Water, salt and nutrient fluxes of tropical tidal salt flats

Mangroves and Salt Marshes - Tập 1 - Trang 229-238 - 1997
Peter Ridd1, Renagi Sam1, Suzanne Hollins1, Gregg Brunskill2
1Marine Geophysics Laboratory, Physics Department, James Cook University, Townsville, Australia
2Australian Institute of Marine Science, Townsville, Australia

Tóm tắt

The water budget of a tropical tidal salt flat in dry tropical Australia has been studied with particular emphasis on estimating the groundwater fluxes. Salt was used as a passive tracer to determine some of these fluxes. Groundwater salt accumulation (or loss) was less than 1 kg/m3/month. Surface water leaving the flat at a higher salt concentration than flood water causes a net outwelling of salt of between 0.4 and 1 kg/m2/month. Evaporation from the salt flat was estimated to be 70 mm/month. Using these measurements and a simple model of the groundwater flows, it is concluded that the groundwater loss is less than 40 mm/month. The accuracy of the salt budget was insufficient to rule out the possibility that the net groundwater motion was upwards. Measurements of Si and PO_4 fluxes indicated that the net outwelling due to surface water flows were respectively 3 mmole/m2/month and 0.014 mmole/m2/month. A net groundwater loss of 10 mm would produce a similar magnitude outwelling due to groundwater discharge. The mangrove-fringed tropical tidal salt flats are the source of large quantities of nutrients that are released to the near-shore zone.

Tài liệu tham khảo

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