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半干旱区县域尺度土壤有机碳的空间变异特征

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选择赤峰市敖汉旗为研究对象,收集0~20、20 ~ 40、40~ 60、60~ 80、80~100 cm深度土壤样品,采用半变异函数及克里格插值方法,分析研究区土壤有机碳的空间变异及其垂直分布特征.结果表明,研究区0~100 cm土壤深度内,土壤有机碳含量在0.23~20.71g·kg-1,主要富集在0~40 cm深度的土壤中(47.80%).呈现出随着土壤深度的增加,有机碳含量逐渐降低的趋势.表层(0~20 cm)土壤有机碳的空间相关度[C0/(C+C0)]为36.61%,具有中等强度的空间相关性.20~ 100 cm间4层土壤有机碳的C0/(C+C0)均小于25%,具有强烈的空间相关性.土壤类型是决定土壤有机碳空间分布的主导因素.防止土壤沙化、控制水土流失是提高研究区土壤有机碳含量的有效措施.
Spatial variability of soil organic carbon in semi-arid zone at a county scale
The semivariograms and geo-statistical method were used to analyze the spatial variations of soil organic carbon (SOC) in Aohan Chifeng,Inner Mongolia,based on soil samples from 0-20,20-40,40-60,60-80 and 80-100 cm layers.The results showed that SOC contents ranged between 0.23 and 20.71 g · kg-1 and decreased gradually with increasing soil depth.The spatial correlations [C0/(C+C0) ratio] of SOC contents in the soil layer of 0-20 cm was 36.61% with a moderate spatial correlation,and the C0/(C+C0) ratio of SOC contents in the soil layers of 20-100 cm was <25% with a strong spatial correlation.Soil type was the major factor affecting the spatial variability of SOC content.Prevention of soil and water loss and control of soil desertification might be the effective measures to increase SOC content in the study region.

soil organic carbongeostatisticsspatial variationsoil depth

李龙、姚云峰、秦富仓、郭月峰、高玉寒、张美丽

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内蒙古农业大学生态环境学院,呼和浩特010018

土壤有机碳 地统计学 空间变异 土层深度

内蒙古应用研究与开发计划项目

20110732

2016

生态学杂志
中国生态学学会

生态学杂志

CSTPCDCSCD北大核心
影响因子:1.439
ISSN:1000-4890
年,卷(期):2016.35(8)
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