Land-Use Change on Soil C and N Stocks in the Humid Savannah Agro-Ecological Zone of Ghana

Johnny Kofi Awoonor, F. Adiyah, Bright Fafali Dogbey
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引用次数: 3

Abstract

Land-use conversion and unsustainable farming practices are degrading native forest ecosystems of Ghana’s humid savannah agro-ecological zone. This study assessed the impact of land-use change on soil C and N stocks in different land-use systems and soil types. A total of eighty (80) composite soil samples at two depths (0 - 20 cm and 20 - 50 cm) were sampled from five land use types (Forest, Woodland savannah, Grassland, Fallow and Cropland) for laboratory analyses. Particle size distribution, bulk density, pH, SOC and TN were determined using standard procedures. Results of the study indicated that C and N stocks were significantly lower in croplands (p < 0.05) compared to other land-use systems. There were significant interactions (p < 0.05) within land-use systems, soil types, and soil depth for soil C and N stocks. Acrisol and associated soils had the highest C and N stocks. A strong positive significant correlation (p < 0.05) was observed between C and N stocks with an R 2 value of 0.85 and 0.93 for the 0 - 20 and 20 - 50 cm depth, respectively. Soil C and N stocks in the study area were estimated to be 34.56 kg/m 2 and 4.63 kg/m 2 for soil types and 26.89 kg/m 2 and 3.39 kg/m 2 for land use types, respectively for the 0 to 50 cm soil depth. Our findings indicated that the conversion of native forest to arable land has significantly reduced soil C and N stocks in the top 50 cm (0.50 m) soil layer by 50.77% and 47.77%, respectively. Therefore, we conclude that land-use change, soil type, and soil depth influenced soil C and N stocks of land-use systems in the humid savannah agro-ecological zone of Ghana.
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加纳湿润草原农业生态区土地利用变化对土壤碳氮储量的影响
土地利用转换和不可持续的耕作方式正在使加纳潮湿的草原农业生态区的原生森林生态系统退化。本研究评估了不同土地利用制度和土壤类型下土地利用变化对土壤碳氮储量的影响。从5种土地利用类型(森林、林地稀树草原、草地、休耕和农田)中,在0 - 20 cm和20 - 50 cm两个深度共采集80个复合土壤样本进行实验室分析。采用标准程序测定粒径分布、堆积密度、pH、SOC和TN。研究结果表明,与其他土地利用系统相比,农田碳、氮储量显著降低(p < 0.05)。土壤碳氮储量在土地利用系统、土壤类型和土壤深度之间存在显著的交互作用(p < 0.05)。Acrisol及其伴生土壤的碳氮储量最高。在0 ~ 20 cm和20 ~ 50 cm深度,碳储量与氮储量呈显著正相关(p < 0.05), r2分别为0.85和0.93。研究区0 ~ 50 cm土壤深度土壤C、N储量分别为34.56 kg/m 2和4.63 kg/m 2,土地利用类型分别为26.89 kg/m 2和3.39 kg/m 2。结果表明:原生林还田后,50 cm (0.50 m)表层土壤C和N储量分别显著减少50.77%和47.77%。因此,我们认为土地利用变化、土壤类型和土壤深度影响加纳湿润草原农业生态区土地利用系统的土壤C和N储量。
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