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Biogeochemical processes and buffering capacity concurrently affect acidification in a seasonally hypoxic coastal marine basin

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Academic year: 2021

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Figure

Figure 1. (a) Map of the Netherlands; (b) bathymetry of Lake Grev- Grev-elingen (data from the executive arm of the Dutch Ministry of  In-frastructure and the Environment)
Table 1. Stoichiometric coefficients for the proton (ν H x + ) for each reaction considered in the proton budget
Figure 3. (a) Temperature ( ◦ C), (b) salinity, (c) density anomaly (kg m −3 ), (d) O 2 (µmol L −1 ), (e) stratification parameter φ (J m −3 ) and (f) light penetration and Secchi disc depths at the Den Osse basin in 2012
Figure 4. (a) pH T (at in situ temperature), (b) DIC (µmol kg −1 ), (c) TA (µmol kg −1 ), (d) pCO 2 (ppmv), (e) buffering capacity (β) and (f) concentration of Chl a (µg L −1 ) at Den Osse in 2012
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