大兴安岭北部兴安落叶松树干液流规律及影响因子分析

池波; 蔡体久; 满秀玲; 李奕

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

大兴安岭北部兴安落叶松树干液流规律及影响因子分析

池波, 蔡体久, 满秀玲, 李奕

文章导航 > 北京林业大学学报 > 2013 > 35(4): 21-26

池波, 蔡体久, 满秀玲, 李奕. 大兴安岭北部兴安落叶松树干液流规律及影响因子分析[J]. 北京林业大学学报, 2013, 35(4): 21-26.

引用本文:

池波, 蔡体久, 满秀玲, 李奕. 大兴安岭北部兴安落叶松树干液流规律及影响因子分析[J]. 北京林业大学学报, 2013, 35(4): 21-26.

CHI Bo, CAI Ti-jiu, MAN Xiu-ling, LI Yi.. Effects of influencing factors on stem sap flow in Larix gmelinii in northern Da Hinggan Mountains, northeastern China.[J]. Journal of Beijing Forestry University, 2013, 35(4): 21-26.

Citation:

CHI Bo, CAI Ti-jiu, MAN Xiu-ling, LI Yi.. Effects of influencing factors on stem sap flow in Larix gmelinii in northern Da Hinggan Mountains, northeastern China.[J]. Journal of Beijing Forestry University, 2013, 35(4): 21-26.

大兴安岭北部兴安落叶松树干液流规律及影响因子分析

1.
东北林业大学林学院

Effects of influencing factors on stem sap flow in Larix gmelinii in northern Da Hinggan Mountains, northeastern China.

1.
College of Forestry, Northeast Forestry University, Harbin, 150040,P. R. China.

摘要: 利用Granier 热扩散植物液流技术(TDP),于2012 年5—9 月连续对大兴安岭北部兴安落叶松蒸腾进行测定, 结合同步观测的环境因子,分析兴安落叶松树干液流规律及其与环境因子的关系。结果表明:1) 兴安落叶松蒸腾速率具有明显的昼夜变化规律,晴天和阴天均为单峰曲线,雨天为双峰曲线,且晴天和阴天的蒸腾速率高于雨天。夜间液流通量占整日液流通量的百分比为晴天(5.91%) 雨天(4.88%) 阴天(2.57%),在高温无雨情况下,液流通量呈现随高温无雨日数的增加而逐渐降低的趋势。2) 6—8 月兴安落叶松蒸腾量占观测期总耗水量的80%, 液流速率日峰值较高,其中7 月最高达23.6 cm3 / (cm2·h),5 月次之,9 月最低为2.03 cm3 / (cm2·h)。3) 边材液流速率与环境因子存在良好的相关性,多元回归模型决定系数为0郾79;影响兴安落叶松树干液流的主要影响因子为蒸汽压亏缺和光合有效辐射。4) 生长季内兴安落叶松林蒸腾耗水量为566郾49 t/ hm2 ,即56郾65 mm,占同期降雨量的12%。
- Granier 热扩散法 /
- 兴安落叶松 /
- 树干液流 /
- 环境因子 /
- 林分蒸腾量
Abstract: In this study, by Granier thermal dissipation probe (TDP) method, Larix gmelinii transpiration was continuously observed in northern Da Hinggan Mountains, northeastern China from May to September in 2012. Integrated with simultaneous environmental factors, transpiration of L. gmelinii and its relationship with influencing factors were investigated. The results showed that: 1) L. gmelinii transpiration rate showed significant diurnal variations, which presented unimodal curves in sunny and cloudy days, and bimodal or multimodal curves in rainy days, respectively. Transpiration rates of sunny and cloudy days were higher than those of rainy days. The ratio list of night sap flow flux accounting for a full day's flow flux was: sunny day(5.91%) rainy day (4.88%) cloudy day(2.57%). In the case of high temperature and no rain, the sap flow presented a decreasing trend with the rainless and hot days increasing. 2) Daily peak of L. gmelinii sap flow rate was high in June to August, and it reached the highest value of 23.6 cm3 / (cm2·h) in July, the transpiration in June to August accounted for 80% of the total water consumption during observation period. The daily peak in May was less and it got the lowest value of 2.03 cm3 / (cm2·h) in September. 3) Good correlation existed between sap flow rate and environmental factors, just as the coefficient of determination of their multiple regression model was 0.79. Further correlation analyses indicated that main environmental factors influencing sap flow density in the growing season were vapor pressure deficit and photosynthetic active radiation. 4) The total transpiration of L. gmelinii stand during the growing season was 566.49 t/ hm2, i. e. 56.65 mm, accounted for 12% of rainfall in the same period.
- Granier's thermal dissipation probe method /
- Larix gmelinii /
- stem sap flow /
- environmental factors /
- stand transpiration

