Treatment of Domestic Wastewater by Three Plant Species in Constructed Wetlands

Three common Appalachian plant species (Juncus effusus L., Scirpus validus L., and Typha latifolia L.) were planted into small-scale constructed wetlands receivingprimary treated wastewater. The experimental design includedtwo wetland gravel depths (45 and 60 cm) and five plantingtreatments (each species in monoculture, an equal mixture of the three species, and controls without vegetation), with two replicates per depth × planting combination. Inflow rates (19 L day^-1) and frequency (3 times day^-1) were designed to simulate full-scale constructed wetlands as currently used for domestic wastewater treatmentin West Virginia. Influent wastewater and the effluent from each wetland were sampled monthly for ten physical, chemical and biological parameters, and plant demographic measurements were made. After passing through these trough wetlands, the average of all treatments showed a 70% reduction in total suspended solids (TSS) and biochemical oxygen demand (BOD), 50 to 60% reduction in nitrogen (TKN), ammonia and phosphate, anda reduction of fecal coliforms by three orders of magnitude. Depth of gravel (45 or 60 cm) had little effect on wetland treatment ability, but did influence Typha and Scirpus growth patterns. Gravel alone provided significant wastewater treatment, but vegetation further improved many treatment efficiencies. Typha significantly out-performedJuncus and Scirpus both in growth and in effluent quality improvement. There was also some evidence that the species mixture out-performed species monocultures.Typhawas the superior competitor in mixtures, but a decline in Typha growth with distance from the influent pipe suggested that nutrients became limiting or toxicities may have developed.     

Third-generation biomedical materials

Whereas second-generation biomaterials were designed to be either resorbable or bioactive, the next generation of biomaterials is combining these two properties, with the aim of developing materials that, once implanted, will help the body heal itself.     

Circulation and larval fish transport within a tidally dominated estuary

In March 1996 two surveys of larval fish abundance and water flow were carried out within the estuarine region near Beaufort Inlet, NC. Each survey extended over two full semidiurnal tidal cycles and included measurements of larvae concentration and velocity distribution at several locations. There was a large across-channel variation in the subtidal flow passing through Beaufort Inlet, with net inflow over the eastern and central portions of the inlet and net outflow on the western side of the inlet. This pattern was consistent with moored current meter measurements of a previous study, and was reproduced by a numerical model circu-lation forced only by the M₂ tide. A net ingress of larvae from the open ocean into the estuary was observ-ed during both surveys. Most larvae entered the estuary over the eastern and central portions of the inlet, where the subtidal flow was up-estuary. However, the mean circulation played a minor role in the net movement of larvae into the estuary. Rather, net up-estuary transport of larvae was principally due to variation of larval abundance with tidal flow; with abundance during flood tide usually far exceeding ebb tide abundance. This mode of transport was likely driven by a behavioural response to tidal flow in which larvae tended to descend to the bottom on falling tides and reside throughout the water column on rising tides.     

Tidal and subtidal fluctuations in temperature, salinity and pressure for the winter 1996 larval ingress experiment—Beaufort Inlet, NC

A multidisciplinary field experiment was conducted to compare water properties, larval abundances, and transport and retention processes at Beaufort Inlet and two channels leading to the estuarine nursery grounds. Temperature, salinity and subsurface pressure were monitored in situ for a six-week period during March and April 1996 in each channel. Intensive sampling was performed during two neap-tide periods when water mass conditions in the estuary were significantly different. Currents were stronger in the eastern channel during both experiments. Ebb currents were stronger than flood in both channels. Decreasing subtidal sea level appeared to account for the stronger ebb currents. Subtidal sea level in the inlet responded optimally to north–south (along the inlet axis) wind stress and along a line 15° clockwise of north–south. This direction closely parallels the channel axis of Core Sound and may provide an efficient conduit to carry large volumes of low-salinity Pamlico Sound water into the estuarine complex when winds blow south in this sector. The tidal stream in Beaufort Inlet sets up strong cross-inlet gradients by the advection on the east side of higher salinity shelf water and advection on the west side of Beaufort Inlet plume water. The axial fronts produced by differential advection of these two water masses might play some role in redistributing larvae present in one tidal stream to another.