[1]LIU Kaixi,ZENG Biao,YANG Taibao,et al.Analysis of Tree Ring Width Index and Its Relationship with NDVI in Qinghua Forest of Chongqing[J].Research of Soil and Water Conservation,2015,22(03):170-175.
Copy

Analysis of Tree Ring Width Index and Its Relationship with NDVI in Qinghua Forest of Chongqing

References:
[1] 徐德应.中国森林与全球气候变化的关系[J].林业科技管理,2002(4):23-27.
[2] 宫超,汪思龙,曾掌权,等.中亚热带常绿阔叶林不同演替阶段碳储量与格局特征[J].生态学杂志,2011,30(9):1935-1941.
[3] 沃晓棠,田松岩,韩丽冬,等.小兴安岭两种林型的土壤有机碳研究[J].水土保持研究,2014,21(5):13-23.
[4] 库姆斯J,霍尔D O,朗S P,等.生物生产力和光合作用测定技术[M].北京:科学出版社,1986.
[5] 刘正佳,邵全琴.三江源地区植被覆盖度变化及其与气候因子的关系[J].水土保持研究,2014,21(6):334-339.
[6] 何吉庆,王丽丽,邵雪梅.漠河樟子松树轮指数与标准化植被指数的关系研究[J].第四纪研究,2005,25(2):252-257.
[7] Wang J, Rich P M, Price K P, et al. Relations between NDVI and tree productivity in the central Great Plains[J]. International Journal of Remote Sensing,2004,25(16):3127-3138.
[8] 范玮熠,王孝安.树木年轮宽度与气候因子的关系研究进展[J].西北植物学报,2004,24(2):345-351.
[9] 李坚,刘一星,崔永志,等.人工林杉木幼龄与成熟材的界定及材质早期预测[J].东北林业大学学报,1999,27(4):24-28.
[10] Fritts H C. Tree Rings and Climate[M]. London:Academic Press,1976.
[11] Cook E R. A Time Series Analysis Approach to Tree Ring Standardization[M]. Tucson:Univ. of Arizona,1985.
[12] 吴文斌,杨鹏,唐华俊,等.两种NDVI时间序列数据拟合方法比较[J].农业工程学报,2009,25(11):183-188.
[13] 商志远,王建,崔明星,等.樟子松树轮δ13C的年内变化特征及其对气候要素的响应[J].植物生态学报,2012,36(12):1256-1267.
[14] 吴祥定.树木年轮与气候变化[M].北京:气象出版社,1990.
[15] 崔明星,何兴元,陈玮,等.河北木兰围场油松年轮生态学的初步探究[J].应用生态学报,2008,19(11):2339-2345.
[16] 刘灿,高阳华,李月臣,等.基于NDVI的重庆市植被覆盖变化及其对气候因子的响应[J].长江流域资源与环境,2013,22(11):1514-1520.
[17] 陈忠辉.植物与植物生理[M].北京:中国农业出版社,2001.
[18] Smith J L, Paul E A. Use of anin situ labeling technique for the determination of seasonal 14C distribution in Ponderosa pine[J]. Plant and Soil,1988,106(2):221-229.
[19] Lacointe A, Kajji A, Daudet F A, et al. Mobilization of carbon reserves in young walnut trees[J]. Acta Botanica Gallica,1993,140(4):435-441.
[20] Hoch G, Richter A, K?rner C. Non-structural carbon compounds in temperate forest trees[J]. Plant, Cell & Environment,2003,26(7):1067-1081.
[21] Robertson I, Loader N J, McCarroll D, et al. δ13C of Tree-ring lignin as an indirect measure of climate change[J]. Water, Air and Soil Pollution:Focus,2004,4(2/3):531-544.
[22] Leavitt S W, Long A. Evidence for 13C/12C fractionation between tree leaves and wood[J]. Nature,1982,298:742-743.
[23] 罗宗洛.植物生理知识[M].北京:科学出版社,1973.
[24] Porté A, Loustau D. Seasonal and interannual variations in carbon isotope discrimination in a maritime pine (Pinus pinaster) stand assessed from the isotopic composition of cellulose in annual rings[J]. Tree Physiology,2001,21(12/13):861-868.
Similar References:

Memo

-

Last Update: 1900-01-01

Online:11450       Total Traffic Statistics:27380715

Website Copyright: Research of Soil and Water Conservation Shaanxi ICP No.11014090-10
Tel: 029-87012705 Address: Editorial Department of Research of Soil and Water Conservation, No. 26, Xinong Road, Yangling, Shaanxi Postcode: 712100