Weathering regime associated with subsurface circulation on volcanic islands |
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Authors: | Sétareh Rad Karine Rivé Claude Jean Allègre |
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Institution: | 1.Institut de Physique du Globe de Paris,Sorbonne Paris Cité,Paris Cedex 05,France;2.BRGM, Geology Division,Regolith and Reservoirs Unit,Orléans Cedex 2,France |
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Abstract: | Volcanic islands, being characterized by highly porous basaltic/andesitic lava flows and pyroclastic deposits, are subject
to important chemical weathering by subsurface waters. Moreover, such subsurface weathering is impacted by hydrothermal springs
in both active and non-active volcanic areas, thus increasing dissolved load concentrations. Here, we focus on the subsurface
water chemistry in the volcanic islands of the Lesser Antilles and Réunion and on the origin of these subsurface flows. We
are able, through the use of various isotopic tools (C, Sr, U–Th), to identify hydrothermal influences in river water. For
example, Li concentrations show a positive correlation with temperature of hot and cold springs and also a relationship with
δ13C; from this, we can show that several sources of hydrothermal activity influence the rivers of the Lesser Antilles and that
some rivers also reveal an important organic influence. As much as 20% of the subsurface hydrothermal springs go to feed the
rivers. The increasing temperatures result in more dissolved elements being mobilized and an increase in chemical weathering
rates. In addition, using the (230Th/238U) isochron for the well and river dissolved loads in Martinique, Guadeloupe and Réunion, we can evaluate residence times
in the river water, i.e. the average residence time in the water along the circulation path to the sampling point. Alteration
takes longer when the water circulates through thick soil, for example, 400–5,000 years when circulating under an ash profile
and 1,200–15,000 years when circulating through a collapse zone. It would appear that waters circulation is globally three
times longer for subsurface water than for surficial water. The weathering regime in tropical volcanic environments seems
to be controlled mainly by such subsurface circulation with high chemical concentration from hydrothermal inputs. The origin
of these compositions is varied and not controlled by a single hydrothermal spring. Consequently, it is subsurface circulation
that determines the weathering regime in tropical volcanic islands with the main controlling parameters being temperature
and residence time. |
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