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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 />

67

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