1. 湖南师范大学地理科学学院,长沙,410081
2. 湖南师范大学地理空间大数据挖掘与应用湖南省重点实验室,长沙,410081
[ "夏银华(1995-),女,硕士研究生,主要从事亚热带生态水文研究。E-mail:939973367@qq.com" ]
纸质出版:2021
移动端阅览
夏银华, 章新平, 戴军杰, 等. 亚热带季风区樟树蒸腾与气象因子之间的时滞效应[J]. 水土保持学报, 2021,35(5):194-203.
XIA Yinhua, ZHANG Xinping, DAI Junjie, et al. Time-lag Effects Between Meteorological Factors and Transpiration of[J]. 2021, 35(5): 194-203.
夏银华, 章新平, 戴军杰, 等. 亚热带季风区樟树蒸腾与气象因子之间的时滞效应[J]. 水土保持学报, 2021,35(5):194-203. DOI: 10.13870/j.cnki.stbcxb.2021.05.027.
XIA Yinhua, ZHANG Xinping, DAI Junjie, et al. Time-lag Effects Between Meteorological Factors and Transpiration of[J]. 2021, 35(5): 194-203. DOI: 10.13870/j.cnki.stbcxb.2021.05.027.
以亚热带地区常绿阔叶树种樟树(Cinnamomum camphora)为研究对象,利用Grainer热扩散式探针技术,于2019年6月至2020年10月测定了樟树小时尺度的蒸腾速率,并同步监测了气象因子和土壤含水量,分析了樟树蒸腾在日间不同时段与主要气象因子的关系、时滞的变化特征以及时滞校正对蒸腾预测模型的影响。结果表明:蒸腾在生长季(6—10月)与太阳辐射的时滞回环呈逆时针,与饱和水汽压差和气温的时滞回环呈顺时针。利用Gauss方程拟合发现,2019年与2020年生长季蒸腾平均滞后于太阳辐射0.94 h,提前于饱和水汽压差和气温2.60,2.61 h。这种时滞效应是蒸腾在日内不同阶段对气象因子的响应不同导致的,蒸腾在上升阶段(7:00—11:00)对太阳辐射变化的响应较下降阶段(17:00—21:00)敏感,而在上升阶段蒸腾对饱和水汽压差和气温变化的响应不如下降阶段敏感。蒸腾与太阳辐射、饱和水汽压差和气温的时滞效应存在明显的季节变化,2019年与2020年的归一化时滞回环面积存在一定差异,但均在10月最大,8月或9月最小。小时尺度上,土壤水分充足时,时滞随主要日均气象因子的增大而增大,土壤水分胁迫时,随主要日均气象因子的增大,时滞变化不明显。时滞校正后,太阳辐射和饱和水汽压差与蒸腾的回归方程的决定系数分别提高了4%和9%,运用主成分分析构造的综合气象因子对蒸腾模拟的决定系数提高了7%,时滞校正可以提高蒸腾预测模型的精度。旨在加深对植物生理过程与环境变化过程关系的认识,并为提高蒸腾预测模型的精度提供依据。
In this study
the hourly transpiration rate of Cinnamomum camphora was measured from June 2019 to October 2020 using the Grainer-type thermal dissipation probes. Meteorological factors and soil water content were simultaneously monitored during the study period. To deepen the understanding of the relationship between plant physiological changes and environmental changes
and to provide a basis for improving the accuracy of transpiration predicting model
this study analyzed the relationship between the transpiration of C. camphora and the main meteorological factors at different periods during the day. The variation characteristics of time lag and the change of hysteresis correction on the predicting model of transpiration were also investigated. The results showed that the time lag between transpiration and solar radiation is counterclockwise
and that between transpiration and saturated water vapor pressure or temperature is clockwise during the growing seasons (from June to October). Based on Gauss equations
it was found that on average transpiration in the growing seasons of 2019 and 2020 lagged behind solar radiation by 0.94 hours
and advanced by 2.60 and 2.61 hours on saturated vapor pressure difference and temperature. This time-lag effect was caused by the different responses of transpiration to meteorological factors at different stages of the day. In the rising stage (7:00-11:00)
transpiration was more sensitive to changes of solar radiation than that in the descending stage (17:00-21:00). On the contrary
in the rising stage
transpiration was less sensitive to variation in saturated vapor pressure and temperature than that in the descending stage. The time-lag effects between transpiration and solar radiation or saturated vapor pressure or temperature had obvious seasonal variation. There were certain differences in the hysteresis loop area between the growing seasons of 2019 and 2020
but the maximum area appeared in October and the minimum area appeared in August or September. On the hourly scale
when soil moisture was sufficient
the hysteresis added with the increase of the main daily mean meteorological factors
but under soil moisture stress
the time lag did not change significantly with the increase of the major daily mean meteorological factors. After correcting time lag
the determinants of the regression equations of transpiration and solar radiation increased by 4% and 9%
and the coefficient of determination of the regression equations of transpiration and integrated meteorological factors constructed by principal component analysis increased by 7%. Therefore
eliminating time lag could improve the accuracy of transpiration predicting model.
