树木径向生长测量仪的应用研究

doi:10.13466/j.cnki.lyzygl.2019.01.020

摘要/Abstract

摘要：

树轮气候学是研究全球气候变化的重要方法。长期监测树木径向生长是揭示树木径向生长对气候变化响应机理的基础。通过树木径向生长测量仪可以长期、连续且高分辨率地监测记录树木的径向生长。本文从树木径向生长测量仪的研究与应用出发,综述了国内外的研究进展情况,并对未来发展趋势提出展望。

关键词: 树木径向生长测量仪, 日径向生长, 树轮气候学, 季节动态, 全球变化

Abstract:

Dendroclimatology is an important means of studying global climate change.Long-term monitoring of radial growth of trees is the basis for revealing the mechanism of tree radial growth response to climate change.The Tree Radial Growth Gauge is a long-term,continuous,and high-resolution method for monitoring the radial growth of trees.Based on the research and application of tree radial growth measuring instrument,this paper reviews the research progress at home and abroad,and puts forward the prospect of future development trend.

Key words: dendrometer, daily radial grow, dendroclimatology, seasonal dynamics, global change

中图分类号:

S757.2

张月莹, 周志勇. 树木径向生长测量仪的应用研究[J]. 林业资源管理, 2019,(1): 129-135.

ZHANG Yueying, ZHOU Zhiyong. Progress in the Application of Dendrometer[J]. FOREST RESOURCES WANAGEMENT, 2019,(1): 129-135.

