Saline seepage and vertical distribution of oxygen in a brackish ditch

Summary Seepage caused salinity gradients in a 120 cm deep ditch adjacent to Lake Veere in the Dutch Delta area. The water was mixed by strong horizontal currents, forced by a pumping engine. The restoration of vertical chloride and oxygen gradients was studied.During summer when the level of Lake Veere was raised by 70 cm, a rapid seepage into the ditch was observed, ranging from 6 to 10 mm.h^–1. This caused an anoxic saline layer. At the anaerobic-aerobic interface 1.4 to 2.4 mg O₂.l^–1.h^–1 of the oxygen present in the upper water column was taken up. Sulfide oxidation required one quarter of this amount of oxygen.During winter the level of Lake Veere was lowered again. Normally seepage was absent then, and chloride entered the water column by diffusion; the mud chlorinity decreased from 15 to 3 Cl^– on its way to the ditch. Only after maximum discharge of polder water a moderate seepage of less than 4.4 mm.h^–1 restored a chloride gradient; about 1.6 mg O₂.l^–1.h^–1, produced by benthic diatoms, had to be supplied to the reducing materials in the seepage water in less than 12 hours.A saline seepage was simulated in the laboratory. These simulation tests showed that seepage below 1 mm.h^–1, as well as benthic respiration only, had a small impact on the vertical oxygen profile in the water column. Bottom oxygen demand increased with seepage velocity. At a strong seepage the water column could become entirely anaerobic.Communication no. 226.