...
首页> 外文期刊>Hydrological Processes >Impact of stem water storage on diurnal estimates of whole-tree transpiration and canopy conductance from sap flow measurements in Japanese cedar and Japanese cypress trees
【24h】

Impact of stem water storage on diurnal estimates of whole-tree transpiration and canopy conductance from sap flow measurements in Japanese cedar and Japanese cypress trees

机译:从日本雪松和日本柏树的汁液流量测量结果来看,茎干蓄水对整棵树蒸腾和冠层导度的日估算的影响

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

The amount of water stored in the stem introduces uncertainty when estimating diurnal whole-tree transpiration (E_T) and canopy stomatal conductance (G_C) using sap flow measured at the base of the stem (Q). Thus, to examine how E_T can be calculated from Q, we obtained E_T using sap flow and stem water content measurements and a whole-tree water balance equation, and compared it with Q. In this study, we measured sap flows in 33-year-old individual trees of Cryptomeria japonica D. Don and Chamaecyparis obtusa Endl. using constant-heat sap flow probes. Sap flows were measured at several depths at the base of the stem, and at the upper trunk as a surrogate of E_T. Stem water contents were measured at three vertical positions on the trunk using amplitude-domain reflectometry (ADR) sensors. We also measured sapwood volumes of the study trees. Using simultaneous sap flow and stem water content measurements along the tree stem, we confirmed that stem water storage has impacts on the transpiration stream. These include sap flow lags along the tree heights and an enhanced peak of transpiration from stem sap flow. These results enabled us to calculate the correct E_T by multiplying Q by 1.18 and shifting its time series forward by 30 min. The E_T value was then used to calculate G_C for both tree species. The factor of 1.18 is based on the fact that at noon, the value of E_T was higher than that of Q, due to the prolonged Q during the evening. Establishing the time lag was relatively simple and was determined by comparing Q and vapor pressure deficit. The multiplier is more challenging to ascertain due to the difficulty in obtaining E_T correctly.
机译:当使用茎干基部(Q)测得的树液流量估算昼夜全树蒸腾量(E_T)和冠层气孔导度(G_C)时,茎干中存储的水量会带来不确定性。因此,为了检验如何从Q中计算出E_T,我们使用了树液流量和茎干水含量测量值以及整棵树的水平衡方程式获得了E_T,并将其与Q进行了比较。在这项研究中,我们测量了33年的树液流量日本柳杉D. Don和Chamaecyparis obtusa Endl的老树。使用恒温树液流量探头。在茎基部和上部躯干的多个深度处测量汁液流量,作为E_T的替代物。使用幅度域反射法(ADR)传感器在树干上的三个垂直位置测量茎中的水分含量。我们还测量了研究树木的边材体积。通过同时测量沿树茎的汁液流量和茎干水分含量,我们证实了茎干水分的储存对蒸腾流有影响。这些包括沿树高的树液流动滞后和茎液流动增加的蒸腾峰。这些结果使我们能够通过将Q乘以1.18并将其时间序列向前移动30分钟来计算正确的E_T。然后,将E_T值用于计算两种树木的G_C。 1.18的系数基于以下事实:由于晚上Q延长,中午E_T的值高于Q。建立时间滞后相对简单,是通过比较Q和蒸气压不足来确定的。由于难以正确获得E_T,因此很难确定乘数。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号