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Impact of deforestation on soil fertility, soil carbon and nitrogen stocks: the case of the Gacheb catchment in the White Nile Basin, Ethiopia.

2017; Elsevier BV; Volume: 247; Linguagem: Inglês

10.1016/j.agee.2017.06.034

1873-2305

Henok Kassà, Stefaan Dondeyne, Jean Poesen, Amaury Frankl, Jan Nyssen,

Conservation, Biodiversity, and Resource Management

The evergreen forests of southwest Ethiopia are important for soil fertility sustenance and climate change mitigation. However, the increasing human population and expansion of agricultural land have led to deforestation. We determine the effect of deforestation on soil fertility, soil carbon and nitrogen stocks and hypothesize that tropical forests and agroforestry have similar characteristics, in contrast to the deforested areas used as cropland. Hence, soil samples (n = 360) have been taken from the natural forest, agroforestry and croplands at four depths (0–20 cm, 20–40 cm, 40–60 cm and 60–80 cm) in three altitudinal belts. The topsoil and subsoil physico-chemical characteristics, pH, organic carbon, total nitrogen, available phosphorus, exchangeable calcium, magnesium, cation exchange capacity and exchangeable base cations were significantly higher in both the forest and agroforestry than in croplands, at all elevation zones. Soil organic carbon and nitrogen stocks in soil under forest are similar to those under agroforestry at all elevation zones (0–20 cm, 20–40 cm, 40–60 cm and 60–80 cm soil depths). However, soil organic carbon and nitrogen stocks in soil under both forest and agroforestry were significantly different from cropland in all elevation zones at all depths except 60–80 cm. The highest total soil organic carbon stocks were recorded in the forest (412 Mg ha−1 at the FH site and 320 Mg ha−1 at the FL site) and agroforestry (357 Mg ha−1 at the DM site, 397 Mg ha−1 at the ZH site and 363 Mg ha−1 at the ZM site). The total organic carbon loss due to the conversion of forest to cropland ranges from 3.3 Mg ha−1 y−1 at the FL site to 8.0 Mg ha−1 y−1 at the FH site. The soil organic carbon and nitrogen losses due to the conversion of forest to cropland are similar to the losses when converting agroforestry to cropland. The total carbon dioxide emission due to the conversion of forest to cropland ranges from 12 Mg ha−1 y−1 at the FL site to 28 Mg ha−1 y−1 at the FH site. Agroforestry has the potential to maintain soil fertility, and stores higher soil organic carbon and nitrogen in proportion to the natural forest. Therefore, it can be suggested that agroforestry has a similar capacity as Afromontane forests to sustain soil fertility as well as to regulate greenhouse gas emissions.