[1]刘潇潇,李国庆,闫美杰,等.黄土高原主要树种树干液流研究进展[J].水土保持研究,2017,24(03):369-373.
　LIU Xiaoxiao,LI Guoqing,YAN Meijie,et al.Research Progress on Stem Sap Flow in Major Tree Species on the Loess Plateau[J].Research of Soil and Water Conservation,2017,24(03):369-373.
点击复制

黄土高原主要树种树干液流研究进展

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 24 期数: 2017年03期 页码: 369-373 栏目: 出版日期: 2017-06-28
Title:
Research Progress on Stem Sap Flow in Major Tree Species on the Loess Plateau
作者:
刘潇潇1,2, 李国庆1,2, 闫美杰1,2, 杜盛1,2
1. 中国科学院 水利部 水土保持研究所, 陕西 杨凌 712100;
2. 西北农林科技大学 黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西 杨凌 712100
Author(s):
LIU Xiaoxiao1,2, LI Guoqing1,2, YAN Meijie1,2, DU Sheng1,2
1. Institute of Soil and Water Conservation, CAS & MWR, Yangling, Shaanxi 712100, China;
2. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A & F University, Yangling, Shaanxi 712100, China
关键词:
黄土高原; 树干液流; 蒸腾耗水; 人工造林
Keywords:
Loess Plateau; sap flow; transpiration water use; artificial afforestation
分类号:
S715
摘要:
为了明晰黄土高原主要树种树干液流的动态特征，该文通过对已发表相关文献搜集与整理（19篇涉及11个树种），采用meta分析手段归纳黄土高原主要树种树干液流动态、耗水规律及其影响因素。研究发现：（1）该区主要树种树干液流存在明显的昼夜变化规律；（2） 太阳辐射、水汽压亏缺、土壤含水率是影响树干液流的主要环境因素；（3）树干液流测量手段、树木生长阶段以及测量时的天气条件会给树木蒸腾耗水估算带来不确定性；（4）11个树种的蒸腾耗水量大小的顺序为：针叶树种（侧柏、油松） < 乡土阔叶树种（白榆、辽东栎、旱柳、柠条、河北杨、小叶杨、山杏） < 外来阔叶树种（刺槐、苹果）。本研究为黄土高原地区造林树种的合理选择及树种耗水评价提供参考。
Abstract:
To clarify the sap flow dynamic characteristics of main tree species on the Loess Plateau, we collected and arranged the relevant 19 published literatures with 11 tree species and a meta analysis was used to summarize the daily dynamics of stem sap flow, water consumption situation and their influence of environmental factors of the 11 tree species. The results suggested that: (1) stem sap flow of the main tree species exhibited diurnal patterns in this area; (2) solar radiation, vapor pressure deficit and soil moisture were the principal factors affecting stem sap flow; (3) estimate of tree water-consumption for transpiration always had uncertainty because of the difference in the methods of measurement, trees growing stage and the weather condition of the measurement; (4) the order of the transpiration in 11 tree species was as following: native coniferous species (Platycladus orientalis, Pinus tabuliformis) < native broadleaved species (Ulmus pumila, Quercus liaotungensis, Salix matsudana, Caragana korshinskii, Populus hopeiensis, Populus simonii, Armeniaca sibirica) < exotic broadleaved species (Robinia pseudoacacia, Malus pumila). This study will provide the reference for selection of afforestation tree species and evaluation of tree water consumption on the Loess Plateau of China.

参考文献/References:

