挪威东南部耕地与混种奶牛长期试验下的土壤碳

H. Riley, T. Henriksen, T. Torp, A. Korsaeth
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引用次数: 2

摘要

在0 ~ 30 cm土壤初始有机碳水平为2.6%的条件下,研究了耕牛混合轮作28年后0 ~ 45 cm土壤有机碳(SOC)。测量包括碳浓度(SOC%)和土壤容重(BD)。总碳投入是根据产量计算的。各系统表层土壤有机碳含量的平均值显著下降(0 ~ 15 cm为- 0.20%,p = 0.04, 15 ~ 30 cm为- 0.39%,p = 0.05),但在30 ~ 45 cm变化不大(+0.11%,p = 0.15)。耕作系统的表层土壤有机碳含量下降幅度往往大于混合乳系统。生物密度的变化与有机碳%的变化呈负相关,强调在评估有机碳储量时需要同时测量两者。0-45 cm的总有机碳质量从98 Mg ha - 1显著下降到89 Mg ha - 1,相当于初始有机碳损失0.3%。系统内的变异很大,但耕地种植表现出高有机碳损失的趋势,而有机碳储量在50%的常规混合奶业和75%的有机混合奶业中变化不大。这些变化与C输入水平有关。混合乳的平均C投入比耕作系统高22%。
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Soil carbon under arable and mixed dairy cropping in a long-term trial in SE Norway
ABSTRACT Soil organic carbon (SOC) was studied at 0–45 cm depth after 28 years of cropping with arable and mixed dairy rotations on a soil with an initial SOC level of 2.6% at 0–30 cm. Measurements included both carbon concentration (SOC%) and soil bulk density (BD). Gross C input was calculated from yields. Averaged over all systems, topsoil SOC% declined significantly (−0.20% at 0–15 cm, p = 0.04, −0.39% at 15–30 cm, p = 0.05), but changed little at 30–45 cm (+0.11%, p = 0.15). Declines in topsoil SOC% tended to be greater in arable systems than in mixed dairy systems. Changes in BD were negatively related to those in SOC%, emphasizing the need to measure both when assessing SOC stocks. The overall SOC mass at 0–45 cm declined significantly from 98 to 89 Mg ha−1, representing a loss of 0.3% yr−1 of the initial SOC. Variability within systems was high, but arable cropping showed tendencies of high SOC losses, whilst SOC stocks appeared to be little changed in conventional mixed dairy with 50% ley and organic mixed dairy with 75% ley. The changes were related to the level of C input. Mean C input was 22% higher in mixed dairy than in arable systems.
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