INVESTING IN TREES AND LANDSCAPE ... - PROFOR
INVESTING IN TREES AND LANDSCAPE ... - PROFOR
INVESTING IN TREES AND LANDSCAPE ... - PROFOR
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Carbon storage in fertilizer tree systems<br />
Carbon storage in tree biomass and in soils is one of the most important strategies to mitigate the<br />
global greenhouse gas effect. Nair, Kumar, and Nair studied soil carbon under-tree systems in five<br />
countries (Brazil, India, Mali, Spain, and the United States) and concluded that “tree-based agricultural<br />
systems, compared to treeless systems, stored more carbon in deeper soil layers up to 1 m depth<br />
under comparable conditions” (Nair et al. 2009). They also found that higher species richness and<br />
tree density were associated with higher soil organic carbon and that C3 plants appeared to generate<br />
more stable carbon in the soil than C4 plants. Studies in southern Africa have shown that improved<br />
fallows can store large quantities of carbon stocks in plant biomass and in the soil (Kaonga 2005,<br />
Makumba et al. 2007) and thus provide the opportunity to potentially mitigate global greenhouse<br />
gas emissions (Sileshi et al. 2007). Several studies and reviews have highlighted soil carbon stored<br />
at depths below the plow layer. The amount of carbon sequestered varies depending on the type of<br />
fertilizer tree system, the specific tree species, and the depth of the soil.<br />
Depommier, Janodet, and Oliver (1992) documented a 54 percent increase in soil organic carbon<br />
in the first 20 cm soil depth and a 35 percent increase in the 20–40 cm depth under mature<br />
Faidherbia compared with away from Faidherbia in Burkina Faso. Okorio documented a 9.3 percent<br />
increase in soil organic carbon with seven-year-old Faidherbia trees in Tanzania. The data in table<br />
5 support the theory that carbon stocks can be brought above 100 tonnes per hectare in eastern<br />
Africa, where rainfall is sufficient. Contrast that to the performance of Gliricidia in Mali, with 300<br />
mm rainfall, in the study by Takimoto, Nair, and Nair (2008). West African systems may develop<br />
the same levels of soil carbon (see Dossa et al. 2007) but must be in a rainfall zone sufficient for<br />
biomass production.<br />
TABLE 1.5. CARBON SEQUESTRATION <strong>IN</strong> FERTILIZER TREE SYSTEMS (ALL FIGURES <strong>IN</strong> TONNES PER HECTARE)<br />
SOIL DEPTH<br />
BIOMASS<br />
AUTHOR<br />
TREE<br />
(cm) Aboveground Belowground SOIL TOTAL<br />
Dossa et al. Shade coffee 40 62 15 97.3 174<br />
Nonshade coffee 40 13.8 9.2 95.8 119<br />
Kaonga et al. (Msek-2 yr-coppicing) 6.1<br />
(4.3–9.5) a 2.4<br />
(1.7–3.7)<br />
(Kalu-2 yr-coppicing) 5.5<br />
(2.1–9.5)<br />
(Kalu-2 yr-noncoppicing) 200 5.75<br />
(3.0–7.9)<br />
1.8<br />
(0.8–3.2)<br />
3.3<br />
(1.5–9.0)<br />
25.7<br />
(23–31)<br />
(Kali-2 yr-noncoppicing) 200 78 (48–127)<br />
(Msek-4-noncoppicing) 200 120 (102.0–<br />
184.5)<br />
(Msek-10-noncoppicing) 200 255<br />
(154–291)<br />
Makumba et al. (MZ12-Gliricidia) 20 negligible negligible 30<br />
200 negligible negligible 123<br />
Makumba et al. (MZ21-Gliricidia) 20 negligible negligible 30<br />
34.75<br />
Chapter 1. TREE-BASED <strong>AND</strong> OTHER L<strong>AND</strong> MANAGEMENT TECHNOLOGIES FOR L<strong>AND</strong>SCAPE RESTORATION <strong>AND</strong> LIVELIHOOD <strong>IN</strong> AFRICA<br />
35