[1] Braun S, Thomas V F D, Quiring R, et al. Does nitrogen deposition increase forest production? The role of phosphorus[J]. Environmental Pollution, 2010, 158(6):2043-2052. doi: 10.1016/j.envpol.2009.11.030
[2] 李德军, 莫江明, 方运霆, 等.氮沉降对森林植物的影响[J].生态学报, 2003, 23(9):1891-1900. doi: 10.3321/j.issn:1000-0933.2003.09.022
[3] 赵鹏武, 舒洋, 张波, 等.兴安落叶松林凋落物量动态对模拟氮沉降的响应[J].内蒙古农业大学学报:自然科学版, 2016, 37(2):34-39.
[4] 刘修元, 杜恩在, 徐龙超, 等.落叶松原始林树木生长对氮添加的响应[J].植物生态学报, 2015, 39(5):433-441.
[5] Magill A H, Aber J D, Berntson G M, et al. Long-term nitrogen additions and nitrogen saturation in two temperate forests[J]. Ecosystems, 2000, 3(3):238-253. doi: 10.1007/s100210000023
[6] Gough C M, Seiler J R. Belowground carbon dynamics in loblolly pine (Pinus taeda) immediately following diammonium phosphate fertilization[J]. Tree Physiology, 2004, 24(7):845-851. doi: 10.1093/treephys/24.7.845
[7] Janssens I A, Dieleman W, Luyssaert S, et al. Reduction of forest soil respiration in response to nitrogen deposition[J]. Nature Geoscience, 2010, 3(5):315-322. doi: 10.1038/ngeo844
[8] McNulty S G, Aber J D, Newman S D. Nitrogen saturation in a high elevation New England spruce-fir stand[J]. Forest Ecology and Management, 1996, 84(1-3):109-121. doi: 10.1016/0378-1127(96)03742-5
[9] Nakaji T, Fukami M, Dokiya Y, et al. Effects of high nitrogen load on growth, photosynthesis and nutrient status of Cryptomeria japonica and Pinus densiflora seedlings[J]. Trees-Structure and Function, 2001, 15(8):453-461.
[10] 孙涛, 刘瑞鹏, 李兴欢, 等.模拟氮沉降对东北地区兴安落叶松树干呼吸的影响[J].生态学报, 2015, 35(11):3684-3691
[11] Martinelli L A, Piccolo M C, Townsend A R, et al. Nitrogen stable isotopic composition of leaves and soil:tropical versus temperate forests[J]. Biogeochemistry, 1999, 46(1-3):45-65. doi: 10.1007/BF01007573
[12] Thomas R Q, Canham C D, Weathers K C, et al. Increased tree carbon storage in response to nitrogen deposition in the US[J]. Nature Geoscience, 2010, 3(1):13.
[13] Vitousek P M, Howarth R W. Nitrogen limitation on land and in the sea:how can it occur?[J]. Biogeochemistry, 1991, 13(2):87-115.
[14] 胡海清, 罗碧珍, 魏书精, 等.大兴安岭5种典型林型森林生物碳储量[J].生态学报, 2015, 35(17):5745-5760.
[15] 石磊, 盛后财, 满秀玲, 等.兴安落叶松林降雨再分配及其穿透雨的空间异质性[J].南京林业大学学报:自然科学版, 2017, 41(2):90-96.
[16] 闫国永, 王晓春, 邢亚娟, 等.兴安落叶松林细根解剖结构和化学组分对N沉降的响应[J].北京林业大学学报, 2016, 38(4):36-43.
[17] Wright R F, Roelofs J G M, Bredemeier M, et al. NITREX:responses of coniferous forest ecosystems to experimentally changed deposition of nitrogen[J]. Forest Ecology and Management, 1995, 71(1-2):163-169. doi: 10.1016/0378-1127(94)06093-X
[18] 杜恩在.氮添加对兴安落叶松原始林碳收支主要过程的影响[D].北京: 北京大学, 2013.
[19] 顾峰雪, 黄玫, 张远东, 等. 1961-2010年中国区域氮沉降时空格局模拟研究[J].生态学报, 2016, 36(12):3591-3600.
[20] Sheng W, Yu G, Jiang C, et al. Monitoring nitrogen deposition in typical forest ecosystems along a large transect in China[J]. Environmental Monitoring and Assessment, 2013, 185(1):833-844. doi: 10.1007/s10661-012-2594-0
[21] 江泽平.欧洲森林生态系统的氮循环研究近况[J].世界林业研究, 1997, 10(5):55-61.
[22] De Vries W, Du E, Butterbach-Bahl K. Short and long-term impacts of nitrogen deposition on carbon sequestration by forest ecosystems[J]. Current Opinion in Environmental Sustainability, 2014, 9:90-104.
[23] Wang C. Biomass allometric equations for 10 co-occurring tree species in Chinese temperate forests[J]. Forest Ecology and Management, 2006, 222(1):9-16.
[24] 刘欣.不同坡向兴安落叶松径向生长对气候变化响应[D].哈尔滨: 东北林业大学, 2016.
[25] 勾晓华, 陈发虎, 杨梅学, 等.青藏高原东北部树木年轮记录揭示的最高最低温的非对称变化[J].中国科学(D辑:地球科学), 2007, (11):1480-1492.
[26] 刘博奇, 牟长城, 邢亚娟, 等.模拟氮沉降对云冷杉红松林土壤呼吸的影响[J].林业科学研究, 2012, 25(6):767-772. doi: 10.3969/j.issn.1001-1498.2012.06.015
[27] Aber J, McDowell W, Nadelhoffer K, et al. Nitrogen saturation in temperate forest ecosystems[J]. BioScience, 1998, 48(11):921-934. doi: 10.2307/1313296
[28] 王建宇, 王庆贵, 闫国永, 等.原始云冷杉、红松林树木生长对氮沉降的响应[J].北京林业大学学报, 2017, 39(4):21-28.
[29] 郭爱雪, 郭亚芬, 崔晓阳.大兴安岭马尾松林下土壤在不同火烧强度下的养分变化[J].东北林业大学学报, 2011, 39(5):69-71. doi: 10.3969/j.issn.1000-5382.2011.05.022
[30] LeBauer D S, Treseder K K. Nitrogen limitation of net primary productivity in terrestrial ecosystems is globally distributed[J]. Ecology, 2008, 89(2):371-379. doi: 10.1890/06-2057.1