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Variation in Total Soil Organic Carbon Stocks in Relation to Some Land Use Systems in the Bamenda Highlands, Cameroon
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作者 Christian Tegha Kum Aaron Suh Tening +1 位作者 Martin Ngwabie Cornelius Tsamo 《Journal of Geoscience and Environment Protection》 2021年第9期150-165,共16页
Climate change and food security are among the pressing challenges facing humanity in the 21</span><sup><span style="font-family:Verdana;">st</span></sup><span style="fo... Climate change and food security are among the pressing challenges facing humanity in the 21</span><sup><span style="font-family:Verdana;">st</span></sup><span style="font-family:Verdana;"> century. Soil organic carbon (SOC) stocks, total nitrogen (TN), texture, and bulk density (BD) are important soil properties, which control climate change. Three land use systems (smallholder </span></span><span style="font-family:Verdana;">farmlands</span><span style="font-family:Verdana;">, grazing land</span><span style="font-family:Verdana;">s</span><span style="font-family:Verdana;">, and forest lands) that coexist in the </span><span style="font-family:Verdana;">Bamenda Highlands (BH) influence ecosystem</span><span style="font-family:Verdana;"> services and induce soil degradation with the loss of SOC. The objective of this study was to evaluate the variation of SOC and some soil physicochemical properties as affected by the three land use systems (LUS). A total of 21 composite soil samples collected from 7 microclimatic zones of BH following “S” shape plots to the depth of 0 - 30 cm, were analysed for moisture content (MC), SOC, TN, BD, available phosphorus (Av.P), pH and texture. The results revealed that grazing land had the lowest mean sand content (40.79 ± 4.07). Mean MC, TN</span><span style="font-family:Verdana;"> and</span><span style="font-family:Verdana;"> SOC (%) content were significantly higher </span><span style="font-family:""><span style="font-family:Verdana;">(</span><i><span style="font-family:Verdana;">p</span></i><span style="font-family:Verdana;"> < 0.05) </span></span><span style="font-family:Verdana;">in forest land than those </span><span style="font-family:Verdana;">in</span><span style="font-family:Verdana;"> the grazing land </span><span style="font-family:Verdana;">and smallholder farmlands</span><span style="font-family:Verdana;">. Conversely, BD and Av.P were significantly higher</span><span style="font-family:""> </span><span style="font-family:""><span style="font-family:Verdana;">(</span><i><span style="font-family:Verdana;">p</span></i><span style="font-family:Verdana;"> < 0.05)</span></span><span style="font-family:""> </span><span style="font-family:Verdana;">in smallholder farmlands than grazing and forest lands probably due to different</span><span style="font-family:Verdana;"> litter accumulation and agricultural practices. </span><span style="font-family:""><span style="font-family:Verdana;">Moisture content and TN revealed positive significant correlations (</span><i><span style="font-family:Verdana;">p</span></i></span><span style="font-family:""> </span><span style="font-family:Verdana;"><</span><span style="font-family:""> </span><span style="font-family:""><span style="font-family:Verdana;">0.05) with SOC, while BD and Av.P revealed negative significant correlations (</span><i><span style="font-family:Verdana;">p</span></i></span><span style="font-family:""> </span><span style="font-family:Verdana;"><</span><span style="font-family:""> </span><span style="font-family:Verdana;">0.05)</span><span style="font-family:Verdana;">. Mean SOC density in </span><span style="font-family:Verdana;">smallholder farmlands (132.91 ± 9.48 tC/ha)</span><span style="font-family:Verdana;"> was </span><span style="font-family:Verdana;">the </span><span style="font-family:""><span style="font-family:Verdana;">lowest among the three land use types. Losses in CO</span><sub><span style="font-family:Verdana;">2</span></sub><span style="font-family:Verdana;"> equivalence, as a result of land use change </span></span><span style="font-family:Verdana;">from forest lands to smallholder farmlands</span><span style="font-family:Verdana;"> w</span><span style="font-family:Verdana;">ere</span><span style="font-family:Verdana;"> 137.33 t/ha while that from </span><span style="font-family:Verdana;">grazing lands to smallholder farmlands were</span><span style="font-family:Verdana;"> 109.13 t/ha. </span><span style="font-family:""><span style="font-family:Verdana;">Total organic carbon (TOC) stocks differed significantly (</span><i><span style="font-family:Verdana;">p</span></i></span><span style="font-family:""> </span><span style="font-family:Verdana;"><</span><span style="font-family:""> </span><span style="font-family:Verdana;">0.05) from smallholder farmlands (10.73 Mt) to forest lands (91.13 Mt)</span><span style="font-family:Verdana;">. A sustainable farming</span><span style="font-family:""><span style="font-family:Verdana;"> technique that enhances SOC sequestration and minimizes soil CO</span><sub><span style="font-family:Verdana;">2</span></sub><span style="font-family:Verdana;"> emissions is therefore recommended to replace tillage ridges formation commonly practiced by smallholder farmers. 展开更多
关键词 soil soil Organic Carbon Land Use Systems Bamenda Highlands soil co2 emissions
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