cbd-ts-66-en
cbd-ts-66-en
cbd-ts-66-en
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Part I: Impac<strong>ts</strong> of Climate-related Geo<strong>en</strong>gineering on Biological Diversity<br />
likely to require considerable transport, burying and processing, which could compromise the growth, nutri<strong>en</strong>t<br />
cycling and viability of the ecosystems involved.357<br />
There is a great deal of uncertainty surrounding the impac<strong>ts</strong> of biochar on biodiversity and ecosystem services due to<br />
a lack of published research on biochar. Compounding this limitation is the fact that many field trials have relied on<br />
charcoal produced by wildfires rather than by the modern method of pyrolysis proposed for biochar geo<strong>en</strong>gineering.358<br />
Two other unint<strong>en</strong>ded impac<strong>ts</strong> warrant m<strong>en</strong>tion. First, biochar application may decrease soil N2O emissions,<br />
thereby pot<strong>en</strong>tially providing additional b<strong>en</strong>efi<strong>ts</strong>.359 Second, if used on light-coloured soils, biochar can decrease<br />
albedo, at least on a seasonal basis.360 Whilst unlikely to have a climatically significant effect, the pot<strong>en</strong>tial for that<br />
additional, negative, impact should nevertheless also be tak<strong>en</strong> into account if very large-scale use of biochar is<br />
proposed for geo<strong>en</strong>gineering purposes.<br />
5.6.3 Ocean storage of terrestrial biomass<br />
Ocean biomass storage (for example, the CROPS proposal: Crop Residue Oceanic Perman<strong>en</strong>t Sequestration),<br />
involves the deep ocean sequestration of terrestrial crop residues on or in the seabed.361, 362 These proposals suggest<br />
that up to 0.6 Gt C (30% of global annual crop residues of 2 Gt C) could be available sustainably, deposited in<br />
an annual layer 4m deep in an area of seabed of ~1,000 km2. However, an annual sequestration rate < 1 Gt C/yr<br />
would only make a modest contribution to slowing climate change.363 Pot<strong>en</strong>tially, charcoal (biochar), timber or<br />
other organic remains could also be deposited on the seabed, if suitably ballasted. Nevertheless, it seems unlikely<br />
that deposition on the seabed would be the most effective use of such materials; e.g., it would seem more effective<br />
to obtain at least some <strong>en</strong>ergy from them, via a BECCS approach.<br />
It should be noted that this technique would seem to be covered by the existing category of wastes “Organic material<br />
of natural origin” in Annex I of the London Protocol and “Uncontaminated organic material of natural origin” in<br />
Annex I of the London Conv<strong>en</strong>tion.364 That does not mean such disposal is prohibited; however, an appropriate<br />
regulatory framework would seem to be in place.<br />
Impac<strong>ts</strong> on biodiversity<br />
Where crop residues are deposited as ballasted bales, it is likely that there will be significant physical impact<br />
(although of a relatively local nature) on the seabed due to the sheer mass of the material. In addition, there may<br />
be wider chemical and biological impac<strong>ts</strong> through reductions in oxyg<strong>en</strong> and pot<strong>en</strong>tial increases in H2S, CH4 , N2O<br />
and nutri<strong>en</strong><strong>ts</strong> arising from the degradation of the organic matter.<br />
The degradation of crop residue bales is likely to be slow due to the ambi<strong>en</strong>t conditions of low temperature and<br />
limited oxyg<strong>en</strong> availability; the appar<strong>en</strong>t lack of a marine mechanism for the breakdown of ligno-cellulose material;<br />
and the anaerobic conditions within the bales.365 While it can be argued that pot<strong>en</strong>tial impac<strong>ts</strong> could be reduced<br />
if deposition occurred in areas of naturally high sedim<strong>en</strong>tation, such as off the mouths of major rivers (e.g.,<br />
Mississippi),3<strong>66</strong> many such areas are already susceptible to eutrophication and anoxia from existing anthropog<strong>en</strong>ic,<br />
357 The Royal Society (2009).<br />
358 Shackley & Sohi (2011).<br />
359 Clough & Condron (2010).<br />
360 G<strong>en</strong>esio et al. (2012).<br />
361 Metzger & B<strong>en</strong>ford (2001).<br />
362 Strand & B<strong>en</strong>ford (2009).<br />
363 L<strong>en</strong>ton & Vaughan (2009).<br />
364 International Maritime Organization (IMO) (2010).<br />
365 Strand & B<strong>en</strong>ford (2009).<br />
3<strong>66</strong> Strand & B<strong>en</strong>ford (2009).<br />
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