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Impact of topographic aspect and vegetation (native and reforested areas) on soil organic carbon and nitrogen budgets in Mediterranean natural areas
Soil organic carbon (SOC) plays a critical role in the global carbon (C) cycle, and C sequestration in forest soils can represent a C sink. A relevant question is how does SOC changes in space and time; consequently, the study of the influence of topographic aspect on SOC stocks (SOCS) is very impor...
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Published in: | The Science of the total environment 2016-02, Vol.544, p.963-970 |
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Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Soil organic carbon (SOC) plays a critical role in the global carbon (C) cycle, and C sequestration in forest soils can represent a C sink. A relevant question is how does SOC changes in space and time; consequently, the study of the influence of topographic aspect on SOC stocks (SOCS) is very important to build a complete understanding of the soil system. In this line, four topographic aspects, north (N), south (S), east (E) and west (W) were studied under two different plant communities; native forests (NF) and reforested areas (RF) in the Despeñaperros Natural Park (S Spain). Five soil profiles were sampled at each of six different sites, 2 sites for NF (N and E) and 4 sites for RF (N, S, E and W). Soil properties were studied at different depths using soil control sections (S1: 0–25cm; S2: 25–50cm; S3: 50–75cm). The results indicate that RF (N: 147.1Mgha−1; E: 137.3Mgha−1; W: 124.9Mgha−1 and S: 87.0Mgha−1) had increased total SOCS compared to NF (N: 110.4Mgha−1 and E: 80.9Mgha−1), and that SOCS in the N position were higher than in the other topographic aspects. Therefore, the results suggest that topographic aspect should be included in SOCS models and estimations at local and regional scales.
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•The SOC stock was higher in reforested areas than native forest in all aspects.•The soil organic carbon stock depended on topographic aspect.•The behavior of nitrogen stock was similar to soil organic carbon stock.•The stratification ratio of soil organic carbon and nitrogen increased with depth.•All the stratification ratios calculated were >2, this indicated high soil quality. |
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ISSN: | 0048-9697 1879-1026 |
DOI: | 10.1016/j.scitotenv.2015.12.022 |