[1] 王进鑫,黄宝龙,王明春,等.不同供水条件下侧柏和刺槐幼树的蒸腾耗水与土壤水分应力订正[J].应用生态学报,2005,16(3):419-425.
[2] 周海光,刘广全,焦醒,等.黄土高原水蚀风蚀复合区几种树木蒸腾耗水特性[J].生态学报,2008,28(9):4568-4574.
[3] ?ermák J, Deml M, Penka M. A new method of sap flow rate determination in trees[J]. Biologia plantarum, 1973,15(3):171-178.
[4] Grime V L, Morison J I L, Simmonds L P. Sap flow measurements from stem heat balances:A comparison of constant with variable power methods[J]. Agricultural and Forest Meteorology, 1995,74(1):27-40.
[5] Nadezhdina N E. Apple tree water relations studied by means of the relative rate of water flow in the trunk xylem[J]. Biologia plantarum, 1992,34(5/6):431-437.
[6] Nadezhdina N, Vandegehuchte M W, Steppe K. Sap flux density measurements based on the heat field deformation method[J]. Trees, 2012,26(5):1439-1448.
[7] Köstner B, Biron P, Siegwolf R et al. Estimates of water vapor flux and canopy conductance of Scots pine at the tree level utilizing different xylem sap flow methods[J]. Theoretical and Applied Climatology, 1996,53(1/3):105-113.
[8] Morikawa Y, Hattori S, Kiyono Y. Transpiration of a31-year-old Chamaecyparis obtusa Endl stand before and after thinning[J]. Tree physiology, 1986,2(1/2/3):105-114.
[9] Misra R K, Sands R. A comparison of sap flux and water relations of leaves of various isolated trees with special reference to foundation movement in clay soil[J]. Plant and Soil, 1992,140(2):269-278.
[10] Grime V L, Morison J I L, Simmonds L P. Including the heat storage term in sap flow measurements with the stem heat balance method[J]. Agricultural and Forest Meteorology, 1995,74(1):1-25.
[11] Lundblad M, Lagergren F, Lindroth A. Evaluation of heat balance and heat dissipation methods for sapflow measurements in pine and spruce[J]. Annals of Forest Science,2001,58(6):625-638.
[12] Ktj?era J,?ermák J, Penka M. Improved thermal method of continual recording the transpiration flow rate dynamics[J]. Biologia Plantarum, 1977,19(6):413-420.
[13] Braun P, Schmid J. Sap flow measurements in grapevines(Vitis vinifera L.)Stem morphology and use of the heat balance method[J]. Plant and Soil, 1999,215(1):39-45.
[14] Burgess S S O, Adams M A, Turner N C, et al. An improved heat pulse method to measure low and reverse rates of sap flow in woody plants[J]. Tree Physiologist, 2001,21(9):589-598.
[15] González-Altozano P, Pavel E W, Oncins J A, et al. Comparative assessment of five methods of determining sap flow in peach trees[J]. Agricultural Water Management, 2008,95(5):503-515.
[16] Poblete-Echeverría C, Ortega-Farias S, Zuñiga M, et al. Evaluation of compensated heat-pulse velocity method to determine vine transpiration using combined measurements of eddy covariance system and microlysimeters[J]. Agricultural Water Management, 2012,109:11-19.
[17] Weibel F P, Boersma K. An improved stem heat balance method using analog heat control[J]. Agricultural and Forest Meteorology, 1995,75(1):191-208.
[18] 张建国,久米朋宣,大规恭一,等.黄土高原半干旱区辽东栎的树干液流动态[J].林业科学,2011,47(4):63-69.
[19] 于占辉,陈云明,杜盛.黄土高原半干旱区侧柏树干液流动态[J].生态学报,2009,29(7) 3970-3976.
[20] 张涵丹,卫伟,陈利顶,等.典型黄土区油松树干液流变化特征分析[J].环境科学,2015,36(1):349-356.
[21] 张建国.黄土高原半干旱区天然辽东栎林蒸腾耗水研究[D].陕西杨凌:中国科学院研究生院(教育部水土保持与生态环境研究中心),2011.
[22] 彭小平.水蚀风蚀交错区不同立地条件下柳树树干液流差异研究[D].陕西杨凌:西北农林科技大学,2014.
[23] 臧春鑫,杨劼,袁劼,等.黄土丘陵沟壑区中间锦鸡儿整株丛树干液流特征与环境因子的关系[J].生态学杂志,2010,29(3):420-426.
[24] 郭宝妮,张建军,王震,等.晋西黄土区刺槐和油松树干液流比较[J].中国水土保持科学,2012,10(4):73-79.
[25] 郭宝妮,张建军,王震,等.晋西黄土区刺槐林耗水特征[J].生态学杂志,2012,31(11):2736-2741.
[26] 孟秦倩,王健,张青峰,等.黄土山地苹果树树体不同方位液流速率分析[J].生态学报,2013,33(11):3555-3561.
[27] 王力,王艳萍.黄土塬区苹果树干液流特征[J].农业机械学报,2013,44(10):152-158.
[28] 吴芳,陈云明,于占辉.黄土高原半干旱区刺槐生长盛期树干液流动态[J].植物生态学报,2010,34(4):469-476.
[29] 张建国,闫美杰,时伟宇,等.辽东栎不同方位边材液流季节动态及其对蒸腾耗水测算的影响[J].水土保持学报,2011,25(3):193-197.
[30] 彭小平,樊军,米美霞,等.黄土高原水蚀风蚀交错区不同立地条件下旱柳树干液流差异[J].林业科学,2013,49(9):38-45.
[31] 夏永秋,邵明安.黄土高原半干旱区柠条(Caragana korshinskii)树干液流动态及其影响因子[J].生态学报,2008,28(4):1376-1382.
[32] 胡伟,杜峰,徐学选,等.黄土丘陵区刺槐树干液流动态分析[J].应用生态学报,2010,21(6):1367-1373.
[33] 于占辉,陈云明,杜盛.黄土高原半干旱区人工林刺槐展叶期树干液流动态分析[J].林业科学,2009,45(4):53-59.
[34] 胡兴波,韩磊,张东,等.黄土半干旱区白榆和侧柏夜间液流动态分析[J].中国水土保持科学,2010,8(4):51-56.
[35] 刘彩风,张志强,郭军庭,等.晋西黄土丘陵沟壑区油松刺槐混交林蒸腾耗水[J].中国水土保持科学,2010,8(5):42-48.
[36] 王华,赵平,王权,等.马占相思夜间树干液流特征和水分补充现象的分析[J].生态学杂志,2007,26(4):476-482.
[37] Ford C R, Goranson C E, Mitchell R J, et al. Diurnal and seasonal variability in the radial distribution of sap flow:predicting total stem flow in Pinus taeda trees[J]. Tree Physiology, 2004,24(9):951-960.
[38] 刘静,孙旭,布和.河套灌区节水措施与黄河下游农业可持续发展[J].生态农业研究,2000,8(4):64-66.
[39] 韩蕊莲,梁宗锁,侯庆春,等.黄土高原适生树种苗木的耗水特性[J].应用生态学报,1994,5(2):210-213.
[40] 周平,李吉跃,招礼军.北方主要造林树种苗木蒸腾耗水特性研究[J].北京林业大学学报,2002,24(5):50-55.

