Temporal variability and annual budget of inorganic dissolved matter in Andean Pacific Rivers located along a climate gradient from northern Ecuador to southern Peru

2018

Article référencé dans le Web of Science WOS:000427076100009

Moquet J. S., Guyot Jean-Loup, Morera S., Crave A., Rau P., Vauchel Philippe, Lagane Christelle, Sondag Francis, Lavado C. W., Pombosa R., Martinez Jean-Michel

Comptes Rendus Geoscience, 2018, 350 (1-2), p. 76-87 ISSN 1631-0713

In Ecuador and Peru, geochemical information from Pacific coastal rivers is limited and scarce. Here, we present an unedited database of major element concentrations from five HYBAM observatory stations monitored monthly between 4 and 10 years, and the discrete sampling of 23 Andean rivers distributed along the climate gradient of the Ecuadorian and Peruvian Pacific coasts. Concentration (C) vs. discharge (Q) relationships of the five monitored basins exhibit a clear dilution behavior for evaporites and/or pyrite solutes, while the solute concentrations delivered by other endmembers are less variable. Spatially, the annual specific fluxes for total dissolved solids (TDS), Ca2+, HCO3, K+, Mg2+, and SiO2 are controlled on the first order by runoff variability, while Cl, Na+ and SO42 are controlled by the occurrence of evaporites and/or pyrite. The entire Pacific basin in Ecuador and Peru exported 30 Mt TDS.yr (1), according to a specific flux of similar to 70 t.km (2).yr (1). This show that, even under low rainfall conditions, this orogenic context is more active, in terms of solute production, than the global average.

Sciences du milieu [021] ; Hydrologie [062] ; Géologie et formations superficielles [064]

EQUATEUR ; PEROU ; ANDES ; PACIFIQUE

Fonds IRD [F B010072728]

fdi:010072728