城乡梯度森林土壤原易位N矿化

以位于南昌市城乡生态界面的湿地松(Pinus elliottii)人工林为研究对象,开展城区、郊区、乡村3个不同梯度土壤N原位、易位培养试验.结果表明:培养土壤来源对土壤的氨化、硝化速率影响差异极显著(P＜0.001),对净矿化速率影响差异显著(P＜0.05);氨化速率表现为乡村土壤来源(0.11 mg·kg-1·30 d-1)＞郊区土壤来源(-0.92mg·kg-1·30d-1)＞城区土壤来源(-2.02 mg·kg-1·30 d-1);硝化速率表现为乡村土壤来源(0.44 mg·kg-1·30 d-1)较低,城区(3.18 mg·kg-1·30 d-1)和郊区土壤来源(3.35 mg·kg-1·30 d-1)较高;净矿化速率表现为乡村土壤来源(0.54 mg·kg-1·30 d-1)＜城区土壤来源(1.16 mg·kg-1·30 d-1)＜郊区土壤来源(2.43 mg·kg-1·30 d-1).培养位置对氨化速率影响差异不显著(P＞0.05),对硝化速率、净矿化速率影响差异极显著(P＜0.001);硝化速率和净矿化速率均表现为乡村(0.68 mg·kg-1·30 d-1和-0.29 kg·kg-1·30 d-1)和郊区(1.78 mg·kg-1·30 d-1和1.06 mg·kg-1-30 d-1)较低,城区(4.51 mg·kg-1·30 d-1和3.36mg·kg-1·30 d-1)较高.总体来看,土壤N的矿化过程既与土壤理化特性有关,又明显受到城市化的影响.

Soil Nitrogen Mineralization of in situ and Exchange-location Incubation in Forest along an Urban-to-Rural Gradient

Soil nitrogen mineralization of in situ and exchange-location incubation was studied in Pinus elliottii.plantations along a 30 km urban-suburban-rural transect in Nanchang City.The results showed that the effects of incubation soil source on the rates of ammonification,nitrification and net mineralization were significant at the levels of P<0.001 and P<0.05,respectively.The ammonification rate for different incubation soil sources showed an increase tendency with further away from the urban,they were-2.02 m...