[1]龙海川,丁超,李策,等.中度火干扰下不同火烧时间对喀纳斯泰加林土壤有机碳的影响[J].黑龙江农业科学,2018,(08):35-38.[doi:DOI:10.11942/j.issn1002-2767.2018.08.0035]
 LONG Hai-chuan,DING Chao,LI Ce,et al.Effects of Different Fire Time on Soil Organic Carbon Under Moderate Fire Disturbance of Taiga Forests in Kanas[J].HEILONGJIANG AGRICULTURAL SCIENCES,2018,(08):35-38.[doi:DOI:10.11942/j.issn1002-2767.2018.08.0035]
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中度火干扰下不同火烧时间对喀纳斯泰加林土壤有机碳的影响

参考文献/References:

[1]孙龙,赵俊,胡海清.中度火干扰对白桦落叶松混交林土壤理化性质的影响[J].林业科学,2011,47(2):103-110.

[2]李媛,程积民,魏琳,等.云雾山典型草原火烧不同恢复年限土壤化学性质变化[J].生态学报,2013,33(7):2131-2138.
[3]孔健健,杨健.林火对大兴安岭落叶松林土壤性质的短期与长期影响[J].生态学杂志,2014,33(6):1445-1450.
[4]王艳霞,杨桂英,张政.火干扰对森林土壤理化性质的影响[J].防护林科技,2012(4):1-3.
[5]Dixon R K,Brown S,Houghton R A,et al.Carbon pools and flux of global forest ecosystems[J].Scienece,1994,263:185-190.
[6]周剑芬,管东生.森林土地利用变化及其对碳循环的影响[J].生态环境,2004,13(4):674-676.
[7]Schlesinger W H,Bernhardt E S.Biogeochemistry:An analysis of global change[J].Academic Press,1991(6):1445-1450.
[8]Trumbore S E,Chadwick O A,Amundson R.Rapid exchange between soil carbon and atmospheric carbon dioxide driven by temperature change[J].Science,1996,272(5260):393-396.
[9]Kimble J M,Heath L S,Birdsey R,et a1.The potential of US forest soils to sequester carbon and mitigate the greenhouse effect[J].CRC Press,2003(1):135-142.
[10]周玉荣,于振良,赵士洞.我国主要森林生态系统碳储量和碳平衡[J].植物生态学报,2000,24(5):518-522.
[11]方运霆,莫江明,Sandra B,等.鼎湖山自然保护区土壤有机碳贮量和分配特征[J].生态学报,2004(1):135-142.
[12]李强,马明东,陈暮初.中亚热带4种森林类型土壤碳密度和碳贮量研究[J].浙江林业科技,2007,27(4):8-12.
[13]Wang Q K,Wang S L.Soil organic matter under different forest types in Southern China[J].Geoderma,2007,142(3/4):349-356.
[14]黄从德,张健,杨万勤,等.四川森林土壤有机碳储量的空间分布特征[J].生态学报,2009,29(3):1217-1225.
[15]Shi Z,Li Y Q,Wang S J,et al.Accelerated soil CO2 efflux after conversion from secondary oak forest to pine plantation in southeastern China[J].Ecological Research,2009,24(6):1257-1265.
[16]孙文义,郭胜利.天然次生林与人工林对黄土丘陵沟壑区深层土壤有机碳氮的影响[J].生态学报,2010,30(10):2611-2620.
[17]Wang H,Liu S R,Mo J M,et al.Soil organic carbon stock and chemical composition in four plantations of indigenous tree species in subtropical China[J].Ecological Research,2010,25(6):1071-1079.
[18]Luan J W,Xiang C H,Liu S R,et al.Assessments of the impacts of Chinese fir plantation and natural regenerated forest on soil organic matter quality at Longmen Mountain,Sichuan,China[J].Geoderma,2010,156(3/4):228-236.
[19]Luan J W,Liu S R,Zhu X L,et al.Soil carbon stocks and fluxes in a warm temperate oak chrono sequence in China[J].Plant and Soil,2011,347(1-2):243-253.
[20]Rashid G H.Effects of fire on soil carbon and nitrogen in a mediterranean oak forest of algeria[J].Plant and Soil,1987,103(1):89-93.
[21]Johnson D W,Curtis P S.Effects of forest management on soil C and N storage:meta analysis[J].Forest Ecology and Management,2001,140(2):227-238.
[22]张荟荟.新疆喀纳斯旅游区森林群落物种多样性特征研究[D].乌鲁木齐:新疆农业大学,2008.
[23]刘光崧.中国生态系统研究网络观测与分析标准方法—土壤理化分析与剖面描述[M].北京:中国标准出版社,1996:103-110.
[24]李媛,程积民,魏琳,等.云雾山典型草原火烧不同恢复年限土壤化学性质变化[J].生态学报,2013,33(7):2131-2138.
[25]骆土寿,陈步峰,陈永富,等.海南岛霸王岭热带山地雨林采伐经营初期土壤碳氮储量[J].林业科学研究,2000(2):123-128.
[26]谷会岩,金屿淞,张芸慧,等.林火对大兴安岭偃松—兴安落叶松林土壤养分的影响[J].北京林业大学学报,2016,38(7):48-54.
[27]孙龙,赵俊,胡海清.中度火干扰对白桦落叶松混交林土壤理化性质的影响[J].林业科学,2011,47(02):103-110.
[28]Hicke J A,Asner G P,Kasischke E S,et al.Postfire response of North American boreal forest net primary productivity analyzed with satellite observations[J].Global Change Biology,2003,9:1145-1157.
[29]Amiro B D,Mac Pherson J I,Desjardins R L.Boreas flight measurements of forestfire effects on carbon dioxide and energy fluxes[J].Agricultural and Forest Meteorology,1999,96:199-208.
[30]Bond Lamberty B,Wang C,Gower S T.Net primary production and net ecosystem production of a boreal black spruce wild fire chrono sequence[J].Global Change Biology,2004,10:473-487.
[31]宿海峰,闫德民,董木森,等.不同强度火烧对恢复植被生态系统碳储量的影响[J].森林防火,2016(1):1002-2511.

备注/Memo

收稿日期:2018-03-13

基金项目:国家级大学生创新训练计划资助项目(2016-10758062)。
第一作者简介:龙海川(1995-),男,在读学士,从事森林碳的研究。E-mail:1207875219@qq.com。

更新日期/Last Update: 2022-12-28