That would surely depend on the ocean circulation around reefs.  It
would be impractical to exert short-term control over reef pH if the
surrounding water was from the ocean.  Only where ripurine and coastal
flows were a significant part of the local budget would adjusting the
pH of either be effective.  There's only so much adjustment to a
river's pH you could make before destroying its ecosystem, so
well-mixed reef water wouldn't be controllable using river pH tweaks.

A

On 15 May 2013 13:09, Oliver Tickell <[email protected]> wrote:
> This problem of ocean acidification is surely best solved by application of
> ground up olivine bearing rock to land / coast, so removing carbonic acid
> and replacing it with alkaline Mg++ and HCO3- (bicarbonate). The runoff from
> land will of course end up in the oceans.
>
> Oliver.
>
>
> On 15/05/2013 12:52, Andrew Lockley wrote:
>>
>> Please see below and attached.
>>
>> A
>>
>>
>> ---------- Forwarded message ----------
>> From: E Couce <[email protected]>
>> Date: 15 May 2013 12:47
>> Subject: Re: Tropical coral reef habitat in a geoengineered, high-CO2
>> world
>> To: Andrew Lockley <[email protected]>
>> Cc: geoengineering <[email protected]>
>>
>>
>> Dear Andrew and all,
>>
>> thanks for the interest on the paper. It can be accessed on
>> http://onlinelibrary.wiley.com/doi/10.1002/grl.50340/abstract
>>
>> Attached is an unformatted draft (also available for download free of
>> charge on my website)
>>
>> Best regards,
>> Elena
>>
>>
>>
>> On 15 May 2013 00:26, Andrew Lockley <[email protected]> wrote:
>>>
>>> Poster's note:  Hopefully the author (see cc ) will be kind enough to
>>> submit her paper to this list, as I lack a URL or copy
>>>
>>> Citation
>>>
>>> Couce, EM, Irvine, PJ, Gregorie, L, Ridgwell, AJ & Hendy, E 2013,
>>> ‘Tropical coral reef habitat in a geoengineered, high-CO2world’. Geophysical
>>> Research Letters, vol 40.
>>>
>>> Abstract
>>>
>>> Continued anthropogenic CO2 emissions are expected to impact tropical
>>> coral reefs by further raising sea surface temperatures (SST) and
>>> intensifying ocean acidification (OA). Although geoengineering by means of
>>> Solar Radiation Management (SRM) may mitigate temperature increases, OA will
>>> persist, raising important questions regarding the impact of different
>>> stressor combinations. We apply statistical Bioclimatic Envelope Models to
>>> project changes in shallow-water tropical coral reef habitat as a single
>>> niche (without resolving biodiversity or community composition) under
>>> various Representative Concentration Pathway and SRM scenarios, until 2070.
>>> We predict substantial reductions in habitat suitability centered on the
>>> Indo-Pacific Warm Pool under net anthropogenic radiative forcing of
>>> ≥3.0 W/m2. The near-term dominant risk to coral reefs is increasing SSTs;
>>> below 3 W/m2 reasonably favorable conditions are maintained, even when
>>> achieved by SRM with persisting OA. ‘Optimal’ mitigation occurs at 1.5 W/m2
>>> because tropical SSTs over-cool in a fully-geoengineered (i.e.
>>> pre-industrial global mean temperature) world.
>>>
>>> Key Points:
>>>
>>> • Large reductions in reef habitat suitability under net radiative
>>> forcing >3 W/m2
>>> • Rising SSTs are greater threat for tropical coral reefs than ocean
>>> acidification
>>> • Solar Radiation Management may help maintain coral reef habitat over
>>> near-term
>>
>>
>>
>>
>> --
>>
>> -------------------------------
>> Dr. Elena Couce
>> School of Geographical Sciences
>> Department of Earth Sciences
>> University of Bristol
>> E-mail: [email protected]
>> Web: http://www.bristol.ac.uk/earthsciences/people/elena-m-couce
>>
>
>
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