File:Particulate organic carbon in the ocean interior 2.png
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Particulate organic carbon in the ocean interior
Summary
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English: Fluxes of particulate organic carbon in the ocean interior based on the Martin curve and model predictions using different parameterisation for organic matter degradation. The one-G has a fixed k of 0.03 (d−1), the three G-model and reactive continuum (RC) parameters were taken from Boudreau and Ruddick (1991), the two G-model has similar k parameterisation as the three-G model but without a refractory fraction. The RC fit curve was based on fitting parameter ν to the Martin curve (ν = 0.59). Such a high ν implies a dominance of fresh material
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| Date | |
| Source | [1] doi:10.1007/978-3-030-10822-9_3 |
| Author | Jack J. Middelburg |
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| current | 03:31, 29 May 2021 | | 785 × 813 (73 KB) | Epipelagic (talk | contribs) | Uploaded a work by Jack J. Middelburg from [https://link.springer.com/chapter/10.1007/978-3-030-10822-9_3] {{doi|10.1007/978-3-030-10822-9_3}} with UploadWizard |
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