from 0.6 ± 0.1 to 5.6 ± 0.3 μg·ℓ-1. Present state conditions can thus be described as those where water column chlorophyll a seldom exceeds 5 μg·ℓ-1 and small flagellates (3.5 μm x 2.8 μm) dominate the phytoplankton. The diatoms introduced via freshwater have been lost. Under reference conditions before the Mpofu Dam was built, baseflow would have been greater than 1 m3·s-1 for approximately 8 months of the year. The flocculation of fine particles associated with the mixing of fresh and saline waters would have resulted in phytoplankton peaks (chl a >10 μg·ℓ-1) in the middle reaches of the estuary. A more suitable habitat might also have been present for the epipelic (mud associated) benthic microalgae. An assessment of the future runoff scenarios indicated that the most beneficial for the microalgae would be a flow release from the Mpofu Dam of 5 x 106 m3 in October and then again in January. This would stimulate a 25 to 33% increase in phytoplankton chlorophyll a and a doubling in intertidal benthic chlorophyll a for a period of two months following the releases. Water SA Vol 32(1)pp:71-80
Highlights
The Kromme Estuary is located in the Eastern Cape Province, 80 km west of Port Elizabeth
The results reported in this study were a component of a Department of Water Affairs and Forestry comprehensive Ecological Reserve study on the Kromme Estuary
River inflow has been severely decreased into the Kromme Estuary primarily due to dam construction
Summary
The Kromme Estuary is located in the Eastern Cape Province, 80 km west of Port Elizabeth. The estuary is relatively narrow with an average width of approximately 80 m, and extends for 14 km from the permanently open mouth to a rocky sill that forms the tidal head of the estuary. Its major tributary is the Geelhoutboom River which enters 8 km from the mouth. The catchment area and length of the Kromme River are approximately 1 000 km and 100 km respectively. The rainfall in the catchment occurs throughout the year, with bimodal maxima in autumn and spring. January and February tend to have the lowest rainfall (Bickerton and Pierce, 1988)
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