Soil respiration studies in two sites of different post-logging ages in a moist-semi deciduous forest in Ghana
| dc.contributor.author | Opoku-Ameyaw, Adu | |
| dc.date.accessioned | 2016-10-25T10:10:56Z | |
| dc.date.accessioned | 2023-04-19T13:25:13Z | |
| dc.date.available | 2016-10-25T10:10:56Z | |
| dc.date.available | 2023-04-19T13:25:13Z | |
| dc.date.issued | NOVEMBER, 2015 | |
| dc.description | A thesis submitted in partial fulfillment of the requirements for the degree of Master of Philosophy in Silviculture and Forest Management. | en_US |
| dc.description.abstract | A large proportion of carbon is stored up in forest soils. Nevertheless, carbon is also released into the atmosphere via soil respiration, a process which determines ecosystem function and a great contributor in the global carbon cycle. This study investigated soil respiration in the Bobiri Forest Reserve, a moist- semi deciduous forest in Ghana. The aim was to investigate the seasonality, magnitude and abiotic controls on total soil respiration and its component contributions from root-and-rhizosphere, mycorrhizae, surface litter and soil organic matter in a 12- and 55-year-old post-logged site over a full seasonal cycle. Soil respiration was measured at monthly intervals from May 2013 to April 2014, by means of a dynamic closed chamber method. Total soil respiration had a strong seasonal influence whereby average fluxes were higher during the wet season and lower during the dry season. Estimated total soil respiration was 18.03 and 17.83 Mg C ha -1 year -1 at the 12- and 55-year-old sites respectively. In addition, estimated component contributions at the 12- and 55-year-old post-logged sites were 24.02 and 34.58 % for root-and-rhizosphere, 16.97 and 14.26 % for mycorrhizae, 27.42 and 25.17 % for litter and 31.59 and 25.99 % for soil organic matter, respectively. This depicted a higher autotrophic percentage at 55-year-old post-logged site (48.84 %) in comparison to 12-year-old post-logged site (40.99 %) and conversely, a higher heterotrophic percentage at 12-year-old post-logged site (59.01 %) in comparison to 55-year-old post-logged site (51.16 %). Relationship between soil respiration and soil moisture was quadratic, however observed variation was only explained at 12-year-old post-logged site (R 2 = 0.75; p < 0.01). A quadratic—quadratic regression of soil respiration and both soil temperature and soil moisture accounted for 83 % of observed variation in soil respiration at 12-year-old post-logged site (p < 0.01) but still did not improve variation at the 55-year-old post-logged site (p = 0.84). The study shows the influence of forest age on soil respiration and confirms the importance of separating total soil respiration into source components. Thus, the information should serve as a baseline for respiration studies in Ghana as iv well as assist in the understanding of forests and their influence on carbon cycling and global warming | en_US |
| dc.description.sponsorship | KNUST | en_US |
| dc.identifier.uri | https://ir.knust.edu.gh/handle/123456789/9381 | |
| dc.language.iso | en | en_US |
| dc.title | Soil respiration studies in two sites of different post-logging ages in a moist-semi deciduous forest in Ghana | en_US |
| dc.type | Thesis | en_US |
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