韩磊, 孙兆军, 展秀丽, 等.宁夏河东沙区柠条植株叶片蒸腾对干旱胁迫的响应[J]. 生态环境学报, 2015, 24(5):756-761.
贾国栋, 陈立欣, 李瀚之, 等.北方土石山区典型树种耗水特征及环境影响因子[J]. 生态学报, 2018, 38(10):3441-3452.
Phillips N, Oren R, Zimmermann R, et al. Temporal patterns of water flux in trees and lianas in a Panamanian moist forest[J]. Trees, 1999, 14(3):116-123.
Zhang R F, Xu X L, Liu M X, et al. Hysteresis in sap flow and its controlling mechanisms for a deciduous broad-leaved tree species in a humid karst region[J]. Science China Earth Sciences, 2019, 62(11):1744-1755.
韩磊, 展秀丽, 王芳, 等.河东沙区侧柏树干液流与蒸腾驱动因子的时滞效应研究[J]. 生态环境学报, 2018, 27(8):1417-1423.
Liu H, Guo J B, Liu Z B, et al. Time-Lag effect between sap flow and environmental factors of Larix principis-rupprechtii Mayr[J]. Forests, 2019, 10(11):642-650.
鱼腾飞, 冯起, 司建华, 等.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[J]. 北京林业大学学报, 2017, 39(7):8-16.
杨洁, 吕金林, 何秋月, 等.黄土丘陵区辽东栎和刺槐树干液流时滞效应与蒸腾特征的关联性[J]. 应用生态学报, 2019, 30(8):2607-2613.
O'Grady A P, Eamus D, Hutley L B. Transpiration increases during the dry season:Patterns of tree water use in eucalypt open-forests of northern Australia[J]. Tree Physiology, 1999, 19(9):591-597.
Zeppel M J B, Murray B R, Barton C, et al. Seasonal responses of xylem sap velocity to VPD and solar radiation during drought in a stand of native trees in temperate Australia[J]. Functional Plant Biology, 2004, 31(5):461-470.
罗紫东, 关华德, 章新平, 等.亚热带樟树树干液流通量变化规律[J]. 热带地理, 2016, 36(4):658-665.
李景刚, 李纪人, 黄诗峰, 等.基于TRMM数据和区域综合
Z
指数的洞庭湖流域近10年旱涝特征分析[J]. 资源科学, 2010, 32(6):1103-1110.
戴军杰, 章新平, 吕殿青, 等.南方红壤丘陵区樟树林土壤水分动态变化[J]. 水土保持研究, 2019, 26(4):123-131.
戴军杰, 章新平, 罗紫东, 等.长沙地区典型树木蒸腾对环境因子的响应及模拟[J]. 长江流域资源与环境, 2021, 30(3):699-711.
Granier A. Evaluation of transpiration in a Douglas-fir stand by means of sap flow measurements[J]. Tree Physiology, 1987, 3(4):309-320.
Dingman S L. Physical hydrolog[M]. Illinois:Waveland Press, 2015:28-86.
Oishi A C, Hawthorne D A, Oren R. Baseliner:An open-source, interactive tool for processing sap flux data from thermal dissipation probes[J]. SoftwareX, 2016, 18(5):139-143.
Wang H L, Doerthe T, Chris S. Hysteretic response of sap flow in Scots pine (
Pinus sylvestris
) to meteorological forcing in a humid low-energy headwater catchment[J]. Ecohydrology, 2019, 12(6):1-31.
陈琪, 李远航, 王琼琳, 等.基于Penman-Monteith模型分时段模拟华北落叶松日蒸腾过程[J]. 中国水土保持科学, 2019, 17(5):54-64.
王尚涛.干旱绿洲区农田葡萄树蒸散耗水及水分利用策略研究[D].兰州:兰州大学, 2019.
Bai Y, Li X Y, Liu S M, et al. Modelling diurnal and seasonal hysteresis phenomena of canopy conductance in an oasis forest ecosystem[J]. Agricultural and Forest Meteorology, 2017, 246:98-110.
Chen L X, Zhang Z Q, Li Z D, et al. Biophysical control of whole tree transpiration under an urban environment in Northern China[J]. Journal of Hydrology, 2011, 402(3/4):388-400.
Bai Y, Zhu G F, Su Y H, et al. Hysteresis loops between canopy conductance of grapevines and meteorological variables in an oasis ecosystem[J]. Agricultural and Forest Meteorology, 2015, 214/215:319-327.
姚增旺, 褚建民, 吴利禄, 等.民勤绿洲荒漠过渡带梭梭树干液流的时滞特征[J]. 应用生态学报, 2018, 29(7):2339-2346.
Xu S Q, Yu Z B. Environmental control on transpiration:A case study of a desert ecosystem in northwest China[J]. Water, 2020, 12(4):1-16.
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