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施氮与凋落物去除影响下中亚热带阔叶林土壤氮素矿化潜势和硝化潜势研究
引用本文:陈灿灿,马红亮,高人,尹云峰. 施氮与凋落物去除影响下中亚热带阔叶林土壤氮素矿化潜势和硝化潜势研究[J]. 生态环境学报, 2021, 0(3): 503-511
作者姓名:陈灿灿  马红亮  高人  尹云峰
作者单位:福建师范大学/湿润亚热带山地生态国家重点实验室培育基地;福建师范大学地理科学学院
基金项目:国家自然科学基金项目(31770659);福建省自然科学基金项目(2018J01716)。
摘    要:氮沉降影响土壤氮循环,而凋落物是土壤有机氮的主要来源,因此,为了探讨氮沉降和凋落物是否去除作用下,亚热带森林土壤潜在的氮素矿化与硝化作用,选择已进行8年模拟氮沉降试验的亚热带罗浮栲(Castanopsis fabri)常绿阔叶林土壤为研究对象,野外样地氮添加设置3个水平:对照(CK,0 kg·hm?2·a?1)、低氮(...

关 键 词:氮沉降  森林土壤  凋落物  矿化潜势  硝化潜势

Study on the Potential of Nitrogen Mineralization and Nitrification in Mid-subtropical Broad-leaved Forest Soil Already Treated with Nitrogen Addition and Litter Removal
CHEN Cancan,MA Hongliang,GAO Ren,YIN Yunfeng. Study on the Potential of Nitrogen Mineralization and Nitrification in Mid-subtropical Broad-leaved Forest Soil Already Treated with Nitrogen Addition and Litter Removal[J]. Ecology and Environment, 2021, 0(3): 503-511
Authors:CHEN Cancan  MA Hongliang  GAO Ren  YIN Yunfeng
Affiliation:(State Key Laboratory for Subtropical Mountain Ecology of the Ministry of Science and Technology and Fujian Province/Fujian Normal University,Fuzhou 350007,China;School of Geographical Sciences,Fujian Normal University,Fuzhou 350007,China)
Abstract:Nitrogen (N) deposition impacts soil N cycling by changing nitrogen availability,mineralization rate,and nitrate leaching in a forest ecosystem.Litter input is the main source of soil organic N.However,how N deposition and litter removal or not affect the N cycling remains unclear.Therefore,it is important to study the effects of nitrogen deposition and litter on nitrogen mineralization and nitrification potential in subtropical forest soil.Soil samples were collected from subtropical evergreen broad-leaved forest soil subjected with N deposition[control (CK,0),low nitrogen (LN,75),high nitrogen (HN,150 kg·hm-2·a-1)]and litter removal or not[litter retained (L),litter removal (R)]for 8 years.Then,the difference of N mineralization potential among these soils was studied by intermittent leaching incubation method.The change of nitrification potential under different addition of ammonium N levels (N,0,100,150,200 mg·kg-1) was also investigated.The results showed that the rapid mineralization of soil N mainly occurred before 7 days of incubation.The cumulative amount of N mineralization (Nt) in different soils ranged from 102.81 to153.71 mg·kg-1,and mineralization potential (N0) ranged from 193.84 to 289.80 mg·kg-1.N0 value was in the order:(LN-L)>(CK-L)>(LN-R)>(CK-R)>(HN-R)>(HN-L).Under the conditions with or without litter,Nt and N0 in LN treatment were higher than those in CK and HN,suggesting the organic N in LN soil would be easier to be mineralized,and the N deposition altered the N mineralization potential in the field soil.Under the conditions without the addition of (NH4)2SO4,the nitrification potential was higher in soils subjected with higher N deposition levels.However,the nitrification potential was not increased with the enhancement of the added (NH4)2SO4,and the nitrification potential was the maximum when the (NH4)2SO4 addition was N 100 mg·kg-1 soil.These results suggest that N deposition might alter the N mineralization potential in the subtropical forest soil,even though litter input could increase it.N deposition increases soil nitrate concentration,which might result in a decline of (NH4)2SO4 required for the optimal nitrification potential.Thus,the concentration of (NH4)2SO4 applied in studying soil nitrification potential should be considered according to the soil types and other factors.
Keywords:nitrogen deposition  forest soil  litter  mineralization potential  nitrification potential
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