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Dynamics of dissolved inorganic carbon and aquatic metabolism in the Tana River basin, Kenya

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Academic year: 2017

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Fig. 1. Conceptual model showing the main watershed and in- in-stream biogeochemical processes controlling riverine DIC  concen-tration and δ 13 C DIC signatures.
Fig. 3. Discharge measurements for the Tana River (2008–2010) as recorded at Garissa station
Fig. 4. Altitudinal profiles of (A) dissolved inorganic carbon con- con-centrations and (B) δ 13 C DIC along the Tana River basin during all three sampling seasons
Fig. 9b), and values during different seasons were not sig- sig-nificantly different (paired t test, p > 0.05)
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