[1]	马菁, 郭建斌, 刘泽彬, 王彦辉, 张紫优. 六盘山华北落叶松林分蒸腾日内变化及其对环境因子的响应 . 北京林业大学学报, 2020, 42(): 1-11. doi: 10.12171/j.1000-1522.20190468
[2]	孙振静, 赵慧颖, 朱良军, 李宗善, 张远东, 王晓春. 大兴安岭北部不同降水梯度下兴安落叶松生长对升温的响应差异 . 北京林业大学学报, 2019, 41(6): 1-14. doi: 10.13332/j.1000-1522.20190007
[3]	张俪予, 张军辉, 张蕾, 陈伟, 韩士杰. 兴安落叶松和白桦细根形态对环境变化的响应 . 北京林业大学学报, 2019, 41(6): 15-23. doi: 10.13332/j.1000-1522.20180396
[4]	刘崴, 魏天兴, 朱清科. 水蚀风蚀交错区河北杨树干液流密度特征及其对环境因子的响应 . 北京林业大学学报, 2018, 40(5): 73-81. doi: 10.13332/j.1000-1522.20180003
[5]	鱼腾飞, 冯起, 司建华, 张小由, 赵春彦. 胡杨的夜间蒸腾——来自树干液流、叶片气体交换及显微结构的证据 . 北京林业大学学报, 2017, 39(9): 8-16. doi: 10.13332/j.1000-1522.20160332
[6]	姜立春, 潘莹, 李耀翔. 兴安落叶松枝条特征联立方程组模型及树冠形状模拟 . 北京林业大学学报, 2016, 38(6): 1-7. doi: 10.13332/j.1000-1522.20150339
[7]	欧光龙, 胥辉, 王俊峰, 肖义发, 陈科屹, 郑海妹. 思茅松天然林林分生物量混合效应模型构建 . 北京林业大学学报, 2015, 37(3): 101-110. doi: 10.13332/j.1000-1522.20140316
[8]	李小梅, 张秋良. 环境因子对兴安落叶松林生态系统CO2通量的影响 . 北京林业大学学报, 2015, 37(8): 31-39. doi: 10.13332/j.1000-1522.20150020
[9]	赵冰清, 王云琦, 王彬, 王玉杰, 张会兰. 环境因子对重庆缙云山林地土壤呼吸动态特征的作用 . 北京林业大学学报, 2014, 36(3): 83-89. doi: 10.13332/j.cnki.jbfu.2014.03.012
[10]	林健, 刘文波, 孟昭军, 严善春. 落叶松单萜类挥发物微胶囊缓释剂对落叶松毛虫寄主选择行为的影响 . 北京林业大学学报, 2014, 36(3): 42-47. doi: 10.13332/j.cnki.jbfu.2014.03.006
[11]	李新宇, 李延明, 孙林, 许蕊1, 赵松婷, 郭佳. 银杏蒸腾耗水与环境因子的关系研究 . 北京林业大学学报, 2014, 36(4): 23-29. doi: 10.13332/j.cnki.jbfu.2014.04.008
[12]	王秀伟, 毛子军. 输导组织结构对液流速度和树干CO2 释放通量的影响 . 北京林业大学学报, 2013, 35(4): 9-15.
[13]	楚旭, 邸雪颖, 杨光. 林火对兴安落叶松根生物量及碳氮养分浓度的影响 . 北京林业大学学报, 2013, 35(2): 10-16.
