Chin J Plant Ecol ›› 2010, Vol. 34 ›› Issue (8): 915-923.DOI: 10.3773/j.issn.1005-264x.2010.08.004
• Research Articles • Previous Articles Next Articles
MA Jian-Xin1,2, CHEN Ya-Ning1,*(), LI Wei-Hong1, HUANG Xiang1, ZHU Cheng-Gang1,2, MA Xiao-Dong1,2
Received:
2009-10-12
Accepted:
2010-01-25
Online:
2010-10-12
Published:
2010-09-28
Contact:
CHEN Ya-Ning
MA Jian-Xin, CHEN Ya-Ning, LI Wei-Hong, HUANG Xiang, ZHU Cheng-Gang, MA Xiao-Dong. Response of sap flow in Populus euphratica to changes in groundwater depth in the middle and lower reaches of the Tarim River of northwestern China[J]. Chin J Plant Ecol, 2010, 34(8): 915-923.
Fig. 1 The distribution of the monitoring section in the middle and lower reaches of the Tarim River. A, Shajilik; B, Shazihe; C, Wusiman; D, Aqik; E, Tieyzi; F, Akdun; G, Yahopmarhan; H, Yingsu; I, Abudali; J, Karday; K, Tugmailai; L, Argan; M, Yikanbujima; N, Korgan.
Fig. 2 Relationship between sap flow flux density in Populus euphratica (mean ± SD, n = 3) and groundwater depth (mean ± SD, n = 2) in the middle and lower reaches of the Tarim River.
液流通量密度 Sap flow flux density | 风速 Vw | 空气相对湿度 RH | 气温 Ta | 地温 Ts | 叶温 Tl | |
---|---|---|---|---|---|---|
风速 Wind velocity (Vw) | -0.214 | |||||
空气相对湿度 Relative humidity (RH) | 0.212 | -0.650 | ||||
气温 Air temperature (Ta) | -0.139 | 0.687 | -0.990** | |||
地温 Soil temperature (Ts) | -0.108 | 0.710 | -0.915** | 0.943** | ||
叶温 Leaf temperature (Tl) | 0.281 | 0.735 | -0.762* | 0.829* | 0.822* | |
地下水埋深 Groundwater depth | -0.887** | 0.140 | -0.343 | 0.270 | 0.266 | -0.113 |
Table 1 Pearson correlation between sap flow flux density in Populus euphratica and groundwater depth and enviromental factor
液流通量密度 Sap flow flux density | 风速 Vw | 空气相对湿度 RH | 气温 Ta | 地温 Ts | 叶温 Tl | |
---|---|---|---|---|---|---|
风速 Wind velocity (Vw) | -0.214 | |||||
空气相对湿度 Relative humidity (RH) | 0.212 | -0.650 | ||||
气温 Air temperature (Ta) | -0.139 | 0.687 | -0.990** | |||
地温 Soil temperature (Ts) | -0.108 | 0.710 | -0.915** | 0.943** | ||
叶温 Leaf temperature (Tl) | 0.281 | 0.735 | -0.762* | 0.829* | 0.822* | |
地下水埋深 Groundwater depth | -0.887** | 0.140 | -0.343 | 0.270 | 0.266 | -0.113 |
控制变量 Control variables | 地下水埋深 Groundwater depth | 液流 Sap flow | ||
---|---|---|---|---|
总盐 Total salt | 液流 Sap flow | 相关系数 r | -0.72 | |
p | 0.10 | |||
地下水埋深 Groundwater depth | 总盐 Total salt | 相关系数 r | 0.31 | |
p | 0.56 |
Table 2 Partial correlation between sap flow flux density and groundwater depth and soil salt
控制变量 Control variables | 地下水埋深 Groundwater depth | 液流 Sap flow | ||
---|---|---|---|---|
总盐 Total salt | 液流 Sap flow | 相关系数 r | -0.72 | |
p | 0.10 | |||
地下水埋深 Groundwater depth | 总盐 Total salt | 相关系数 r | 0.31 | |
p | 0.56 |
Fig. 4 Relationship between population characters of Populus euphratica (mean ± SD, n = 10) and groundwater depth in the middle and lower reaches of the Tarim River.
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