http://www.agu.org/pubs/crossref/2012/2010GB004008.shtml

GLOBAL BIOGEOCHEMICAL CYCLES, VOL. 26, GB3002, 14 PP., 2012
doi:10.1029/2010GB004008

The effect of vertical and horizontal dilution on fertilized patch experiments

Key Points
Efficiency of carbon export decreases for increased size of fertilized patch
Lateral supply of silicic acid is critical to blooms in iron-fertilized patches
Carbon export resulting from iron fertilization is minimal

A great deal of attention, both negative and positive, has been
directed at the potential of large-scale iron fertilization schemes to
sequester carbon by inducing phytoplankton blooms that would, in
theory, result in significant export of organic carbon to the deep
ocean in high nitrogen - low chlorophyll regions. A suite of iron
manipulation or ‘patch’ experiments has been performed over
length-scales of 10s of km. Here, we use a
physical-ecological-chemical model, with prognostic nitrogen, silica
and iron dynamics, to study one of the most successful of these
experiments, the Subarctic Ecosystem Response to Iron Enrichment Study
(SERIES), focusing on the vertical export of organic material, which
is difficult to observe in the field. The implications of large-scale
fertilization, i.e. increasing patch size, are investigated. Our
results agree with the general conclusions obtained from the field
experiments. Only a modest export of organic carbon occurs (less than
25% of carbon uptake by phytoplankton) at the base of the mixed layer.
Furthermore, we show that lateral and vertical supply of silicic acid
is necessary to fuel a sustained phytoplankton bloom. Increasing patch
size results in less lateral nutrient supply relative to patch area
and so a decrease, not only in total production (per unit area), but
in the contribution by large phytoplankton due to silica limitation.
Most importantly, the export of organic carbon (per unit area)
decreases substantially, by nearly an order of magnitude, as scales of
1000 km are approached.

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