论文部分内容阅读
对中国科学院沈阳生态实验站潮棕壤在水稻田、玉米地、撂荒地和林地等经过14年不同利用方式后0-150cm各土层(2003年11月取样)N的剖面分布及N储量进行研究的结果表明:不同利用方式下土壤全N、碱解N、NH4+-N和NO3--N含量发生明显的剖面差异;土壤N储量为林地>玉米地>撂荒地>水稻田,NO3--N含量为玉米地>水稻田>林地>撂荒地,说明不同利用方式下生物量差异及N的生物循环对N行为的影响.100cm深度林地土壤平均N储量为11.41 t@hm-2,分别是水稻田和玉米地土壤的1.65和1.25倍,而玉米地和撂荒地的土壤N储量无显著差异.玉米地和水稻田相对较高的NO3--N 含量可能由于过量施用N肥和人为干扰所致.土壤碱解N与全N含量呈线性正相关关系(R2≥0.929, pmaize field > fallow field > paddy field, while that of NO3--N content was maize field > paddy field > woodland > fallow field, suggesting the different root biomass and biological N cycling under various land uses. The STN storage in the depth of 0-100 cm of woodland averaged to 11.41 t·hm-1, being 1.65 and 1.25 times as much as that in paddy and maize fields, respectively, while there was no significant difference between maize and fallow fields. The comparatively higher amount of NO3--N in maize and paddy fields may be due to nitrogen fertilization and anthropogenic disturbance. Soil alkali N was significantly related with STN, and the correlation could be expressed by a linear regression model under each land use (R2≥0.929, p<0.001). Such a correlation was slightly closer in nature (woodland and fallow field) than in agro ecosystems (paddy and maize fields). Heavy N fertilization induced an excess of crop need, and led to a comparatively higher amount of soil NO3--N in cultivated fields than in fallow field and woodland. It is suggested that agroforestry practices have the potential to make a significant contribution to both crop production and environment protection.