图/表 1

参考文献 52

[1]	陈章和, 张德明, 郭志华. 南亚热带气候下三种树木径向生长季节节律研究[J]. 生态学报, 1999,19(6):939-943.
[2]	朱良军, 杨婧雯, 朱辰, 等. 林隙干扰和升温对小兴安岭红松和臭冷杉径向生长的影响[J]. 生态学杂志, 2015,34(8):2085-2095.
[3]	李江风, 袁玉江, 周文盛. 新疆年轮气候年轮水文研究[M]. 北京: 气象出版社, 1989.
[4]	Patrick G J, Farmer J G. A stable lead isotopic investigation of the use of sycamore tree rings as a historical biomonitor of environmental lead contamination[J]. Sci.Total Environ, 2006,362:278-291.
[5]	陈峰, 袁玉江, 魏文寿, 等. 福建沙县马尾松树轮宽度与夏季亚洲-太平洋涛动指数的关系[J]. 第四纪研究, 2011,31(1):96-103.
[6]	D'Arrigo R, Villalba R, Wiles G. Tree-ring estimates of Pacific decadal climate variability[J]. Clim.Dynam., 2001,18:219-224.
[7]	朱良军, 金光泽, 王晓春. 典型阔叶红松林干扰历史重建及干扰形成机制[J]. 植物生态学报, 2015,39(2):125-139.
[8]	Oliveira J M, Roig F A, Pillar V D. Climatic signals intree-rings of Araucaria angustifolia in the southern Brazilian highlands[J]. Austral Ecology, 2010,35(2):134-147.
[9]	Ghasem A. The impact of soil moisture on stem growth of spruce forest during a 22-year period[J]. Forest Ecology and Management, 2002,166:17-33.
[10]	Makinen H, Nêjd P, Saranp3/43/4P.Seasonal changes in stem radius and production of new tracheids in Norway spruce[J]. Tree Physiology, 2003,23:959-968. doi: 10.1093/treephys/23.14.959 pmid: 12952782
[11]	刘玉佳, 朱良军, 苏金娟, 等. 模拟降水减少对帽儿山地区兴安落叶松径向生长的影响[J]. 生态学报, 2015,35(13):4527-4537.
[12]	Sergio R, Tommaso A, Roberto M. Trephor:A new tool forsampling microcores from tree stems[J]. IAWA Journal, 2006,27(1):89-97.
[13]	朱良军, 李宗善, 王晓春. 树轮木质部解剖特征及其与环境变化的关系[J]. 植物生态学报, 2017,41(2):238-251.
[14]	Van Der Werf G W, Sass-Klaassen U G W, Mohren G M J. The impact of the 2003 summer drought on the intra-annualgrowth pattern of beech and oak on a dry site in the Netherlands[J]. Dendrochronologia, 2007,25:103-112.
[15]	Jeong W S, Dieter E, Uwe S. The pinning method:from pinning to data preparation[J]. Dendrochronologia, 2007,25:79-86.
[16]	Herzog KM, H.sle R, Thum R. Diurnal changes in the radius of a subalpine Norway spruce stem:their relation to the sap flow and their use to estimatetranspiration[J]. Trees, 1995,10:94-101.
[17]	Deslauriers A, Morin H, Urbinati C, et al. Daily weather response of balsam fir(Abiesbalsamea(L.)Mill.)stem radius increment from dendrometeranalysis in the boreal forests of Qubec(Canada)[J]. Trees, 2003,17:477-484.
[18]	Braeuning A, Burchardt I. Detection of growth dynamics in tree species of a tropical mountain rain forest in southern Ecuador,trace-tree rings inarchaeology,climatology and ecology[J].Proceedings of the Dedrosymposium, 2005(4):127-131.
[19]	Bohmerle, K. Die Pfister’scheZuwachsuhr[J].Zentralblatt fur das gesamteForstwesen, 1883,9:83-93.
[20]	Friedrich J. Zuwachsmesser[J].Zentralblatt fur das GesamteForstwesen, 1890,16:174-179.
[21]	Breitsprecher A, Hughes W. Arecording dendrometer for humidenvironments[J]. Biotropica, 1975,7:90-99. doi: 10.2307/2989752
[22]	David M D, Geoffrey M D. The use of precision dendrometers in research on daily stem size and wood property variation:A review[J]. Dendrochronologia, 2009,27:159-172. doi: 10.1016/j.dendro.2009.06.008
[23]	Deslauriers A, Rossi S, Anfodillo T. Dendrometer and intra-annual tree growth:What kind of information can be inferred[J]. Dendrochronologia, 2007,25:113-124. doi: 10.1016/j.dendro.2007.05.003
[24]	Deslauriers A, Morin H, Urbinati C, et al. Daily weather response of balsam ﬁr(Abiesbalsamea(L.)Mill.)stem radius increment from dendrometer analysis inthe boreal forests of Quebec(Canada)[J]. Trees 2003,17:477-484. doi: 10.1007/s00468-003-0260-4
[25]	Giovanelli A, Deslauriers A, Fragnelli G, et al.Evaluation of drought response of two poplar clones through high resolution analysis of stem growth[J]. Journal of Experimental Botany, 2007,58:2673-2683. doi: 10.1093/jxb/erm117 pmid: 17545226
[26]	Oberhuber W, Kofler W, Schuster R, et al. Environmental effects on stem water deficit in co-occurring conifers exposed to soil dryness[J]. International Journal of Biometeorology, 2015,59(4):417-426. doi: 10.1007/s00484-014-0853-1 pmid: 24871430
[27]	Aldea J, Bravo F, Vázquez-Piqué J, et al.Species-specific weather response in the daily stem variation cycles of Mediterranean pine-oak mixed stands[J].Agricultural & Forest Meteorology, 2018, s256-257:220-230.
