Water and nutrient fluxes from three coastal Mediterranean Rivers (N-E Algeria)
Main Article Content
Abstract
The objectives of the present study were to estimate water delivery and dissolved nutrients loads (nitrogen N, phosphorus P and silicates Si) from three minors coastal rivers (about 14% of Algerian coastal watersheds). Freshwater flow dissolved inorganic nitrogen DIN (NH4, NO3 and NO2), dissolved organic nitrogen DON, dissolved inorganic phosphorus DIP, phosphate (PO4), dissolved organic phosphorus DOP and silicates SiO4 were measured monthly at River outlet in the year 2011. The rivers were characterized by high values of ammonia (NH4) and phosphate (PO4) which reveal the dominance of organic and domestic pollutions. In contrast, values of SiO4 were very low and will be in relation to the retention in dams. Dissolved nitrogen loads varied considerably from 43 to 227 kg/km²/y where DON formed 20 to 40%. Loads of total dissolved phosphorus (TDP) fluctuated in the range of 20- 80 kg/km²/y in which the organic fraction forms largely dominated (51 to 74%). At River outlets, the loading ratio of nutrients (Si: N: P) were altered by agricultural and household wastes. Here, Si:N and N:P mass ratios ranged from 3-6 and 10-20 respectively, indicating large N and P inputs. These biogeochemical conditions would induce deep impacts on the ecology and the productivity of the adjacent coastal waters.
Article Details
This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License.
References
Bernard C.Y., Dürr H.H., Heinze, C., Segschneider M.R.E. (2010). Contribution of riverine
nutrients to the silicon biogeochemistry of the global ocean-a model study. Biogeosci.Discuss,
: 4919-4951.
Billen G., Garnier J. (2007). River basin nutrient delivery to the coastal sea: assessing its
potential to sustain new production of non-siliceous algae. Mar. Chem. 106: 148-160.
Bosc E., Bricaud A., Antoine D. (2004). Seasonal and inter-annual variability in algal biomass
and primary production in the Mediterranean Sea, as derived from 4 years of Sea WiFS
observations. Global Biogeochem. Cy. 18, GB1005, doi:10.1029/2003GB002034.
Cloern J.E. (2001). Our evolving conceptual model of the coastal eutrophication problem.
Mar. Ecol. Prog. Ser. 210: 223-253.
Conley D.J., Stalnacke P., Pitkanen H., Wilander A. (2000). The transport and retention of
dissolved silicate by rivers in Sweden and Finland. Limnol. Oceanogr. 45(8): 850-853.
Howarth, R.W., Billen G., Swaney D., Townsend A., Jaworski N., Lajtha K., Downing
J.A., Elmgren R., Caraco N., Jordan T., Berendse E., Freney J., Kudeyarov V., Murdoch
P., Zhao-Liang Z. (1996). Regional nitrogen budgets and riverine N & P fluxes for the
drainages to the North Atlantic Ocean: Natural and human influences. Biogeochemistry 35: 75-
Liu K. K., Seitzinger S., Mayorga E., Harrison J., Ittekkot V. (2008). Fluxes of
nutrients and selected organic pollutants carried by rivers, Chapter 8 in: E. Urban & S.
Greenwood (Eds.) PACKMEDS - Dynamics and vulnerability of semi-enclosed marine
systems: the integrated effects of changes in sediment and nutrient input from land.
Scientific Committee on Progress in the Environment (SCOPE), New York, 141-167.
Ludwig W., Dumont E., Meybeck M., Heussner S. (2009). River discharges of water
and nutrients to the Mediterranean and Black Sea: Major drivers for ecosystem changes
duringpast and future decades. Prog. Oceanogr., doi:10.1016/j.pocean.2009.02.001.
Margat J., Treyer S. (2004). L’eau des Méditerranéens: situation et perspectives. MAP
Technical Report Series No. 158, 366 pp. Available from:
Meybeck M. (2003). Global analysis of river systems: from Earth system controls to
Anthropocene syndromes. Phil. Trans. R. Soc. Lond. B 358, 1935-1955.
Nixon S. W. (2003). Replacing the Nile: are anthropogenic nutrients providing the
fertility once brought to the Mediterranean by Great River? Ambio 32, 30-39.
Ounissi M., Bouchareb N. (2013). Nutrient distribution and fluxes from three
Mediterranean coastal rivers (NE Algeria) under large damming. Comptes Rendus
Géoscience 345 (2), 81–92.
Ounissi M., Aicha Beya A., François. D. (2018). Riverine and wet atmospheric inputs
of materials to a North Africa coastal site (Annaba Bay, Algeria) 165: 19-34.
Preston S. D., Bierman J.R.V. J., Silliman S.E. (1989). An evaluation of methods for
the estimation of tributary mass loads. Water Resour. Res. 25 (6): 1379-1389.
Rabalais N. N. (2002). Nitrogen in aquatic ecosystems. Ambio 31: 102-112.
Rabalais N. N., Turner R. E. (2001). Coastal hypoxia. Coastal Estuary Studies 52.
Washington, DC: American Geophysical Union Ragueneau O., Conley D.J., Leynaert
A., Longphuirt S.N., Slomp C.P. (2006). Responses of Coastal Ecosystems to
Anthropogenic Perturbations of Silicon Cycling. In: Unger, D., C. Humborg, N. Tac
Ad, V. Ittekkot (eds).The Silicon Cycle. Human Perturbations and Impacts on Aquatic
Systems. Scientific Committee on Problems of the Environment (SCOPE) Series Vol.
, 296 p.
Rodier J. (1984). L’analyse de l’eau : eaux naturelles, eaux résiduaires, eaux de mer.
Dunod, 1365 p.
Seitzinger S.P., Sanders R.W (1997). Contribution of dissolved organic nitrogen from
rivers to estuarine eutrophication. Mar.Ecol. Prog. Ser. 159: 1-12.
Skliris N., Sofianos S., Lascaratos A. (2007). Hydrological changes in the
Mediterranean Sea in relation to changes in the freshwater budget: A numerical
modeling study 65(1-4): 400-416.
Turner R.E., Rabalais N.N., Justic D., Dortch Q. (2003). Global patterns of dissolved
N, P and Si in large rivers. Biogeochemistry 64, 297-317.