[14]	周海宾, 江京辉, 王学顺, 任海青. 兴安落叶松目测等级锯材抗拉强度的宽度尺寸效应 . 北京林业大学学报, 2012, 34(1): 127-130.
[15]	夏磊, 赵志新, 汤玲, 李小乐, 刘磊, 李名扬. 重庆地区加拿利海枣夏季光合日变化与主要环境因子的关系 . 北京林业大学学报, 2011, 33(4): 75-80.
[16]	杨爱国, 张建秋, 毕庆玲, 张玉玲, 王凤林, 范鹏辉. 吉林省西部不同造林密度杨树耗水特性的研究 . 北京林业大学学报, 2011, 33(6): 142-145.
[17]	王连春, 翟明普, 刘道平, 周志峰, . 酸枣树干液流速率与环境因子的关系 . 北京林业大学学报, 2009, 31(6): 134-138.
[18]	董百丽, 王淼, 姜萍, 姬兰柱. 长白山北坡水甲虫多样性与环境因子的关系 . 北京林业大学学报, 2008, 30(1): 74-78.
[19]	许景伟, 高克昌, 张志山, 邵杰, 奚如春, 金则新, 周睿, 张春晓, 李俊, 武林, 郑景明, 李黎, 周艳萍, 吴家兵, 陆平, 于海霞, 雷妮娅, 郎璞玫, 于文吉, 张建军, 孙志蓉, 宋先亮, 刘足根, 焦雯珺, 索安宁, 马玲, 吕文华, 盖颖, 陈勇, 蔡锡安, 张小由, 葛剑平, 习宝田, 赵文喆, 马履一, 纳磊, 朱教君, 韦方强, Kwei-NamLaw, 饶兴权, 李传荣, 毕华兴, 关德新, 李钧敏, 郑红娟, 赵秀海, 戴伟, 余养伦, 赵广杰, 于志明, 翟明普, 陈少良, 朱清科, 马履一, 朱艳燕, ClaudeDaneault, 王瑞刚, 袁小兰, 方家强, 崔鹏, 李俊清, 于波, 贾桂霞, 张弥, 谭会娟, 江泽慧, 杨永福, 张春雨, 张宇清, 曾小平, 夏良放, 王文全, 樊敏, 赵平, 李笑吟, 王天明, 李增鸿, 张欣荣, 李丽萍, 邓宗付, 王卫东, 刘丽娟, 袁飞, 王贺新, 贺润平, 唐晓军, 殷宁, 韩士杰, 陈雪梅, 郭孟霞, 李庆卫, 何明珠, 吴秀芹, 王旭琴, 王月海, 王娜, 熊颖, 郑敬刚, 孔俊杰, 刘鑫, 毛志宏, 吴记贵, 于贵瑞, 蒋湘宁, 江杰, 孙晓敏, 李新荣, 林靓靓, 王瑞辉, 聂立水, 王贵霞, 葛剑平, 郭超颖, 董治良. 马占相思整树蒸腾的日变化和季节变化特征 . 北京林业大学学报, 2007, 29(1): 67-73.
[20]	李黎, 张德荣, 戴松香, 马宇飞, 李雪玲, 高岩, 赵晓松, 郭明辉, 田晶会, 王小丹, 王瑞刚, 华丽, 黄荣凤, 董运斋, 曹世雄, 邵海荣, 黄华国, 贺庆棠, 陈少良, 陈少良, 张晓丽, 闫丽, 习宝田, 王四清, 陈斌如, 金幼菊, 阎海平, 贺庆棠, 关德新, 古川郁夫, 于志明, 冷平生, 李文彬, 贺康宁, 李俊清, 高攀, 高双林, 刘力源, 邹祥旺, 王百田, 任云卯, 阎海平, 杨永福, 吴家兵, 李建章, 鲍甫成, 王蕾, 李海英, 陈莉, 赵有科, 郝志勇, 程根伟, 侯智, 王金满, 侯智, 陈华君, 张卫强, 陈源泉, 金小娟, 金昌杰, 杜建军, 韩士杰, 尹婧, 李涛, 高旺盛, 翁海娇, 赵琼, 李鹤, 杨爽, 段杉. 黄土半干旱区侧柏蒸腾作用及其与环境因子的关系 . 北京林业大学学报, 2005, 27(3): 53-56.