[28]	Achim B, Franziska V V, Iris B, et al. Climatic control of radial growth of Cedrelamontana in a humid mountain rain forest in southern Ecuador[J]. Erdkunde, 2009,63:337-345. doi: 10.3112/erdkunde
[29]	Downes G M, Beadle C, Worledge D. Daily stem growth patterns in irrigated Eucalyptus globulus and E.nitens in relation to climate[J]. Trees, 1999,14:102-111.
[30]	David M D, Geoffrey M D, Valerie G, et al.Differences in daily stem size variation and growth in two hybrid eucalypt clones[J]. Trees, 2009,23:585-595. doi: 10.1007/s00468-008-0303-y
[31]	Dietrich L, Zweifel R, Kahmen A. Daily stem diameter variations can predict the canopy water status of mature temperate trees[J]. Tree Physiology, 2018: 941-952. doi: 10.1093/treephys/16.11-12.941 pmid: 14871787
[32]	Biondi F, Hartsough P. Using automated point dendrometers to analyze tropical treeline stem growth at Nevado de Colima[J]. Mexico.Sensors, 2010,10:5827-5844.
[33]	Wang M, Jiang Y, Dong M, et al. The contributions of rate and duration of stem radial increment to annual increments of Piceameyeri in a sub-alpine habitat,North-Central China[J]. Trees, 2018: 1-13.
[34]	Franco B, Peter H. Using automated point dendrometer to analyze tropical treelin stem growth at Nevado de Colima,Mexico[J]. Sensors, 2010,10:5827-5844. doi: 10.3390/s100605827 pmid: 22219689
[35]	MacDougal, D.T. DendrographicMeasurements[J]. Carnegie Institution of Washington Publication, 1924,350:1-88.
[36]	Marco C, Tommaso A, Carlo U, et al. High-altitude forest sensitivity to global warming:Results from long-term and short-term analyses in the Eastern Italian Alps [C]//Beniston M,Innes J L.The Impacts of Climate Variability on Forest,Lecture Notes in Earth Sciences.Berlin:Springer, 1998: 171-189.
[37]	D. Miller, S.R. Archer, S.F. Zitzer, et al. Annual rainfall,topoedaphic heterogeneity and growth of an arid land tree(Prosopisglandulosa)[J]. Journal of Arid Environments, 2001,48:23-33. doi: 10.1006/jare.2000.0739
[38]	Roseana Pereira daSilva, Joaquim dos Santos, EdgardSiza Tribuzy, et al. Diameter increment and growth patterns for individual tree growing in Central Amazon,Brazil[J]. Forest Ecology and Management, 2002. 166:295-301. doi: 10.1016/S0378-1127(01)00678-8
[39]	McLaughlin S.B., Downing, D.J.Interactive effects of ambient ozone and climate measured on growth of loblolly pine trees[J]. Canadian Journal of Forest Research, 1996,26:670-681. doi: 10.1139/x26-077
[40]	McLaughlin S B, Wullschleger S D, Nosal M. Diurnal and seasonal changes in stem increment and water use by yellow poplar trees in response to environmental stress[J]. Tree Physiology, 2003,23:1125-1136. doi: 10.1093/treephys/23.16.1125 pmid: 14522718
[41]	Karlsson,P E, Orlander G, Uddling J,et al.Verifying the impact of tropospheric ozone on mature Norway spruce trees e a statistical analysis of stem growth of Norway spruce trees in relation to climate change and ozone exposure[C]//In:UNECE workshop report,establishing ozone critical levels II, 2003: 32-335.
[42]	Louis Duchesne, Daniel Houle, Loic” D’Orangeville.Influence of climate on seasonal patterns of stem increment of balsam fir in a boreal forest of Québec,Canada[J]. Agricultural and Forest Meteorology, 2012: 162-163.
[43]	Louis Duchesne, Daniel Houle. Modelling day-to-day stem diameter variation and annual growth of balsam fir(Abiesbalsamea(L.)Mill.)from daily climate[J]. Forest Ecology and Management, 2011,262:863-872. doi: 10.1016/j.foreco.2011.05.027
[44]	杨艳刚, 江源, 张文涛, 等. 芦芽山林线附近华北落叶松茎干生长特征及其与环境因子的关系[J]. 应用与环境生物学报, 2009,15(2):169-174.
[45]	杨艳刚, 张文涛, 任斐鹏, 等. 芦芽山林线组成树种白杄径向生长特征及其与环境因子的关系[J]. 生态学报, 2009,29(12):6793-6804.
[46]	江源, 杨艳刚, 董满宇, 等. 芦芽山林线白杄与华北落叶松径向生长特征比较[J]. 应用生态学报, 2009,20(6):1271-1277.
[47]	董满宇, 江源, 杨浩春, 等. 芦芽山林线白杄生长季径向生长动态[J]. 植物生态学报, 2012,36(9):956-964. doi: 10.3724/SP.J.1258.2012.00956
[48]	熊伟, 王彦辉, 于澎涛, 等. 六盘山南坡华北落叶松(Larix principis-rupprechtii)树干直径生长及其对气象因子的响应[J]. 生态学报, 2007,27(2):432-441.
[49]	管伟, 熊伟, 王彦辉, 等. 六盘山北侧华北落叶松树干直径生长变化及其对环境因子的响应[J]. 林业科学, 2007,43(9):1-6. doi: 10.11707/j.1001-7488.20070901
[50]	王琛, 余新晓, 陈丽华, 等. 树干径向变化对茎液流以及气象因子的响应[J]. 水土保持研究, 2010,17(1):45-55.
[51]	肖生春, 肖洪浪, 司建华, 等. (胡杨Populus euphratica)径向生长日变化特征分析[J]. 冰川冻土, 2010,32(4):816-822.
[52]	肖生春, 肖洪浪, 彭小梅. 黑河下游胡杨季节尺度径向生长变化研究.[J]. 冰川冻土, 2012,34(3):706-712.