相似文献/References:

[1]白桦,穆兴民,王双银.水土保持措施对秃尾河径流的影响[J].水土保持研究,2010,17(01):40.
　BAI Hua,MU Xing-min,WANG Shuang-yin.Impact of Soil and Water Conservation on River Flow of Tuwei River[J].Research of Soil and Water Conservation,2010,17(03):40.
[2]杨国安,徐勇,郭腾云.基于脆弱性和可持续生计视角的黄土高原生态环境治理研究[J].水土保持研究,2010,17(02):64.
　YANG Guo-an,XU Yong,GUO Teng-yun.Eco-environmental Construction on the Loess Plateau Based on the Perspective of the Vulnerability and Sustainable Livelihoods Approaches[J].Research of Soil and Water Conservation,2010,17(03):64.
[3]肖培青,姚文艺,张海峰.黄土高原植被固土减蚀作用研究进展[J].水土保持研究,2012,19(06):282.
　XIAO Pei-qing,YAO Wen-yi,ZHANG Hai-feng.Research Progress of the Role of Vegetation in Soil Conservtion and Soil Erosion Reduction on the Loess Plateau[J].Research of Soil and Water Conservation,2012,19(03):282.
[4]马芹,张晓萍,万龙,等.黄土高原河龙区间最大日雨量(PMP)极值拟合及时空演变特征[J].水土保持研究,2012,19(02):71.
　MA Qin,ZHANG Xiao-ping,WAN Long,et al.Fitting of the PMP Values and Identifying Its Spatiotemporal Characteristics in the Helong Section on the Loess Plateau[J].Research of Soil and Water Conservation,2012,19(03):71.
[5]卓玛兰草,刘普幸,张亚宁,等.甘肃黄土高原区潜在蒸散量时空变化与成因研究[J].水土保持研究,2012,19(01):70.
　ZHUO Malancao,LIU Pu-xing,ZHANG Ya-ning,et al.Study on Temporal and Spatial Changes of the Potential Evapotranspiration and Its Impact Factors in Loess Plateau of Gansu Province[J].Research of Soil and Water Conservation,2012,19(03):70.
[6]施宇,温仲明,龚时慧,等.黄土丘陵区植物功能性状沿气候梯度的变化规律[J].水土保持研究,2012,19(01):107.
　SHI Yu,WEN Zhong-ming,GONG Shi-hui,et al.Trait Variations along a Climatic Gradient in Hilly Area of Loess Plateau[J].Research of Soil and Water Conservation,2012,19(03):107.
[7]穆兴民,陈国良,徐学选.黄土高原降水量与地理因素关系分析[J].水土保持研究,1992,(02):80.
　Mu Xingmin,Chen Guoliang,Xu Xuexuan.ANALYSIS OF THE RELATIONSHIP BETWEEN PRECIPITATION AND GEOGRAPICAL FACTORS IN LOESS PLATEAU[J].Research of Soil and Water Conservation,1992,(03):80.
[8]刘静.数字化地形模型（DTM）在水土保持中的应用[J].水土保持研究,1992,(02):96.
　Liu Jeng.ESTABLSHING AND APPLICATION OF DTM FOR SOIL AND WATER CONSERVATION[J].Research of Soil and Water Conservation,1992,(03):96.
[9]赵安成.陇东黄土高原沟壑区典型小流域治理模式剖析[J].水土保持研究,1994,1(01):45.
　Zhao Ancheng.Analysis of Control Models of Typical Small Watershedin Gully Area of Loess Plateau, the East Part of Gansu Province[J].Research of Soil and Water Conservation,1994,1(03):45.
[10]吴钦孝,汪有科,韩冰,等.黄土高原水土流失区的林草资源和植被建设[J].水土保持研究,1994,1(03):2.
　Wu Qinxiao,Wang Youke,Han Bing,et al.Forest and Grassland Resources and Vegetation Construction in The Soil and Water Loss Region of The Loess Plateau[J].Research of Soil and Water Conservation,1994,1(03):2.

备注/Memo

收稿日期:2016-05-17;改回日期:2016-06-02。
基金项目:国家自然科学基金（41471440，41411140035，41171419）
作者简介:刘潇潇(1992-),女,陕西省洋县人,硕士研究生,研究方向为植物生理生态。E-mail:530397914@qq.com
通讯作者:杜盛(1965-),男,内蒙古鄂尔多斯人,博士,研究员,主要从事森林生态、流域生态与管理研究。E-mail:shengdu@ms.iswc.ac.cn

更新日期/Last Update: 1900-01-01