The general pattern —
iron fertilization reduces some acidity at the surface, but increases it at depth — is clear.
Not exact matches
According to Ingall, removal of
iron by diatom - dominated phytoplankton communities may dampen the intended outcome of enhanced carbon uptake through
iron fertilization by
reducing the productivity of other phytoplankton, which take up carbon dioxide more efficiently.
Paul Beckwith has done both a blog and a You tube video on the possibilities of
iron fertilization to
reduce carbon in the atmosphere.
Understanding
iron cycling in Antarctic phytoplankton is crucial for determining whether
iron fertilization can be an effective strategy for
reducing atmospheric carbon dioxide.
Paul Beckwith has done both a blog and a You tube video on the possibilities of
iron fertilization to
reduce carbon in the atmosphere.