点击查看大图

计量

文章访问数: 782
HTML全文浏览量: 78
PDF下载量: 91
被引次数: 0

大兴安岭北部兴安落叶松树干液流规律及影响因子分析

1. 东北林业大学林学院

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2013-07-30

关键词:

摘要: 利用Granier 热扩散植物液流技术(TDP),于2012 年5—9 月连续对大兴安岭北部兴安落叶松蒸腾进行测定, 结合同步观测的环境因子,分析兴安落叶松树干液流规律及其与环境因子的关系。结果表明:1) 兴安落叶松蒸腾速率具有明显的昼夜变化规律,晴天和阴天均为单峰曲线,雨天为双峰曲线,且晴天和阴天的蒸腾速率高于雨天。夜间液流通量占整日液流通量的百分比为晴天(5.91%) 雨天(4.88%) 阴天(2.57%),在高温无雨情况下,液流通量呈现随高温无雨日数的增加而逐渐降低的趋势。2) 6—8 月兴安落叶松蒸腾量占观测期总耗水量的80%, 液流速率日峰值较高,其中7 月最高达23.6 cm3 / (cm2·h),5 月次之,9 月最低为2.03 cm3 / (cm2·h)。3) 边材液流速率与环境因子存在良好的相关性,多元回归模型决定系数为0郾79;影响兴安落叶松树干液流的主要影响因子为蒸汽压亏缺和光合有效辐射。4) 生长季内兴安落叶松林蒸腾耗水量为566郾49 t/ hm2 ,即56郾65 mm,占同期降雨量的12%。

English Abstract

Effects of influencing factors on stem sap flow in Larix gmelinii in northern Da Hinggan Mountains, northeastern China.

1. College of Forestry, Northeast Forestry University, Harbin, 150040,P. R. China.

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2013-07-30

Keywords:

Granier's thermal dissipation probe method /
Larix gmelinii /
stem sap flow /
environmental factors /
stand transpiration

Abstract: In this study, by Granier thermal dissipation probe (TDP) method, Larix gmelinii transpiration was continuously observed in northern Da Hinggan Mountains, northeastern China from May to September in 2012. Integrated with simultaneous environmental factors, transpiration of L. gmelinii and its relationship with influencing factors were investigated. The results showed that: 1) L. gmelinii transpiration rate showed significant diurnal variations, which presented unimodal curves in sunny and cloudy days, and bimodal or multimodal curves in rainy days, respectively. Transpiration rates of sunny and cloudy days were higher than those of rainy days. The ratio list of night sap flow flux accounting for a full day's flow flux was: sunny day(5.91%) rainy day (4.88%) cloudy day(2.57%). In the case of high temperature and no rain, the sap flow presented a decreasing trend with the rainless and hot days increasing. 2) Daily peak of L. gmelinii sap flow rate was high in June to August, and it reached the highest value of 23.6 cm3 / (cm2·h) in July, the transpiration in June to August accounted for 80% of the total water consumption during observation period. The daily peak in May was less and it got the lowest value of 2.03 cm3 / (cm2·h) in September. 3) Good correlation existed between sap flow rate and environmental factors, just as the coefficient of determination of their multiple regression model was 0.79. Further correlation analyses indicated that main environmental factors influencing sap flow density in the growing season were vapor pressure deficit and photosynthetic active radiation. 4) The total transpiration of L. gmelinii stand during the growing season was 566.49 t/ hm2, i. e. 56.65 mm, accounted for 12% of rainfall in the same period.

池波, 蔡体久, 满秀玲, 李奕. 大兴安岭北部兴安落叶松树干液流规律及影响因子分析[J]. 北京林业大学学报, 2013, 35(4): 21-26.

引用本文:

池波, 蔡体久, 满秀玲, 李奕. 大兴安岭北部兴安落叶松树干液流规律及影响因子分析[J]. 北京林业大学学报, 2013, 35(4): 21-26.

Citation: