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Soil organic carbon sequestration rate and its influencing factors in
Authors
师晨迪
张晓伟
许明祥
邱宇洁
Publication date
1 January 2012
Publisher
Abstract
通过对甘肃省庄浪县梯田土壤采样分析,结合第二次土壤普查及庄浪县耕地质量评价数据,估算梯田土壤固碳速率并分析其影响因素。结果表明:1)该县农田土壤沟谷台地的有机碳含量最高,沟谷、梁峁坡地次之,沟谷川坪地有机碳最低,不同地形有机碳含量差异显著(P<0.05);2)80%的样点土壤有机碳含量在6.0~11.0 g/kg之间,总体上0—20 cm农田土壤有机碳含量呈现正态分布,剖面有机碳含量从上至下呈逐渐递减规律;3)现阶段庄浪县0—20 cm农田土壤有机碳密度为20.02 t/hm2,低于全国耕层土壤有机碳密度平均水平(33.45 t/hm2),近30年0—20 cm土壤固碳速率为C 63 kg/(hm2.a),近5年固碳速率为C 26 kg/(hm2.a);4)在半干旱区县域尺度上,地形部位可解释43%的有机碳变异性,有机肥、坡向和田面坡度三者之和可解释47.1%的有机碳变异性,土壤类型可解释9.9%的有机碳变异性。综合分析表明,庄浪县农田土壤有机碳密度在过去30年间呈增加趋势,可能与庄浪县在60年代开始的大规模梯田建设和水土流失治理有关。</span
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Institute of Soil and Water Conservation,Chinese Academy of Sciences and Ministry of Water Resources
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Last time updated on 21/09/2018