土壤水分
碳纤维
土壤碳
环境科学
土壤科学
总有机碳
采样(信号处理)
数学
环境化学
化学
算法
计算机视觉
计算机科学
复合数
滤波器(信号处理)
出处
期刊:Soil Science
[Lippincott Williams & Wilkins]
日期:1986-11-01
卷期号:142 (5): 279-288
被引量:627
标识
DOI:10.1097/00010694-198611000-00006
摘要
Previously published data from 625 paired soil samples were used to predict carbon in cultivated soil as a function of initial carbon content. A 30-cm sampling depth provided a less variable estimate (r2 = 0.9) of changes in carbon than a 15-cm sampling depth (r2 = 0.6). Regression analyses of changes in carbon storage in relation to years of cultivation confirmed that the greatest rates of change occurred in the first 20 yr. An initial carbon effect was present in all analyses: soils very low in carbon tended to gain slight amounts of carbon after cultivation, but soils high in carbon lost at least 20% during cultivation. Carbon losses from most agricultural soils are estimated to average less than 20% of initial values or less than 1.5 kg/cm2 within the top 30 cm. These estimates should not be applied to depths greater than 30 cm and would be improved with more bulk density information and equivalent sample volumes.
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